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  • 2005-2009  (16)
  • 1990-1994  (330,859)
  • 1980-1984  (410,164)
  • 1993  (330,836)
  • 1984  (220,235)
  • 1980  (189,998)
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  • 1
    Call number: M 16.90217
    Type of Medium: Monograph available for loan
    Pages: 144 S. , graph. Darst.
    Language: German
    Note: Kiel, Univ., Diss., 1984.
    Location: Upper compact magazine
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  • 2
    Call number: M 18.91455
    Type of Medium: Monograph available for loan
    Pages: 449 S. : Ill., graph. Darst., Kt. , S. 159-608
    ISBN: 0006-6729
    Series Statement: Bollettino di geofisica teorica ed applicata 40, 3-4
    Note: Table of contents --- C. Morelli: The contributions of the International Gravimetric Commission (IGC) to global surface-gravity determinations // pp. 165-177 --- C Kotsakis and M. G. Sideris: Study of the gravity field spectrum in Canada in view of cm-geoid determination // pp. 179-188 --- S.D. Pagiatakis, D. Fraser, K. McEwen, A. K. Goodacre and M. Veronneau: Topographic mass density and gravimetric geoid modelling // pp. 189-194 --- H. Denker and I.N. Tziavos: Investigation of the Molodensky series terms for terrain reduced gravity field data // pp. 195-203 --- S.A. Benhamed Daho and S. Kahlouche: Gravimetry data validation in Algeria // pp. 205-210 --- M. Mojzeš and J. Janák: New gravimetric quasigeoid of Slovakia // pp. 211-217 --- I.N. Tziavos, R. Forsberg and M.G. Sideris : Marine gravity field recovery by combining satellite altimetry and shipborne gravimetry // pp. 219-226 --- G. Fotopopulos, C. Kotsakis and M.G. Sideris: Development and evaluation of a new Canadian geoid model // pp. 227-238 --- C. Jekeli: A further evaluation of the EG M96 geopotential model based on deflections of the vertical // pp. 239-243 --- N.K. Pavlis, C.M. Cox, E.C. Pavlis and F.G. Lemoine: Intercomparison and evaluation of some contemporary global geopotential models // pp. 245-254 --- J.C. Catalao and M.J. Sevilla: Comparison between EGM96 and FCUL96B tailored geopotential model for the north-east Atlantic // pp. 255-259 --- J. Kusche, K.H. Ilk and S. Rudolph: Two-step data analysis for future satellite gravity field solutions: a simulation study // pp. 261-266 --- C. Jekeli: An analysis of geopotential difference determination from satellite-to-satellite tracking // pp. 267-272 --- J. Verdun , R. Bayer , E. Klingelé , M. Cerniar , M. Cocard , A. Geiger and M. Halliday: The Alpine Swiss French Airborne Gravimetry Project (ASFAG Project) // pp. 273-276 --- A. Albertella, F. Migliaccio and F. Sansò: New simulations for the spaceborne gravimetry inversion // pp. 277-283 --- Ch. Reigber, P. Schwintzer and H. Lühr: The CHAMP geopotential mission // pp. 285-289 --- B.D. Tapley and C. Reigber: GRACE: a satellite-to-satellite tracking geopotential mapping mission // pp. 291-291 --- S. Bettadpur, J.R. Kim and B.D. Tapley: Results from simulations studies of the GRACE mission // pp. 293-293 --- M. Aguirre-Martinez and S. Cesare: GOCE mission concept, error derivation and performances // pp. 295-302 --- H. Oberndorfer, R. Orobantu, C. Gerlach, J. Muller, R. Rummel, N. Sneetuw, R. Koop, P. Visser, P. Hoyng, A. Selig and M. Smit: GOCE sensor combination and error analysis // pp. 303-307 --- G. Balmino, F. Perosanz, R. Rummel, N. Sneeuw and H. Sunkel: CHAMP, GRACE and GOCE: mission concepts and simulations // pp. 309-319 --- P. Touboul, E. Willemenot, B. Foulon and V. Josselin: Accelerometers for CHAMP, GRACE and GOCE space missions: synergy and evolution // pp. 321-327 --- Ch. Reigber, F. Barthelmes, H. Greiner-Mai, Th. Gruber, H. Jochmann and J. Wünsch: Temporal gravity field variations from oceanic, atmospheric and inner core mass redistributions and their sensitivity to new gravity missions CHAMP and GRACE // pp. 329-340 --- R. Barzaghi, A. Borghi, L. De Stefani, A. Piatti and G. Venuti: SST estimation using collocation: method refinements and seasonal variability // pp. 341-346 --- R. Blinken and K.R. Koch: Estimation of geoid and sea surface topography from satellite altimetry by the adjoint method // pp. 347-352 --- R. Devoti, V. Luceri, P. Rutigliano, C. Sciarretta and G. Bianco: Time series of low degree zonals obtained analyzing different geodetic satellites // pp. 353-358 --- N.K. Pavlis, C.M. Cox, Y.M. Wang and F.G. Lemoine: Further analyses towards the introduction of ocean circulation model information into geopotential solutions // pp. 359-367 --- O.B. Andersen, P. Knudsen, S. Kenyon and R. Trimmer: Recent improvement in the KMS global marine gravity field // pp. 369-377 --- T. Bašic and M. Brkic: The latest efforts in geoid determination in Croatia // pp. 379-386 --- M. Rentsch, Th. Gruber and M. Anzenhofer: A global grid of high-resolution gravity anomalies based on Geosat and ERS-1 altimetry // pp. 387-394 --- G. Rodríguez, M.J. Sevilla and C. De Toro: Crossover analysis in the Canary-Azores region of ERS-1 altimetric data // pp. 395-401 --- G. Tóth, J. Ádám, I.N. Tziavos and V.D. Andritsanos: Gravimetric geoid computations in Hungary and the sorrounding area // pp. 403-409 --- D. Arabelos, S.D. Spatalas, I.N. Tziavos, M.J. Sevilla, G. Rodriguez, C. De Toro, J. Catalao and J. Calvao: A new high resolution geoid for the Iberian Atlantic continental shelf area // pp. 411-419 --- D. Dreher, M.F. Lalancette and M. Maia: Roughness of the gravity and seafloor topography used to infer geodynamic settings // pp. 421-426 --- O.B. Andersen: Shallow water tidal determination from altimetry - the M4 constituent // pp. 427-437 --- P. Knudsen and O. Andersen: A global high resolution mean sea surface from multi mission satellite altimetry // pp. 439-443 --- P. Holota: A construction of Galerkin’ smatrix in quasi-geoid determination // pp. 445-450 --- M.G. Doufexopoulou and V.N. Pagounis: Investigation of raw variance and variability spectra from non gravimetric geoidal signals // pp. 451-460 --- G. Gerstbach: Inversion of vertical deflection data by the program GREMMO // pp. 461-468 --- C. Braitenberg and M. Zadro: Iterative 3D gravity inversion with integration of seismologic data // pp. 469-475 --- V. Baiocchi, M. Crespi and F. Riguzzi: Mean density map for the Italian region by GIS techniques // pp. 477-482 --- V. Josselin, E. Willemenot and P. Touboul: Digital electronics for electrostatic accelerometers interest for high resolution and in-orbit calibration // pp. 483-486 --- J.M. Brown, T.M. Niebauer and F.J. Klopping: Results from a new interferometric ballistic differential gravity meter // pp. 487-496 --- G. Berrino, G. Cerrutti, G. Corrado, P. De Maria and U. Riccardi: Gravity studies on active Italian volcanoes: a comparison between absolute and relative gravimetry // pp. 497-510 --- Y. Fukuda, T. Sato, Y. Tamura and Y. Aoyama: The effects of sea-surface height variations on the long-period gravity changes // pp. 511-517 --- M. Amalvict, J. Hinderer and J.P. Boy: A comparative analysis between an absolute gravimeter (FG5-206) and a superconducting gravimeter ( GWR CO26) in Strasbourg: new results on calibration and long-term gravity changes // pp. 519-525 --- E. Willemenot, P.Touboul and V. Josselin: Gradiometer calibration and performance verification: GOCE approach // pp. 527-532 --- M.F. Lalancette-Le Quentrec, B. Simon, D. Orseau, N. Florisch, M. Llubes, m. Amalvict and J. Hinderer: Ocean loading and crustal deformation in Bretagne (France ) an experiment involving differential GPS, gravimetry and tide gauges // pp. 533-536 --- Y. Kuroishi: Improvement of Japanese geoid with lD- FFT method and its comparison with altimetry-derived geoid // pp. 537-543 --- N. Kühtreiber: Combining gravity anomalies and deflections of the vertical for a precise Austrian geoid // pp. 545-553 --- M. Kuhn: The influence of different crust models on the gravity field of the Earth // pp. 555-562 --- H.A. Abd-Elmotaal: Comparison among different geoid solutions for the Egyptian south-western desert using FFT technique // pp. 563-569 --- J. Ádám: Difference between geoid undulation and quasigeoid height in Hungary // pp. 571-575 --- C. Braitenberg and M. Zadro: The Grotta Gigante horizontal pendulums - instrumentation and observations // pp. 577-582 --- P. Baldi, G. Casula, J. Hinderer and M. Amalvict: Calibration of a superconducting gravimeter: a comparison between the mass attraction method and the use of FG5 absolute gravity measurements // pp. 583-588 --- L. Biagi, R. De Stefano, F. Sansó and C. Sciarretta: RTC and density variations in the estimation of local geoids // pp. 589-595 --- A. De Bruijne, R. Haagmans and E. De M
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  • 3
    Monograph available for loan
    Monograph available for loan
    Durham, N.C [u.a.] : Duke Univ. Press
    Call number: IASS 16.90430
    Type of Medium: Monograph available for loan
    Pages: VIII, 327 S. , Ill.
    ISBN: 0822313723 (pbk) , 9780822313724 (pbK) , 0822313545
    Language: English
    Branch Library: RIFS Library
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  • 4
    Call number: M 17.90776
    Type of Medium: Monograph available for loan
    Pages: 191 S. , Illustrationen, graphische Darstellungen
    ISBN: 9789090217987
    Classification:
    Photogrammetry, Remote Sensing
    Language: English
    Location: Upper compact magazine
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  • 5
    Call number: M 17.90778
    Type of Medium: Monograph available for loan
    Pages: 159 S. , Illustrationen, graphische Darstellungen
    ISBN: 908659204X , 9789086592043
    Language: English
    Location: Upper compact magazine
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  • 6
    Call number: AWI A12-17-90537
    Type of Medium: Monograph available for loan
    Pages: 267 S. , Ill., graph. Darst.
    Language: Russian
    Note: Contents: Preface. - I. INSTRUMENT AND TECHNIQUES OF MEASUREMENTS OF OZONE, SOLAR ULTRAVIOLET AND CONSTITUENTS OF THE ATMOSPHERE INFLUENCING THE OZONE. MEASUREMENT RESULTS. - The set of measurements for optical observations of ozone and other constituents of the atmosphere influcencing the ozone / G. I. Kuznetzov. - Investigation of time variations of ozone / G. I. Kuznetzov. - Analytical aspects of atmospheric ozone and oxidants studies / L. N. Tchernyh, V. A. Popov, E. V. Pechennikova. - Results of the airborne measurements of total ozone and nitrogen dioxide / A. Ya. Arabov, N. F. Elansky, Yu. L. Truttse. - Rocket head design of meteorological rockets MR-12 and M-100B for measuring of optical characteristics of the upper atmosphere / N. I. Brezgin, E. A. Krohina, S. G. Linnik, A. F. Chijov, O. V. Shtirkov. - Simultaneous measurements of the vertical ozone distribution by rocket and goundbased spectrometric methods / P. F. Boychenko, N. I. Brezgin, G. I. Kuznetzov, A. F. Chijov, O. V. Shtirkov. - The apparatus and method for investigation of ozone-sensitive chemiluminescent detectors at low pressures / S. P. Perov, V. I. Konkov, V. A. Kononkov, L. A. Udonova. - On the application of the chemiluminescent method of the investigation of atmospheric ozone with the help of meteorological rocket M100-B / V. I. Konkov, S. P. Perov. - Water vapour distribution in the ozonosphere / A. V. Fedinsky, V. A. Yuskov. - Sounding rocket measurements of aerosol concentration in the atmosphere up to 90 km / T. I. Orishich. - Basic problems of automation of total ozone measurements and the results of development of automatic ozonometer / V. A. Bajenov, T. D. Jukovskaya, A. N. Otto. - Automatic calculation of the common maintance of atmospheric ozone by filter ozonometers by means of methods of analogue transformation of functions / V. A. Bajenov. - II. OZONOSPHERE CHEMISTRY. - Systems modelling of stratospheric ozone transport and photochemistry / I. L. Karol. - Numerical methods of global transport of freons in the atmosphere and assessment of their effect on ozone / I. L. Karol, V. V. Babanova, A. A. Kiselev, L. A. Romanovskaya. - The stratosphere photo-chemical model / I. G. Dyominov. - The impact of galactic cosmic rays and solar proton events upon the ozone layer / I. G. Dyominov. - Mechanism of cosmic rays effect on earth ozonosphere / P. S. Vinogradov, I. K. Larin, A. I. Poroykova, V. L. Talrose. - Qualitative estimation of some stratospheric reactions rates based on orbital symmetry conservation rules / P. S. Vinogradov, I. K. Larin, V. L. Talrose, O. A. Travina. - On starting prerequisites of mesospheric ozone photochemical theory / G. M. Martynkevich. - Studies of ozone in urban atmosphere as an indicator of photochemical processes / V. A. Popov, L. N. Tchernyh, E. V. Pechennikova. - On the use of silver thin films for measuring of atomic oxygen concentration in the upper atmosphere / S. J. Toktomishev. - On the photochemistry of ozone in the laser sounding of the stratosphere / A. P. Sukhorukov, I. M. Sizova. - Aerosols and ozone in the lower stratosphere / A. P. Bobrovsky, V. N. Ivanov, L. S. Ivlev, V. G. Sirota. - III. THE INTERELAXION OF PROCESSES IN OZONOSPHERE WITH HYDROMETEOROLOGICAL PHENOMENA. - Spatial distribution of atmospheric ozone concentration over the USSR in the upper troposphere and lower stratosphere as derived from aircraft measurements / S. V. Solonin, V. V. Osetchkin. - Variations of the total ozone content of ozone depending on the type of jet streams and their comlexes / V. G. Bakhtiyarov, L. I. Bordovskaya, B. D. Belan. - The stratospheric circulation change in spring and preceeding to it the change of total ozone field in autumn / L. A. Uranova. - Some results of the investigation of ozone vertical distribution in the atmosphere in connection with meteorological phenomena / D. V. Harchilava. - Ozone vertical profiles and the solar activity / P. F. Bojchenko, Yu. N. Rybin. - The effect of solar activity on the general circulation and thermal regime of the atmosphere / L. R. Rakipova. - Seasonal variations of total ozone in the stratospheric circumpolar vortex / V. J. Bekoryukov. - On the relation of the total amount of atmospheric ozone and the near-ground concentrations of radioactive isotopes / V. J. Lujanas, V. K. Jocius, P. K. Zinkevichus. - A certain low-governed nature of ozone, radioactive and nonradioactive aerosols and electric field intensity distribution in the lower troposphere / A. G. Amiranashvily, A. A. Aphaidze, A. Sh. Balavadze, A. G. Nodia, D. V. Harchilava. - On a certain relation between ozone content in the atmosphere and thunderstorm hail phenomena under the conditions of East Georgia / D. V. Harchilava, A. I. Kartsivadze, T. G. Gzirishvily. - On the changeobility of ozone content during the thunderstorm situation / A. I. Kartsivadze, D. V. Harchilava. - Variation of atmospheric ozone and some parameters of jet streams / N. N. Vinogradova. , In kyrill. Schr. , Zsfassungen in engl. Sprache
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  • 7
    Call number: IASS 16.90607
    Type of Medium: Monograph available for loan
    Pages: VIII, 56 S , Ill., 1 Kt
    ISBN: 2831701880 (kart.)
    Series Statement: Report / E & P Forum 2.55/184
    Language: English
    Branch Library: RIFS Library
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  • 8
    Monograph available for loan
    Monograph available for loan
    Rockville, MD : U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, Environmental Data and Information Service,
    Call number: PIK N 454-17-90910
    Type of Medium: Monograph available for loan
    Pages: x, 290 Seiten , Diagramme, Karten , 28 cm
    Language: English
    Location: A 18 - must be ordered
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  • 9
    Monograph available for loan
    Monograph available for loan
    Madrid : Secc
    Call number: PIK N 456-17-90913
    Type of Medium: Monograph available for loan
    Pages: 536 Seiten
    Series Statement: Ministerio de Transportes Turismo Y Comunicaciones : Publicación Serie A 114
    Parallel Title: 1,1=6; 2,1=13 von Publicaciones / D / Ministerio del Aire, Subsecretaria de Aviación Civil, Servicio Meteorológico Nacional
    Language: Spanish
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  • 10
    Call number: MOP Per 799(10)
    Type of Medium: Series available for loan
    Pages: 122 Seiten , Illustrationen
    Series Statement: Materialy meteorologičeskich issledovanij 10
    Language: Russian
    Location: MOP - must be ordered
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  • 11
    Call number: MOP B 17136
    In: Hochschulbücher für Mathematik, Bd. 40
    Type of Medium: Monograph available for loan
    Pages: 777 S. , Ill., graph. Darst.
    Series Statement: Hochschulbücher für Mathematik 40
    Uniform Title: Rachunek prawdopodobienstwa i statystyka matematyczna 〈dt〉
    Language: German
    Note: Aus d. Poln. übers.
    Location: A 18 - must be ordered
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  • 12
    Series available for loan
    Series available for loan
    Leipzig : Dt. Verl. für Grundstoffindustrie
    Associated volumes
    Call number: SR 99.0015(391)
    In: Beiträge zur allgemeinen und speziellen Paläontologie, Teil III
    In: Freiberger Forschungshefte : Reihe C, Geowissenschaften, Paläontologie, 391
    Type of Medium: Series available for loan
    Pages: 94 S. , Ill., graph. Darst.
    Edition: 1. Aufl.
    ISSN: 0071-9404
    Series Statement: Freiberger Forschungshefte : Reihe C, Geowissenschaften, Paläontologie 391
    Language: German
    Note: Inhaltsverzeichnis: Annotation. - Autorenverzeichnis. - Die Blattodea (Insecta) des Paläozoikums, Teil II: Morphogenese der Flügelstrukturen und Phylogenie / Jörg Schneider. - Zur Taxonomie und Biostratigraphie der Conchostraca (Phyllopoda, Crustacea) des Rotliegenden (oberes Karbon bis Perm) im Saar-Nahe-Gebiet (BRD) / Thomas Martens. - Zur Ichnologie der Arthropoda / Harald Walter.
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  • 13
    Series available for loan
    Series available for loan
    Aachen : Lehrstuhl für Ingenieurgeologie und Hydrogeologie der RWTH
    Associated volumes
    Call number: AWI G4-18-91534
    In: Mitteilungen zur Ingenieurgeologie und Hydrogeologie, Heft 54
    Type of Medium: Series available for loan
    Pages: XV, 164 S. , Ill., graph. Darst., Kt. , 4 Kt.-Beil. (7 S.)
