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  • 2010-2014  (52,618)
  • 1980-1984
  • 2014  (52,618)
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  • 2010-2014  (52,618)
  • 1980-1984
Year
  • 1
    Description / Table of Contents: The Caledonides are a major orogenic belt that stretches from the Arctic, through Scandinavia, East Greenland, Britain and Ireland into the Atlantic coast of North America. Following the break-up of Rodinia, the Caledonides formed in the Palaeozoic by the drifting of various continents and their eventual aggregation in the Silurian and Devonian. The orogen subsequently fragmented during the opening of the Atlantic Ocean. This volume brings together 25 papers presenting the results of modern research that investigates the orogenic processes and the provenance of specific components of the belt. The contributions reflect different lines of research, linking traditional field studies with modern analytical techniques. In addition three overview papers summarize the main features of the belts in Scandinavia, Svalbard, East Greenland, Britain and Ireland, highlighting the advances made since the last major synthesis of the Scandinavian Caledonides 30 years ago, and discussing important open questions.
    Pages: Online-Ressource (VI, 718 Seiten)
    ISBN: 9781862393776
    Language: English
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  • 2
    Monograph available for loan
    Monograph available for loan
    Princeton [u.a.] : Princeton University Press
    Call number: PIK B 030-15-0122
    Description / Table of Contents: Contents: Introduction ; I. Torts and Misalignments ; 1. Prices, Sanctions, and Discontinuities ; 2. The Injurer's Self-Risk Puzzle ; 3. Negligence Per Se and Unaccounted Risks ; 4. Lapses and Substitution ; 5. Total Liability for Excessive Harm ; II. Contracts and Victims' Incentives ; 6. Unity in the Law of Torts and Contracts ; 7. Anti-Insurance ; 8. Decreasing Liability Contracts and the Assistant Interest ; III. Restitution and Positive Externalities ; 9. A Public Goods Theory of Restitution ; 10. Liability Externalities and Mandatory Choices ; 11. The Relationship between Nonlegal Sanctions and Damages ; Conclusion
    Type of Medium: Monograph available for loan
    Pages: 232 S. : graph. Darst.
    ISBN: 9780691151595
    Location: A 18 - must be ordered
    Branch Library: PIK Library
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  • 3
    Monograph available for loan
    Monograph available for loan
    Cambridge : Cambridge University Press
    Call number: AWI G1-15-0007
    Description / Table of Contents: Flooding caused by a rise in global mean sea Ievel has the potential to affect the lives of more than 1 billion people in coastal areas worldwide. There have been significant changes in sea Ievel over the past 2 million years, both at the local and global scales, and a compIete understanding of natural cycles of change as well as anthropogenic effects is imperative for future global development. This book reviews the history of research into these sea-level changes and summanses the methods and analytical approaches used to interpret evidence for sea-level changes. lt provides an overview of the changing climates of the Ouaternary, examines the processes responsible for global variability of sea-level records, and presents detailed reviews of sea-level changes for the Pleistocene and Holocene. The book concludes by discussing current trends in sea Ievel and likely future sea level changes. This is an important and authoritative summary of evidence for sea-level changes in our most recent geological period, and provides a key resource for academic researchers, and graduate and advanced undergraduate students, working in tectonics, stratigraphy, geomorphology and physical geography, environmental science and other aspects of Quaternary studies.
    Type of Medium: Monograph available for loan
    Pages: XVIII, 484 S. : Ill., graph. Darst., Kt.
    Edition: 1. publ.
