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  • 2015-2019
  • 1990-1994  (43)
  • 1992  (43)
  • 1
    Call number: M 92.0753 ; AWI G6-92-0394
    Description / Table of Contents: This volume summarizes the main results of a priority programme of the Deutsche Forschungsgemeinschaft (DFG), Bonn-Bad Godesberg
    Type of Medium: Monograph available for loan
    Pages: XXIX, 544 Seiten , Illustrationen
    ISBN: 3-540-54034-2 , 0-387-54034-2
    Classification:
    Geochemistry
    Language: English
    Note: Contents 1 Scope / G. Matthess 2 Polar Organic Substances and Their Role in the Water-Saturated and -Unsaturated Zones 2.0 Introduction / F.H. Frimmel 2.1 Isolation Procedures and Characterization Methods 2.1.1 Isolation and General Characterization of Organic Acids from Pore Water / F.H. Frimmel 2.1.2 Isolation and Characterization of Soil Humic Matter / W. Finger, B. Post and H. Klamberg 2.1.3 Isolation and Characterization of Organic Substancesin Ground Water and Sediments / F. Selenka and A. Hack 2.1.4 Chromatographie Characterization of the Acid-Soluble Part of Humic Substances / F.H. Frimmel 2.1.5 Spectroscopic Characterization of Humic Substances in the Ultraviolet and Visible Region and by Infrared Spectroscopy / G. Abbt-Braun 2.1.6 Temperature-Programmed/Time-Resolved Pyrolysis Field lonization Mass Spectrometry - a New Method for the Characterization of Humic Substances / H.-R. Schulten 2.1.7 Interpretation of the Pyrolysis Products of Isolated Humic and Fulvic Acids / G. Abbt-Braun 2.1.8 Characterization of Isolated Humic Material by 13C Nuclear Magnetic Resonance Spectroscopy /J. Buddrus and P. Burba 2.1.9 Characterization of Humic Substances Extracted by Organic Solvents / B. Post and H. Klamberg 2.2 Interaction of Inorganics with Humic Substances 2.2.1 Investigation of Metal Complexation by Polarography and Fluorescence Spectroscopy / F.H. Frimmel 2.2.2 Determination of Complexation Equilibria by the Ion-Exchange Method / W. Finger and H. Klamberg 2.2.3 Sorption of Metals on Humic Material / R. Becker and H. Klamberg 2.2.4 Interactions of Humic Substances with Iodine / K. G. Heumann and C. Reifenhäuser 2.2.5 Experiments on the Influence of Organic Ligands upon Kinetics of Feldspar Weathering / A. Petersen, G. Matthess and D. Schenk 2.3 Characterization of Some Organic Acids in the Subsurface of the Sandhausen Ecosystem / T. Cordt and H. Kussmaul 2.3.4 Organic Acids 2.3.5 Conclusions 3 Carbonate Systems 3.0 Introduction / E. Usdowski 3.1 Dissolution Kinetics in the Generation of Carbonate Ground Waters 3.1.1 Theoretical and Experimental Results of the Kinetics of Calcite Dissolution and Precipitation / W. Dreybrodt 3.1.2 Field Measurements and Laboratory Experiments on Calcite Dissolution Kinetics of Natural Porous Media / J. Baumann and H.D. Schulz 3.2 Field Studies on Subsurface Water of Selected Sites / B. Merkel and J. Grossmann 3.2.1 Pore Water Sampling in Carbonate Terrains 3.2.2 Variation of Inorganic Carbon in the Unsaturated Zone of a Carbonate Gravel System / L. Eichinger and B. Merkel 3.2.3 Isotope Geochemistry of the Subsurface Carbonate System in Sandhausen and Bocholt / H. Dörr, W. Leuchs, P. Obermann, W. Regenberg and C. Sonntag 3.2.4 Application of Stable Carbon and Sulfur Isotope Models to the Development of Ground Water in a