    Series Statement: Mitteilungen zur Ingenieurgeologie und Hydrogeologie 54
    Language: German
    Note: Zugl.: Aachen, Techn. Hochsch., Diss. , Inhaltsverzeichnis: Abbildungsverzeichnis. - Tabellenverzeichnis. - Vorwort. - 1. Einleitung. - 1.1 Problemstellung und Ziel. - 1.2 Bevölkerungsentwicklung im Großraum Monterrey. - 1.3 Geographische und morphologische Übersicht. - 1.4 Lage des Arbeitsgebietes. - 2. Geologisch-tektonischer Überblick. - 2.1 Bisherige geologische Erkundung. - 2.2 Tektonik und Paläogeographie. - 3. Stratigraphie. - 3.1 Ober-Jura. - 3.1.1 Minas Viejas-Formation (Oxford/Kimmeridge). - 3.1.2 Zuloaga-Formation (Kimmeridge). - 3.1.3 La Casita-Formation (Kimmeridge/Unter-Berrias). - 3.2 Kreide. - 3.2.1 Taraises-Formation (Berrias/Unter-Hauterive). - 3.2.2 Cupido-Formation (Mittel-Hauterive/Mittel-Apt). - 3.2.3 La Peña-Formation (Ober-Apt). - 3.2.4 Aurora-Formation (Unter-Alb). - 3.2.5 Cuesta del Cura-Formation (Ober-Alb/Unter-Turon). - 3.2.6 Agua Nueva-Formation (Unter-Turon/Mittel-Turon). - 3.2.7 San Felipe-Formation (Coniac/Santon). - 3.2.8 Mendez-Formation (Campan/Maastricht). - 4. Homogenbereiche in Fest- und Lockergesteinen. - 4.1 Homogenbereiche in FestgesteinenfSchichtenfolge des Mesozoikums. - 4.1.1 Karbonatische Gesteine. - 4.1.2 Karbonatische Gesteine mit tonig-mergeligen Zwischenlagerungen. - 4.1.3. Tonig-mergelige Gesteine. - 4.2 Homogenbereiche in Lockergesteinen/Quartär. - 4.2.1 Genetische Gliederung der Lockergesteine. - 4.2.1.1 Kolluvium. - 4.2.1.2 Derrubium. - 4.2.1.3 Proluvium (Kegelschutt). - 4.2.1.4 Alluvium. - 4.2.2 Gliederung nach dem Kornaufbau. - 4.2.2.1 Brekzien. - 4.2.2.2 Blockströme. - 4.2.2.3 Blockschutt (〉 2m ⌀), miteinander in Kontakt. - 4.2.2.4 Blockschutt mit Blöcken 〉 2 m ⌀ in Grundmasse von eckigen Komponenten in Stein- bis Sandkorngröße "schwimmend". - 4.2.2.5 Blockschutt mit weitgestufter Korngrößenverteilung (Sandkorn- bis Blockgröße 〈 2 m ⌀). - 4.2.2.6 Steine, Kies und Sand (Hangschutt). - 4.2.2.7 Pelitische Sedimentation vor undräniertem Straßendamm (Schluff, Feuchtgebiet). - 5. Geologisch-klimatologische Grundlagen zur Bewertung der Hangstabilität. - 5.1 Ingenieurgeologische Kartierungen. - 5.2 Tektonische Elemente des Arbeitsgebietes. - 5.3 Geomorphologie. - 5.4 Klima. - 5.5 Hydrologie des Großraumes Monterrey. - 5.6 Hurrikans. - 5.6.1 Entstehung von Hurrikans. - 5.6.2 Hurrikan "GILBERTO". - 6. Böschungsstabilität. - 6.1 Grundsatzüberlegung. - 6.1.1 Autochthon. - 6.1.2 Parautochthon (Hakenschlagen). - 6.1.3 Allochthon. - 6.2 Massenbewegungen. - 6.2.1 Alte Kriechmasse im Zentralteil des Kartiergebietes. - 6.2.2 Entwässerungsnetz im Arbeitsgebiet und innerhalb der alten Kriechmasse. - 6.2.3 Allgemeine Ursachen der Hangbewegung im Kartiergebiet. - 6.3 Anthropogene Beeinträchtigungen der Böschungsstabilität und unzweckmäßige Baumaßnahmen. - 6.3.1 Bisherige Gründungsmethoden. - 6.3.2 Rodungen und Blockstürze. - 6.3.3 Regenwasser-Ableitungen. - 6.3.4 Bautechnische Mängel. - 6.3.5 Massenbewegungen im Fels durch starke Niederschläge. - 6.3.5.1 Klassifizierung von Hanggleitungen. - 6.3.5.2 Massenbewegungen in Tonsteinen der Méndez-Formation. - 6.3.5.3 Massenbewegungen in den Karbonatgesteinen mit tonig-mergeliger Zwischenlagerung. - 6.4 Standsicherheitsberechnungen. - 6.4.1 Zweck und Ziel der Berechnungen. - 6.4.2 Mechanik und Geometrie von Kriechbewegungen und Rutschmassen. - 6.4.3 Berechnungsverfahren. - 6.4.4 Tiefe der Gleitfläche. - 6.4.5 Standsicherheitsberechnungen für die große Kriechmasse (im mittleren Bereich des Kartiergebietes). - 6.4.5.1 Berechnungsansatz nach JANBU und Wahl der Kennwerte. - 6.4.5.2 Ergebnisse. - 7. Geologische Risiken und Empfehlungen für das Gebiet Chipinque. - 7.1 Zone 1: Flache Hänge, 〈 5° Neigung (Proluviurn). - 7.1.1 Risiken. - 7.1.2 Empfehlungen. - 7.2 Zone 2: Hänge, 5-15° Neigung, Schutt unverfestigt. - 7.2.1 Risiken. - 7.2.2 Empfehlungen. - 7.3 Zone 3: Hänge 〉 15° Neigung; Schutt aus allochthonen Fels- und Lockergesteinsmassen; lokale Rutsch- oder Kriechzonen. - 7.3.1 Risiken. - 7.3.2 Empfehlungen. - 7.4 Zone 4: Hänge meist 〉 15° Neigung in Tongesteinen der Méndez-Formation. - 7.4.1 Risiken. - 7.4.2 Empfehlungen. - 7.5 Zone 5: Autochthone Gipfelregion. - 7.5.1 Risiken. - 7.5.2 Empfehlungen. - 7.6 Zone 6: Erosionsrinnen. - 7.6.1 Risiken. - 7.6.2 Empfehlungen. - 7.7 Allgemeine Empfehlungen für eine Besiedlung der Steilhänge im Raum Monterrey. - 8. Zusammenfassung/Resumen. - 9. Literaturverzeichnis. - Anlagen. - Anlage 1: Geologische Karte 1:10.000 San Pedro Garza García, Nuevo León (Chipinque). - Anlage 1a: A-B Geologischer Profilschnitt. - Anlage 1b: C-D Geologischer Profilschnitt. - Anlage 1b': C-D Geologischer Profilschnitt. - Anlage 2: Karte der Massenbewegungen 1:10.000. - Anlage 3: Geologische Risikokarte 1:10.000. - Anlage 4: Geologische Karte 1:40.000 (Monterrey). - Anlage 4a: A-B Geologischer Profilschnitt. - Anlage 5: Tektonische Übersicht (Monterrey). - Anlage 6: Geologische Karte 1:20.000 (San Pedro Garza García). - Anlage 7: Aufschlusskarte 1:10.000.
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  • 14
    Call number: AWI G6-18-91531
    In: Karlsruher geochemische Hefte, Nr. 3
    Type of Medium: Series available for loan
    Pages: IV, 157 S. , Ill., graph. Darst.
    Series Statement: Karlsruher geochemische Hefte 3
    Language: German
    Note: Zugl.: Karlsruhe, Univ., Diss., 1992 , Inhalt: 1. Einleitung und Zielsetzung. - 2. Das Untersuchungsgebiet. - 2.1. Lage des Untersuchungsgebiets. - 2.2. Geologische Situation an der Galapagos-Mikroplatte. - 3. Die Sedimente im Untersuchungsgebiet. - 3.1. Übersicht. - 3.2. Die Beschreibung der Sedimentkerne. - 3.2.1. Kern 50. - 3.2.2. Kern 54. - 3.2.3. Kern 68. - 3.2.4. Kern 69. - 3.2.5. Kern 76. - 3.2.6. Kern 93. - 3.2.7. Kern 95. - 4. Die Vorbereitung der Proben. - 4.1. Probennahme. - 4.2. Aufbereitung der Proben. - 4.2.1. Zur Dichte der Beprobung. - 5. Analytik. - 5.1. Kontrolle der Meßqualität. - 5.2. Wassergehalt. - 5.3. Korngrößenbestimmung. - 5.4. Glühverlust (L.O.I.). - 5.5. Kohlenstoff-Schwefel-Analyse (CSA). - 5.6. Titrimetrische Bestimmung von Fe2+. - 5.7. Wellenlängendispersive Röntgenfluoreszenz-Analyse. - 5.8. Energiedispersive Röntgenfluoreszenz-Analyse (EDRFA). - 5.9. Graphitrohr-Atom-Absorptions-Spektrometrie. - 5.10. Instrumentelle Neutronenaktivierungs-Analyse (INAA). - 6. Spezielle Anwendungen und Weiterentwicklungen im analytischen Bereich. - 6.1. Entsalzung durch Dialyse. - 6.2. Die Trennung von Karbonat-Kohlenstoff und organischem Kohlenstoff mit Hilfe der CSA. - 6.2.1. Beschreibung des Verfahrens. - 6.2.2. Ergebnisse. - 6.3. Die Bestimmung des Calcitgehalts aus dem Glühverlust. - 6.4. Erstellung eines Auswerteprogramms für die winkeldispersive RFA. - 7. Die Bestimmung der Mineralphasen. - 7.1. Diffraktometrie. - 7.2. Differenz-Thermo-Analyse - Thermogravimetrie (DTA-TG). - 8. Wärmeflußmessungen. - 8.1. Beschreibung. - 8.2. Ergebnisse. - 9. Datierungen. - 9.1. Thorium-Datierung. - 9.2. Elektronenspin-Resonanz-Darierung (ESR). - 9.3. Sauerstoff-Isotopen-Datierung. - 9.3.1. Beschreibung. - 9.3.2. Interpretation der d 180-Kurve von Kern 93. - 9.4. Mikropaläontologie. - 9.4.1. Kern 93. - 9.4.2. Kern 68. - 9.4.3. Kern 69. - 10. Interpretation der geochemischen Daten am Beispiel von Kern 93. - 10.1. Sedimentologische Parameter. - 10.1.1. Sedimenteintrag. - 10.1.2. Bioturbation. - 10.2. Redoxprozesse während der Diagenese, eine Diskussion. - 10.2.1. Parameter. - 10.2.2. Diagenetische Mobilisation von Mangan. - 10.2.3. Die Redoxfaktoren. - 10.2.3.1. Der Eh-Wert. - 10.2.3.2. Probendichte und Untersuchungstiefe. - 10.2.3.3. Modelle. - 10.2.4. Die Einflußgrößen im einzelnen. - 10.2.4.1. Reduktion und Oxidation. - 10.2.4.2. Eh-pH Bedingungen. - 10.2.4.3. Reduktionsmittel. - 10.2.4.4. MnO2 und Mn2+. - 10.2.4.5. Tiefere Bohrungen. - 10.2.4.6. Eisen. - 10.2.5. Zusammenfassung. - 10.3. Klimatisch bedingte Parameter und Elemente. - 10.3.1. d18O. - 10.3.2. Foraminiferen. - 10.3.3. Calcit. - 10.3.4. Organischer Kohlenstoff. - 10.3.5. Phosphat. - 10.3.6. Weitere wichtige Spurenelemente. - 10.3.6.1. Brom. - 10.3.6.2. Die Seltenen Erden. - 10.3.7. Modelle zur Erklärung der Anreicherung von Mangan und Diskussion der Ergebnisse. - 11. Die Interpretation von Kern 68. - 11.1. Datierung. - 11.2. Die Asche-reiche Lage in 120 cm Teufe. - 11.3. Klimatische Parameter. - 11.4. Der Vergleich von Kern 69 mit Kern 68. - 12. Die Interpretation der Kerne 50 und 54. - 13. Die Interpretation von Kern 76. - 13.1. Die Aschelagen. - 13.1.1. Beschreibung und Genese. - 13.1.2. Zur Geochemie der Aschen. - 13.2. Die Normalsedimente in Kern 76. - 13.2.1. Anwendung der klimatischen Parameter. - 13.2.2. Weitere Elemente. - 13.3. Zusammenfassung. - 14. Die Interpretation von Kern 95. - 14.1. Übersicht. - 14.2. Die Serpentin-Schicht. - 14.3. Die hydrothermalen Sedimente oberhalb und unterhalb der Serpentin-Schicht. - 14.4. Die Klimaparameter. - 14.5. Zusammenfassung Kern 95. - 15. Zusammenfassung und Fazit. - 16. Perspektiven. - 17. Literatur. - Anhang.
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  • 15
    Series available for loan
    Series available for loan
    Karlsruhe : Institut für Petrographie und Geochemie, Universität Karlsruhe
    Associated volumes
    Call number: AWI G6-18-91533
    In: Karlsruher geochemische Hefte, Nr. 1
    Type of Medium: Series available for loan
    Pages: III, 149 S. , graph. Darst., Kt.
    Series Statement: Karlsruher geochemische Hefte 1
    Language: German
    Note: Zugl.: Karlsruhe, Univ., Diss., 1992 , Inhalt: 1. Einleitung. - 2. Geologische und geographische Übersicht. - 2.1. Geographische Lage. - 2.2. Petrologische Übersicht.. - 2.3. Mineralisation. - 2.4. Besiedlung und wirtschaftliche Nutzung. - 2.5. Klima und Verwitterungsbedingungen. - 3. Probenentnahme und Aufbereitung. - 3.1. Schwermineralabtrennung. - 4. Analytik. - 4.1. EDXRF-Analytik. - 4.1.1. Instrumentierung. - 4.1.2. Meßbedingungen. - 4.1.3. Auswertung der EDXRF-Daten im mobilen LABOR. - 4.2. Neutronenaktivierungsanalyse. - 4.2.1. Vergleich INAA- EDXRF. - 4.3. Königswasseraufschluß. - 5. Univariate Statistik und geochemische Kartierung. - 5 .I. Robuste univariate Verfahren. - 5 .1.1. 5-Number Summary und Box-Plot. - 5 .1.2. Dichtespur (Density Traces). - 5 .1. 3. Verteilungsformen. - 5.2. Geochemische Karten. - 5.2.1. Symbolkarten. - 5.2.2. Kontur-Karten. - 5.2.3. Wichtung mit dem reziproken Abstand (1/d"-Filter). - 5.2.4. Gauß-Filter. - 5.2.5. Kolmogorov- Smirnov- Filter. - 5.2.6. Fence-Filter. - 5.2.7. Notch-Filter. - 5.3. Variographie. - 5.4. Krige-Verfahren. - 5.4.1. Punkt-Krigen. - 5.4.2. Ko-Krigen. - 5.4.3. Bewertung der verschiedenen Techniken. - 6. Elementverteilung im Untersuchungsgebiet. - 6.1. Gesteinscharakterisiemde Elemente. - 6.1.1. Rubidium. - 6.2. Elemente mit Gesteins- und möglichem Lagerstätten-Einfluß. - 6.2.1. Nickel. - 6.2.2. Strontium und Barium. - 6.2.3. Cer (als Vertreter der Seltenen Erden) und Niob. - 6.2.4. Blei. - 6.3. Indikatorelemente für Vererrungen oder hydrothermale Überprägung. - 6.3.1. Arsen. - 6.3.2. Kupfer. - 6.3.3. Brom. - 6.3.4. Sonstige. - 7. Multivariate Verfahren. - 7 .1. Abschätzung hydraulischer Effekte über Elementverhältnisse. - 7.2. Clusteranalyse. - 7.2.1. Hierarchische Cluster der Elemente in den Einzugsgebieten. - 7.2.2. "Harte" Clusteranalyse der Proben. - 7.2.3. Fuzzy Cluster. - 8. Ergebnisse. - 9. Zusammenfassung. - 10. Literatur. - Anhang. - A. Statistische Kenndaten. - B. Blockbild des Programms GEOCHEM. - C. Berechnungsbeispiel fiir Filterfunktionen. - D. Experimentelle Variogramme und angepaßte Modelle.
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  • 16
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-84/17
    In: CRREL Report, 84-17
    Description / Table of Contents: VHF-band radiowave short pulses were transmitted within the permafrost tunnel at Fox, Alaska, over distances between 2.2 and 10.5 m. The propagation medium was a frozen silt containing both disseminated and massive ice with temperatures varying from -7°C near the transmitter to probably -2 C near the center of the tunnel overburden. The short pulses underwent practically no dispersion in the coldest zones but did disperse and refract through the warmer overburden, as suggested by calculations of the effective dielectric constant. Most significantly the measured frequency content decreased as the effective dielectric constant increased. The results indicate that deep, cross-borehole pulse transmissions over distances greater than 10 m might be possible, especially when the ground is no warmer than -4°C. The information thus pined could be used for identifying major subsurface variations, including ground ice features.
    Type of Medium: Series available for loan
    Pages: ii, 14 Seiten , Illustrationen
    Series Statement: CRREL Report 84-17
    Language: English
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  • 17
    Call number: ZSP-201-84/16
    In: CRREL Report, 84-16
    Description / Table of Contents: Phase composition curves are presented for a typical saline silt from Lanzhou, P.R.C., and compared to some silts from Alaska. The unfrozen water content of the Chinese silt is much higher than that of the Alaskan silts due to the large amount of soluble salts present in the silts from China, which are not present in silt from interior Alaska. When the salt is removed, the unfrozen water content is then similar for both the Chinese and Alaskan silt. Here we introduce a technique for correcting the unfrozen water content of partially frozen soils due to high salt concentrations. We calculate the equivalent molality of the salts in the unfrozen water at various temperatures from a measurement of the electrical conductivity of the extract from saturated paste.
    Type of Medium: Series available for loan
    Pages: iii, 25 Seiten , Illustrationen
    Series Statement: CRREL Report 84-16
    Language: English
    Note: Contents Abstract Preface Introduction Background Materials Sample preparation Nuclear magnetic resonance Specific surface area Electrical conductivity Results and discussion Summary Literature cited Appendix A: Unfrozen water content vs temperature data for Lanzhou silt
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  • 18
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-84/12
    In: CRREL Report, 84-12
    Description / Table of Contents: Icing on stationary structures such as oil rigs is becoming an increasingly serious problem as offshore drilling operations in the subpolar regions become more common. Little information exists on this subject. Extensive observations have been made of icing on the upper structures of moving ships, but the complexity of this problem makes analysis of the results very difficult. Even the generation of water drops in this case involves many factors, such as windspeed, wave direction relative to the bearing of the ship, and size and free-board of the ship. On stationary structures, however, the problem is much simpler, since the major factor in drop generation is whitecaps produced by wind, and no motion of the structure is involved. In the present study, a theoretical calculation was made by combining the data available on the generation of drops by wind with data on the proportion of ice frozen from the collected water. The rate of ice accumulation on stationary structures was calculated using published data. The results were compared with icing measured on board ships. Although the general trend of this calculation indicated parallelism with the onboard measurements, the measured ice accumulation rate on ships needed a 5 to 8 m/s higher windspeed to correspond with the calculated rate for stationary structures.
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    Pages: ii, 13 Seiten , Illustrationen
    Series Statement: CRREL Report 84-12
    Language: English
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  • 19
    Call number: MOP 46237
    Type of Medium: Monograph available for loan
    Pages: 138 S. , Kt.
    Language: German
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  • 20
    Monograph available for loan
    Monograph available for loan
    Amsterdam [u.a.] : Elsevier Scientific Publ.
    Associated volumes
    Call number: AWI Bio-99-0079-2
    In: The Northwest European Pollen Flora, II
    Type of Medium: Monograph available for loan
    Pages: V, 265 S. , zahlr. Ill.
    ISBN: 0444418806
    Language: English
    Note: CONTENTS: Preface / G. C. S. Clarke and W. Punt. - 8. Solanaceae / W. Punt and M. Monna-Brands. - 9. Saxifragaceae / A. A. M. L. Verbeek-Reuvers. - 10. Boraginaceae / G. C. S. Clarke. - 11. Escalloniaceae / A. A. M. L. Verbeek-Reuvers. - 12. Grossulariaceae / A.A.M.L. Verbeek-Reuvers. - 13. Hydrangeaceae / A. A. M. L. Verbeek-Reuvers. - 14. Parnassiaceae / A. A. M. L. Verbeek-Reuvers. - 15. Plantaginaceae / G. C. S. Clarke and M. R.Jones. - 16. Valerianaceae / G. C. S. Clarke and M. R. Jones. - 17. Aceraceae / G. C. S. Clarke and M. R. Jones. - 18. Hippuridaceae / M. S. Engel. - 19. Haloragaceae / M. S. Engel. - 20. Papaveraceae / A. J. Kalis. - Index. - Errata.
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  • 21
    Monograph available for loan
    Monograph available for loan
    Osnabrück : Naturwissenschaftliches Museum
    Call number: G 8547/1
    Type of Medium: Monograph available for loan
    Pages: XVI, 672 Seiten , Illustrationen : , Begleitmaterial: Anlageband mit 30 Anlagen und der Geologischen Karte 1:200 000 CC 39/10 Bielefeld
    Language: German
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  • 22
    Monograph available for loan
    Monograph available for loan
    Osnabrück : Naturwissenschaftliches Museum
    Call number: G 8547/2
    Type of Medium: Monograph available for loan
    Pages: 31 Blatt , Karten
    Language: German
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  • 23
    Call number: ZSP-SCAR-570-2
    In: Report to SCAR on Antarctic research activities of Germany (FRG), 2
    Type of Medium: Series available for loan
    Pages: 16 Seiten
    ISSN: 0179-0072
    Series Statement: Report to SCAR on Antarctic research activities of Germany (FRG) 2
    Language: English
    Note: Contents: Membership of the National Committee on Antarctic Research of the Federal Republic of Germany. - Introduction. - Station. - Antarctic Research Activities 1979-1980. - Planned Research Activities 1980-1981. - References.
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  • 24
    Call number: ZSP-SCAR-570-6
    In: Antarctic Research Report to SCAR, No. 6
    Type of Medium: Series available for loan
    Pages: 38 Seiten
    ISSN: 0179-0072
    Series Statement: National Antarctic Research Report to SCAR 6
    Language: English
    Note: Contents: Membership of the National Committee on Antarctic Research in the Federal Republic of Germany. - Introduction. - Stations. - I. Record of Activities (past and ongoing), April 83-October 84. - II. Planned Activities, October 84-October 85. - References.
