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  • 11
    Call number: 9/M 07.0421(468)
    In: Geological Society Special Publication
    Type of Medium: Monograph available for loan
    Pages: 208 Seiten , Diagramme
    ISBN: 978-1-78620-366-3
    Series Statement: Geological Society Special Publication 468
    Classification:
    Geochemistry
    Language: English
    Note: Hydrocarbon systems, by nature, are a complex interplay of elements that must be spatially and temporally aligned to result in the generation and preservation of subsurface hydrocarbon accumulations. To meet the increasing challenges of discovering hydrocarbon resources, it is essential that we advance our understanding of these systems through new geochemical approaches and analytical developments. Such development requires that academic- and industry-led research efforts converge in ways that are unique to the geosciences. The aim of this volume is to bring together a multidisciplinary geochemical community from industry and academia working in hydrocarbon systems to publish recent advances and state-of-the-art approaches to resolve the many remaining questions in hydrocarbon systems analysis. From Source to Seep presents geochemical and isotopic studies that are grouped into three themes: (1) source-rock identification and the temperature/timing of hydrocarbon generation; (2) mechanisms and time-scales associated with hydrocarbon migration, trapping, storage and alteration; and (3) the impact of fluid flow on reservoir properties. | Contents: Geochemical applications in petroleum systems analysis: new constraints and the power of integration / M. Lawson, M. J. Formolo, L. Summa and J. M. Eiler / Geological Society, London, Special Publications, 468, 1-21, 19 February 2018, https://doi.org/10.1144/SP468.6 --- Source-rock identification and the temperature/timing of hydrocarbon generation --- The utility of methane clumped isotopes to constrain the origins of methane in natural gas accumulations / Daniel A. Stolper, Michael Lawson, Michael J. Formolo, Cara L. Davis, Peter M. J. Douglas and John M. Eiler / Geological Society, London, Special Publications, 468, 23-52, 14 December 2017, https://doi.org/10.1144/SP468.3 --- The isotopic structures of geological organic compounds / John M. Eiler, Matthieu Clog, Michael Lawson, Max Lloyd, Alison Piasecki, Camilo Ponton and Hao Xie / Geological Society, London, Special Publications, 468, 53-81, 14 December 2017, https://doi.org/10.1144/SP468.4 --- Vanadium isotope composition of crude oil: effects of source, maturation and biodegradation / Yongjun Gao, John F. Casey, Luis M. Bernardo, Weihang Yang and K. K. (Adry) Bissada / Geological Society, London, Special Publications, 468, 83-103, 14 December 2017, https://doi.org/10.1144/SP468.2 --- Carbon and hydrogen isotopic compositions of n-alkanes as a tool in petroleum exploration / Nikolai Pedentchouk and Courtney Turich / Geological Society, London, Special Publications, 468, 105-125, 14 December 2017, https://doi.org/10.1144/SP468.1 --- Mechanisms and time-scales associated with hydrocarbon migration, trapping, storage and alteration --- Noble gases in conventional and unconventional petroleum systems / David J. Byrne, P. H. Barry, M. Lawson and C. J. Ballentine / Geological Society, London, Special Publications, 468, 127-149, 14 December 2017, https://doi.org/10.1144/SP468.5 --- Differentiating between biogenic and thermogenic sources of natural gas in coalbed methane reservoirs from the Illinois Basin using noble gas and hydrocarbon geochemistry / Myles T. Moore, David S. Vinson, Colin J. Whyte, William K. Eymold, Talor B. Walsh and Thomas H. Darrah / Geological Society, London, Special Publications, 468, 151-188, 18 January 2018, https://doi.org/10.1144/SP468.8 --- The impact of fluid flow on reservoir properties --- Testing clumped isotopes as a reservoir characterization tool: a comparison with fluid inclusions in a dolomitized sedimentary carbonate reservoir buried to 2–4 km / John M. MacDonald, Cédric M. John and Jean-Pierre Girard / Geological Society, London, Special Publications, 468, 189-202, 14 December 2017, https://doi.org/10.1144/SP468.7
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  • 12
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-83/29
    In: CRREL Report, 83-29
    Description / Table of Contents: A literature review indicated that the effects or permafrost on streambank erodibility and stability are not yet understood because systematic and quantitative measurements are seriously lacking. Consequently, general controversy exists as to whether perennially frozen ground inhibits lateral erosion and bankline recession, or whether it increases bank recession rates. Perennially frozen streambanks erode because of modification of the bank's thermal regime by exposure to air and water, and because of various erosional processes. Factors that determine rates and locations of erosion include physical, thermal and structural properties of bank sediments, stream hydraulics and climate. Thermal and physical modification of streambanks may also induce accelerated erosion within permafrost terrain removed from the immediate river environment. Bankline or bluffline recession rates are highly variable, ranging from less than 1 m/year to over 30 m/year and, exceptionally, to over 60 m/year. Long-term observations of the physical and thermal erosion processes and systematic ground surveys and measurements of bankline-bluffline recession rates are needed.