Limestone-Dolomite-Anhydrite-Gypsum Area / K.W. Schaefer and E. Usdowski 3.2.5 A dissolution Front at the Contact of Sandsto Marly Limestone Aquifers / H.R. Langguth and R. Schulz 3.2.6 Carbonate Rock Dissolution Under Intermediate System Conditions / J. Michaelis 3.3 Alteration in Karst Systems 3.3.1 Mineralogy and Hydrogeochemistry of the Gypsum Karst of Foum Tatahouine, South Tunisia / W. Smykatz-Kloss, H. Hötzl and H. Kössl 3.3.2 Dedolomitization and Salt Formationin a Semi-Arid Environment / W. Smykatz-Kloss, and J. Goebelbecker 3.3.3 Transformation Processes in Paleokarst Sediments and Chemistry of Modern Waters in the Aladag Region, Turkey / M. Cevrini and W. Echle 4 Silicate Systems 4.0 Introduction / G. Matthess 4.1 Redox Reactions in the Subsurface 4.1.1 Anoxic Reaction Zones in an Aquifer Influenced by Increasing Nitrate and Sulfate Contents / W. Leuchs and P. Obermann 4.1.2 Nitrogen and Oxygen Isotopes as Indicators for Nitrification and Denitrification / H.-L. Schmidt, S. Voerkelius and A. Amberger 4.1.3 Redox Conditions and Microbial Sulfur Reactions in the Fuhrberger Field Sandy Aquifer / J. Böttcher, O. Strebet and W. Kölle 4.1.4 Influence of Fine-Grained Cover Beds on the Chemistry of Shallow Ground Water / G. Ebhardt and P. Fritsch 4.1.5 Hydrogeochemical Processes During the Passage of Surface Water and Ground Water Through Genetically Different Organic Sediments / H. Brühl, A. Moschick and H. Verleger 4.1.6 Hydrochemical Phenomena in the Dorsten Leakage System / M. Hoffmann, H.R. Langguth and J. Larue 4.1.7 Hydrogeochemical Processes in the Hamburg Deep Aquifer System / E.P. Loehnert, W. Bauhus and C. Sonntag 4.2 Rock-Water Interaction 4.2.1 Aluminium Speciation in Acid Soil Water and Ground Water / G. Dietze and B. Ulrich 4.2.2 Mineral-Pore Water Interaction in Two Soil Types on Pleistocene Sediments at Hamburg / F. Sztuka and I. Valeton 4.2.3 Subsurface Hydrochemical Reactions in the Sandhausen Forest Ecosystem / H. Jacob, W. Regenberg and C. Sonntag 4.3 Reaction Kinetics 4.3.1 Experimental Methods for Determining Dissolution Rates of Silicates - a Comparison / D. Schenk, G. Matthess, A. Dahmke and A. Petersen 4.3.2 Field Studies on the Kinetics of Silicate Minerals/Water Interaction / G. Matthess, A. Petersen, D. Schenk and A. Dahmke 5 Microbiology 5.0 Introduction / P. Hirsch 5.1 Characterization of the Natural Subsurface Environment 5.1.1 Morphological and Taxonomic Diversity of Ground Water Microorganisms / P. Hirsch, E. Rades-Rohkohl, J. Kölbel-Boelke and A. Nehrkorn 5.1.2 Methods of Studying Ground Water Microbiology: Critical Evaluations and Method suggestions / P. Hirsch, E. Rades-Rohkohl, J. Kölbel-Boelke, A. Nehrkorn, R. Schweisfurth, F. Selenka and A. Hack 5.1.3 Organic Substances in Ground Water and Sediments and Their Relationships to Microorganisms in a Sandy Aquifer / E Selenka and A. Hack 5.2 Microbial Activities 5.2.1 Observations on the Physiology of Microorganisms from Pristine Ground Water Environments / P. Hirsch 5.2.2 Formation and Transformation of Manganese Oxidation States by Bacteria / J. Gottfreund and R. Schweisfurth 5.2.3 Interactions Between Humic Acids and Microorganisms / G.