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  • 25
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-84/32
    In: CRREL Report, 84-32
    Description / Table of Contents: Orwell Lake, in west-central Minnesota, is a flood-control, water-management reservoir first impounded in 1953. Subsequent erosion of the shoreline and a lack of knowledge of slope erosion processes in this region prompted this study to identify and quantify the processes there. The processes were measured at selected sites between June 1980 and June 1983. Erosion of the banks is primarily caused by three processes: rain, frost thaw, and waves. The first two processes tend to move sediment to the base of the steep slopes, forming 4 relatively gentle surface of accumulation. Wave action then tends to move this sediment into the lake. Analysis of the data collected over three years has confirmed that wave action is the dominant erosion process, providing almost 77% of the erosion during the 1981-82 study year. During the 1981 high pool level, 2,089 Mg of sediment, mostly colluvium, was removed from the lower slopes by wave action striking the 1.62 km of eroding shoreline. More than 4,300 Mg was eroded by waves accompanying the higher pool levels of 1982., During years in which the pool level does not exceed 325.5 m in elevation, the colluvium slope builds up at the expense of the steeper slope. But during successive years with higher pool levels, the resulting thin colluvium is quickly eroded. Erosion of the primary sediment, a compact till, then occurs, forming the S typical nearly vertical banks. In winter the upland surface adjacent to the lake freezes to a depth of between 1 and 2 m, depending on the surface temperature, the mow cover, and the distance from exposed banks. In late winter soil aggregates, released by the sublimation of interstitial ice within the banks, begin to accumulate at the base of the slopes, often veneering snowbanks there. Once thaw begins, slab failure of bank sediment is followed by mudflows and earthflows. Thaw failure at Orwell Lake in the winter of 1981-82 accounted for over 20% of the erosion; in the spring of 1982, 824 Mg was eroded by this process and 746 Mg the following spring. Such slope failure is most intense along north-facing banks and considerably less intense on south-facing banks, where more effective desiccation and sublimation reduce the soil moisture content. Summer rainfall is responsible for the remaining 3% of the total erosion, amounting to 102 Mg in 1981 and 208 Mg in 1982. Because the banks are steep and relatively short, rainwash is infrequent; rainsplash is the most consistent process during the summer, but the infrequent storms during which rainwash occurscause greater total erosion. Erosion by rain has increased in each of the past three summers, largely because of increased precipitation. Infrequent massive slope failures (slumps) have occurred at the east end of the lake where a buried clay rich unit is stratigraphically and topographically positioned to favor such failures. Drought years followed by heavy spring rains probably will result in additional slope failures of this type at the east end. Unless changes are made, the banks at Orwell Lake will continue to recede. Restriction of the pool level to less than 325.5-m elevation is the least expensive solution to the problem.
    Type of Medium: Series available for loan
    Pages: ix, 110 Seiten , Illustrationen
    Series Statement: CRREL Report 84-32
    Language: English
    Note: CONTENTS Abstract Preface Summary Chapter 1. Introduction Location Purpose of study Previous work Chapter 2. Methodology Geology Overland erosion Wave erosion Frost penetration and heave Thaw failure Bank recession Ground water Soil moisture Chapter 3. Results Geology Geotechnical properties Overland erosion Wave erosion Freeze-thaw phenomena Ground water fluctuations Other slope failures Chapter 4. Discussion Overland erosion Wave erosion Thaw failure Universal soil loss equation Chapter 5. Summary and conclusions Techniques Erosion processes at Orwell lake Bank recession Literature cited Appendix A1: Average cumulative change of surface at erosion stations #2-12, 1980-81 Appendix A2: Cumulative net changes at overland erosion stations #1-12, 1980-81 Appendix A3: Cumulative net changes at overland erosion stations #1 -12, 198 1-82 Appendix A4: Cumulative average erosion at overland erosion stations #1-12, 1980-81 Appendix AS: Cumulative average erosion at overland erosion stations #1-12, 1981-82 Appendix A6: Cumulative average erosion at overland erosion stations #1 -1 2A, 1982 Appendix B: Dimensions of erosion sections, Orwell Lake, Minnesota Appendix C: Piezometer installation data, Orwell Lake, Minneso
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  • 26
    Monograph available for loan
    Monograph available for loan
    Jena : VEB Gustav Fischer Verlag
    Call number: MOP 45081 / Mitte
    Type of Medium: Monograph available for loan
    Pages: IX, 196 Seiten , Illustrationen
    Edition: 3., überarbeitete und ergänzte Auflage
    Language: German
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  • 27
    Call number: MOP 46084 / Mitte
    Description / Table of Contents: This document is a report of research, design, environmental, coordination, and public involvement activities of the Water and Power Resources Service SCPP (Sierra Cooperative Pilot Project). The SCPP ia an investigation of the technical feasibility and social acceptability of winter cloud seeding in the Sierra Nevada to supplement the region's future water supply. This report explains the results of the 1979-80 winter field season and reviews research undertaken by the SCPP in previous seasons.
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    Pages: vi, 72 Seiten , Illustrationen, Karten
    Language: English
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  • 28
    Call number: MOP 46138 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 196 Seiten , Illustrationen , 22 cm
    Language: Russian
    Note: In kyrillischer Schrift
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  • 29
    Monograph available for loan
    Monograph available for loan
    Asheville, NC
    Call number: MOP 45073 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 300 S.
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  • 30
    Call number: MOP 45034 / Mitte
    Type of Medium: Monograph available for loan
    Pages: XII, 371 Seiten
    Language: Russian
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  • 31
    Call number: MOP 45162 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 32 Seiten , Illustrationen, Karten
    Series Statement: Abteilung für theoretische Meteorologie der Universität Wien 25
    Language: German
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  • 32
    Call number: MOP 45232 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 288 Seiten , Illustrationen , 22 cm
    Language: Russian
    Note: In kyrillischer Schrift
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  • 33
    Monograph available for loan
    Monograph available for loan
    Alma-Ata : Izdatel'stvo "Nauka" Kazachskoj SSR
    Call number: MOP 46038 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 174 Seiten , Illustrationen , 21 cm
    Language: Russian
    Note: In kyrillischer Schrift
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  • 34
    Monograph available for loan
    Monograph available for loan
    Boston, Massachusetts : American Meteorological Society
    Call number: MOP 46673 / Mitte
    Type of Medium: Monograph available for loan
    Pages: XIV, 276 Seiten
    Language: English
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  • 35
    Call number: MOP 47852 / Mitte
    Type of Medium: Monograph available for loan
    Language: German
    Note: Diplomarbeit, Humboldt-Universität zu Berlin, 1993
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  • 36
    Call number: MOP 47315 / Mitte
    Type of Medium: Monograph available for loan
    Language: Russian
    Note: In kyrillischer Schrift
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  • 37
    Call number: MOP 46325 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 445 Seiten , Illustrationen
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  • 38
    Call number: MOP 46283 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 148 Seiten , Illustrationen
    Language: German
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  • 39
    Call number: MOP 45063 / Mitte
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  • 40
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-80/2
    In: CRREL Report, 80-2
    Description / Table of Contents: Winter thermal structure and ice conditions in the land-fast ice cover of Lake Champlain were studied in detail for the winters of 1975-76 and 1976-77. The lake was instrumented to a depth of 8.5 m with a string of highly calibrated thermistors attached to an ice mooring system and connected to a data logger at Shelburne Point, Vermont, during the winter of 1975-76 and at Gordon Landing on Grand Isle, Vermont, during 1976-77. This data logger automatically recorded water temperatures from the surface of the lake though snow, ice and water vertical profiles to the bottom of the lake every four hours. Pertinent meteorological parameters are presented for the appropriate measurement sites during the two winter periods, November '75-April '76, and November '76-April '77. Computations were made of freezing degree days (C) for both winters and correlated with ice formation dates. Predictions of ice growth, using the Stefan equation with an empirical coefficient, were correlated with actual ice growth. Documentation was made of the Lake Champlain Transportation Company's first attempt at wintertime navigation by ferry from Gordon Landing, Vermont, to Cumberland Head, New York, in a land fast ice cover during one of the coldest winters of this century.
    Type of Medium: Series available for loan
    Pages: iv, 26 Seiten , Illustrationen
    Series Statement: CRREL Report 80-2
    Language: English
    Note: CONTENTS Abstract Preface Introduction Objectives Climate Site preparation and data collection Instrumentation, measurements and calibration Relocation of measurement site, Fall 1976 Visual observations, ice conditions, and pertinent photography Analysis Air temperature comparisons Degree days of freezing Prediction of ice growth Water and ice temperature Wind Solar radiation Grand Isle ferry operations 1976-77 Conclusions Recommendations Literature cited Appendix A. General observations of ice conditions on Lake Champlain
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  • 41
    Monograph available for loan
    Monograph available for loan
    Boston, Mass. : American Meteorological Society
    Call number: MOP 45485 / Mitte
    Type of Medium: Monograph available for loan
    Pages: iv, 322 Seiten , Illustrationen, Diagramme
    ISBN: 0933876513
    Language: English
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  • 42
    Call number: AWI G3-22-94894
    Description / Table of Contents: The collection includes papers containing new data on spores-pollen complexes, mammal remnants, stratigraphy, lithological-mineralogical characteristics and paleogeography of the Cenozoic in Yakutia, mainly in the Kolyma basin. Summarizing papers are devoted to the history of vegetation in Yakutia during the Cenozoic and to main stages of the relief-formation of the Primorsk lowland. Stages in which thermoabrasive transformation of the shelf and the sea shore during the Holocene became more active are recognized and related to sea transgressions. An analysis of recent crust movements is given. A method for drawing up neotectonic schemes of a lowland formed on the Cenozoic sedimentary cover is proposed.
    Description / Table of Contents: Сборник объединяет статьи, содержащие новые данные по спорово-пыльцевым комплексам, остаткам млекопитающих, стратиграфии, литолого-минералогической характеристике и палеогеографии кайнозоя Якутии, главным образом бассейна р. Колымы . Обобщающие статьи посвящены истории развития растительности севера Якутии в кайнозое и основным этапам рельефообразования Приморской низменности. Выделены этапы активизации термоабразионного преобразования шельфа и морского побережья в голоцене, связанные с трансгрессиями. Анализируются современные движения земной коры. Предлагается методика составления неотектонических схем низменности, развитой на кайнозойском осадочном чехле. Сборник издается к XI Конгрессу Международного союза по изучению четвертичного периода. Книга рассчитана на специалистов в области палеонтологии, стратиграфии, геоморфологии, падеогеографии, неотектоники, геологического картирования и поисков месторождений полезных ископаемых, в особенности в низменных районах с широким развитием рыхлых отложений осадочного чехла.
    Type of Medium: Monograph available for loan
    Pages: 164 Seiten , Illustrationen
    Language: Russian
    Note: CONTENTS The history of vegetation during the Cenozoic in northern Yakutia / A. I. Tomskaya Paleogene spores pollen complexes from the Kolyma right bank / L. P. Zharikova On a finding of a fossil bison on the Indigirka river / P. A. Lazarev Burial conditions of skeleton and body remains of Pleistocene mammals / P. A. Lazarev On the formation of fish fauna in Yakutian reservoirs / F. N. Kirillov, V. F. Vozin The Iithological-mineraloglcal character of Cenozoic sediments of the Primorsk lowland / O. V. Grinenko, A. I. Sergeyenko Stratigraphy of Paleogene-Neogene loose deposits on the Kolyma right bank / A. S. Kazantsev, L. P. Zharikova Quarternary deposits of the Primorsk lowland (Khallerchinsk tundra) / V. B. Spector Upper Cenozoic deposits of the Kolyma lowland / O. V. Grinenko Main stages in the formation of the relief of the Primorsk lowland, East Jakutia, and its mountain surroundings / A. G. Savchenko Recent crust movements and their geomorphologic expression in the nearshore zone of the Kolyma lowland / Ya. A. Ben A comprehensive investigation of closed territory neotectonics (in the light of the Yano-Kolyma lowland) / V. A. Balandin The geomorphological expression of the Ichen overthrust zone of the Moma range / Ya. A. Ben Variations of the Laptev Sea and the East Siberian Sea level and their role in the formation of shore deposits / K. S. Yefremov Modelling as a method of structural geomorphic analysis / V. A. Balandin , СОДЕРЖАНИЕ История развития растительности севера Якутии в кайнозое / А. И. Томская Палеогеновые спорово-пыльцевые комплексы правобережья реки Колымы / Л. П. Жарикова О находке ископаемого бизона на реке Индигирке / П . А. Лазарев Условия захоронения скелетных и трупных остатков плейстоценовых млекопитающих / П. А. Лазарев О формировании ихтиофауны в водоемах Якутии / Ф. Н. Кириллов, В. Ф. Возин Литолоrо-минералогическая характеристика кайнозойских отложений Приморской низменности / О. В. Гриненко, А. И. Серrеенко Стратиграфия рыхлых палеоген-неогеновых отложений правобережья реки Колымы / А. С. Казанцев, Л. П. Жарикова Четвертичные отложения Приморской низменности (Халлерчинская тундра) / В. Б. Спектор Верхнекайнозойские отложения Колымской низменности / О. В. Гриненко Основные этапы рельефообразования Приморской низменности Восточной Якутии и ее горного обрамления / А. Г. Савченко Современные движения земной коры и их геоморфологическое выражение в прибрежной зоне Колымской низменности / Я. А. Бень Комплексное изучение неотектоники закрытых территорий (На примере Яне-Колымской низменности) / В. А. Баландин Геоморфологическое выражени е Иченской надвиговой зоны Момского хребта / Я. А. Бень Колебания уровней морей Лаптевых и Восточно-Сибирского В голоцене и их роль в формировании прибрежно-морских отложений / К. С. Ефремов Моделирование как метод структурно-геоморфологического анализа / В. А. Баландин , In kyrillischer Schrift
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  • 43
    Call number: AWI G3-22-94975
    Type of Medium: Series available for loan
    Pages: XIII, 263 Seiten , Illustrationen , 1 Karte
    Edition: First edition 1983, reprinted edition 1993
    Series Statement: Guidebook / Division of Geological & Geophysical Surveys, Department of Natural Resources, State of Alaska 1
    Language: English
    Note: Kartenbeilage unter dem Titel: Physiographic map and field trip localities of the Upper Cook Inlet area, Alaska / compiled by R. D. Reger and R. G. Updike (1982) , CONTENTS Introduction General statement Organization and acknowledgments Selected references Middle Tanana River valley R&sum& of the permafrost and Quaternary geology Road log and locality descriptions Selected references Delta River area. Alaska Range R&sum& of the permafrost and Quaternary geology Road log and locality description Trans-Alaska Pipeline System Thawing problems Construction modes Conventional burial Special burial Conventional elevated and anchor support Selected references Copper River basin Rèsumè of Quaternary geology Road log and locality description Gakona section Richardson Highway Simpson Hill roadcut Copper River Bluff section Glenn Highway Selected references Overview of the Matanuska Glacier Selected references Upper Cook Inlet region and the Matanuska Valley Introduction Physiography and geology Upper Cook Inlet region Matanuska Valley Climate Vegetation. Soils Rèsumè of Quaternary geology General statement Late Pliocene-early Pleistocene glaciations and interglaciations Mt. Susitna Glaciation Mt. Susitna-Caribou Hills interglaciation Caribou Hills Glaciation Late Pleistocene glaciations and interglaciations Caribou Hills-Eklutna interglaciation Eklutna Glaciation Eklutna-Knik interglaciation Knik Glaciation Knik-Naptowne nonglacial interval Naptowne Glaciation Early Holocene Glaciations Middle to Late Holocene events Alaskan Glaciation Tustumena advances Tunnel advances Other events Road log and locality descriptions Selected references Appendix A - Radiocarbon dates related to late Quaternary events in the Upper Cook Inlet region, Alaska
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  • 44
    Call number: AWI G3-22-94972
    In: Mitteilungen der Versuchsanstalt für Wasserbau, Hydrologie und Glaziologie an der Eidgenössischen Technischen Hochschule Zürich, 122
    Type of Medium: Series available for loan
    Pages: 222 Seiten , Illustrationen
    Series Statement: Mitteilungen der Versuchsanstalt für Wasserbau, Hydrologie und Glaziologie an der Eidgenössischen Technischen Hochschule Zürich 122
    Language: German
    Note: Zürich, Eidgenössische Technische Hochschule, Dissertation, 1993 , Inhaltsverzeichnis Vorwort Zusammenfassung Abstract 1. Einleitung 1.1 Permafrost und Blockgletscher 1.2 Die Permafrostforschung in der Schweiz 1.3 Klassische Untersuchungsmethoden 1.4 Problemstellung 1.5 Glossar 2. Die untersuchten Gebiete 2.1 Allgemeines 2.2 Der Blockgletscher Murtel-Corvatsch 2.2.1 Lokalitätsbeschreibung 2.2.2 Feldarbeiten 2.3 Der Blockgletscher Muragl 1 2. 3.1 Lokalitätsbeschreibung 2.3.2 Feldarbeiten 2.4 Der Blockgletscher Suvretta 2.4.1 Loka!itätsbeschreibung 2.4.2 Feldarbeiten 2.5 Pontresina - Schafberg 2.5.1 Lokalitätsbeschreibung 2.5.2 Feldarbeiten 3. Geophysikalische Sondiermethoden im Permafrost 3.1 Allgemeines 3.2 Refraktionsseismik 3.2.1 Einleitung 3.2.2 Zielsetzung der Refraktionsseismik im Permafrost 3.2.3 Ausrüstung, Messtechnik 3.2.4 Herauslesen der Ersteinsätze 3.2.4.1 Ersteinsätze mit geringer Amplitude und grosser Periode 3.2.4.2 Rauschen 3.2.5 Auswertungsmethoden 3.2.5.1 Intercept-Methode, Knickpunkt-Methode 3.2.5.2 Die Plus-Minus-Methode 3.2.5.3 Hales-Methode 3.2.5.4 Die 'Generalized Reciprocal Method (GRM) 3.2.5.5 Auswertung der Sprengseismik im Pennafrost 3.2.5.6 Abfolge der Auswertung mittels dem GRMVerfahren am Beispiel des Profils MGL S5 3.2.6 Blockgletscher Murtel-Corvatsch 3.2.6.1 Profil MRT S1 3.2.6.2 Profil MRT S2 3.2.6.3 Schlussfolgerungen Seismik Murtel-Corvatsch 3.2.7 Blockgletscher Muragl 3.2.7.1 Profil MGL S1 3.2.7.2 Profil MGL S2 3.2.7.3 Profil MGL S3 3.2.7.4 Profil MGL S4 3.2.7.5 Profil MGL S5 3.2.7.6 Zusammenfassung Seismik Blockgletscher Muragl 3.2.8 Blockgletscher Suvretta 3.2.8.1 Profil SUV S1 3.2.8.2 Profil SUV S2 3.2.8.3 Profil SUV S3 3.2.8.4 Profil SUV S4 3.2.8.5 Profil SUV S5 3.2.8.6 Zusammenfassung Blockgletscher Suvretta 3.2.9 Pontresina - Schafberg 3.2.9.1 Profile beim Bohrloch 2/1990 3.2.9.2 Profile beim Bohrloch 1/1990 3.2.9.3 Zusammenfassung Pontresina - Schafberg 3.2.10 Schlussfolgerungen Refraktionsseismik 3.3 Gleichstrom - Geoelektrik 3.3.1 Einleitung 3.3.1.1 Allgemeines 3.3.1.2 Spezifischer Widerstand verschiedener Eisarten 3.3.1.3 Geoelektrik im Permafrost 3.3.2 Ankoppelungsversuche 3.3.3 Beispiel einer Auswertung 3.3.3.1 Allgemeines 3.3.3.2 Schlumberger-Anordnung (symmetrisch) 3.3.3.3 Hummel-Anordnung oder Halbe Schlumberger-Anordnung 3.3.4 Blockgletscher Murtel-Corvatsch I 3.3.4.1 Diskussion der einzelnen Sondierkurven 3:3.4.2 Zusammenfassung Blockgletscher Murtel-Corvatsch 3.3.5 Blockgletscher Muragl 1 3.3.5.1 Diskussion der einzelnen Sondierkurven 3.3.5.2 Zusammenfassung Blockgletscher Muragl 3.3.6 Blockgletscher Suvretta 3.3.6.1 Diskussion der einzelnen Sondierkurven 3.3.6.2 Zusammenfassung Blockgletscher Suvretta 3.3.7 Pontresina-Schafberg 3.3.7.1 Diskussion der einzelnen Sondierkurven 3.3.7.2 Zusammenfassung Pontresina-Schafberg 3.3.8 Schlussfolgerungen Gleichstrom-Geoelektrik 3.4 Georadar 3.4.1 Allgemeines 3.4.2 Messungen auf dem Blockgletscher Murtel-Corvatsch 3.4.3 Schlussfolgerungen Georadar.und Ausblick 3.5 Gravimetrie 3.5.1 Einleitung 3.5.2 Theoretische Grundlagen 3.5.2.1 Effekt der geographischen Breite 3.5.2.2 Effekt der Höhe über Meer 3.5.2.3 Topographischer Effekt 3.5.3 Gravimetrische Messungen und Korrekturen 3.5.4 Modellierung 3.5.5 Resultate und Diskussion 3.5.6 Schlussfolgerungen Gravimetrie 3.6 Very-Low-Frequency Resistivity (VLF-R) 3.6.1 Einleitung 3.6.2 Theoretische Grundlagen 3.6.2.1 Messungen mit mehreren Frequenzen 3.6.2.2 Messungen in mehreren Richtungen 3.6.3 VLF0R Messungen im alpinen Permafrost 3.6.3.1 Allgemeines 3.6.3.2 Bohrloch Murtel-Corvatsch 3.6.3.3 Pontresina-Schafberg 3.6.3.4 Blockgletscher Muragl I 3.6.3.5 Gruben 3.6.4 Zusammenfassung VLF-R und Ausblick 4 Bohrlochsondierungen 4.1 Allgemeines 4.2 Bohrlochlogging 4.2.1 Das Kaliber-Log 4.2.2 Das Garnma-Ray-Log 4.2.3 Das Gamma-Gamma-Log 4.2.4 Das Neutron-Neutron-Log 4.2.5 Das Resistivity-Log 4.2.6 Das Sonic-Log 4.2.7 Korrelationen zwischen den einzelnen Logs im Bohrloch 1/1990 4.2.8 Schlussfolgerung Bohrloch-Logging 4.3 Bohrlochseisrnik im Bohrloch 2/1987 (Murtel-Corvatsch) 4.3.1 Einleitung 4.3.2 Konzept der Messung 4.3.3 Schwierigkeiten bei der Auswertung der bohrlochseismischen Daten 4.3.3.1 Bestimmen der Nullzeit 4.3.3.2 Herauslesen der Ersteinsätze 4.3.3.3 Korrektur der Einsatzzeiten 4.3.4 Berechnung der seismischen Geschwindigkeiten 4.3.4.1 P-Wellen 4.3.4.2 S-Wellen (average velocity) 4.3.5 Spezialexperirnent 4.3.6 Schlussfolgerungen Bohrlochseisrnik 5 Temperaturmessungen im Permafrost 5.1 Einleitung 5.2 Ausrüstung.und Messgenauigkeit 5.3 Temperaturen im Bohrloch Murtel-Corvatsch 5.3.1 Analyse der Jahreszeitenschwankungen 5.3.2 Kommentar zu den Temperaturreihen im Bohrloch 2/1987 5.3.2.1 Temperaturentwicklung in 1.6 m Tiefe (mittlere Differenz der Extremwerte: 9°C) 5.3.2.2 Temperaturentwicklung in 2.6 m Tiefe (mittlere Differenz der Extremwerte: 5°C) 5.3.2.3 Temperaturentwicklung in 3.6 m Tiefe (mittlere Differenz der Extremwerte: 3.5°C) 5.3.2.4 Temperaturentwicklung in 7.6 m Tiefe (mittlere Differenz der Extremwerte: 1.5°C) 5.3.2.5 Temperaturentwicklung in 11.6 m Tiefe (mittlere Differenz der Extremwerte: 0.6°C) 5.3.2.6 Temperaturentwicklung in 15.6 m Tiefe (mittlere Differenz der Extremwerte: 0.2°C) 5.3.2.7 Temperaturentwicklung in 21.6 m Tiefe (mittlere Differenz der Extremwerte: 〈 0.1 °C) 5.3.3 Vertikale Temperaturverteilung im Bohrloch 2/1987 5.3.4 Saisonale Temperaturschwankungen zwischen 52 m und 56 m Tiefe 5.4 Temperaturen in den Bohrlöchern am Pontresina-Schafberg 5.4.1 Vertikale Temperaturverteilung auf dem Pontresina-Schafberg 5.5 Auswirkungen von Variationen der Oberflächentemperaturen auf vertikale Temperaturprofile 5.6 Schlussfolgerungen Permafrosttemperaturen 6 Schlussfolgerungen 7 Literaturverzeichnis ANHANG Geoelektrische Tiefensondierungen Blockgletscher Murtel-Corvatsch Sondierung MRT E1 Sondierung MRT E2 Sondierung MRT E3 Sondierung MRT E4 Sondierung MRT E5 Blockgletscher Muragl Sondierung MGL E1 Sondierung MGL E2 Sondierung MGL E3 Blockgletscher Suvretta Sondierung SUV E1 Sondierung SUV E2 Sondierung SUV E3 Pontresina-Schafberg Sondierung SFB E1 Sondierung SFB E2 Sondierung SFB E3 Sondierung SFB E4 Temperaturreihen im Bohrloch 2/1987 (Murtel-Corvatsch)
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  • 45
    Series available for loan
    Series available for loan
    Moscow : Academy of Sciences of the USSR, Soviet Committee on Antarctic Research
    Associated volumes
    Call number: MOP 46294/B / Mitte
    In: USSR national report to SCAR, No. 26
    Type of Medium: Series available for loan
    Series Statement: USSR national report to SCAR 26
    Language: English
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  • 46
    Monograph available for loan
    Monograph available for loan
    Tulsa, Oklahoma : American Ass. of Petroleum Geologists
    Call number: MR 22.94992
    Type of Medium: Monograph available for loan
    Pages: 237 Seiten , überwiegend Illustrationen, graphische Darstellungen
    ISBN: 0-89181-653-4
    Series Statement: AAPG methods in exploration series 4
    Language: English
    Note: INTRODUCTION WHY SEM ANALYSIS? FORMAT SAMPLE PREPARATION HOW THE SEM WORKS THE SEM MICROGRAPH ELEMENTAL ANALYSIS BY SEM EDX ANALYSIS OF MINERALS SILICATES Silica Quartz Cristobalite (Opal-CT) Opal (Opal-A) Feldspars Potassium Feldspar Resorbed Potassium Feldspar Plagioclase Feldspar with K-Feldspar Overgrowths Resorbed Plagioclase Feldspar Clays Chlorite Illite Kaolinite Halloysite Smectite Nontronite Hectorite Illite-smectite Corrensite Glauconite Rectorite Palygorskite Vermiculite Zeolites Analcime Chabazite Clinoptilolite Erionite Heulandite Laumontite Mordenite Phillipsite Thomsonite Yugawaralite Micas Biotite Muscovite Phlogopite Amphiboles Hornblende Actinolite Riebeckite Pyroxenes Augite Hypersthene Others Talc Chrysotile Sphene CARBONATES Calcite Dolomite Ferroan Dolomite/Ankerite Siderite Chalk PHOSPHATES Apatite Collophane Florencite HALIDES Halite SULFIDES Pyrite Sphalerite SULFATES Gypsum Anhydrite Copiapite Melanterite Barite OXIDES Hematite and Goethite Rutile Magnetite llmenite MISCELLANEOUS Wood ENERGY TABLE OF CHARACTERISTIC X-RAY TRANSITIONS GLOSSARY REFERENCES
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  • 47
    Monograph available for loan
    Monograph available for loan
    Boca Raton : Smoley
    Call number: PIK N 601-93-0043
    Type of Medium: Monograph available for loan
    Pages: VIII, 308 S , graph. Darst.