    ISBN: 9780521820837
    Note: Contents: Preface. - List of abbreviations. - 1. Sea-level changes: the emergence of a Quaternary perspective. - 1.1 Introduction. - 1.2 The Quaternary Period. - 1.3 Sea-Jevel changes: historical development of ideas. - 1.4 Observations from classical antiquity until the nineteenth century. - 1.4.1 Early Mediterranean studies. - 1.4.2 Eighteenth-century writings on universal changes to the Earth. - 1.4.3 Diluvial Theory - the universal flood. - 1.4.4 The Temple of Serapis: a compelling case for relative sea-level change. - 1.4.5 Lavoisier and the concepts of transgression and regression. - 1.5 Glacial action and recognition of the Ice Ages. - 1.5.1 Louis Agassiz and the Glacial Theory. - 1.5.2 The Croll-Milankovitch Hypothesis. - 1.6 Vertical changes in land and sea Ievel related to Quaternary climate. - 1.6.1 Charles Darwin and James Dana. - 1.6.2 Insights from around the world. - 1. 7 Evolution of ideas in the twentieth century. - 1. 7.1 Developments in Europe. - 1.7.2 Advances in geochemistry and geochronology. - 1.7.3 Oxygen-isotope records from marine sediments and ice cores. - 1.7.4 Geophysical models of sea-level changes. - 1.7.5 Sequence stratigraphy. - 1.7.6 International concern and a focus on current and future sea-level trends. - 1.8 Theoretical concepts relevant to the study of Quaternary sea-level changes. - 1.9 Synthesis and way forward. - 1.9.1 Revisiting old ideas. - 1.9.2 Quaternary sea-level changes: the status quo. - 2. The causes of Quaternary sea-level changes. - 2.1 Introduction. - 2.2 Sea Ievel and sea-level changes: some definitions. - 2.2.1 Sea Ievel and base Ievel. - 2.2.2 Relative sea-level changes. - 2.3 Processes responsible for relative sea-level changes in the Quaternary. - 2.3.1 Glacio-eustasy. - 2.3.2 lsostasy. - 2.3.3 Glacial isostasy and relative sea-Ievel changes. - 2.3.4 Hydro-isostasy and relative sea-level changes. - 2.3.5 The geoid and changes to its configuration. - 2.3.6 Global variation in geophysical response and equatorial ocean siphoning. - 2.4 Tectonism, volcanism, and other processes resulting in relative sea-level changes. - 2.4.1 Teetonic movements. - 2.4.2 Volcanism and its link to sea-level changes. - 2.4.3 Lithospheric flexure. - 2.4.4 Changes in tidal range. - 2.4.5 Steric changes, meteorological changes, and the role of ENSO events. - 2.5 Geophysical models and the sea-!evel equation. - 2.6 Synthesis and conclusions. - 3. Palaeo-sea-level indicators. - 3.1 Introduction. - 3.1.1 Fixed and relational sea-level indicators. - 3.1.2 Relative sea-level changes, sea-level index points, and indicative meaning. - 3.1.3 Sources of uncertainty in palaeo-sea-Ievel estimation. - 3.1.4 Palaeo-sea-level curve or envelope?. - 3.1.5 Facies architecture, allostratigraphy, and sea-level changes. - 3.2 Pleistocene and Holocene palaeo-sea-level indicators compared. - 3.3 Corals and coral reefs. - 3.3.1 Reefs and Pleistocene sea Ievels. - 3.3.2 Reefs and Holocene sea Ievels. - 3.3.3 Conglomerates and recognition of in-situ corals. - 3.3.4 Microatolls. - 3.4 Other biological sea-level indicators. - 3.4.1 Fixed biological indicators. - 3.4.2 Mangroves. - 3.4.3 Salt-marsh sediments and microfossil analysis. - 3.4.4 Seagrass. - 3.4.5 Marine molluscs. - 3.4.6 Submerged forests. - 3.5 Geomorphological and geological sea-level indicators. - 3.5.1 Marine terraces and shore platforms. - 3.5.2 Shoreline notches and visors. - 3.5.3 Isolation basins. - 3.5.4 Beach ridges. - 3.5.5 Cheniers. - 3.5.6 Aeolianites. - 3.5.7 Calcretes. - 3.5.8 Beachrock. - 3.6 Geoarchaeology and sea-level changes. - 3.7 Synthesis and conclusions. - 4. Methods of dating Quaternary sea-level changes. - 4.1 Introduction. - 4.1.1 Terminology. - 4.1.2 Historical approaches used for evaluating geological age of coastal deposits. - 4.2 Radiocarbon dating. - 4.2.1 Underlying principles of the radiocarbon method. - 4.2.2 Age range. - 4.2.3 Measurement techniques. - 4.2.4 Isotopic fractionation. - 4.2.5 Marine reservoir and hard-water effects. - 4.2.6 Secular 14C/ 12C variation and the calibration of radiocarbon ages to sidereal years. - 4.2.7 Cantamination and sample pre-treatment strategies. - 4.2.8 Statistical considerations: comparisons of radiocarbon age and pooling of results. - 4.3 Uranium-series disequilibrium dating. - 4.3.1 Underlying principles of U-series disequilibrium dating. - 4.3.2 U-series dating of marine carbonates. - 4.3.3 U-series dating of other materials. - 4.4 Oxygen-isotope stratigraphy. - 4.5 Luminescence dating methods. - 4.5.1 Quantifying the cumulative effects of environmental radiation dose. - 4.5.2 Age range of luminescence methods. - 4.5.3 Anomalaus fading and partial bleaching. - 4.6 Electron spin resonance dating. - 4.7 Amino acid racemisation dating. - 4.7.1 The amino acid racemisation reaction. - 4.7.2 Environmental factors that influence racemisation. - 4.7.3 Sources of uncertainty in AAR dating. - 4.7.4 Application of AAR to dating coastal successions. - 4.8 Cosmogenic dating. - 4.9 Other dating techniques. - 4.9.1 Event markers. - 4.9.2 Palaeomagnetism. - 4.10 Synthesis and conclusions. - 5 Vertical displacement of shorelines. - 5.5.1 Introduction. - 5.2 Plate tectonics and implications for coastlines globally. - 5.2.1 Lithospheric plate domains. - 5.2.2 Plate margins. - 5.2.3 Plate tectonics and coastal classification. - 5.2.4 Ocean plate dynamics and island types. - 5.3 Styles of tectonic deformation and rates of uplift or subsidence. - 5.3.1 Coseismic uplift. - 5.3.2 Epeirogenic uplift. - 5.3.3 Folding and warping. - 5.3.4 Isostasy. - 5.3.5 Lithospheric flexure. - 5.3.6 Mantle plumes. - 5.3.7 Subsidence and submerged shorelines. - 5.4 The last interglacial shoreline: a reference for quantifying vertical displacement. - 5.4.1 Terrace age and elevation. - 5.4.2 Constraints on using the last interglacial shoreline as a benchmark. - 5.5 Coastlines in tectonically 'stable' cratonic regions. - 5.5.1 Australia. - 5.5.2 Southern Africa. - 5.6 Coastlines of emergence. - 5.6.1 Huon Peninsula. - 5.6.2 Barbados. - 5.6.3 Convergent continental margins: Chile. - 5.7 Vertical crustal movements associated with glacio-isostasy: Scandinavia. - 5.8 The Mediterranean Basin . - 5.8.1 Italy. - 5.8.2 Greece. - 5.9 The Caribbean region. - 5.9.1 Southern Florida and the Bahamas. - 5.9.2 Other Caribbean sites and more tectonically active islands. - 5.10 Divergent spreading-related coastlines: Red Sea. - 5.11 Pacific Plate. - 5.11.1 Pacific islands. - 5.11.2 Hawaii. - 5.11.3 Japan. - 5.11.4 New Zealand. - 5.12 Synthesis and conclusions. - 6. Pleistocene sea-level changes. - 6.1 Introduction. - 6.2 Prelude to the Pleistocene. - 6.3 Pleistocene icesheets. - 6.4 Early Pleistocene sea Ievels. - 6.4.1 Roe Calcarenite, Roe Plains, southern Australia. - 6.4.2 The Crag Group, southeastern England. - 6.S The middle Pleistocene Transition. - 6.6 Middle Pleistocene sea-level changes. - 6.7 Sea-level highstands of the middle Pleistocene. - 6.7.1 Marine Isotope Stage 11. - 6.7.2 Marine Isotope Stage 9 - the pre-penultimate interglacial. - 6.7.3 Marine Isotope Stage 7 - the penultimate interglacial. - 6.8 Middle Pleistocene sea-level lowstands. - 6.9 Late Pleistocene sea-level changes. - 6.9.1 The last interglacial maximum (MIS 5e). - 6.9.2 Timing and duration of the last interglacial maximum. - 6.9.3 Global estimates of last interglacial sea Ievels - the sanctity of the 6 m APSL datum?. - 6.10 Interstadial sea Ievels of the last glacial cycle (MIS 5c and 5a). - 6.11 Interstadial sea Ievels during MIS 3. - 6.12 Late Pleistocene interstadial sea Ievels: Dansgaard-Oeschgerand Heinrich Events. - 6.13 Eustatic sea Ievels during the Last Glacial Maximum (MIS 2). - 6.14 Long records of Pleistocene sea-level highstands. - 6.14.1 Coorong Coastal Plain and Murray Basin, southern Australia. - 6.14.2 Wanganui Basin, New Zealand. - 6.14.3 Sumba Island, Indonesia. - 6.15 Synthesis and conclusions. - 7. Sea-level changes since the Last Glacial Maximum. - 7.1 Introduction. -
    Branch Library: AWI Library
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  • 4
    Call number: PIK B 190-12-0174(2014,05)
    In: Working paper
    Description / Table of Contents: Contents: 1. Introduction ; 2. Background and related empirical literature ; 3. Data description and methodology ; 4. Empirical results ; 5. Conclusions
    Type of Medium: Monograph available for loan
    Pages: III, 27 S.