-J. Tuschewitzki, B. Langer and H. Otremba 5.3 Microbiology of Selected Locations 5.3.1 Subsurface Microbial Activities in the Sandhausen Forest Ecosystem / R. Weyandt and R. Schweisfurth 5.3.2 Heterotrophic Bacterial Communities in the Bocholt Aquifer System / J. Kölbel-Boelke and A. Nehrkorn 5.3.3 The Natural Microflora of the Segeberger Forest Aquifer System / P. Hirsch and E. Rades-Rohkohl 5.3.4 Microbiological Observations of the Unsaturated Zone of a Quaternary Gravel Profile / I. Alexander, G. Freitag, J. Grossmann, Β. Merkel, P. Udluft and I. Ullsperger 6 Hydrogeochemical and Geochemical-Hydraulic Models and Model Concepts 6.0 Introduction / H.-D. Schulz 6.1 Hydrogeochemical Models and Concepts 6.1.1 Development of Secondary Permeability of a Fracture Aquifer in Carbonate Rocks: a Model / W. Dreybrodt 6.1.2 Some Aspects of Modelling the Carbon System in the Unsaturated Zone / B. Merkel, L. Eichinger and P. Udluft 6.1.3 Methodical Concepts in Silicate-Water Interaction - a Comparison of Results / A. Dahmke, G. Matthess, A. Petersen and D. Schenk 6.2 Combination of Transport and Geochemical Reactions 6.2.1 Water Movement and Geochemical Reactions in the Unsaturated Zone of Sands with Low Calcite Contents / H.-D. Schulz 6.2.2 Physical and Biochemical Processes Affecting Mass Transport in the Bocholt Aquifer System / C. Bugner and R. Mull 6.2.3 Tritium and 3He Measurements as Calibration Data for Ground Water Transport Models / H. Dörr, P. Schlosser, M. Stute and C. Sonntag 6.2.4 39Ar-, 85Kr-, 3He- and 3H Isotope Dating of Ground Water in the Bocholt and Segeberger Forst Aquifer Systems / M. Forster, H. Loosli and S. Weise 6.2.5 Modelling of Mass Balance and of Microbial Transformations in the Fuhrberger Feld Sandy Aquifer / O. Strebet, J. Böttcher and W.H.M. Duynisveld 6.3 Description of Geochemical Environments with Thermodynamic Equilibrium Models / M. Rolling and H.-D. Schulz 6
    Location: Upper compact magazine
    Location: AWI Reading room
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  • 2
    Electronic Resource
    Electronic Resource
    [S.l.] : American Institute of Physics (AIP)
    Review of Scientific Instruments 63 (1992), S. 966-966 
    ISSN: 1089-7623
    Source: AIP Digital Archive
    Topics: Physics , Electrical Engineering, Measurement and Control Technology
    Notes: The signal/background ratio is the main problem for microcrystal diffraction experiments. Background scattering can be reduced by special mounting techniques, by reducing or avoiding air scattering, and reducing diffuse scattering from the crystal. Furthermore, the intrinsic noise of the counter system has to be made as small as possible. To avoid very long measuring time per diffraction event, area counters have to be applied in order to register several of such events at a time.
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  • 3
    ISSN: 1434-6052
    Source: Springer Online Journal Archives 1860-2000
    Topics: Physics
    Notes: Abstract The production ofD *(2010)+ andJ/ψ mesons and prompt leptons has been investigated ine + e − interactions at the Ψ(1S) resonance energy. The data were collected at the storage ring DORIS II at DESY with the ARGUS detector. We obtain upper limits of BRdir (ϒ (1S)→D *(2010)±+X)〈0.019 (forx p 〉0.2) and BRdir (ϒ(1S)→J/ψ+X)〈0.68×10−3, both at the 90% confidence level. From the prompt lepton analysis, a model dependent limit of BRdir (ϒ(1S)→Y c +X)〈0.034 (Y c denoting a charm-containing particle) is derived.