    ISBN: 0849387221
    Language: English
    Location: A 18 - must be ordered
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  • 48
    Monograph available for loan
    Monograph available for loan
    Jena : Univ.
    Call number: PIK N 602-21-94422
    Type of Medium: Monograph available for loan
    Pages: 31 S. , Ill.
    Edition: 4., neu erarb. Aufl.
    Language: German
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  • 49
    Call number: MOP 46828/1 / Mitte ; MOP 46828/2 / Mitte
    Type of Medium: Monograph available for loan
    Pages: xv, 642 Seiten , Illustrationen , 30 cm
    Language: English
    Note: Introduction Climatic changes as possible consequences of human activities Impact study Case study: the impacts of a CO₂-induced climatic change on the agricultural sector of the European Communities Case study: the impacts of a CO₂-induced climatic change on water availability in the European Communities Case study: the impacts of a CO₂-induced climatic change on the energy sector of the European Communities Case study: the economic consequences of a change in climate on agriculture.
    Location: MOP - must be ordered
    Location: MOP - must be ordered
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  • 50
    Call number: AWI G6-23-95004
    Type of Medium: Monograph available for loan
    Pages: vii, 100 Seiten , Illustrationen
    Language: English
    Note: Bachelorarbeit, Wilfrid Laurier University, 1993 , TABLE OF CONTENTS Chapter 1 Introduction Chapter 2 Literature Review 2.1 Introduction 2.2 Water Balance 2.3 Nutrient Inputs 2.4 Models Chapter 3 Study Site and Site Characteristics 3.1 Study Site Location 3.2 Geology 3.3 Surface Cover 3.4 Permafrost Depth 3.5 Lake Formation 3.6 Lake Characteristics 3.7 Lake Sub Basin Characteristics 3.8 Climate 3.9 Precipitation and Melt 3.10 Evaporation Chapter 4 Methods 4.1 Introduction 4.2 Physical Sampling 4.2.1 Water Level 4.2.2 Stream Discharge 4.2.3 Precipitation 4.2.4. Radiation 4.2.5 Evaporation 4.2.6 Groundwater 4.3 Chemical Sampling 4.3.1 Total Phosphorus 4.4 Biological Sampling 4.4.1 Chlorophyll a 4.5 Water Balance 4.6 Nutrient Inputs 4.7 Models 4.7.1 Predicting Total Phosphorus Concentrations 4.7.2 Chlorophyll a Chapter 5 Results 5.1 Introduction 5.2 Water Balance 5.2.1 Lake Storage 5.2.2 Stream Discharge 5.2.3 Precipitation 5.2.4 Radiation 5.2.5 Evaporation 5.2.6 Groundwater 5.3 Nutrient Inputs 5.4 Models 5.4.1 Predicting Total Phosphorus Concentrations 5.4.2 Chlorophyll a Chapter 6 Discussion 6.1 Introduction 6.2 Water Balance 6.3 Nutrient Inputs 6.4 Models Chapter 7 Further Study Appendices Appendix 1 Lake Storage Appendix 2 Discharge Data Appendix 3 Precipitation Appendix 4 Radiation Appendix 5 Evaporation Appendix 6 Nutrient Data Appendix 7 Chlorophyll a Bibliography , Englisch
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  • 51
    Monograph available for loan
    Monograph available for loan
    Anchorage, Alas. : Bureau of Land Management, Alaska State Office | Anchorage, Alas. : Alaska Natural History Association
    Call number: AWI G3-23-95156
    Type of Medium: Monograph available for loan
    Pages: 128 Seiten , Illustrationen, Karten , 27 cm
    ISBN: 0930931106 , 0-930931-10-6
    Language: English
    Note: Contents Foreword Introduction Oil - Catalyst for change The Haul Road - Highway to the Arctic Origins: The geologic setting Glaciers shape the land Glaciation and wildlife distribution Permafrost and the periglacial environment The Dalton Highway road log Glossary Selected references
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  • 52
    Call number: MR 22.94948
    Type of Medium: Monograph available for loan
    Pages: XIII, 395 Seiten , graphische Darstellungen, Karten , 5 Database microfiche cards
    ISBN: 0-620-06650-4
    Series Statement: Geological Society of South Africa: Special publication 13
    Language: English
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  • 53
    Monograph available for loan
    Monograph available for loan
    Washington, DC : American Geophysical Union
    Call number: MR 22.94951
    Type of Medium: Monograph available for loan
    Pages: 76 Seiten , Illustrationen, Karten
    Edition: Revised Edition
    ISBN: 0-87590-234-0
    Language: English
    Note: Introduction Trip 1. A Streetcar to Subduction Trip 2. To Fort Mason and Subducted Sandstone Trip 3. Baker's Beach and Fort Point: A Trip to Melange and Serpentine Trip 4. A Sedentary Survey of the Structure of the City (With Side Trips Afoot) Trip 5. Marin Headlands: Pillow Basalt and Chert Trip 6. A Boat Trip to the Blueschist Facies: Angel Island and the Metamorphosed Francisan Trip 7. After Subduction Is Over: A BART Trip to a Transform Fault Appendix Glossary Selected Bibliography
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  • 54
    Monograph available for loan
    Monograph available for loan
    Novosibirsk : Izdatel'stvo "Nauka", Sibirskoe otdelenie
    Associated volumes
    Call number: AWI G3-24-95571-8
    In: Tektonika Sibiri, Tom 8
    Description / Table of Contents: Рассмотрены теоретические и методологические вопросы тектоники, в частности, тектоническое районирование и создание тектонических карт, периодизация тектонической истории Земли, иерархия тектонических объектов, изучение пликативных и дизъюнктивных форм, дистанционные методы в тектонике. Подведены итоги исследования тектоники отдельных регионов Сибири и Дальнего Востока. Сборник рассчитан на широкий круг геологов.
    Description / Table of Contents: Translation of the abstract: Theoretical and methodological issues of tectonics are considered, in particular, tectonic zoning and the creation of tectonic maps, periodization of the tectonic history of the Earth, the hierarchy of tectonic objects, the study of plicative and disjunctive forms, remote sensing methods in tectonics. The results of the study of tectonics of individual regions of Siberia and the Far East are summed up. The collection is intended for a wide range of geologists.
    Type of Medium: Monograph available for loan
    Pages: 152 Seiten , Illustrationen
    Series Statement: Tektonika Sibiri / Akademija Nauk SSSR, Sibirskoe Otdelenie, Naučnyj Sovet po Tektonike Sibiri i Dalʹnego Vostoka Tom 8
    Language: Russian
    Note: СОДЕРЖАНИЕ Предисловие Принципы тектонического районирования / Т. Н. Спижарский Периодизация тектонической истории Земли / Ч. В. Ворукаев Тектоника и "тектоники" / В. Ю Забродин, В. А. Кулындышев, В. А. Соловьев Иерархия тектонических объектов, их геоценозы и тектонические карты / В. И. Драгунов Глубинное строение и тектоника фундамента Сибирской платформы / Э. Э. Фотиади, М. П. Гришин, В. И. Лотышев, В. С. Сурков Место тектоники среди других наук о Земле / Ю. Н. Карогодин К теории дизъюнктивов / В. Ю. Забродин Методологические аспекты и критерии выделения основных структурных элементов земной коры / В. С. Бочкарев Карта разломов территории СССР и сопредельных стран масштаба 1:2 500 000 / Н. А. Беляевский, А. И. Суворов, В.А. Унксов, С. Н. Тихомиров, С. К. Барыкин, Б. В. Ермков, А. Е. Михайлов, Ю. Е. Погребицкий, Г. З. Попова, Ю. М. Саркисов, В. Н. Семов, К. А. Шуркин О размещении промышленно-перспективных районов в поле плотности дизъюнктивов Сибири / В. В. Вогацкий, В. И. Витязь, В. Я. Ероменко, М. А. Чурилин Энергетика и эволюция мантийной циркуляции / К. И. Хейсканен Тектоническая позиция глубинных гранулитов и особенности строения нижних горизонтов земной коры / Л. П. Карсаков Спиральные системы геологических структур и некоторые приемы их выяв-ления / М. А. Чурилин Новая ротационная гипотеза структурообразования и тектоника плит / К. Ф. Тяпкин Значение будинажа при картировании немых толщ докембрия / С. Н. Кудрин Определение простракственной связи трещин отрыва со сместителем при комбинированных тектонических перемещениях / О. А. Сокольников Унаследованные и новообразованные Структуры многоэтапных деформаций / М. М. Константинов Применение дистанционных методов при тектонических исследованиях в западной части Сибирской платформы / Л. М. Герасимов, В. Ю. Лускина Разрывные нарушения Сибирской платформы по данным дешифрирования телевизионных космических снимков / В. Я. Ероменко Структурное районирование и металлогеническая специфика вых областей юга азиатской части СССР / В. А. Амантов, Е. В. Выковская, Г. Л. Добрецов, А. Л. Додин, Е. М. Заблоцкий, П. С. Матросов, У. И. Моисееnко, В. R. Путинцев, Ж. Н. Рудакова, Г. Н. Шапошников, А. Д. Щеглов Основные этапы развития древних платформ / К. Б. Мокшанцев, А. Ф. Петров, Г. С. Фрадкин Континенты и океаны раннего докембрия Сибири / А. М. Лейтес, В. С. Федоровский Тектоническая позиция анортозитовой формации Сибирской платформы и ее место в истории становления земной коры / В. Н. Мошкин , CONTENT Preface Principles of tectonic zoning / T. N. Spizharsky Periodization of the tectonic history of the Earth / Ch. V. Vorukaev Tectonics and “tectonics” / V. Yu Zabrodin, V. A. Kulyndyshev, V. A. Solovyov Hierarchy of tectonic objects, their geocenoses and tectonic maps / V. I. Dragunov Deep structure and tectonics of the foundation of the Siberian Platform / E. E. Fotiadi, M. P. Grishin, V. I. Lotyshev, V. S. Surkov The place of tectonics among other earth sciences / Yu. N. Karogodin On the theory of disjunctive / V. Yu. Zabrodin Methodological aspects and criteria for identifying the main structural elements of the earth's crust / V. S. Bochkarev Map of faults in the territory of the USSR and neighboring countries on a scale of 1:2,500,000 / N.A. Belyaevsky, A.I. Suvorov, V.A. Unksov, S. N. Tikhomirov, S. K. Barykin, B. V. Ermkov, A. E. Mikhailov, Yu. E. Pogrebitsky, G. Z. Popova, Yu. M. Sarkisov, V. N. Semov, K. A. Shurkin On the placement of industrially promising areas in the field of density of disjuncts of Siberia / V. V. Vogatsky, V. I. Vityaz, V. Ya. Eromenko, M. A. Churilin Energy and evolution of mantle circulation / K. I. Heiskanen Tectonic position of deep granulites and structural features of the lower horizons of the earth’s crust / L. P. Karsakov Spiral systems of geological structures and some techniques for their identification / M. A. Churilin New rotational hypothesis of structure formation and plate tectonics / K. F. Tyapkin The importance of boudinage when mapping silent Precambrian strata / S. N. Kudrin Determination of the spatial connection of detachment cracks with a displacement fault during combined tectonic movements / O. A. Sokolnikov Inherited and newly formed Structures of multi-stage deformations / M. M. Konstantinov Application of remote sensing methods in tectonic studies in the western part of the Siberian platform / L. M. Gerasimov, V. Yu. Luskina Discontinuity violations of the Siberian platform according to the interpretation of television space images / V. Ya. Eromenko Structural zoning and metallogenic specificity of the southern Asian parts of the USSR / V. A. Amantov, E. V. Vykovskaya, G. L. Dobretsov, A. L. Dodin, E. M. Zablotsky, P. S. Matrosov, U. I. Moiseenko, V. R. Putintsev, Zh. N. Rudakova, G. N. Shaposhnikov, A. D. Shcheglov The main stages of the development of ancient platforms / K. B. Mokshantsev, A. F. Petrov, G. S. Fradkin Continents and oceans of the Early Precambrian of Siberia / A. M. Leites, V. S. Fedorovsky Tectonic position of the anorthosite formation of the Siberian platform and its place in the history of the formation of the earth’s crust / V. N. Moshkin , In kyrillischer Schrift
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  • 55
    Monograph available for loan
    Monograph available for loan
    Novosibirsk : Izdatel'stvo "Nauka", Sibirskoe otdelenie
    Associated volumes
    Call number: AWI G3-24-95571-9
    In: Tektonika Sibiri, Tom 9
    Description / Table of Contents: Представлены материалы XII сессии Научного совета no тектонике Сибири и Дальнего Востока, посвященной 60-летию Великой Октябрьской социалистической революции (Красноярск, 1977 r.). Рассмотрены общие вопросы тектоники нефтегазоносных областей, приведены соответствующие конкретные материалы по отдельным районам Сибири и Дальнего Востока. Изложены новые представления о региональной тектонике Западно-Сибирской плиты, Сибирской платформы, Алданского щита, северо-западной части Тихоокеанскоrо пояса. Сборник рассчитан на широкий круr rеолоrов.
    Description / Table of Contents: Translation of abstract: The materials of the XII session of the Scientific Council on the tectonics of Siberia and the Far East, dedicated to the 60th anniversary of the Great October Socialist Revolution (Krasnoyarsk, 1977), are presented. General issues of tectonics of oil and gas bearing areas are considered, and relevant specific materials on individual regions of Siberia and the Far East are presented. New ideas about the regional tectonics of the West Siberian Plate, the Siberian Platform, the Aldan Shield, and the northwestern part of the Pacific Belt are presented. The collection is designed for a wide audience.