    Series Statement: Working paper 05/2014
    Location: A 18 - must be ordered
    Branch Library: PIK Library
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  • 5
    Unknown
    West Lafayette, Indiana : Purdue University Press
    Keywords: energy policy ; energy crisis ; climate change ; global warming ; alternative energy
    Description / Table of Contents: We are facing a global energy crisis caused by world population growth, an escalating increase in demand, and continued dependence on fossil-based fuels for generation. It is widely accepted that increases in greenhouse gas concentration levels, if not reversed, will result in major changes to world climate with consequential effects on our society and economy. This is just the kind of intractable problem that Purdue University’s Global Policy Research Institute seeks to address in the Purdue Studies in Public Policy series by promoting the engagement between policy makers and experts in fields such as engineering and technology. Major steps forward in the development and use of technology are required. In order to achieve solutions of the required scale and magnitude within a limited timeline, it is essential that engineers be not only technologically-adept but also aware of the wider social and political issues that policy-makers face. Likewise, it is also imperative that policy makers liaise closely with the academic community in order to realize advances. This book is designed to bridge the gap between these two groups, with a particular emphasis on educating the socially-conscious engineers and technologists of the future. In this accessibly-written volume, central issues in global energy are discussed through interdisciplinary dialogue between experts from both North America and Europe. The first section provides an overview of the nature of the global energy crisis approached from historical, political, and sociocultural perspectives. In the second section, expert contributors outline the technology and policy issues facing the development of major conventional and renewable energy sources. The third and final section explores policy and technology challenges and opportunities in the distribution and consumption of energy, in sectors such as transportation and the built environment. The book’s epilogue suggests some future scenarios in energy distribution and use.
    Pages: Online-Ressource (XIV, 304 Seiten)
    Edition: Knowledge Unlatched Open Access Edition
    ISBN: 9781612493091
    Language: English
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  • 6
    Description / Table of Contents: This volume addresses the challenges facing explorers and developers alike in a region that is becoming a major focus of the petroleum industry in the United Kingdom, Faroes and North Norway. Several West of Shetland fields are still in the appraisal phase almost a decade after discovery. Sub-volcanic exploration risks remain high: sub-volcanic structural traps are imaged poorly, and so the geophysical community is responding with the application of latest technology. The more simple reservoirs might not be large enough to prompt informed and speedy development decisions; larger fields might have a combination of complexities, requiring a phased approach to the development. Infrastructure has been slow to arrive and planned developments have been subject to dramatic swings in fiscal regime ranging from special allowances to unexpected tax increases. Environmental challenges are significant when moving into more remote, deeper water. The perception of these challenges by the third parties has become much more acute. To sustain its right to operate, the industry has to demonstrate safe drilling operations and appropriate response capability with government agencies.