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  • 4
    ISSN: 1434-6052
    Source: Springer Online Journal Archives 1860-2000
    Topics: Physics
    Notes: Abstract Using the ARGUS detector at thee + e − storage ring DORIS II at DESY, we have studiedB meson decays into baryonsp and Λ. From the simultaneous analysis ofp and Λ yields,p $$\bar p$$ and Λ $$\bar p$$ correlations, and various lepton-baryon and lepton-baryon-antibaryon correlations the inclusive branching ratio is found to be BR (B→baryons)=(6.8±0.5±0.3)%.
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  • 5
    ISSN: 1434-6052
    Source: Springer Online Journal Archives 1860-2000
    Topics: Physics
    Notes: Abstract An analysis of the decay τ-→π-π0 v τ has been performed using the ARGUS detector at the DORIS II storage ring. The branching ratio has been determined to be Br(τ-→π-π0 v τ=(22.6±0.4±0.9)%. The shape of the π-π0 invariant mass spectrum is found to be in good agreement with the predictions obtained using the conserved vector current (CVC) hypothesis, suggesting that the π-π0 system is produced in aJ P=1− state. An analysis of the measured decay angular distribution of the pions with respect to the flight direction of the π-π0 system demonstrates the vector nature of the coupling at the τv τ vertex. With the assumption of zerov τ mass thev τ spin has been shown to be $$J_{v_\tau } = \tfrac{1}{2} $$ .
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  • 6
    ISSN: 1434-6052
    Source: Springer Online Journal Archives 1860-2000
    Topics: Physics
    Notes: Abstract Using the ARGUS detector at thee + e − storage ring DORIS II at DESY, we have observed the decaysD +→K − K 0π+π+ andD s + →K − K 0π+π+. The branching ratios were determined to be BR(D +→K − K 0π+π+)=(1.0±0.5±0.3)% and BR(D s + →K − K 0π+π+)/BR(D s + →φπ+)=1.2±0.2±0.2. These decays are found to proceed mostly via the $$\bar K*^0 K*^ + $$ decay channel, with BR(D +→ $$\bar K*^0 K*^ + $$ )=2.6±0.8±0.7)% and BR(D s + → $$\bar K*^0 K*^ + $$ )/BR(D s + →φπ+)=1.5±0.4±0.4.
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  • 7
    ISSN: 1434-6052
    Source: Springer Online Journal Archives 1860-2000
    Topics: Physics
    Notes: Abstract The production ofD S + mesons inB meson decays, and inq $$\bar q$$ continuum events, has been studied with the ARGUS detector at thee + e − storage ring DORIS II. In addition to the measurement of inclusiveD S + production in γ(4S)→B $$\bar B$$ decays, all eight two-body decay modesB→D S (*) D (*) have been measured with branching ratios between 1% and 3%. By comparing our inclusive and exclusive results to predictions of heavy quark effective theory, a value of (267±28) MeV × [2.7%/BR(D s + →φπ+)]1/2 is obtained for the weak decay constant fD S (*) , averaged overD S + andD S *+ mesons.
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  • 8
    ISSN: 1434-6052
    Source: Springer Online Journal Archives 1860-2000
    Topics: Physics
    Notes: Abstract We have measured theR value in non-resonante + e − annihilation using the ARGUS detector at the storage ring DORIS II. At a centre-of-mass energy $$\sqrt s = 9.36$$ GeV the ratio of the hadronic cross-section to the μ-pair cross section in lowest order QED has been determined to beR=3.46±0.03±0.13. In addition, we have measured the charged-particle multiplicities in non-resonant hadron production at $$\sqrt s = 10.47$$ GeV just below theB $$\bar B$$ threshold and in ϒ (4S) resonance decays. For the average charged-particle multiplicities in continuum events and ϒ(4S)→B $$\bar B$$ decays we obtain 〈n〉cont=8.35±0.02±0.20 and 〈n〉ϒ(4s)=10.81±0.05±0.23.