    Type of Medium: Series available for loan
    Pages: iv, 26 Seiten , Illustrationen
    Series Statement: CRREL Report 83-29
    Language: English
    Note: CONTENTS Abstract Preface Introduction Stream bank erosional processes Permafrost and related factors Permafrost and erosion General Erosional processes Bank zone processes Bluff zone processes Factors affecting perm afrost erodibility Exposure to currents and wind waves Texture and stratigraphy Ice content, distribution and type Slope aspect Coriolis force Timing and depth of thaw Water level and temperature Vegetation Ice and snow cover Groundwater Rates and timing of erosion and recession Overall effects of permafrost Recommendations for research Literature cited Appendix A : Processes of stream bank modifications
    Location: AWI Archive
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  • 13
    Call number: IASS 18.91780
    Description / Table of Contents: Part I - The Polar code and Beyond -- Part II - Arctic Ship Monitoring/Tracking -- Part III - Arctic Governance -- Part IV - Protection and Response in the Arctic Marine Environment -- Part V - Training and Capacity Building -- Part VI - Sustainable Arctic Business Development -- Part VII - Conclusion
    Description / Table of Contents: This volume brings together multiple perspectives on both the changing Arctic environment and the challenges and opportunities it presents for the shipping sector. It argues for the adoption of a forward-looking agenda that respects the fragile and changing Arctic frontier. With the accelerated interest in and potential for new maritime trade routes, commercial transportation and natural resource development, the pressures on the changing Arctic marine environment will only increase. The International Maritime Organization Polar Code is an important step toward Arctic stewardship. This new volume serves as an important guide to this rapidly developing agenda. Addressing a range of aspects, it offers a valuable resource for academics, practitioners, environmentalists and affected authorities in the shipping industry alike
    Type of Medium: Monograph available for loan
    Pages: ix, 486 Seiten , Illustrationen
    ISBN: 9783319784243 , 9783319784250 (eBook)
    Series Statement: WMU Studies in Maritime Affairs 7
    Language: English
    Branch Library: RIFS Library
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  • 14
    Call number: ZSP-201-87/17
    In: CRREL Report, 87-17
    Description / Table of Contents: The ability to map frazil ice deposits and water channels beneath an ice-covered river in central Alaska using the magnetic induction conductivity (MI) technique has been assessed. The study was performed during the first week of March of 1986 on the Tanana River near Fairbanks and employed a commercially available instrument operating at a fixed frequency with a fixed antenna (coil) spacing and orientation. Comparisons of the MI data with theoretical models based upon physical data measured along three cross sections of the river demonstrate the sensitivity of the MI technique to frazil ice deposits. The conductivity generally derived for the frazil ice deposits encountered is very low (approx. .00063 s/m) when compared with the measured value for water (approx. 0.011 S/m), and is similar to the calculated values for gravel and sandy gravel bed sediments. In all three cross sections, maxima in the apparent conductivity profiles correlated with frazil ice deposits. Difficulties, possibly due to adverse effects of cold weather upon instrument calibration, affected the quantitative performance of the instrument on one cross section, although the interpretation of the data (locations of open channels vs frazil deposits) was qualitatively unaffected.