    Pages: Online-Ressource (229 Seiten)
    ISBN: 9781862396523
    Language: English
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  • 7
    Keywords: fractured reservoirs; hydrocarbon resources
    Description / Table of Contents: Advances in the study of naturally fractured hydrocarbon reservoirs: a broad integrated interdisciplinary applied topic / Guy H. Spence, Gary D. Couples, Tim G. Bevan, Roberto Aguilera, John W. Cosgrove, Jean-Marc Daniel and Jonathan Redfern / Geological Society, London, Special Publications, 374, 1-22, 9 July 2014, https://doi.org/10.1144/SP374.19 --- Investigating fracture networks using outcrop, core and geophysical data --- Sedimentological controls on the fracture distribution and network development in Mesaverde Group sandstone lithofacies, Uinta Basin, Utah, USA / Ryan Sonntag, James P. Evans, Paul La Pointe, Meagan Deraps, Hope Sisley and David Richey / Geological Society, London, Special Publications, 374, 23-50, 10 September 2012, https://doi.org/10.1144/SP374.4 --- Comparison of digital outcrop and conventional data collection approaches for the characterization of naturally fractured reservoir analogues / Thomas D. Seers and David Hodgetts / Geological Society, London, Special Publications, 374, 51-77, 19 April 2013, https://doi.org/10.1144/SP374.13 --- Fault linkage and damage zone architecture in tight carbonate rocks in the Suez Rift (Egypt): implications for permeability structure along segmented normal faults / A. Rotevatn and E. Bastesen / Geological Society, London, Special Publications, 374, 79-95, 10 September 2012, https://doi.org/10.1144/SP374.12 --- Quantifying fracture density and connectivity of fractured chalk reservoirs from core samples: implications for fluid flow / D. A. Sagi, M. Arnhild and J. F. Karlo / Geological Society, London, Special Publications, 374, 97-111, 26 June 2013, https://doi.org/10.1144/SP374.16 --- Characterizing discontinuities in naturally fractured outcrop analogues and rock core: the need to consider fracture development over geological time / S. R. Hencher / Geological Society, London, Special Publications, 374, 113-123, 9 May 2013, https://doi.org/10.1144/SP374.15 --- Numerical and statistical simulations and models --- What can we learn from high-resolution numerical simulations of single- and multi-phase fluid flow in fractured outcrop analogues? / Sebastian Geiger and Stephan Matthäi / Geological Society, London, Special Publications, 374, 125-144, 5 September 2012, https://doi.org/10.1144/SP374.8 --- Geomechanical impacts on flow in fractured reservoirs / Gary D. Couples / Geological Society, London, Special Publications, 374, 145-172, 25 June 2013, https://doi.org/10.1144/SP374.17 --- Geomechanical mechanisms involving faults and fractures for observed correlations between fluctuations in flowrates at wells in North Sea oilfields / Kes J. Heffer / Geological Society, London, Special Publications, 374, 173-186, 28 August 2012, https://doi.org/10.1144/SP374.2 --- Fluid flow through porous sandstone with overprinting and intersecting geological structures of various types / Xiaoxian Zhou, Mohammad Karimi-Fard, Louis J. Durlofsky and Atilla Aydin / Geological Society, London, Special Publications, 374, 187-209, 14 March 2013, https://doi.org/10.1144/SP374.11 --- Influences of nodular chert rhythmites on natural fracture networks in carbonates: an outcrop and two-dimensional discrete element modelling study / Guy H. Spence and Emma Finch / Geological Society, London, Special Publications, 374, 211-249, 7 March 2014, https://doi.org/10.1144/SP374.18 --- Sills as fractured hydrocarbon reservoirs: examples and models / Agust Gudmundsson and Ingrid F. Løtveit / Geological Society, London, Special Publications, 374, 251-271, 10 September 2012, https://doi.org/10.1144/SP374.5 --- A methodology to characterize fractured reservoirs constrained by statistical geological analysis and production: a real field case study / Matthieu Delorme, Rosane Oliveira Mota, Nina Khvoenkova, André Fourno and Benoit Nœtinger / Geological Society, London, Special Publications, 374, 273-288, 29 July 2013, https://doi.org/10.1144/SP374.14 --- Case studies --- Characterization of highly fractured basement, Say'un Masila Basin, Yemen / Ann Murray and David W. Montgomery / Geological Society, London, Special