    Type of Medium: Monograph available for loan
    Pages: 158 Seiten , Illustrationen
    Series Statement: Tektonika Sibiri / Akademija Nauk SSSR, Sibirskoe Otdelenie, Naučnyj Sovet po Tektonike Sibiri i Dalʹnego Vostoka Tom 9
    Language: Russian
    Note: СОДЕРЖАНИЕ Предисловие Принципы и методика построения тектонических карт нефтегазоносных территорий СССР / Г. Х. Дикенштейн, Ю. Н. Швембергер, И. М. Алиев Требования к содержанию и принципы построения тектонических карт нефтегазоносных территорий / В. С. Старосельцев Количественные подходы к тектоническому районированию нефтегазоносных областей (на примере Енисей-Ленского регионального мегапрогиба) / Ю. Н. Карогодин, А. И. Прокопенко Тектоника палеозойского нефтегазоносного комплекса юга Западно-Сибирской плиты / Н. П. Запивалов, В. И. Московская, И. И. Плуман Тектоника и генезис Западно-Сибирской плиты в свете новых геолого-геофизических данных / М. Я. Рудкевич Связь трещиноватости пород с пликативными структурами первого порядка (на примере Западно-Сибирской плиты и Вилюйской гемисинеклизы) / К. И. Микуленко, Е. Д. Глухманчук, Л. А. Сечкина, Г. Г. Шемин Эпикаледонские наложенные впадины и их газоносность / Е. Д. Думнов Особенности строения фундамента Минусинского межгорного прогиба / Я. В. Шатов, П. С. Долгушин, 3. В. Разилова Структурные особенности платформенного чехла западной части Сибирской платформы в связи с оценкой перспектив поисков месторождений нефти и газа / В. Д. Накаряков, К. Н. Васильева, А. М Иванов, В. Е. Кучеров, В. Г. Сибгатуллиn, Ю. А. Шарыгин Анализ палеотектонических движений Сибирской платформы в связи с оценкой генерации и аккумуляции углеводородов и консервация их залежей в домезозойских отложениях / Т. К Баженова, Ю. И. Ипатов, К. К. Макаров, Ю. М. Шуменкова Тектоническое районирование Вилюйской гемисинеклизы в связи с ее нефтегазоносностью / В. Е. Бакин, В. А. Богдашев, А. А. Гудков, К. И. Микуленко, В. С. Ситников О блоковом строении и иефтегазоносности Тунгусского бассейна / Б. А.Соколов, В. А. Егоров, Ю. Р. Мазор, Ю. В. Пискарев История формирования и перспективы нефтегазоносности Момо-3ырянской впадины / Б. И. Ким Результаты и проблемы изучения тектоники западной части Сибирской платформы и Енисей-Хатангского прогиба по геолого-геофизическим данным / В. И. Яскевич, Ю. К. Яковлев, А. П. Четвергов, В. П. Ключко, В. И. Степанов Тектонический анализ платформенных структур методом построения графиков амплитуд / Е, М. Максимов Тектоника о. Сахалин и прилегающего шельфа / В. В Харахинов, В. Э. Kононов, Ю. С. Мавринский, А. А. Терещепков, Ю. А. Тронов Разломы о. Сахалин и прилегающего шельфа / В. В Харахинов, С. Д. Гальцев-Безюк, Ю. С. Мавринский, А. А. Терещенко, И. М. Альперович Основные структурные елементы Хоккайдо-Сахалинской складчатой области / В. И. Головинский, И. И. Тютрин Прогибы зоны сочленения Сихотэ-Алинской и Хоккайдо-Сахалинской складчатых систем / Н. В. Kуликов, А. А. Терещенков Эндогенный режим Сахалина / Д. Ф. Семенов, Л. С. Маргулис, А. А. Апдреев, В. Ф. Евсеев О тектонике Охотского моря / Ю. С. Мавринский, В. А. Бабошина, Н. В. Kуликов, В. В. Харахинов Строение, развитие и перспективы нефтегазоносности подводных окраин Западной Африки и Восточной Азии / А. Ю. Юнов Формационный анализ осадочных бассейнов северо-западной части Тихоокеанскоrо пояса / Ю. K. Вурлин, О. K. Важенова Методика неотектонического анализа переходной зоны от континента к океану / Г. Ф. Уфимцев , Translation of Contents Preface Principles and methods for constructing tectonic maps of oil and gas-bearing territories of the USSR / G. Kh. Dikenshtein, Yu. N. Shvemberger, I. M. Aliev Content requirements and principles for constructing tectonic maps of oil and gas-bearing territories / V. S. Staroseltsev Quantitative approaches to tectonic zoning of oil and gas-bearing regions (on the example of the Yenisei-Lena regional megatrough) / Yu. N. Karogodin, A. I. Prokopenko Tectonics of the Paleozoic oil and gas complex of the south of the West Siberian Plate / N. P. Zapivalov, V. I. Moskovskaya, I. I. Pluman Tectonics and genesis of the West Siberian plate in the light of new geological and geophysical data / M. Ya. Rudkevich Relationship between rock fracturing and first-order plicative structures (using the example of the West Siberian Plate and the Vilyui hemisyneclise) / K. I. Mikulenko, E. D. Glukhmanchuk, L. A. Sechkina, G. G. Shemin Epicaledonian superimposed depressions and their gas content / E. D. Dumnov Features of the structure of the foundation of the Minusinsk intermountain trough / Ya. V. Shatov, P. S. Dolgushin, Z. V. Razilova Structural features of the platform cover of the western part of the Siberian platform in connection with the assessment of prospects for prospecting for oil and gas fields / V. D. Nakaryakov, K. N. Vasilyeva, A. M. Ivanov, V. E. Kucherov, V. G. Sibgatullin, Yu. A. Sharygin Analysis of paleotectonic movements of the Siberian platform in connection with the assessment of the generation and accumulation of hydrocarbons and the conservation of their deposits in pre-Mesozoic deposits / T. K. Bazhenova, Yu. I. Ipatov, K. K. Makarov, Yu. M. Shumenkova Tectonic zoning of the Vilyui hemisyneclise in connection with its oil and gas potential / V. E. Bakin, V. A. Bogdashev, A. A. Gudkov, K. I. Mikulenko, V. S. Sitnikov On the block structure and oil and gas content of the Tunguska basin / B. A. Sokolov, V. A. Egorov, Yu. R. Mazor, Yu. V. Piskarev History of formation and prospects for oil and gas potential of the Momo-3yryansk depression / B. I. Kim Results and problems of studying the tectonics of the western part of the Siberian platform and the Yenisei-Khatanga trough based on geological and geophysical data / V. I. Yaskevich, Yu. K. Yakovlev, A. P. Chetvergov, V. P. Klyuchko, V. I. Stepanov Tectonic analysis of platform structures by constructing amplitude graphs / E, M. Maksimov Tectonics o. Sakhalin and the adjacent shelf / V. V. Kharakhinov, V. E. Kononov, Yu. S. Mavrinsky, A. A. Tereshchepkov, Yu. A. Tronov Faults o. Sakhalin and the adjacent shelf / V. V. Kharakhinov, S. D. Galtsev-Bezyuk, Yu. S. Mavrinsky, A. A. Tereshchenko, I. M. Alperovich Main structural elements of the Hokkaido-Sakhalin folded region / V. I. Golovinsky, I. I. Tyutrin Deflections of the junction zone of the Sikhote-Alin and Hokkaido-Sakhalin fold systems / N. V. Kulikov, A. A. Tereshchenkov Endogenous regime of Sakhalin / D. F. Semenov, L. S. Margulis, A. A. Apdreev, V. F. Evseev On the tectonics of the Sea of Okhotsk / Yu. S. Mavrinsky, V. A. Baboshina, N. V. Kulikov, V. V. Kharakhinov Structure, development and prospects for oil and gas potential of the underwater margins of West Africa and East Asia / A. Yu. Yunov Formational analysis of sedimentary basins of the northwestern part of the Pacific belt / Yu. K. Vurlin, O. K. Vazhenova Methodology for neotectonic analysis of the transition zone from the continent to the ocean / G. F. Ufimtsev , In kyrillischer Schrift
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  • 56
    Monograph available for loan
    Monograph available for loan
    München [u.a.] : Hanser
    Call number: MOP 46332 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 308 S.
    Edition: Rev. dt. Ausg. unter Berücks. d. Unterlagen von Standard-UNIX / von A.-T. Schreiner u. T. Mandry
    ISBN: 3446139753
    Series Statement: PC professionell
    Uniform Title: UNIX - the book
    Language: German
    Note: Inhaltsverzeichnis: Vorwort. - Vorwort zur deutschen Ausgabe. - 1 Starthilfen. - 1.1 Einleitung. - 1.2 Die Anmeldung. - 1.3 Ein einfaches Kommando. - 1.4 Die „Shell". - 1.5 Das Handbuch. - 1.6 Das Terminal. - 1.7 Ihr Paßwort. - 1.8 Fragen. - 2 Dateien und einfache Kommandos. - 2.1 Dateien. - 2.1.1 Was ist ein Name?. - 2.2 Das Dateisystem und die Kataloge. - 2.3 Kataloge auflisten. - 2.4 Erzeugen und Verändern von Katalogen. - 2.5 Schützen Sie Ihre Privatsphäre (Dateischutz). - 2.6 Standard-Ein-und Ausgabe und ihre Umlenkung. - 2.7 Dateien und Kataloge entfernen. - 2.8 Dateien verlagern. - 2.9 Pipelines und Filter. - 2.10 Kommandoablauf im Hintergrund. - Kommando Übersicht. - Shell-Programmierung. - 2.11 Generierung von Dateinamen und Mustererkennung. - 2.12 Shell-Variablen. - 2.13 Shell-Prozeduren. - 2.13.1 Argumente in Shell-Prozeduren. - 2.14 Shell-Programmierung: Ablaufkontrolle. - 2.14.1 „for". - 2.14.2 „case". - 2.14.3 „if". - 2.14.4 „while" und „until". - 2.15 Zusammenfassung. - Eine Version des „man" Kommandos. - 2.16 Fragen. - 3 Der Editor. - 3.1 Einige willkürliche Gedanken. - 3.2 Der UNIX Editor. - 3.3 Verwendung des Editors „ed". - 3.4 Start von „ed". - 3.5 Das Kommando „append". - 3.6 Einige spezielle Adressen. - 3.7 Vorläufige Zusammenfassung. - 3.8 Das Kommando „substitute". - 3.9 Kontextsuche. - 3.10 Das Kommando „change". - 3.11 Das Kommando „move". - 3.12 Zeichen mit Sonderbedeutung. - 3.12.1 Der Pfeil "A". - 3.12.2 Der Dollar „$". - 3.12.3 Der Punkt ".". - 3.12.4 Der Stern "*". - 3.12.5 Die Klammern „[" und „]". - 3.12.6 Das Zeichen „&". - 3.13 Die Kommandos „global" und „veto". - 3.14 Zusammenfassung. - 4 C. - 4.1 Einführung. - 4.2 Einleitende Bemerkungen. - 4.3 Starthilfen. - 4.4 Zeichenketten. - 4.5 Datentypen. - 4.6 Variablen und Kommentare. - 4.7 Inkrementieren und Dekrementieren. - 4.8 Kontrollstrukturen. - 4.8.1 Die „for" Anweisung. - 4.8.2 Die „while" Anweisung. - 4.8.3 Die „do" Anweisung. - 4.8.4 Die „continue" und „break" Anweisungen. - 4.8.5 Die „if" Anweisung. - 4.8.6 Die „switch" Anweisung. - 4.9 Ausdrücke. - 4.9.1 Vergleiche. - 4.9.2 Bitmanipulationen. - 4.9.3 Logische Verknüpfungen. - 4.10 Zuweisungen. - 4.10.1 Zuweisungen als Anweisungen. - 4.10.2 Werte von Zuweisungen. - 4.10.3 Konstanten. - 4.11 Datenstrukturen. - 4.11.1 Vektoren. - 4.11.2 Strukturen. - 4.12 Zeiger. - 4.12.1 Die Verwendung von Zeigern. - 4.13 Funktionen. - 4.13.1 Funktionen vereinbaren. - 4.13.2 Argumente von C Programmen. - 4.13.3 Was steckt hinter einem Argument?. - 4.14 Die Standard-E/A-Bücherei. - 4.14.1 Lese-und Schreiboperationen. - 4.14.2 Dateiverbindungen. - 4.15 Das Ende!. - 5 Das Dateisystem von UNIX. - 5.1 Kataloge. - 5.2 Radnamen. - 5.3 „Inodes". - 5.4 Die Struktur des Dateisystems. - 5.5 Gerätedateien. - 5.6 Dateischutz. - 5.7 Nichtresidente Dateisysteme. - 5.8 Dateigröße und Dateiblockierung. - 5.9 Fragen. - 6 Software-Werkzeuge. - 6.1 Was ist ein Software-Werkzeug. - 6.2 Filter. - 6.3 Der Werkzeugkasten. - 6.4 „pr". - 6.5 Namen von Kommandos. - 6.6 „grep" und Co. - 6.7 „sort". - 6.8 „awk". - 6.9 „make". - 6.10 Zusammenfassung. - 7 Textverarbeitung. - 7.1 Einfacher Text. - 7.2 Der Gebrauch des Formatierers. - 7.2.1 Einführung. - 7.2.2 Terminologie. - 7.3 Kommandos. - 7.3.1 Absätze. - 7.3.2 Beispiele. - 7.3.3 Abmessungen der Seite ändern. - 7.4 Makros. - 7.4.1 Was ist ein Makro?. - 7.4.2 Makropakete. - 7.4.3 Andere Quellen einfügen. - 7.4.4 Einfache Makros. - 7.4.5 Makros mit Argumenten. - 7.4.6 Fluchtsymbole, das gefürchtete Zeichen \. - 7.5 Seitentitel. - 7.5.1 Titelmakros "pflanzen". - 7.5.2 Titelmakro Beispiele. - 7.6 Andere Möglichkeiten. - 7.6.1 Register. - 7.6.2 Strings. - 7.6.3 Deutsche Probleme. - 7.6.4 Ablenkungen. - 7.6.4.1 Formatierten Text umlenken. - 7.6.4.2 Transparente Zeilen. - 7.6.5 Bedingte Eingabe. - 7.7 Wie man Makros schreiben sollte. - 7.8 Ausblick. - 8 Prozesse. - 8.1 Allgemeines. - 8.2 Die Ausführung eines Programms. - 8.3 Ohne doppelten Boden. - 8.3.1 „fork". - 8.3.2 Fehler bei Systemaufrufen. - 8.4 Privatbesitz. - 8.4.1 Dateiverbindungen. - 8.4.2 Benutzeridentifikation. - 8.5 Verschiedenes. - 8.5.1 Der Arbeitskatalog. - 8.5.2 Die Benutzermaske. - 8.6 „exec". - 8.7 Signale. - 8.8 Eingabe und Ausgabe. - 8.8.1 „open", „dose" und „creat". - 8.8.2 Lesen und Schreiben. - 8.8.3 „ioctl". - 8.9 Zusammenfassung. - 9 Büchereien. - 9.1 Der Preprozessor. - 9.1.1 Textersatz. - 9.1.2 Bedingte Übersetzung. - 9.1.3 Einfügen von Dateien. - 9.1.4 Getrennte Übersetzung. - 9.2 Der Lader. - 9.3 Standard-Eingabe und Ausgabe. - 9.4 Mathematische Funktionen. - 9.5 Verschiedenes. - 9.6. Spezielle Büchereien. - 9.6.1 Arithmetik mit höherer Genauigkeit. - 9.6.2 Grafik-Routinen. - 9.7 Der Bücherei-Manager „ar". - 10 Pflege. - 10.1 Einführung. - 10.2 UNIX starten und anhalten. - 10.2.1 UNIX starten. - 10.2.2 ,,/etc/init". - 10.2.3 UNIX anhalten. - 10.3 „getty" und ,,/etc/ttys". - 10.3.1 Die Prozeßgruppe. - 10.3.2 Entschuldigungen. - 10.4 Überprüfung der Dateihierarchie. - 10.4.1 Die Datenstruktur. - 10.4.2 Algorithmen zur Kontrolle. - 10.4.3 „fsck" und andere Programme. - 10.4.4 Initialisierung. - 10.5 Datensicherung. - 10.5.1 Programme für die Datensicherung. - 10.5.2 „dump". - 10.5.3 „restor". - 10.5.4 „tar". - 10.6 Gerätedateien („Special files"). - 10.6.1 Allgemeine Eigenschaften. - 10.6.2 „mount". - 10.7 Routineaufgaben. - 10.7.1 „Ipr" — das Druckprogramm. - 10.8 Neue Benutzer. - Anhang A Allgemeine Kommandos. - Anhang B Der Editor. - B.1 Aufruf und Einschränkungen. - B.2 Kurze Liste der Kommandos. - B.3 Kommandobeschreibungen. - B.4 Begriffe. - B.4.1 Suchmuster „p". - B.4.2 Ersatztext „t". - B.4.3 „\(" und ,,\)" im Suchmuster. - B.4.4 Adresse einer Zeile „I". - B.4.5 Adressen eines Bereichs „r". - Anhange Shell-Syntax. - C.1 Kommandos. - C.2 Umlenkung der Ein-und Ausgabe. - C.3 Hintergrundkommandos. - C.4 Pipelines. - C.5 Generierung von Dateinamen (Mustererkennung). - C.6 Ersatzdarstellungen. - C.7 Shell-Prozeduren. - C.8 Shell-Parameter. - C.9 Hier-Dokumente. - C.10 Shell-Variablen. - C.11 Kontrollstrukturen. - C.12 Textersatz durch Kommandos. - C.13 Shell-Grammatik. - C. 14 Metazeichen und reservierte Worte. - Anhang D Standard-Büchereien. - D.1 Systemaufrufe. - D.2 Standard-E/A-Bücherei. - D.2.1 Eröffnen einer Dateiverbindung. - D.2.2 Informationen. - D.2.3 Transferoperationen. - D. 2.4 Formatierte Ausgabe und Eingabe. - D.2.5 Prozeßkommunikation. - D.2.6 Positionierung und Puffer. - D.2.7 Lösen einer Dateiverbindung. - D.3 Mathematikbücherei. - D.3.1 Bessel Funktionen. - D.3.2 Trigonometrische Funktionen. - D.3.3 Hyperbolische Funktionen. - D.3.4 Geometrische Funktionen. - D.3.5 Andere Funktionen. - D.4 Verschiedene Hilfsroutinen. - D.5 String-Funktionen. - D.6 Spezielle Büchereien. - D.6.1 Höhere Genauigkeit. - D.6.2 Grafik. - D.6.3 Datenbasis. - Anhang E Systemaufrufe. - UNIX Systemaufrufe. - Fehler. - Signale. - Anhang F „ovp" - Ein Dienstprogramm in C. - Anhang Beantwortung der Fragen. - Fragen im Kapitel 1. - Fragen im Kapitel 2. - Fragen in Kapitel 5. - Anhang Literaturverweise.
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  • 57
    Call number: AWI G3-17-90374
    Type of Medium: Monograph available for loan
    Pages: 197 S , zahl. Ill.
    Language: English
    Note: TABLE OF CONTENTS: List of figures. - List of plates. - List of tables. - Acknowledgements. - Preface. - Itinerary for Canadian portion of tour. - GENERAL DESCRIPTION OF THE AREA. - Physiography and geology. - Quaternary geology. - Northern Yukon Territory and Mackenzie Delta. - Cordilleran Ice Sheet. - Montane glaciers of the southern Ogilvie Ranges. - Correlation and chronology. - Laurentide Glaciation. - Climate. - The Mackenzie Basin. - Northern Yukon. - Soils. - Distribution in the permafrost regions of Canada. - Distribution in Northwestern Canada. - Spil properties. - Patterned Ground Morphology. - Soil Texture and Rate of Decomposition. - Moisture and Ice Ccontent. - Soil Temperatures. - Micromorphology. - Cryoturbation. - Permafrost. - Distribution. - Thickness. - Active layer. - Ground ice. - Permafrost and climate change. - Vegetation. - Agriculture. - Overview. - Yukon. - Northwest Territories. - Forest resources. - Mining and exploration. - Overview. - Yukon. - Northwest Territories. - DESCRIPTION OF SOIL STOPS AND POINTS OF INTEREST. - Site 1, KM 4: Permafrost soil developed on organic terrain. - Organic soils in the Mackenzie Valley. - Mesic organic cryosol (Polygonal peat plateau). - Micromorphology. - Soil Temperature and Moisture. - Snow Depth, Active Layer Depth and Subsidence. - Site 2, KM 36: Permafrost soil developed on earth hummocks. - Orthic turbic cryosol, Peaty phase. - Micromorphology. - Soil Temperature and Moisture. - Snow Depth, Active Layer Thickness and Subsidence. - Site 3: Soil and permafrost development on recent alluvium. - Ecology of the Mackenzie Delta. - Mackenzie Delta ecosystems, Bonbardier Channel. - Site 4: Mackenzie River. - Site 5, KM 30: Richardson Mountains and glacial limit. - Site 6, KM 14: AUFEIS, or icing on James Creek. - Site 7, KM 5: Solifluction Site. - Site 8, KM 0: Continental divide, NWT/Yukon border. - Site 9, KM 425: Pediments and foothills, Richardson Transect. - Micromorphology. - Site 10, KM 403: Arctic circle. - Site 11, KM 400.5: Nonsorted circles (mudboils). - Origin of mudboils. - Orthic turbic cryosol associated with strongly cryoturbated materials. - Micromorphology. - Site 12, KM 366: Eagle plain monitoring site, Dempster Highway. - Soil Temperature and Moisture. - Micromorphology. - Site 13, KM 322: Forest fire site. - Site 14, KM 259: Peel River and Ogilvie Mountains Overview. - Site 15, KM 174: Sulphur Springs. - Site 16, KM 160-180: Tors on limestone ridges. - Site 17, KM 155: Calcareous soil on mid-pleistocene drift. - Brunisolic turbic cryosol. - Micromorphology. - Site 18, KM 115.5: Open-system Pingo. - Site 19, KM 96.5: Ice-wedge Polygons. - Site 20, KM 80: Frost mounds. - Site 21, KM 80: McConnell glacial limit. - Site 22, KM 77: Nonsorted circle site. - Micromorphology. - Site 23, KM 74: Tombstone Mountain Lookout. - Site 24: Midnight Dome Lookout. - Site 25: Agriculture on permafrost-affected soil. - Site 25a: The cleared soil. - Micromorphology. - Site 25b: The forested soil. - Micromorphology. - The impact of disturbance on soil physical properties. - Site 26: Placer gold mining in the Klondike District. - Site 27: Paleosols as indicators of past climate. - Wounded moose paleosol developed on Pre-Reid gravel. - Micromorphology. - Site 28: The effect of aspect on soil development. - Site 28a: Orthic dystric Brunisol (Southeast Aspect). - Micromorphology. - Site 28b: Regosolic Turbic cryosol (Northwest Aspect). - Site 29, KM 4: Sunnydale View. - Site 30, KM 53: Unglaciated Terrain - Tors and cryoplanation terraces. - Site 31, KM 102: Solifluction lobes and soil stripes. - Site 32, KM 107: Soils associated with sorted nets. - Orthic turbic cryosol. - References. - Appendices. - Appendix 1: The Canadian sysetm of soil classification. - Appendix 2: Methods. - Appendix 3: Glossary of micromorphological terms. - Appendix 4: Scientific and common names of plant species.