    Type of Medium: Series available for loan
    Pages: iii, 17 Seiten , Illustrationen
    Series Statement: CRREL Report 87-17
    Language: English
    Note: CONTENTS Abstract Preface Introduction Magnetic induction conductivity method Site description and survey methods Cross section field data and modeling results X6 X3A X4 Conclusions and recommendations Literature cited Appendix A: Discussion of errors Appendix B: Modeling data
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  • 15
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-81/27
    In: CRREL Report, 81-27
    Description / Table of Contents: Existing classifications for deposits in the glacial environment are inadequate and inconsistent. Deposits should be classified both descriptively and genetically; adequate descriptive classifications already exist. A major problem for previous genetic classifications has been that glacial deposition and the resulting deposits' properties were poorly understood. On the basis of three criteria-sediment source, uniqueness to the glacial environment, and preservation of glacier-derived properties-deposits in the glacial environment result from either of two groups of processes: primary or secondary. Primary processes release the debris of the glacier directly and form deposits that may bear properties related to the glacier and its mechanics. Their deposits are classified genetically as till and are the only deposits indicative of glaciation. In contrast, secondary processes mobilize, rework, transport and resediment debris and deposits in the glacial environment. They develop new, nonglacial properties in their deposits, while destroying or substantially modifying glacier-derived properties. Interpretation of their properties may provide information on the depositional are classified genetically according to the depositional process just as they are in other sedimentary environments. This genetic classification differs from previous classifications in that not all diamictons deposited in the glacial environment are classified as till; it is based strictly on process-related criteria. The origin of properties of glacial deposits in relation to the glacier's mechanics and environment must be recognized if the mechanisms and depositional processes of former glaciers are to be precisely understood.
    Type of Medium: Series available for loan
    Pages: iii, 16 Seiten , Illustrationen
    Series Statement: CRREL Report 81-27
    Language: English
    Note: CONTENTS Abstract Preface Introduction Criteria for process grouping Depositional processes Deposit groups-tills and nontills Comparison of melt-out and sediment flow Melt-out Sediment flow Classification of glacial deposits Conclusions Literature cited
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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-201-85/1
    In: CRREL Report, 85-1
    Description / Table of Contents: An expensive drill has been modified to provide researchers with the ability to auger an open hole or to acquire continuous, undisturbed 76-mm-diam core samples of a variety of perennially frozen materials that are suitable for chemical and petrographic analysis. It was developed by field testing in support of research from 1980 to 1983. Operation of the drill is based mainly on using a minimum of power to cut through frozen ground with tungsten carbide cutters on a CRREL coring auger. The ice content, temperature and grain size of the frozen sediments are important variables determining the sampling depth. Perennially frozen sediments with temperatures in the range of -0.5 C to -8.5 C have been continuously cored with this drill. Drilling and sampling are most efficiently conducted when ambient air temperatures are below freezing and the active layer is frozen. The self-contained lightweight drill is readily transportable off-road by helicopter or tracked vehicle, or by towing over roads. It is locally self-mobile by use of a winch. Total cost of the drill and modifications is estimated at approximately $10,000.
    Type of Medium: Series available for loan
    Pages: v, 34 Seiten , Illustrationen
    Series Statement: CRREL Report 85-1
    Language: English
    Note: CONTENTS Abstract Preface Introduction Background on development Drill development and configuration Equipment Modifications Operations Assembly and disassembly Field transport and movement Typical operating procedures Effect of material properties, weather and water Depth and hole completion time Summary Literature cited
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  • 17
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-79/9
    In: CRREL Report, 79-9
    Description / Table of Contents: Sedimentation at the terminus of the Matanuska Glacier has been found to be primarily subaerial in a 100- to 300-m wide, ice-cored zone paralleling the edge of the active ice. Certain physical and chemical characteristics of the ice and debris of the superglacial, englacial and basal zones of the glacier indicate the debris of the basal zone, the primary source of sediment, is entrained during freeze-on of meltwater, probably surficially derived, to the glacier sole. Till formation results from the melting of buried ice of the basal zone. Melt-out till inherits the texture and particle orientations of basal ice debris; other properties are not as well preserved. Most deposits result from resedimentation of till and debris by sediment gravity flows, meltwater sheet and rill flow, slump, spall, and ice ablation. Depositional processes are interrelated in the process of backwasting of ice-cored slopes. Sediment flows are the primary process of resedimentation. Their physical characteristics, multiple mechanisms of flow and deposition, and characteristics of their deposits vary with the water content of the flow mass. Deposits of each process are distinguished from one another by detailed analysis of their internal organization, geometry and dimensions, and the presence of other internal and related external features. Genetic facies are defined by these characteristics. The interrelationship of processes develops a composite depositional sequence defined in terms of genetic facies associations; an upper, resedimented facies association, a middile, till facies association, and a lower, subglacial-resedimental facies association. The lateral and vertical distribution of genetic facies within the associations is mainly nonrepetitive.