Publications, 374, 289-310, 27 July 2012, https://doi.org/10.1144/SP374.1 --- Characterizing seismic-scale faults pre- and post-drilling; Lewisian Basement, West of Shetlands, UK / Clare Slightam / Geological Society, London, Special Publications, 374, 311-331, 11 September 2012, https://doi.org/10.1144/SP374.6 --- Integration of outcrop and subsurface data during the development of a naturally fractured Eocene carbonate reservoir at the East Ras Budran concession, Gulf of Suez, Egypt / William Bosworth, Samir Khalil, Alan Clare, Joe Comisky, Hany Abdelal, Tom Reed and George Kokkoros / Geological Society, London, Special Publications, 374, 333-360, 31 July 2012, https://doi.org/10.1144/SP374.3 --- The Machar Oil Field, UK Central North Sea: impact of seismic reprocessing on the development of a complex fractured chalk field / M. V. Ward, C. Pearse, Y. Jehanno, M. O'Hanlon, A. Zett and D. Houliston / Geological Society, London, Special Publications, 374, 361-377, 17 October 2012, https://doi.org/10.1144/SP374.10 --- Dual-porosity fractured Miocene syn-rift dolomite reservoir in the Issaran Field (Gulf of Suez, Egypt): a case history of the zonal isolation of highly fractured water carrier bed / Ati Saoudi, Adel R. Moustafa, Ramadan I. Farag, Maher M. Omara, Hossam Wally, Ahmed Fouad, Amr Tag and Ramy Z. Ragab / Geological Society, London, Special Publications, 374, 379-394, 5 September 2012, https://doi.org/10.1144/SP374.7 --- The importance of natural fractures in a tight reservoir for potential CO2 storage: a case study of the upper Triassic–middle Jurassic Kapp Toscana Group (Spitsbergen, Arctic Norway) / K. Ogata, K. Senger, A. Braathen, J. Tveranger and S. Olaussen / Geological Society, London, Special Publications, 374, 395-415, 10 September 2012, https://doi.org/10.1144/SP374.9
    Pages: Online-Ressource (VI, 425 Seiten) , Illustrationen, Diagramme, Karten
    ISBN: 9781862396609
    Language: English
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  • 8
    Description / Table of Contents: There is considerable academic and practical interest in stone and stone buildings, as exemplified by the wide range of high-quality and innovative work being conducted in the pursuit of the effective preservation and restoration of historic buildings. This is reflected in the numerous publications on stone and stone buildings that regularly find their way into the public domain. Not least amongst these are a number of Geological Society Special Publications, which have appeared in recent years. This current volume seeks to bring to the attention of the various professionals in the field (geologists, architects, engineers, conservators and conservation scientists) recent work centred on the characterization and performance of this important resource and its use in historic buildings. The volume has wider relevance, including to those interested in the heritage of stone.
    Pages: Online-Ressource (VII, 200 Seiten)
    ISBN: 9781862393769
    Language: English
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  • 9
    Call number: 9/M 07.0421(409)
    In: Geological Society special publication
    Type of Medium: Monograph available for loan
    Pages: 277 S. , Ill., graph. Darst., Kt.
    ISBN: 9781862396883
    Series Statement: Geological Society special publication 409
    Classification:
    Sedimentology
    Note: Ernie Rutter has made, and continues to make, a significant impact in the field of rock deformation. He has studied brittle and plastic deformation processes that occur within both the oceanic and continental crust, as well as other key properties such as the permeability and seismic velocities of these rocks. His approach has been one that integrates field observations, laboratory experiments and theoretical analyses. This volume celebrates Ernie's key contribution to rock deformation and structural geology by bringing together a collection of papers that represent this broad approach. The papers within the volume address key issues that remain within these fields. These range from fundamental studies of brittle and plastic behaviour along with the resultant structures and microstructures from both the field and laboratory, to applied problems where a better understanding of the deformation and properties of the crust is still needed.