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  • 58
    Dissertations
    Dissertations
    Kassel : Fachgebiet Ökochemie der Gesamthochschule Kassel-Universität
    Call number: AWI Bio-18-91639
    Type of Medium: Dissertations
    Pages: 244 Seiten , Illustrationen, graphische Darstellungen
    Language: German
    Note: Kassel, Gesamthochsch., Diss., 1993 , Inhaltsverzeichnis: 1 Einleitung und Problemstellung. - 2 Ökologie der Algen. - 2.1 Lebensraum. - 2.1.1 Wasser. - 2.1.2 Litoral. - 2.1.3 Luft. - 2.1.4 Boden. - 2.1.5 Technische Systeme. - 2.2 Algen als aktive Veränderer ihres Biotops. - 2.2.1 Eutrophierung. - 2.2.2 Algenausscheidungen. - 3 Selbstregulierende Entsorgungsysteme. - 3.1 Natürliche Selbstreinigungsvorgänge. - 3.1.1 Technische Nutzung von Selbstreinigungsvorgängen. - 3.2 Nutzung von Algen in der Abwasserreinigung. - 3.3 Biologische Wasseranalyse. - 3.3.1 Algen als Indikatoren der organischen Belastung. - 4 Material und Methoden. - 4.1 Auswahl der untersuchten Anlagen. - 4.1.1 Anlagenbeschreibung. - 4.2 Beprobungszeit und Probenahmestellen. - 4.2.1 Beprobungstermine. - 4.2.2 Bezeichnung der Probenahmestellen. - 4.3 Untersuchungsmethoden. - 4.3.1 Algenproben. - 4.3.1.1 Algenkulturen. - 4.3.1.2 Artenbestimmung. - 4.3.2 Bodenproben. - 4.3.3 Abwasserproben. - 5 Die Algenvegetation der untersuchten Anlagen. - 5.1 Wurzelraumanlage in Vlotho (A). - 5.2 Versuchsanlage Witzenhausen (B). - 5.3 Wurzelraumanlage in Bünde (C). - 5.4 Anlage Beberbeck (D). - 5.5 Sonstige Biotope. - 6 Veränderung der Algenzönosen entlang der Entsorgungskette. - 6.1 Artendiversität entlang der Entsorgungskette. - 6.1.1 Anlage Vlotho. - 6.1.2 Anlage Witzenhausen. - 6.1.3 Anlage Bünde. - 6.1.4 Anlage Beberbeck. - 6.2 Änderungen durch die technische Ausführung des Biotops. - 6.2.1 Anlage Vlotho. - 6.2.1.1 Ablaufbereich Vlotho. - 6.2.2 Anlage Bünde. - 6.2.2.1 Zulaufbereich Bünde. - 6.2.2.2 Ablaufbereich Bünde. - 6.2.3 Anlage Beberbeck. - 6.2.3.1 Zulaufbereich Beberbeck. - 6.2.3.2 Ablaufbereich Beberbeck. - 7 Vergleich der Teilbiotope ähnlicher technischer Ausführung. - 7.1 Anlagenbeete. - 7.1.1 Bodenalgenkulturen. - 7.1.1.1 Einfluß der organischen Belastung auf die Bodenalgenflora. - 7.1.1.2 Einfluß der Beprobungstiefe auf die Bodenalgenflora. - 7.1.2 Beetoberflächen. - 7.1.2.1 Einfluß der organischen Belastung auf die Algenflora des Beetezulaufes. - 7.2 Offene Wasserkörper. - 7.2.1 Fließwasserstrecken. - 7.2.2 Stehende Wasserkörper. - 8 Ökologische Ansprüche der gefundenen Algenarten. - 8.1 Auswirkungen der organischen Belastung und der technischen Parameter auf die Algenflora. - 8.2 Einschätzung von Leistungen der Algen in Kläranlagen. - 9 Zusammenfassung. - 10 Literaturverzeichnis. - 11 Anhang. - Anhang 1 - Schematische Fließdiagramme der Anlagen A-D. - Anhang 2 - Darstellung der gefundenen Algenarten. - Anhang 3 - Tabellenverzeichnis. - Anhang 4 - Abbildungsverzeichnis. - Anhang 5 - Photographische Biotop- und Algendarstellung.
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  • 59
    Monograph available for loan
    Monograph available for loan
    London : H.M.S.O
    Call number: AWI G10-18-91809
    Type of Medium: Monograph available for loan
    Pages: 45 Seiten , Karte , 30 cm
    Edition: 2nd ed
    ISBN: 0115917179 (pbk.)
    Language: English
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  • 60
    Call number: AWI G9-19-92232
    Type of Medium: Monograph available for loan
    Pages: 28 Seiten
    Language: German
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  • 61
    Call number: M 18.91521
    Type of Medium: Monograph available for loan
    Pages: 56 Seiten , Illustrationen, graphische Darstellungen, Karten
    ISBN: 80-7075-142-8
    Series Statement: Czech Geological Survey special papers 1
    Language: English
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  • 62
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-84/6
    In: CRREL Report, 84-6
    Description / Table of Contents: An expression relating aerosol growth to cold environmental conditions was developed. This was accomplished by solving the diffusion equation with the method of Laplace transformation. The series solution was expressed in terms of the dimensionless parameters K (ratio of vapor density over droplet surface to droplet density), ω (ratio of environmental vapor density at time zero to vapor density over droplet surface), and dimensionless time τ (ratio of product of diffusion coefficient D and time t to square of initial radius of condensation nucleus). To take into account the variation of the vapor density over the surface of an acidic condensation nucleus due to the continuous dilution of the droplet, the solution was obtained by assuming various levels of constant vapor concentration. The final expression [R/R sub o - 1 = 2.4917 x 10 to the minus 18th power) exp(0.0737 θ) (P sub RHS/25) x (100-P sub RHS) τ to the 0.9890 powder] can be used to compute the value of R once the values of initial radius R sub o, relative humidity P sub RH, percent of relative humidity at the droplet surface P sub RHS, and environmental temperature θ are given.
    Type of Medium: Series available for loan
    Pages: vi, 28 Seiten , Illustrationen
    Series Statement: CRREL Report 84-6
    Language: English
    Note: CONTENTS Abstract Preface Nomenclature General background The problem Method of solution Results and discussion Conclusions Literature cited Appendix: Evaluation of rn's in equation 25
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  • 63
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-84/7
    In: CRREL Report, 84-7
    Description / Table of Contents: Experiments were conducted in CRREL's refrigerated flume facility to examine the two-dimensional force distribution of a floating, fragmented ice cover restrained by a boom in a simulated river channel. To determine the force distribution, a vertically walled channel, instrumented for measuring normal and tangential forces, and an instrumented restraining boom were installed in a 40.0- by 1.3-m flume. Two sizes of polyethylene blocks and two similar sizes of fresh-water ice blocks were tested using water velocities ranging from 10 to 30 cm/s. The forces measured at the instrumented boom leveled off with increasing cover length. The contribution of the increasing shear forces developed along theshorelines to this leveling off in the data was clearly evident. The shear coefficients of the polyethylene blocks averaged 0.43, and the freshwater ice averaged 0.044. The normal force measured along the instrumented shoreline could not be related simply by a K coefficient to the longitudinal force; another expression was required, with a term being a function of the cover thickness and independent of the undercover shear stress or cover length. By adding this term, good agreement was then found between the measured and predicted values of the boom forces and the shoreline normal and shear forces
    Type of Medium: Series available for loan
    Pages: iv, 22 Seiten , Illustrationen
    Series Statement: CRREL Report 84-7
    Language: English
    Note: CONTENTS Abstract Preface Introduction Experiments Test flume facility Experimental apparatus Experimental procedure Results Plastic versus freshwater ice Shoreline forces Boom forces Average shear stress under ice cover Internal forces Discussion Data scatter Summary and conclusions Literature cited Appendix A: Experimental results
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  • 64
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-84/8
    In: CRREL Report, 84-8
    Description / Table of Contents: This report describes the equipment and procedures that were used for acquiring, preparing and testing samples of multi-year sea ice. Techniques and procedures are discussed for testing ice samples in compression and tension at constant strain rates and constant loads, as well as in a conventional triaxial cell. A detailed account is given of the application and measurement of forces and dispiacements on the ice test specimens under these different loading conditions.
    Type of Medium: Series available for loan
    Pages: iv, 43 Seiten , Illustrationen
    Series Statement: CRREL Report 84-8
    Language: English
    Note: CONTENTS Abstract Preface Introduction Test material and test specimens Test material Required dimensions for test specimens Acquisition and preparation of specimens Field core sampling Specimen preparation in the laboratory Application of forces and displacements to uniaxial specimens Compression Tension Squareness imperfections Loading devices Universal testing machine Gas actuator for constant load Weight-and-pulley system for constant tension Equipment for triaxial tests Measurement of force and displacement Force Displacement Readouts and recorders Literature cited Appendix A: Phenolic-resin end caps Appendix B: Compliant platens Appendix C: Theoretical factor for converting overall strain to gauge-length strain indumbbell specimens Appci dix D: Items developed but not used in Phase I Appendix E: Use of the Brazil test
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  • 65
    Series available for loan
    Series available for loan
    Leipzig : Akademie der Wissenschaften der DDR, Zentralinstitut für Isotopen- und Strahlenforschung
    Associated volumes
    Call number: ZSP-980-90
    In: ZfI-Mitteilungen, Nr. 90
    Type of Medium: Series available for loan
    Pages: 358 Seiten , Illustrationen
    ISSN: 0323-8776
    Series Statement: ZfI-Mitteilungen 90
    Language: German
    Note: Inhaltsverzeichnis: 1. Wissenschaftliche Beiträge. - (01) Isotopen- und elementgeochemische sowie radiogeochronologische Untersuchungen an der Zinnlagerstätte Ehrenfriedersdorf (Beste wissenschaftliche Arbeit des ZfI 1983 / Autorenkollektiv. - (02) Einsatz ionisationsgasanalytischer Methoden an der Mikroelektronik (Beste wissenschaftlich-technische Arbeit des ZfI 1983) / Autorenkollektiv. - (03) Zur Geschichte der künstlichen Radioaktivität / H. Koch. - (04) 50 Jahre künstliche Radioaktivität / G. Vormum. - (05) Frédéric und Irène Joliot-Curie - Biographische Skizze / K.-P- Dostal. - 2. Institutskolloquien. - 3. Patente. - 4. Veröffentlichungen und Vorträge. - 5. Register. - 5.1. Namensregister. - 5.2. Deskriptorenregister. - 6. Verzeichnis aller bisher erschienenen Hefte der ZfI-Mitteilungen. - 6.1. Titel der bis 1982 erschienenen Hefte 1-61 und Sonder-Nr. 1. - 6.2. Inhaltsverzeichnisse der im Jahre 1983 erschienenen Hefte 62-82. - 6.3. 1984 bisher erschienene Hefte. - 7. Verzeichnis aller bisher erschienenen Preprints.
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  • 66
    Call number: ZSP-980-100
    In: ZfI-Mitteilungen, Nr. 100
    Type of Medium: Series available for loan
    Pages: 184 Seiten , Illustrationen
    Series Statement: ZfI-Mitteilungen 100
    Language: German
    Note: Inhaltsverzeichnis: 15 Jahre Zentralinstitut für Isotopen- und Strahlenforschung der AdW der DDR / K. Wetzel. - Spurenanalyse mittels Ionisationsgasanalyse in der Mikroelektronik / H.-J. Große, P. Popp. - Beiträge der Isotopenforschung im ZfI zum Erkenntnisgewinn in den Geowissenschaften / R. Haberlandt, H. Schütze. - Radioisotopentechnik in der chemischen Industrie / G. Hoffmann. - EDV und moderne Informatik - wesentliche Elemente der Intensivierung des Forschungsprozesses im ZfI / L. Jankowski. - Nukleare Analyseverfahren in der Halbleiterindustrie / H. Koch. - Radionuklide in der Energetik / J. W. Leonhardt. - Ergebnisse der strahlenchemischen Grundlagenforschung und Entwicklungstendenzen der Strahlenchemie / W. Reicherdt. - Gewinnung von Wertmetallen aus Abprodukten / M. Rösseler. - Zur Isotopenproduktion am ZfI / G. Vormum.
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  • 67
    Series available for loan
    Series available for loan
    Leipzig : Akademie der Wissenschaften der DDR, Zentralinstitut für Isotopen- und Strahlenforschung
    Associated volumes
    Call number: ZSP-980-95
    In: ZfI-Mitteilungen, Nr. 95
    Type of Medium: Series available for loan
    Pages: VI, 150 Seiten , Illustrationen
    Series Statement: ZfI-Mitteilungen 95
    Language: German
    Note: Inhaltsverzeichnis: 1. Einleitung. - 1.1. Ausgangssituation. - 1.2. Bestrahlungsanlagen als Basis strahlenchemischer Untersuchungen und Verfahren. - 1.3. Anforderungen der Praxis an ein Programmsystem zur Berechnung von Strahlenfeldern in γ-Bestrahlungsanlagen. - 2. Ableitung des Grundmodells. - 2.1. Ausgangspunkt. - 2.1.1. Punktförmige Strahlenquelle. - 2.1.2. Linienförmige Strahlenquelle. - 2.1.3. Anordnung mehrerer Strahlenquellen. - 2.2. Zugrundegelegte Struktur von Bestrahlungsanlage und Strahlenfeld. - 2.3. Geometrische Zusammenhänge. - 2.4. Berechnung der Bestrahlungsdosisleistung in einem Feldpunkt. - 3. Das Programm DOSKMF2. - 3.1. Übersicht. - 3.2. Eingabe. - 3.3. Aktivitätskorrektur. - 3.4. Auswahl der Feldpunkte. - 3.4.1. Zylinderkoordinaten. - 3.4.2. Quaderkoordinaten. - 3.4.3. Auswahl von Einzelpunkten. - 3.4.4. Variation der Rohrpositionen 3.5. Zyklusgestaltung, statistische Maßzahlen und Aufbereitung für graphische Ausgabe. - 3.5.1. Zylinderkoordinaten. - 3.5.2 Quaderkoordinaten. - 3.6. Programmtechnische Lösung. - 3.6.1. Struktur des Programms. - 3.6.2. Aufruf. - 3.6.3. Einschränkungen und programmtechnische Hinweise. - 3.7. Ein Demonstrationsbeispiel. - 3.7.1. Aufgabenstellung. - 3.7.2. Festlegung der Parameter. - 3.7.3. Resultate. - 4. Nutzung der graphischen Ausgabe. - 4.1. Ausgangspunkt und Voraussetzungen. - 4.2. Das Programm ISORADL. - 4.2.1. Übersicht. - 4.2.2. Die Programme ISOQ, ISOA. - 4.2.3. Problemlösung. - 4.2.4. Programmtechnische Lösung. - 4.2.5. Demonstrationsbeispiel. - 5. Einsatzmöglichkeiten des Programmpaketes. - 5.1. Übersicht. - 5.2. Prüfen von Voraussetzungen. - 5.3. Wechselwirkung Programmpaket-Realität. - 6. Berechnung und Modifikation von Strahlenfeldern bestehender Gammabestrahlungsanlagen. - 6.1. Technische Voraussetzungen. - 6.2. Prüfen der Anwendungsbedingungen für den Programmeinsatz. - 6.3. Durchgeführte Berechnungen. - 6.3.1. Aufklärung der Struktur des vorliegenden Strahlenfeldes. - 6.3.2. Darstellung typischer Bestrahlungskonfigurationen. - 6.3.2.1. Bestrahlung im Käfig. - 6.3.2.2. Bestrahlung flächenartiger Objekte. - 6.4. Berechnungen für eine neue Strahlenquellenkonfiguration. - 6.5. Schlußfolgerungen. - 7. Einsatz des Programmpaketes als Projektierungshilfsmittel. - 7.1. Nutzung für die Pilotanlage des PCK Bitterfeld. - 7.1.1. Vorbemerkungen. - 7.1.2. Berechnungen für Modellreaktoren. - 7.1.3. Auslegung eines Reaktors für die Pilotanlage. - 7.1.4. Kontrollrechnungen zur Dosimetrie des gefertigten Reaktors. - 7.2. Nutzung für eine industrielle Anlage des VEB PROWIKO Schönebeck. - 7.2.1. Vorbemerkungen. - 7.2.2. Entwurf eines Modellreaktors. - 7.2.3. Schlußfolgerungen für den Entwurf einer industriellen Anlage. - 8. Einige Gedanken zur Wechselwirkung Strahlenfeldberechnung - Dosimetrie am Beispiel zweier umschlossener γ-Bestrahlungsanlagen. - 8.1. Vorbemerkungen. - 8.2. Beschreibung der für den Vergleich wesentlichen Anlagenparameter. - 8.3. Durchgeführte dosimetrische Messungen. - 8.4. Durchgeführte Strahlenfeldberechnungen. - 8.5. Diskussion der Ergebnisse. - 9. Erweiterte Nutzungsmöglichkeiten und Ausblick. - 10. Zusammenfassung. - Literaturverzeichnis. - Verzeichnis der Abbildungen. - Verzeichnis der Tabellen.
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  • 68
    Call number: AWI Bio-18-91955
    Type of Medium: Monograph available for loan
    Pages: 85 Seiten , Illustrationen
    Edition: autorisierte deutsche Übersetzung der Originalausgabe
    ISBN: 333460439X (kart.) , 3827406366
    Uniform Title: Textbook of pollen analysis 〈dt.〉
    Language: German
    Note: Inhaltsverzeichnis: Vorwort. - Welche Pflanze? Bestimmungsschlüssel. - Tabelle 1. Skulpturtypen. - Hauptschlüssel. - Tabelle A. Vesiculate (Pinaceae und Podocarpaceae). - Tabelle B. Zusammengesetzte Pollenkörner (PK). - Tabelle B1. Dyaden. - Tabelle B2. Tetraden. - Tabelle B3. Polyaden. - Tabelle C. Polyedrische PK. - Tabelle D. Bilaterale PK. - Tabelle E. Subtetraedrische Sporen. - Tabelle F. Rotationsellipsoide (oder ovate) PK: Hauptschlüssel. - Tabelle F1. Polyplicate (Ephedra). - Tabelle F2. Inaperturate. - Tabelle F3. Trichotomocolpate. - Tabelle F4. Monocolpate. - Tabelle F5. Monoporate. - Tabelle F6. Dicolpate. - Tabelle F7. Tricolpate. Hauptschlüssel zu den Subsektionen. - Tabelle F7.1. Tricolpate, psilat. - Tabelle F7.2. Tricolpate, scabrat. - Tabelle F7.3. Tricolpate, echinat. - Tabelle F7.4. Tricolpate, rugulat-striat. - Tabelle F7.5. Tricolpate, suprareticulat. - Tabelle F7.6. Tricolpate, perreticulat. - Tabelle F7.7. Tricolpate, intectat (clavat). - Tabelle F8. Stephanocolpate. - Tabelle F9. Pericolpate. - Tabelle F10. Dicolporate. - Tabelle F11. Tricolporate: Hauptschlüssel zu den Subsektionen. - Tabelle F11.1 Tricolporate, psilat-scabrat. - Tabelle F11.2. Tricolporate, echinat. - Tabelle F11.3. Tricolporate, striat-rugula. - Tabelle F11.4. Tricolporate, suprareticulat-foveolat. - Tabelle F11.5. Tricolporate, perreticulat-frustillat. - Tabelle F12. Stephanocolporate. - Tabelle F13. Pericolporate. - Tabelle F14. Diporate. - Tabelle F15. Triporate. - Tabelle F16. Stephanoporate. - Tabelle F17. Periporate: Hauptschlüssel zu den Subsektionen. - Tabelle F17.1. Periporate, verrucat-echinat. - Tabelle F17.2. Periporate, vermiculat-rugulat oder reticulat. - Tabelle F17.3. Periporate, psilat-scabrat. - Tabelle F18. Syncolpate. - Tabelle F19. Heterocolpate. - Tabelle F20. Fenestrate. - Caryophyllaceae (periporate). - Cyperaceae. - Gramineae. - Plantaginaceae. - Rosaceae. - Morphologisches Glossar. - Literatur. - Register der Pflanzennamen. , Dublette der Martin-Luther-Universität Halle-Wittenberg
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  • 69
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-93/9
    In: CRREL Report, 93-9
    Description / Table of Contents: Traction on winter surfaces was measured using three test vehicles, each designed to measure traction for a different purpose: vehicle mobility research (CRREL Instrumented Vehicle), commercial tire testing (Uniroyal- Goodrich traction tester), and airport runway safety (Saab friction tester). The traction measured with each method is comparable, but there are systematic differences due to the effects of the surface material and the test and analysis technique. This comparison serves as the fundamental basis for collaboration between the various traction testing communities and illustrates the need for well documented test procedures and data analysis as a standard for traction testing and evaluation.
    Type of Medium: Series available for loan
    Pages: iii, 21 Seiten , Illustrationen
    Series Statement: CRREL Report 93-9
    Language: English
    Note: CONTENTS Preface Introduction Traction test methods Saab friction tester Uniroyal-Goodrich traction tester CRREL Instrumented Vehicle Surfaces tested Reporting results and terminology Factors influencing traction Results Traction curves for each surface Traction coefficients Conclusion Literature cited Appendix A: Vehicle instrumentation and samples of graphic output Appendix B: Comparison of measured traction coefficients with published andpredicted values Abstract
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  • 70
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-93/3
    In: CRREL Report, 93-3
    Description / Table of Contents: Results are presented of a study to determine appropriate methods of flow modification for mitigating ice jam formation in navigable rivers. Based on a review of alternative methods for flow modification, it is concluded that for many rivers, especially large ones, the most appropriate method involves controlled ice-cover formation through the regulation of river flow. Flow discharge and stages would be regulated by controlling the flow releases from reservoirs and flow stages at river dams, such that optimal flow conditions prevail for rapid formation, and subsequent maintenance, of an accumulation ice cover over river reaches in which potentially large amounts of frazil ice may grow. Accumulation covers would be formed of frazil ice pans and floes and, if appropriate, broken ice conveyed from upstream. Existing dams, augmented where needed by navigable ice booms, could serve as retention structures for the development of accumulation covers. A preliminary indication of the feasibility of this method for controlling ice-cover formation on stage-regulated pools of the Ohio River is assessed through the use of a numerical model that simulates ice-cover formation from frazil ice. It is found that this approach holds promise for mitigating jam occurrence, although its implementation necessarily entails management of flow through major portions of the Ohio River. The results of the study are, to a limited extent, generalized to other rivers.