    Type of Medium: Series available for loan
    Pages: X, 112 Seiten , Illustrationen , 1 Beilage
    Series Statement: CRREL Report 79-9
    Language: English
    Note: CONTENTS Abstract Preface Summary Chapter 1. Introduction Field site Historical background Chapter 2. Characteristics of the debris and ice Characteristics of the facies and subfacies Basal zone Characteristics of the debris Discussion Chapter 3. Oxygen isotope analysis Sampling and analysis Results Discussion Chapter 4. Depositional processes—till formation Methods of analysis Environmental setting Till formation Chapter 5. Depositional processes—resedimentation Sediment flows Other resedimentation processes Resedimentation process relationships Chapter 6. Process distribution, sediment dispersal and depositional patterns Physical characteristics Sediment dispersal Sedimentary facies Patterns of terminus sedimentation Chapter 7. Conclusions Literature cited
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  • 18
    Monograph available for loan
    Monograph available for loan
    London : Belhaven Pr. [u.a.]
    Call number: AWI P5-92-0453
    Description / Table of Contents: The first book in Belhaven's new Polar Research Series, published in association with the Scott Polar Research Institute, University of Cambridge, offers a multidisciplinary examination of the historical record and the current developments surrounding Soviet activities and policies in their vast maritime arctic region. The book presents a range of issues in such diverse fields as history, environment, philosophy, law, oceanography, geology, marine transportation and strategic studies. Captain Brigham has brought together a unique group of experts, historians, geographers, polar scientists, legal specialists and environmentalists from North America, Europe and the USSR to provide a broad and up-to-date picture of this vast polar marine region. The book shows how huge resources and vital transport arteries of the polar north will become of increasing importance not only to the new Soviet Union but also to the entire northern hemisphere. The book is the first available in the West to present an integrated and authoritative view of the "last frontier" of the Soviet Union.
    Type of Medium: Monograph available for loan
    Pages: XV, 336 S. , Ill., graph. Darst., Kt. , 24 cm
    ISBN: 1852931698
    Series Statement: Polar Research Series [1]
    Note: Contents: List of figures. - List of tables. - Biographies of the Editor and Contributors. - List of acronyms. - Foreword / James M. Broadus. - Acknowledgements. - 1. Introduction / Lawson W. Brigham. - PART I EXPLORATION: PAST AND PRESENT. - 2. The Arctic Ocean in Russian history to 1945 / William Barr. - 3. The 1987 expedition of the icebreaker Sibir to the North Pole / Ivan Frolov. - PART II MAN AND THE NATURAL SETTING. - 4. Sea ice distribution in the Soviet Arctic / Donald Barnett. - 5 Environmental protection in the Soviet Arctic seas / Alexei Y. Roginko. - 6. The Arctic in the Russian identity / Franklyn Griffiths, Canada. - 7. Oil and gas resources in the offshore Soviet Arctic / James W. Clarke. - PART III. CHALLENGES OF MARINE AND RIVER TRANSPORT. - 8. Technical developments and the future of Soviet Arctic marine transportation / Lawson W. Brigham. - 9. Management of the Northern Sea Route: stages and problems of development / Alexander I. Arikaynen. - 10 Northern Sea Route operations in the 1986-7 Season / Terence Armstrong. - 11. Technical aspects of ice navigation and port construction in the Soviet Arctic / Gordon G. Watson. - 12 The Siberian rivers as a transport system / Robert N. North. - PART IV LEGAL AND GEOPOLITICAL PERSPECTIVES. - 13. The geostrategic conditions of deterrence in the Barents Sea / Willy Østreng. - 14. The legal regime of Soviet Arctic marine areas / William E. Butler. - 15. Canada-USSR Arctic Science Exchange Programme: An historical perspective of arctic cooperation / Walter Slipchenko. - 16. International cooperation in the Arctic: Soviet attitudes and actions / Oran R. Young and Gail Osherenko. - 17. A Comparison of Soviet Arctic and Antarctic policies / Christopher C. Joyner. - PART V APPENDICES. - Appendix I Excerpt on international arctic affairs/foreign policy taken from the speech in Murmansk by Mikhail S. Gorbachev, 1 October 1987. - Appendix II Decree of the Presidium of the Supreme Soviet of the USSR to improve the protection of nature in the regions of the far north and in the sea areas adjacent to the northern coastline of the USSR. - Appendix III Agreement between the government of Canada and the government of the Union of Soviet Socialist Republics on cooperation in the Arctic and the North. - Appendix IV USSR participation in selected international arrangements. - Index.