    Location: Reading room
    Branch Library: GFZ Library
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  • 10
    Description / Table of Contents: Arsenic is perhaps history’s favorite poison, often termed the "King of Poisons" and the "Poison of Kings" and thought to be the demise of fiction’s most famous ill-fated lovers. The toxic nature of arsenic has been known for millennia with the mineral realgar (AsS), originally named “arsenikon” by Theophrastus in 300 B.C.E. meaning literally "potent." For centuries it has been used as rat poison and as an important component of bactericides and wood preservatives. Arsenic is believed to be the cause of death to Napoleon Bonaparte who was exposed to wallpaper colored green from aceto-arsenite of copper (Aldersey-Williams 2011). The use of arsenic as a poison has been featured widely in literature, film, theatre, and television. Its use as a pesticide made it well known in the nineteenth century and it was exploited by Sir Arthur Conan Doyle in the Sherlock Holmes novel The Golden Pince-Nez (Conan-Doyle 1903). The dark comedy Arsenic and Old Lace is a prime example of arsenic in popular culture, being first a play but becoming famous as a movie. Arsenic has figured prominently not only in fiction but in historical crimes as well (Kumar 2010). A high profile case of the mid-nineteenth century involved a hydrotherapist, Dr. Thomas Smethurst, who was accused of using arsenic to poison a woman he had befriended (Wharton 2010). Based on analytical evidence from a renowned toxicologist, Alfred Swaine Taylor, a death sentence was imposed, however Taylor had to confess that his apparatus was contaminated. The verdict was overturned after public opinion was voiced against it and a plea for clemency was made to Queen Victoria. In recent years, arsenic has been recognized as a widespread, low-level, natural groundwater contaminant in many parts of the world, particularly in places such as West Bengal and Bangladesh, where it has given rise to chronic human-health issues. Long-term exposure to arsenic has been shown to cause skin lesions, blackfoot disease, and cancer of the skin, bladder, and lungs, and is also associated with developmental effects, cardiovascular disease, neurotoxicity, and diabetes (WHO 2012). Arsenate’s toxicity is caused by its close chemical similarities to phosphate; it uses a phosphate transport system to enter cells. Arsenic occurs in many geological environments including sedimentary basins, and is particularly associated with geothermal waters and hydrothermal ore deposits. It is often a useful indicator of proximity to economic concentrations of metals such as gold, copper, and tin, where it occurs in hydrothermally altered wall rocks surrounding the zones of economic mineralization. Arsenic is commonly a persistent problem in metal mining and there has been significant effort to manage and treat mine waste to mitigate its environmental impacts. This volume compiles and reviews current information on arsenic from a variety of perspectives, including mineralogy, geochemistry, microbiology, toxicology, and environmental engineering. The first chapter (Bowell et al. 2014) presents an overview of arsenic geochemical cycles and is followed by a chapter on the paragenesis and crystal chemistry of arsenic minerals (chapter 2; Majzlan et al. 2014). The next chapters deal with an assessment of arsenic in natural waters (chapter 3; Campbell and Nordstrom 2014) and a review of thermodynamics of arsenic species (chapter 4; Nordstrom et al. 2014). The next two chapters deal with analytical measurement and assessment starting with measuring arsenic speciation in solids using x-ray absorption spectroscopy (chapter 5; Foster and Kim 2014). Chapter 6 (Leybourne and Johannesson 2014) presents a review on the measurement of arsenic speciation in environmental media: sampling, preservation, and analysis. In chapter 7 (Amend et al. 2014) there is a review of microbial arsenic metabolism and reaction energetics. This is followed by an overview of arsenic toxicity and human health issues (chapter 8; Mitchell 2014) and an assessment of methods used to characterize arsenic bioavailability and bioaccessibility (chapter 9; Basta and Jurasz 2014). This leads into chapter 10 (Craw and Bowell 2014), which describes the characterization of arsenic in mine waste with some examples from New Zealand, followed by a chapter on the management and treatment of arsenic in mining environments (chapter 11; Bowell and Craw 2014). The final three chapters are in-depth case studies of the geochemistry and mineralogy of legacy arsenic contamination in different historical mining environments: the Giant gold mine in Canada (chapter 12; Jamieson 2014), the Sierra Nevada Foothills gold belt of California (chapter 13; Alpers et al. 2014), and finally, the hydrogeochemistry of arsenic in the Tsumeb polymetallic mine in Namibia (chapter 14; Bowell 2014).
    Pages: Online-Ressource (xvi ; 635 Seiten)
    ISBN: 9780939950942
    Language: English
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