    Type of Medium: Series available for loan
    Pages: v, 58 Seiten , Illustrationen
    Series Statement: CRREL Report 93-3
    Language: English
    Note: CONTENTS Preface Nomenclature Introduction Background Scope of the study Control of river ice formation Control methods Controlled ice-cover formation for the upper Ohio River Numerical simulation of ice-cover formation Flow profile Water temperature variation Frazil ice growth Ice-cover progression Thermal growth of ice cover Numerical results Illustration of simulated ice-:over formation Ice-cover formation in the Hannibal and Montgomery pools Generalized results Conclusions and recommendations Literature cited Appendix A: Expression for coefficients Appendix B: Listing of computer program
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  • 71
    Monograph available for loan
    Monograph available for loan
    Leningrad : Gidrometeozidat
    Call number: MOP 45054 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 208 Seiten , Illustrationen , 22 cm
    Language: Russian
    Note: in kyrillischer Schrift
    Location: MOP - must be ordered
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  • 72
    Monograph available for loan
    Monograph available for loan
    Nerja : Patronato de la Cueva de Nerja
    Call number: AWI G1-19-92413
    Type of Medium: Monograph available for loan
    Pages: 354 Seiten , Illustrationen
    Series Statement: Trabajos sobre la Cueva de Nerja 3
    Language: Spanish
    Note: ÍNDICE PRESENTACIÓN INTRODUCCIÓN INTRODUCTION ESTUDIO GEOLÓGICO DEL ENTORNO DE LA CUEVA DE NERJA l. INTRODUCCIÓN 1.1. Localización geográfica 1.2. Metodología de trabajo 1.3. Objetivos 2. ENCUADRE GEOLÓGICO GENERAL 3. ANTECEDENTES 4. ESTRATIGRAFÍA 4.1. Materiales alpujárrides 4.1.1. Manto de Almijara (Alpujárride Intermedio) 4.1.1.1. Esquistos oscuros 4.1.1.2. Esquistos claros 4.1.1.3. Calcosquistos 4.1.1.4. Mármoles de la base 4.1.1.5. Mármoles con intercalaciones de esquistos y calcosquistos 4.1.2. Manto de Guájares (Alpujárride Superior) 4.1.2.1. Esquistos oscuros 4.1.2.2. Esquistos claros 4.1.2.3. Mármoles 4.2. Materiales Neógeno-Cuaternarios 4.2.1. Unidad inferior pliocena 4.2.2. Unidad superior pliocena 4.2.3. Unidad pleistocena 4:2.3.1. Brechas y conglomerados 4.2.3.2. Gravas, arenas y limos 4.2.3.3. Travertinos 4.2.3.4. Depósitos litoquímicos 4.2.4. Unidad Holocena 5. ESTRUCTURA GEOLÓGICA 6. HISTORIA GEOLÓGICA BIBLIOGRAFÍA ANÁLISIS ESTRATIGRÁFICO DE LOS MATERIALES NEÓGENOCUATERNARIOS DE LA REGIÓN DE NERJA 1. INTRODUCCIÓN 2. ESTRATIGRAFÍA 2.1. Brechas rojas basales 2.2. Unidad inferior pliocena 2.2.1. Facies continentales de la Unidad inferior pliocena 2.2.2. Facies marinas de la Unidad inferior pliocena 2.2.3. Medio de depósito 2.3. Discordancia intrapliocena 2.4. Unidad superior pliocena 2.4.1. Facies marinas de la Unidad superior pliocena 2.4.2. Facies continentales de la Unidad superior pliocena 2.4.3. Medio de depósito 2.5. Unidad pleistocena 2.5.1. Descripción de los materiales 2.5.2. Medio de depósito y edad de los materiales 2.6. Otros materiales atribuibles al Pleistoceno 2.6.1. Travertinos 2.6.2. Facies detrítcias y cabonatadas del cruce de la carretera de la Cueva 2.7. Materiales del Holoceno 3. EVOLUCIÓN TECTOSEDIMENTARIA y PALEOGEOGRÁFICA 4. CONCLUSIONES BIBLIOGRAFÍA LA FRACTURACIÓN EN EL ENTORNO DE LA CUEVA DE NERJA 1. INTRODUCCIÓN 1.1. Antecedentes 1.2 Estructura del entorno de la Cueva de Nerja 2. RASGOS GENERALES DE LA FRACTURACIÓN 3. ESTUDIO DE LAS FALLAS 3.1. Las fallas mesoscópicas 3.2. Las grandes fallas 4. ESTUDIO DE LAS DIACLASAS 4.1. Resultado del estudio de la diaclasación en el entorno de la Cueva de Nerja 4.2. Estudio de la diaclasación en el interior de la Cueva 5. COMPARACIÓN DE LOS RESULTADOS OBTENIDOS EN LAS DIACLASAS Y FALLAS 6. ALGUNOS DATOS ACERCA DE LA CRONOLOGÍA DE LA FRACTURACIÓN E IMPORTANCIA DE LA MISMA 7. CONTROLES GEOLÓGICOS DE LA CUEVA DE NERJA: INFLUENCIA DE LA FRACTURACIÓN 8. CONCLUSIONES BIBLIOGRAFÍA ESTUDIO GEOMORFOLÓGICO DEL ENTORNO DE LA CUEVA DE NERJA 1. INTRODUCCIÓN 2. SÍNTESIS GEOLÓGICA Y ÁMBITO BIOCLIMÁTICO 3. ANÁLISIS MORFOMÉTRICO Y DE LA RED DE DRENAJE 3.1. Consideraciones previas. Rasgos hidrográficos generales 3.2. Características de forma 3.3. Características de relieve 3.4. Análisis de la red de drenaje 4. RASGOS GENERALES DEL MODELADO EN EL CONJUNTO MONTAÑOSO 4.1. Erosión hídrica y formas estructurales 4.2. Periglaciarismo y glaciarismo 4.3. Morfologías kársticas 5. EL PIEDEMONTE LITORAL: FORMAS Y PROCESOS 5.1. Morfologías relacionadas con las brechas pleistocenas 5.2. Otras morfologías 6. BOSQUEJO DE EVOLUCIÓN GEOMORFOLÓGICA. PROCESOS ACTUALES BIBLIOGRAFÍA ESTUDIO HIDROGEOLÓGICO DEL ENTORNO DE LA CUEVA DE NERJA 1. INTRODUCCIÓN 2. ANTECEDENTES 3. MARCO CLIMÁTICO 3.1. Precipitciones 3.2. Temperaturas 4. HIDROLOGÍA SUPERFICIAL 5. EL ACUÍFERO DE LAS ALBERQUILLAS 5.1. Descripción 5.2. Puntos de Agua 5.2.1. Pozos perforados 5.2.1.1. Piezometría 5.2.2. Manantiales 5.2.2.1. El manantial de Maro 5.3. Hidrogeoquímica 5.3.1. Aplicación de la hidroquímica a la investigación hidrogeológica 5.3.1.1. Distribución espacial 5.3.1.2. Evolución temporal 5.3.2. Aplicación de la hidroquímica a la karstogénesis 5.3.2.1. El sistema calcocarbónico 5.4. Funcionamiento del acuífero 6. LA CUEVA DE NERJA EN EL ACUÍFERO DE LAS ALBERQUILLAS BIBLIOGRAFÍA INTRODUCCIÓN A LA PETROLOGÍA DE LOS MÁRMOLES DE LA CUEVA DE NERJA Y MATERIALES ASOCIADOS 1. INTRODUCCIÓN 2. CONTEXTO GEOLÓGICO 3. DESCRIPCIÓN DE LAS ROCAS Y PETROGRAFÍA 3.1. Rocas Carbonáticas 3.1.1. Mármoles dolomíticos puros 3.1.2. Mármoles dolomíticos impuros 3.1.3. Mármoles calcíticos y rocas con silicatos cálcicos 4. COMPOSICIÓN QUÍMICA DE LOS MINERALES 5. EVOLUCIÓN METAMÓRFICA 5.1. Antecedentes 5.2. Metamorfismo de las rocas carbonáticas 5.3. Condiciones del metamorfismo 6. CONCLUSIONES BIBLIOGRAFÍA DATACIONES GEOCRONOLÓGICAS ABSOLUTAS (Métodos E.S.R. y Series de Uranio) EN LA CUEVA DE NERJA Y SU ENTORNO. IMPLICACIONES EVOLUTIVAS, PALEOCLIMÁTICAS Y NEOSISMOTECTÓNICAS 1. INTRODUCCIÓN 2. METODOLOGÍA 2.1. Campaña de muestreo 2.2. Métodos geocronológicos empleados 3. LOCALIZACIÓN Y DESCRIPCIÓN DE LAS MUESTRAS 3.1. Muestras del interior de la Cueva de Nerja 3.2. Muestras de depósitos sedimentarios del entorno exterior 4. RESULTADOS OBTENIDOS Y DISCUSIÓN 5. CONCLUSIONES: IMPLICACIONES EVOLUTIVAS, PALEOCLIMÁTICAS Y NEOSISMOTECTÓNICAS 5.1. Relativas a la evolución de la Cueva de Nerja 5.2. Relativas a la edad de algunos materiales del entorno 5.3. Relativas a los cambios paleoclimáticos de la región 5.4. Relativas a la neosismotectónica de la región BIBLIOGRAFÍA . ESTUDIO DE LA VENTILACIÓN DE LA CUEVA DE NERJA MEDIANTE LA CONCENTRACIÓN DE RADÓN 1 INTRODUCCIÓN 1.1. Radioactividad Natural 1.2. Cómo se puede medir la concentración en Rn 1.3. Exhalación en Rn del suelo 1.4. Método para evaluar la ventilación 2 DISPOSITIVO EXPERIMENTAL 2.1. Toma de muestras de aire 2.2. Medida del contenido en Rn de las células 2.3. Medida de la temperatura del aire de la Cueva 3 RESULTADOS 3.1. Concentración de Rn en la Cueva 3.2. Temperatura del aire en la Cueva 3.3. Evaluación del índice de ventilación BIBLIOGRAFIA CARACTERIZACIÓN ISOTÓPICA Y ANÁLISIS DE LOS PROCESOS DE DEGRADACIÓN DE LOS MATERIALES CARBONATADOS DE LA CUEVA DE NERJA. ESTUDIO PRELIMINAR 1. INTRODUCCIÓN 1.1. Antecedentes 1.2. Localización geológica y materiales estudiados 2. METODOLOGÍA 2.1. Muestreo 2.2. Estudio de laboratorio 2.2.1. Análisis mineralógico 2.2.2. Isótopos estables 2.2.3. Elementos traza 2.2.4. Microscopía electrónica de barrido 3 RESULTADOS OBTENIDOS 3.1. Espeleotemas 3.2. Roca encajante 3.3. Travertinos 3.4. Mustras de agua 4. INTERPRETACIÓN Y DISCUSIÓN DE LOS RESULTADOS 4.1. Isótopos estables 4.2. Estudio de las alteraciones 4.2.1. Procesos de alteración de carbonatos 4.2.2. Estudio de elementos traza 4.2.3. Estudio mineralógico 5 CONCLUSIONES AGRADECIMIENTOS BIBLIOGRAFÍA ESTUDIO GEOQUÍMICO DE LAS AGUAS DE INFILTRACIÓN DE LA CUEVA DE NERJA 1. INTRODUCCIÓN 2. METODOLOGÍA DE TRABAJO 2.1. Trabajo de campo 2.2. Trabajo de laboratorio 2.3. Trabajo de gabinete 3. LOS CAUDALES DE GOTEO 4. LOS PARÁMETROS FÍSICO-QUÍMICOS: (pH, TEMPERATURA y CONDUCTIVIDAD) 5. LA INFORMACIÓN HIDROGEOQUÍMICA 5.1. La química de los carbonatos 5.1.1. Los equilibrios calco-carbónicos, el pH de equilibrio y la presión parcial de CO2 5.1.2. La pC02 de las aguas de infiltración 5.1.3. El dpH de las aguas de infiltración 5.2. Las distintas clases de agua 5.3. Consideraciones sobre algunos componentes químicos de interés en las aguas de infiltración sensu stricto 5.3.1. Iones procedentes mayoritariamente del agua de lluvia 5.3.1.1. Cloruros (Cl-) 5.3:1.2. Sílice(SiO2) 5.3.1.3. Nitratos (NO3) 5.3.1.4. Sulfatos (SO4) 5.3.2. Iones procedentes fundamentalmente de los materiales acuíferos 5.3.2.1. Alcalinidad total (TAC) 5.3.2.2. Relación CA2+/Mg2+ 6. ALGUNOS ASPECTOS PARA LA CONSERVACIÓN DE LA CUEVA 7. CONCLUSIONES BIBLIOGRAFÍA MEDIDAS TOPOGRÁFICAS DE PRECISIÓN PARA CONTROL DE MICRODEFORMACIONES EN EL TECHO DE LA CUEVA DE NERJA 1. INTRODUCCIÓN 2. DESCRIPCIÓN DEL SISTEMA 3. MEDIDAS DE IMPLANTACIÓN 4. ALTIMETRÍA 5. RESULTADOS Y CONCLUSIONES AGRADECIMIENTOS BIBLIOGRAFÍA . , In spanischer Sprache , Zusammenfassung in englischer Sprache
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  • 73
    Series available for loan
    Series available for loan
    Associated volumes
    Call number: S 92.0083(1984)
    In: Erdbeben in der Bundesrepublik Deutschland
    Type of Medium: Series available for loan
    Pages: 57 Seiten
    Location: Lower compact magazine
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  • 74
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-84/4
    In: CRREL Report, 84-4
    Description / Table of Contents: Ice problems developed in the Sault Ste. Marie, Michigan, portion of the St. Marys River because of winter navigation. Passing ships and natural influences moved ice from Soo Harbor into Little Rapids Cut in sufficient quantities to jam, cause high water in the harbor, and prevent further ship passage. After physical model and engineering studies, two ice booms with a total span of 1375 ft (419 m) with a 250-ft (76-m) navigation opening between were installed at the head of Little Rapids Cut in 1975. A modest field study program on the booms was conducted for the ensuring four winters to determine ice and boom interaction and the effects of ship passages on the system. Forces on some anchors were recorded and supplemental data were taken by local personnel. Several reports have been written about the booms' early operations. This paper presents four-year summary of the main effects of the booms on ice and ship interaction and vice versa. Throughout the four winter seasons, the small quantities of ice lost over and between the booms were manageable. Ships usually passed through the boom without influencing the boom force levels, but at time they brought about large changes. One boom needed strengthening, and artificial islands were added for upstream ice stability. Coast Guard icebreakers were also a necessary part of winter navigation in this area.
    Type of Medium: Series available for loan
    Pages: iv, 18 Seiten , Illustrationen
    Series Statement: CRREL Report 84-4
    Language: English
    Note: CONTENTS Abstract Preface Introduction St. Marys River Ice problems Remedial measures Field studies Highlights, trends, and major findings Modifications to boom Maximum forces Ship traffic Characteristics Effect of boom forces Effect on ice Conclusion Literature cited Appendix A: Ice boom forces
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  • 75
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-84/5
    In: CRREL Report, 84-5
    Description / Table of Contents: Diatom species composition and relative abundances were determined for ice cores obtained from Weddell Sea pack ice during the October-November 1981 Weddell Polynya Expedition (WEPOLEX). Ice thickness and salinity indicate that the ice was less than one year old. The predominant ice type (70%) was frazil, which has the capacity to mechanically incorporate biological material through nucleation and scavenging. Diatoms were found throughout the length of the cores. Species showed down-core fluctuations in abundance that appeared to be correlated with changes in ice type. Pennate forms were more abundant than centrics, the average ratio being 16:1. Diatom frustules with intact organic material were more abundant (5 billion cells/liter). Differences in species abundances are attributed initially to incorporation of algal cells from a temporally changing water column and subsequently to diatom reproduction within the ice. Scanning electron micrographs illustrating the morphologic characteristics of the predominant species are included.
    Type of Medium: Series available for loan
    Pages: iv, 46 Seiten , Illustrationen
    Series Statement: CRREL Report 84-5
    Language: English
    Note: Contents Abstract Preface Introduction Materials and methods Results Discussion Conclusions Literature cited Appendix A: Taxonomic terms Appendix B: Differences in species composition and abundance in duplicate samples examined under optical and inverted light microscopes Appendix C: Morphologic descriptions and SEM micrographs
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  • 76
    Call number: ZSP-201-84/9
    In: CRREL Report, 84-9
    Description / Table of Contents: This report presents the results of the first phase of a test program designed to obtain a comprehensive understanding of the mechanical properties of multi-year sea ice from the Alaskan Beaufort Sea. In Phase I, 222 constant-strain-rate uni-axial compression tests were performed on ice samples from ten multi-year pressure ridges to examine the magnitude and variation of ice strength within and between pressure ridges. A limited number of constant-strain-rate compression and tension tests, constant-load compression tests, and conventional triaxial tests were also performed on ice samples from a multi-year floe to provide preliminary data for developing ice yield criteria and constitutive laws for multi-year sea ice. Data are presented on the strength, failure strain, and modulus of multi-year sea ice under different loading conditions. The statistical variation of ice strength within and between pressure ridges is examined, as well as the effects of ice temperature, porosity, structure, strain rate and confining pressure on the mechanical properties of multi-year sea ice.
    Type of Medium: Series available for loan
    Pages: v, 107 Seiten , Illustrationen
    Series Statement: CRREL Report 84-9
    Language: English
    Note: CONTENTS Abstract Preface Introduction Field Sampling Site selection and description Ice sampling procedures Shipping and storage of ice samples Testing Techniques Multi-year Pressure Ridge Tests Ice description Sampling scheme and test variables Uniaxial compressive strength Residual compressive strength Failure strains Initial tangent modulus Statistical Variations in Ice Strength Differences in strength above and below level ice Sources of the variation in strength Shape of the strength histograms Multi-year Floe Ice Tests Ice description Uniaxial compressive strength Constant-load compression tests Constant-strain-rate tension tests Triaxial tests Conclusions Literature Cited Appendix A: Structural profile of a multi-year pressure ridge core Appendix B: Ridge uniaxial compression test data Appendix C: Structural profile of the continuous multi-year floe core Appendix D: Multi-year floe test data
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  • 77
    Call number: PIK W 510-19-92835
    Type of Medium: Monograph available for loan
    Pages: 31 Seiten
    ISBN: 952984400X
    Series Statement: Working paper / European Forest Institute 1
    Language: English
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  • 78
    Call number: MOP 47005/1 / Mitte
    In: Rukovodstvo po agrometeorologičeskim prognozam, Tom 1
    Type of Medium: Monograph available for loan
    Series Statement: Rukovodstvo po agrometeorologičeskim prognozam 1
    Language: Russian
    Note: In kyrillischer Schrift
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  • 79
    Monograph available for loan
    Monograph available for loan
    Washington, D.C. : American Geophysical Union
    Associated volumes
    Call number: 5/M 19.93185
    In: Geophysical monograph
    Type of Medium: Monograph available for loan
    Pages: vi, 154 Seiten , graphische Darstellungen
    Edition: Online edition Online-Ausg. [S.l.] : HathiTrust Digital Library
    ISBN: 0-87590-022-4
    Series Statement: Geophysical monograph 22
    Classification:
    Geomagnetism, Geoelectromagnetism
    Language: English
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  • 80
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-80/23
    In: CRREL Report, 80-23
    Description / Table of Contents: The contribution of brine layers to observed reflective anisotropy of sea ice at 100 MHz is quantitatively assessed. The sea ice is considered to be a stratified, inhomogeneous, anisotropic dielectric consisting of pure ice containing ordered arrays of conducting inclusions (brine layers). Below the transition zone, the ice is assumed to have constant azimuthal c-axis orientation within the horizontal plane, so that the orientation of brine layers is uniform. The brine layers are also assumed to become increasingly well-defined with depth, since adjacent brine inclusions tend to fuse together with increasing temperature. A theoretical explanation for observed reflective anisotropy is proposed in terms of an isotropic electric flux penetration into the brine layers. Penetration anisotropy and brine layer geometry are linked to anisotropy in the complex dielectric constant of sea ice. In order to illustrate the above effects we present a numerical method of approximating the reflected power of a plane wave pulse incident on a slab of sea ice. Mixture dielectric constants are calculated for two polarizations of the incident wave: 1) the electric field parallel to the c-axis direction, and 2) the electric field perpendicular to the c-axis direction. These dielectric constants are then used to calculate power reflection coefficients for the two polarizations. Significant bottom reflection (R ~ 0.08) occurs when the polariza-tion is parallel to the c-axis. However, when the polarization is perpendicular to the c-axis, the return may be almost completely extinguished (R 〈 0.001). This extinction is due primarily to absorptive loss associated with the conduct-ing inclusions and secondarily to an impedance match at the ice/water interface that results in transmission of the wave to the water without reflection.