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  • 9
    ISSN: 1438-1168
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Description / Table of Contents: Zusammenfassung An Quarzgängen in Gesteinen des kristallinen Fundamentes Sachsens, Thüringens und des Harzes in der ehemaligen DDR wurden Untersuchungen zur genetischen Charakterisierung im Zusammenhang mit einer industriellen Nutzung durchgeführt. Mit Hilfe der Methoden der EinschluBforschung und ergänzender Spurenelement- und isotopengeochemischer Analysen war es möglich, Unterscheidungsmerkmale abzuleiten. Bereits mikroskopische Beobachtungen an Einschlüssen in den beiden Quarztypen zeigen Unterschiede in Häufigkeit, Größe, Form und Füllungsgrad. Die Homogenisierungs-temperaturen schwanken zwischen 200 und über 300°C für die metamorphogenen und von 100 bis über 250°C für die hydrothermalen. Druckkorrigierte Homogenisierungs-temperaturen übersteigen 500 °C bei den metamorphogen gebildeten Einschlüssen, sind aber nur für diese erhältlich. Die an den metamorphogenen Quarzen bestimmten Drücke nehmen Werte zwischen 120 bis über 300 MPa an. Die kryometrisch bestimmten Salinitäten bewegen sich zwischen niedrigen Konzentrationen (etwa 10 NaCl-Äquiv.-%) für metamorphogene und stark schwankenden (8 bis 26 NaCI Äquiv.-%) für die hydrothermalen. Diese Ergebnisse stimmen gut mit den chemischen Zusammensetzungen der eingeschlossenen Lösungen überein, die Werte zwischen 20 und 160 g/l für die metamorphogenen Quarze sowie 50 bis über 300 g/l für hydrothermale ergeben. Der Chemismus der Lösungen in metamorphogenen Quarzen zeigt dominante Na-, Cl- und HCO3-Ionen, während in den hydrothermalen Ca-Ionen überwiegen. Einige der festgestellten Eigenschaften sind für das Einschmelzverhalten der Quarze bei der Herstellung von Silicaglas von Bedeutung.
    Notes: Summary Investigations were made on quartz veins in rocks of the crystalline basement of the German regions Sachsen, Thüringen and Harz Mountains in the former GDR characterizing them genetically for industrial purposes. Fluid inclusions show differences in frequency, size, shape and filling degree between hydrothermal and metamorphic quartz. Homogenization temperatures range from 200 to more than 300°C for metamorphic quartz and from about 100 to more than 250°C for hydrothermal quartz. Pressure corrected homogenization temperatures of metamorphic quartz fluid inclusions exceed 500°C but are available only for this type. Pressures determined for metamorphic quartzes range from 120 to more than 300 MPa. Cryometrically analysed salinity varies from relatively low values (about 10 equiv.-% NaCl) for metamorphic quartz to widely scattered values (8 to 26 equiv.-% NaCl) for the hydrothermal type. The results agree well with the composition of the occluded solutions determined by chemical analysis which range from 20 to 160 g/l for metamorphic quartz, and from 50 and more than 300 g/l for hydrothermal quartz. Chemistry of the metamorphic quartz inclusions is dominated by Na, Cl and HCO3 ions, whereas Ca ions prevail in hydrothermal quartz. Some of the properties found are important for the melting behaviour of quartz in glass production.
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  • 10
    ISSN: 1434-6052
    Source: Springer Online Journal Archives 1860-2000
    Topics: Physics
    Notes: Abstract Using the ARGUS detector at the DORIS II storage ring, we have studied τ decays with one or three charged particles in the final state, obtaining the following values for the branching ratios: BR(τ−→e − $$\bar v_e v_\tau $$ )=(17.3±0.4±0.5)% BR(τ−→μ− $$\bar v_\mu v_\tau $$ )=(17.2±0.4±0.5)%,BR(τ−→π− v π)+BR(τ−→K − v π)=(11.7±0.6±0.8)% and BR(π−→3-prong)=(13.3±0.3±0.8)%. These measurements confirm the present world averages with a precision, in each case, comparable to the error on the combination of all previous results.
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