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  • 19
    Monograph available for loan
    Monograph available for loan
    Moskva : Nauka
    Call number: MOP B 18577
    Type of Medium: Monograph available for loan
    Pages: 229 S.
    Uniform Title: Solving least squared problems
    Language: Russian
    Location: MOP - must be ordered
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  • 20
    Keywords: geochemical techniques ; isotopic techniques ; hydrocarbon systems
    Description / Table of Contents: Geochemical applications in petroleum systems analysis: new constraints and the power of integration / M. Lawson, M. J. Formolo, L. Summa and J. M. Eiler / Geological Society, London, Special Publications, 468, 1-21, 19 February 2018, https://doi.org/10.1144/SP468.6 --- Source-rock identification and the temperature/timing of hydrocarbon generation --- The utility of methane clumped isotopes to constrain the origins of methane in natural gas accumulations / Daniel A. Stolper, Michael Lawson, Michael J. Formolo, Cara L. Davis, Peter M. J. Douglas and John M. Eiler / Geological Society, London, Special Publications, 468, 23-52, 14 December 2017, https://doi.org/10.1144/SP468.3 --- The isotopic structures of geological organic compounds / John M. Eiler, Matthieu Clog, Michael Lawson, Max Lloyd, Alison Piasecki, Camilo Ponton and Hao Xie / Geological Society, London, Special Publications, 468, 53-81, 14 December 2017, https://doi.org/10.1144/SP468.4 --- Vanadium isotope composition of crude oil: effects of source, maturation and biodegradation / Yongjun Gao, John F. Casey, Luis M. Bernardo, Weihang Yang and K. K. (Adry) Bissada / Geological Society, London, Special Publications, 468, 83-103, 14 December 2017, https://doi.org/10.1144/SP468.2 --- Carbon and hydrogen isotopic compositions of n-alkanes as a tool in petroleum exploration / Nikolai Pedentchouk and Courtney Turich / Geological Society, London, Special Publications, 468, 105-125, 14 December 2017, https://doi.org/10.1144/SP468.1 --- Mechanisms and time-scales associated with hydrocarbon migration, trapping, storage and alteration --- Noble gases in conventional and unconventional petroleum systems / David J. Byrne, P. H. Barry, M. Lawson and C. J. Ballentine / Geological Society, London, Special Publications, 468, 127-149, 14 December 2017, https://doi.org/10.1144/SP468.5 --- Differentiating between biogenic and thermogenic sources of natural gas in coalbed methane reservoirs from the Illinois Basin using noble gas and hydrocarbon geochemistry / Myles T. Moore, David S. Vinson, Colin J. Whyte, William K. Eymold, Talor B. Walsh and Thomas H. Darrah / Geological Society, London, Special Publications, 468, 151-188, 18 January 2018, https://doi.org/10.1144/SP468.8 --- The impact of fluid flow on reservoir properties --- Testing clumped isotopes as a reservoir characterization tool: a comparison with fluid inclusions in a dolomitized sedimentary carbonate reservoir buried to 2–4 km / John M. MacDonald, Cédric M. John and Jean-Pierre Girard / Geological Society, London, Special Publications, 468, 189-202, 14 December 2017, https://doi.org/10.1144/SP468.7
    Pages: Online-Ressource (208 Seiten) , Diagramme
    ISBN: 9781786203687
    Language: English
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