    Type of Medium: Series available for loan
    Pages: vi, 15 Seiten , Illustrationen
    Series Statement: CRREL Report 80-23
    Language: English
    Note: CONTENTS Abstract Preface List of symbols Introduction Anisotropy and sea ice macrostructure Anisotropy and sea ice microstructure A theory of anisotropic radar return from sea ice Anisotropic electric flux penetration into brine layers Implications of normal exclusion, tangential penetration, and brine layer geometry for dielectric behavior of sea ice Modeling of electromagnetic reflection from a stratified, anisotropic, inhomogeneous lossy medium Calculation of mixture complex dielectric constants Calculation of interfacial power reflection coefficients Calculation of bulk power reflection coefficients Calculation of attenuated power reflection coefficients Beam spread Results Anisotropic bottom reflections Anisotropic complex dielectric constants Sensitivity of parameters Internal reflection: the bumps Discussion Conclusions Literature cited
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  • 81
    Call number: ZSP-201-80/19
    In: CRREL Report, 80-19
    Description / Table of Contents: During the period 1975-1978 the Federal Highway Administration sponsored a series of environmental engineering in­vestigations along the Yukon River to Prudhoe Bay Haul Road. In 1976 the Department of Energy joined these in­vestigations with a series of ecological projects which continue to the present. Both agencies research efforts were con­ducted on a cooperative basis with CRREL’s in-house research program. The objectives of the research focused on 1) an evaluation of the performance of the road, 2) an assessment of changes in the environment associated with the road, 3) documentation of flora and vegetation along the 577-km-long transect, 4) methodologies for revegetation and restoration, and 5) an assessment of biological parameters as indicators of environmental integrity. In support of these objectives, specific studies were undertaken that investigated the climate along the road, thaw and subsidence beneath and adjacent to the road, drainage and side slope performance, distribution and properties of road dust, vegetation distribution, vegetation disturbance and recovery, occurrence of weeds and weedy species, erosion and its control, revegetation and restoration, and construction of the fuel gas line. This report presents background, information on the region, detailed results of the road thaw subsidence and dust investigations, and summaries of revegetation, fuel gas line, vegetation distribution, soil, and weed studies.
    Type of Medium: Series available for loan
    Pages: xv, 187 Seiten , Illustrationen
    Series Statement: CRREL Report 80-19
    Language: English
    Note: CONTENTS Abstract Preface Summary Introduction Chapter 1. The road and its environment Introduction General physiography Regional climate Surficial and bedrock geology Permafrost and ground ice General biota Vegetation Floristic survey Vegetation mapping Soils and mapping Chapter 2. Roadbed performance and associated investigations Roadbed investigations Roadbed performance Performance of drainage features Performance of sideslopes Conclusions from road, drainage and sideslope performance studies Fuel gas line construction Chapter 3. Distribution and properties of road dust along the northern portion of the Haul Road Introduction Methods Results of wind direction and velocity measurements Dust load and distribution Particle size analyses of dust Chemical composition properties of dust and related samples Soil cation composition Dust impacts on vegetation Discussion and conclusions Chapter 4. Revegetation and restoration investigations Introduction Revegetation approaches Alyeska erosion control and revegetation program Weeds and weedy plants Performance of revegetation Alyeska willow cutting program CRREL restoration experiments Conclusions Revegetation recommendations General report recommendations Literature cited Appendix A: General environmental guidelines applicable to subarctic and arctic road construction Appendix B: University-based studies along the Yukon River-Prudhoe Bay Haul Road Appendix C: CRREL maps of Haul Road showing locations of all study Sites Appendix D: Additional Haul Road cross-sectional profiles Appendix E: Clay mineralogy of road-related materials Appendix F: List of reports in the Joint State/Federal Fish and Wildlife Ad­visory Team series
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  • 82
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-80/15
    In: CRREL Report, 80-15
    Description / Table of Contents: This report discusses the time constraints on measuring the thermal resistance (R-value) of building components. Temperature changes on either side of a building component perturb measurement accuracy. Long measurement times and measurement times corresponding to a consistent diurnal cycle can be satisfactory; however, individual temperature changes cause significant error for shorter measurement periods. This report shows how to scale the thermal properties of individual constituent materials in a building element to determine its characteristic thermal time constant. The report then demonstrates the size of measurement error resulting from a variety of changes in temperature with representative walls of different time constants.
    Type of Medium: Series available for loan
    Pages: iii, 30 Seiten , Illustrationen
    Series Statement: CRREL Report 80-15
    Language: English
    Note: CONTENTS Abstract Preface Conversion factors Introduction Field measurement and analysis of transient heat flow A closer look at handling the constraints Random change Step change Ramp change Application of theory Literature cited Appendix A. Percentage error from a step input Appendix B. Time constraints of sample walls Appendix C. Percentage error from a ramp input Appendix D. Percentage error from a sinusoidal input Appendix E. Percentage error programs for a Hewlett-Packard HP-25 calculator Appendix F. Experimental determination of time constants Appendix G. Derivation of time constant formula for multiple layers
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  • 83
    Call number: MOP 45169 / Mitte
    Type of Medium: Monograph available for loan
    Language: English
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  • 84
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-80/9
    In: CRREL Report, 80-9
    Description / Table of Contents: Explosive cratering tests were conducted in seasonally frozen and thawed gravel at Ft. Richardson near Anchorage, Alaska, and in seasonallly frozen and thawed silt overlying permafrost and in silt permafrost at Ft. Wainwright near Fairbanks, Alaska. Explosive charge weights ranged from 26 to 3120 lb and charge burial depths ranged from about 3 to 40 ft. The cube root of the charge weight scaling was used to determine maximum scaled crater dimensions and optimum scaled depth of burial of the charge. Test results for frozen and thawed gravel were essentially the same because of the low moisture content and the relatively shallow depth of freezing (5 to 6 ft). The optimum depth of burial of the charge for maximizing the apparent radius and depth and the true radius was about 1.8 times the cube root of the charge weight for both the frozen and thawed conditions. In seasonally frozen silt overlying a talik and silt permafrost the maximum scaled crater dimensions and optimum scaled burial depths of the charge were smaller than for the thawed condition except for the true crater dimensions. The channeling of energy in the talik produces maximum crater dimensions and an optimum burial depth for the true crater that is larger than for the thawed condition. The results for the homogeneous silt permafrost were very similar to the frozen gravel results with much smaller maximum crater dimensions and smaller optimum charge burial depths than for the thawed silt overlying permafrost.
    Type of Medium: Series available for loan
    Pages: v, 21 Seiten , Illustrationen
    Series Statement: CRREL Report 80-9
    Language: English
    Note: CONTENTS Abstract Preface Metric conversion table Introduction Test sites Test procedures and materials Analysis of test data Mobility tests Conclusions Literature cited
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  • 85
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-80/8
    In: CRREL Report, 80-8
    Description / Table of Contents: This report presents the results of the tests on the new U.S. Coast Guard 140-ft icebreaker Katmai Bay (WTGB-101) in the level plate ice and brash ice in Whitefish Bay and the St. Marys River. The results indicate that the vessel can penetrate 22 in. of level freshwater ice with 2-3 in. of snow cover. It can also penetrate up to 48 in. of brash ice in a continuous mode and at least 30 in. of plate ice by backing and ramming. The installed bubbler system decreased the required power of the vessel from 10 to 30% in brash ice and 25 to 35% in level ice. The low friction coating appears to be effective in decreasing the friction factor when it remains intact; when it peels off it appears to make conditions worse than plain paint. An average dynamic friction factor of 0.15 could be used over the entire hull for these tests.
    Type of Medium: Series available for loan
    Pages: iv, 28 Seiten , Illustrationen
    Series Statement: CRREL Report 80-8
    Language: English
    Note: CONTENTS Abstract Preface Metric conversion table Introduction Roughness and friction measurements Level plate ice performance Brash ice performance Ramming icebreaking performance Analysis of the data Propulsion efficiency in ice Regression analysis Conclusions and recommendations Literature cited
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  • 86
    Call number: MOP 45384/5 / Mitte
    In: WMO TD / World Meteorological Organization, No. 1
    Type of Medium: Series available for loan
    Pages: ii, 52 Seiten , 29 cm
    Series Statement: WMO TD / World Meteorological Organization 1
    Language: English
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  • 87
    Call number: ZSP-201-80/10
    In: CRREL Report, 80-10
    Description / Table of Contents: A mathematical model of coupled heat and moisture flow in soils has been developed. The model includes algorithms for phase change of soil moisture and frost heave and permits several types of boundary and initial conditions. The finite element method of weighted residual (Galerkin procedure) was chosen to simulate the spatial regime and the Crank-Nicholson method was used for the time domain portion of the model. To facilitate evaluation of the model, the heat and moisture fluxes were essentially decoupled; moisture flux was then simulated accurately, as were heat flux and frost heave in a laboratory test. Comparison of the simulated and experimental data illustrates the importance of unsaturated hydraulic conductivity. It is one parameter which is difficult to measure and for which only a few laboratory test results are available. Therefore, unsaturated hydraulic conductivities calculated in the computer model may be a significant source of error in calculations of frost heave. The algorithm incorporating effects of surcharge and overburden was inconclusively evaluated. Time-dependent frost penetration and frost heave in laboratory specimens were closely simulated with the model. After 10 days of simulation, the computed frost heave was about 2.3 cm vs 2.0 cm and 2.8 cm in two tests. Frost penetration was computed as 15 cm and was measured at 12.0 cm and 12.2 cm in the two laboratory samples after 10 days.
    Type of Medium: Series available for loan
    Pages: v, 49 Seiten , Illustrationen
    Series Statement: CRREL Report 80-10
    Language: English
    Note: CONTENTS Abstract Preface Introduction One-dimensional equations of simultaneous heat and moisture flux Moisture transport Heat transport Phase change Coupling effects Frost heave algorithm Development of computer model Finite difference vs finite element method Finite element formulation Time domain solution Evaluation of the mathematical model Heat flux Moisture flux Numerical dispersion Frost heave of homogeneous laboratory samples Conclusions Recommended studies to refine the model Literature cited Appendix A. Work plan, staffing and instrumentation requirements for correlating results oflaboratory frost susceptibility tests with field performance Appendix B. Proposed investigation of thaw weakening of subgrade soil and granular unboundbase course Appendix C. Derivation of finite element system matrices
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  • 88
    Monograph available for loan
    Monograph available for loan
    [Reading, Berkshire] : [European Centre for Medium Range Weather Forecasts]
    Call number: MOP 44987 / Mitte
    Type of Medium: Monograph available for loan
    Pages: i, 97 Seiten , Illustrationen , 30 cm
    Language: English
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  • 89
    Call number: ZSP-201-80/5
    In: CRREL Report, 80-5
    Description / Table of Contents: This research comprised laboratory testing to determine the properties of asphalt-aggregate mixtures containing three grades of asphalt cements, and analyses to project the performance of pavements containing each of the asphalts, in resisting thermally induced distress and traffic-associated distress. From the results it is concluded that only the softest asphalt cement tested (AC 2.5) would perform satisfactorily in a cold climatic zone. The moderately soft (AC 5) and moderately hard (AC 20) asphalt cements showed little susceptibility to thermal cracking in a moderate and a warm climatic zone, respectively. The AC 2.5 and AC 5 asphalts are not recommended for use in warm climates, however, owing to increased susceptibility to rutting under traffic.
    Type of Medium: Series available for loan
    Pages: vi, 55 Seiten , Illustrationen
    Series Statement: CRREL Report 80-5
    Language: English
    Note: CONTENTS Abstract Preface Introduction Research setting Objectives Materials, mixture designs, and tests Materials Mixture design tests Brazil test Resilient modulus test Data analysis Marshall tests Asphalt grade Compactive effort Aggregate type Data analysis Brazil tests Indirect tensile strength Tensile strain Vertical deformation Summary of Brazil test results Data analysis-resilIient modulus. Comparison of mixture susceptibility to temperature cracking General asphalt concrete stiffness Thermal cracking. Influence of asphalt cement properties Summary Comparison of mixture susceptibility to traftic-load-associated distress Stress/strain analysis Fatigue damage analysis Rutting analysis Strength correlations Marshall stability and indirect tensile strength Indirect tensile strength and resilient modulus Summary Summary and conclusions Recapitulation of investigations Summary of results Conclusions Literature cited Appendix A: Asphalt adggregate mixture properties by Marshall method Appendix B: Equations for calculating specimen properties from Brazil tests Appendix C: Calculated displacements, strains and stresses
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  • 90
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-80/6
    In: CRREL Report, 80-6
    Description / Table of Contents: Weekly measurements of the thickness of lake, river and fast sea ice made over a period of 10 to 15 years at 66 locations in Canada and Alaska are analyzed, and the portion of the data relating to maximum ice thickness and decay (i.e. the decrease in ice thickness) is examined. Ice thickness curves revealed individual patterns of ice decay, and comparisons between locations disclosed major contrasts in the amount of ice accretion and the times of maximum ice and ice clearance. Although many factors affect the ice decay process, this study investigates in detail the effect of thawing temperatures. Concurrent measurements of the air temperature at each location made it possible to analyze the relationship between accumulated thawing degree-days (ATDD) and ice cover decay. Other factors affecting ice ablation and breakup, such as snow-ice formation, snow cover depth, solar radiation and wind are also discussed.
    Type of Medium: Series available for loan
    Pages: v, 160 Seiten , Illustrationen
    Series Statement: CRREL Report 80-6
    Language: English
    Note: CONTENTS Abstract Preface Introduction Data sources and literature review Canada Alaska Data tabulation Station selection Description of tabulated data Station location and ice measurement site descriptions Review of previous studies on maximum ice in North America Maximum ice thickness maps Date of maximum ice Plotting of the ice decay curves General procedures Categories of water bodies Ice decay at sea ice locations Envelope curves Average curves Snow-ice formation Ice decay at lake ice locations Average curves Regional variations and similarities Ice decay at river ice locations Variations in ice thickness Rapid ice clearance Comparison between Alaskan and Canadian river ice decay curves Incremental extraction of ice decay data for analysis purposes Selection of ice decay intervals Preliminary evaluation of the methodology Further considerations of the methodology Relationships between ice decay and thawing air temperatures Average daily vs maximum daily air temperature 10-day increments vs accumulated values Total years vs year-to-year analysis Evaluation of use of 0°C as a base Final format of the relationship between ice decay and ATDD Evaluation of the final form Possible causes for variations in slope values Decreasing sea ice thickness and thawing air temperatures Factors affecting sea ice decay Relationship between ATDD and sea ice decay Influence of solar radiation and wind on sea ice decay Literature cited Selected bibliography Appendix A. Ice thickness measurements and other related (or associated) observations for stations in Canada and Alaska Appendix B. Maps of least and greatest ice thickness observed at the time of maximum growth, and average date of occurrence Appendix C. Annual ice decay curves for stations in Canada and Alaska
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  • 91
    Call number: ZSP-201-80/4
    In: CRREL Report, 80-4
    Description / Table of Contents: The primary objectives of this study were to 1) prepare a map from Landsat imagery of the Upper Susitna River Basin drainage network, lakes, glaciers and snowfields, 2) identify possible faults and lineaments within the upper basin and within a 100-km radius of the proposed Devil Canyon and Watana dam sites as observed on Landsat imagery, and 3) prepare a Landsat-derived map showing the distribution of surficial geologic materials and poorly drained areas. The EROS Digital Image Enhancement System (EDIES) provided computer- enhanced images of Landsat-1 scene 5470-19560. The EDIES false color composite of this scene was used as the base for mapping drainage network, lakes, glaciers and snowfields, six surficial geologic materials units and poorly drained areas. We used some single-band and other color composites of Landsat images during interpretation. All the above maps were prepared by photointerpretation of Landsat images without using computer analysis, aerial photographs, field data, or published reports. These other data sources were used only after the mapping was completed to compare and verify the information interpreted and delineations mapped from the Landsat images. Four Landsat-1 MSS band 7 winter scenes were used in the photomosaic prepared for the lineament mapping. We mapped only those lineaments related to reported regional tectonics, although there were many more lineaments evident on the Landsat photomosaic.
    Type of Medium: Series available for loan
    Pages: iii, 41 Seiten , Illustrationen
    Series Statement: CRREL Report 80-4
    Language: English
    Note: CONTENTS Abstract Preface Summary Objectives Conclusions Introduction Background Previous cooperative investigations Project rationale and coordination Approach Landsat imagery Interpretation techniques Part I. Use of Landsat imagery in mapping the drainage network, lakes, glaciers and snowfields (Lawrence W. Gatto) Objective Methods Results Conclusions Part II. Use of Landsat imagery in mapping and evaluating geologiclineaments and possible faults (Carolyn J. Merry) Objective Geologic structure Methods Results Conclusions Part Ill. Use of Landsat imagery in mapping surficial materials Section A. Landsat mapping (Harlan L. McKim) Objective Methods Results Section B. Field evaluation (Daniel E. Lawson) Objectives Methods Results Discussion Section C. Conclusions (Daniel E. Lawson and Harlan L. McKim) Literature cited Glossary
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  • 92
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-80/18
    In: CRREL Report, 80-18
    Description / Table of Contents: The use of ice as a structural material is common practice for certain applications in cold regions. Techniques such as surface flooding or water spraying are used to accelerate ice growth rates, thereby lengthening the winter construction season. This report examines the heat and mass transfer rates from freely falling water drops in cold air. Design equations which predict the amount of supercooling of the drops as a function of outdoor ambient temperature, drop size and distance of fall are given
    Type of Medium: Series available for loan
    Pages: v, 14 Seiten , Illustrationen
    Series Statement: CRREL Report 80-18
    Language: English
    Note: CONTENTS Abstract Preface Nomenclature Introduction Velocity problem Heat and mass transfer problem - A single drop Heat and mass transfer - A system of drops Literature cited Appendix A: FORTRAN IV program to calculate final drop temperature, air temperatureand humidity
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  • 93
    Monograph available for loan
    Monograph available for loan
    Freiburg : Lingg Druck
    Call number: MOP 47855 / Mitte
    Type of Medium: Monograph available for loan
    Pages: VII, 164 Seiten , Illustrationen
    Language: German
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  • 94
    Call number: MOP 46028/1983 / Mitte
    In: World weather watch : Consolidated report on the voluntary co-operation programme including projects approved for circulation, 1983
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    Language: English
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  • 95
    Call number: MOP 47005/2 / Mitte
    In: Rukovodstvo po agrometeorologičeskim prognozam, Tom 2
    Type of Medium: Monograph available for loan
    Pages: 264 Seiten , Illustrationen
    Series Statement: Rukovodstvo po agrometeorologičeskim prognozam 2
    Language: Russian
    Note: In kyrillischer Schrift
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  • 96
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-80/31
    In: CRREL Report, 80-31
    Description / Table of Contents: Ice accretion on structures built on the earth’s surface is discussed. Sources of water are the atmosphere or water bodies near or surrounding the structure. Ice types include frost, rime, glaze, and spray; properties and conditions governing their formation are presented. Methods of estimating accretion rates and total accretion on structures are given, and extracts from U.S. and Canadian codes for ice and wind loads on structures are included. Techniques for preventing or removing ice accretion are presented.
    Type of Medium: Series available for loan
    Pages: iv, 18 Seiten , Illustrationen
    Series Statement: CRREL Report 80-31
    Language: English
    Note: CONTENTS Abstract Preface 1. Types of ice accretion a. Frost b. Rime c. Glaze d. Spray ice 2. Conditions governing type of accreted ice a. Meteorological b. Structural 3. Accretion rates a. Fundamentals b. Effect of height c. Geographical distribution 4. Spray icing 5. Structural design factors a. Dead loads b. Wind field in the boundary layer c. Windloads 6. Techniques for minimizing structural icing 7. Data collection needs 8. Literature cited
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  • 97
    Series available for loan
    Series available for loan
    Offenbach am Main : Deutscher Wetterdienst
    Associated volumes
    Call number: MOP 47697/8 / Mitte
    In: Verifikationsbericht zur Güte lokaler Wettervorhersagen / Deutscher Wetterdienst, Zentralamt, Nr. 8
    Type of Medium: Series available for loan
    Series Statement: Verifikationsbericht zur Güte lokaler Wettervorhersagen / Deutscher Wetterdienst, Zentralamt 8
    Language: German
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  • 98
    Series available for loan
    Series available for loan
    Offenbach am Main : Deutscher Wetterdienst
    Associated volumes
    Call number: MOP 47697/9 / Mitte
    In: Verifikationsbericht zur Güte lokaler Wettervorhersagen / Deutscher Wetterdienst, Zentralamt, Nr. 9
    Type of Medium: Series available for loan
    Series Statement: Verifikationsbericht zur Güte lokaler Wettervorhersagen / Deutscher Wetterdienst, Zentralamt 9
    Language: German
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  • 99
    Call number: MOP 46293/A / Mitte
    In: United States Antarctic Research Report to SCAR, No. 26
    Type of Medium: Series available for loan
    Series Statement: United States Antarctic Research Report to SCAR 26
    Language: English
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  • 100
    Call number: MOP 46079 / Mitte
    In: DOE/ER / US Department of Energy, Office of Energy Research, 0083
    Type of Medium: Series available for loan
    Pages: 124 Seiten , Illustrationen , 28 cm
    Series Statement: DOE/ER / US Department of Energy, Office of Energy Research 0083
    Language: English
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