ALBERT

Description / Table of Contents: This handbooks series aims to integrate knowledge of communication structures and processes. It is global in orientation, dedicated to cultural and epistemological diversity as well as different scholarly approaches. The series features volumes on 'messages, codes and channels', 'mode of address: communication situations and context', 'methodology in communication science' and 'application areas'. The latter features volumes devoted to a large range of specialist areas of communication science. The series as a whole aims at meeting the needs of undergraduates, postgraduates, academics and researchers across the area of communication studies.

Description / Table of Contents: The book summarizes the knowledge and experiences concerning the role of halogens during various geochemical processes, such as diagenesis, ore-formation, magma evolution, metasomatism, mineralization, and metamorphism in the crust and mantle of the Earth. It comprises the role of halogens in other terrestrial worlds like volatile-rich asteroids, Mars, and the ice moons of Jupiter and Saturn. Review chapters outline and expand upon the basis of our current understanding regarding how halogens contribute to the geochemical/geophysical evolution and stability of terrestrial worlds overall.

Description / Table of Contents: This work summarizes the historical progression of the field of lithium (Li) isotope studies and provides a comprehensive yet succinct overview of the research applications toward which they have been directed. In synthesizing the historical and current research, the volume also suggests prospective future directions of study. Not even a full decade has passed since the publication of a broadly inclusive summary of Li isotope research around the globe (Tomascak, 2004). In this short time, the use of this isotope system in the investigation of geo- and cosmochemical questions has increased dramatically, due, in part, to the advent of new analytical technology at the end of the last millennium. Lithium, as a light element that forms low-charge, moderate-sized ions, manifests a number of chemical properties that make its stable isotope system useful in a wide array of geo- and cosmochemical research fields.  

Description / Table of Contents: Section I: The Data 1. Who Receives a Geoscience Degree? 2. We are the 20%: Updated Statistics on Female Faculty in Earth Sciences in the U.S Section II: A Framework to Address the Issue 3. A Sociological Framework to Address Gender Parity. Section III: Successful Strategies to Address the Issue 4. Best Practices to Achieve Gender Parity: Lessons Learned from NSF s ADVANCE and Similar Programs. III. A: Institutional Strategies 5. Strategic Institutional Change to Support Advancement of Women Scientists in the Academy: Initial Lessons from a Study of ADVANCE IT Projects 6. Institutional Transformation: The Lamont Doherty Earth Observatory Experience 7. Dual Career, Flexible Faculty 8. Lactation in the Academy: Accommodating

Description / Table of Contents: Geofluids : Developments in Microthermometry, Spectroscopy, Thermodynamics, and Stable Isotopes is the definitive source on paleofluids and the migration of hydrocarbons in sedimentary basins-ideal for researchers in oil and gas exploration. There's been a rapid development of new non-destructive analytical methods and interdisciplinary research that makes it difficult to find a single source of content on the subject of geofluids. Geoscience researchers commonly use multiple tools to interpret geologic problems, particularly if the problems involve fluid-rock interaction. This book perfectly combines the techniques of fluid inclusion microthermometry, stable isotope analyses, and various types of spectroscopy, including Raman analysis, to contribute to a thorough approach to research. Through a practical and intuitive step-by-step approach, the authors explain sample preparation, measurements, and the interpretation and analysis of data related to thermodynamics and mineral-fluid equilibria.* Features working examples in each chapter with step-by-step explanations and calculations* Broad range of case studies aid the analytical and experimental data* Includes appendices with equations of state, stable isotope fractionation equations, and Raman identification tables that aid in identification of fluid inclusion minerals* Authored by a team of expert scientists who have more than 60 years of related experience in the field and classroom combined

Description / Table of Contents: This Special Publication will be an important tool for geoscientists, aimed at increasing the awareness of their societal role and responsibility in conducting education, research and practice activities.What are the responsibilities of a geoscientist ? And what motivations are needed to push geoscientists to practice the Earth sciences in an ethical way?The major environmental challenges affecting human communities require not only a strictly scientific and technical preparation by the geoscientists, but also a reflection on their broader obligations towards society. It is important that geoscientists consider geoethics as an indispensable framework on which to base their training and activity. The principles of geoethics can guide them to pursue the common good by weighing the benefits and costs of each choice, and identifying eco-friendly and society-friendly solutions that guarantee the respect of the right balance between human life and the dynamics of the Earth.Communication and dissemination of geosciences should become core activities in building a knowledge-based society, which is able better to protect itself and the Earth ecosystems in order to guarantee a life in harmony with our planet for future generations.

Description / Table of Contents: Rund 70 Milliarden Euro werden in Deutschland jährlich für Forschung und Entwicklung ausgegeben. Dennoch gelingt es nicht immer, die gewonnenen Erkenntnisse in erfolgreiche Innovationen umzusetzen.Das Praxishandbuch Technologietransfer stellt neun innovative Methoden und Ansätze vor, die neue Impulse für den Erkenntnis- und Technologietransfer aus der wissenschaftlichen Forschung in die industrielle Anwendung geben. Ein Expertenteam aus verschiedenen Institutionen stellt die Methoden anschaulich vor, gibt Tipps für ihre praktische Anwendung und zeigt Wege zu ihrer Implementierung.Das Buch richtet sich an Mitarbeiter in Technologietransferstellen, Verantwortliche in wissenschaftlichen Instituten, bei Projektträgern und Förderinstitutionen, an Wissenschaftler, die selbst aktiv Transfer betreiben, und an Gatekeeper und Schnittstellenverantwortliche in Unternehmen.

Description / Table of Contents: This book provides a comprehensive introduction to the field of geochemistry. The book first lays out the 'geochemical toolbox': the basic principles and techniques of modern geochemistry, beginning with a review of thermodynamics and kinetics as they apply to the Earth and its environs. These basic concepts are then applied to understanding processes in aqueous systems and the behavior of trace elements in magmatic systems. Subsequent chapters introduce radiogenic and stable isotope geochemistry and illustrate their application to such diverse topics as determining geologic time, ancient climates, and the diets of prehistoric peoples. The focus then broadens to the formation of the solar system, the Earth, and the elements themselves. Then the composition of the Earth itself becomes the topic, examining the composition of the core, the mantle, and the crust and exploring how this structure originated. A final chapter covers organic chemistry, including the origin of fossil fuels and the carbon cycle's role in controlling Earth's climate, both in the geologic past and the rapidly changing present.

Description / Table of Contents: Die Festschrift zum zehnjährigen Bestehen der Abteilung Forschung und Entwicklung (F&E) der Niedersächsischen Staats- und Universitätsbibliothek Göttingen in 2012 resümiert entlang ausgewählter Meilensteine die Arbeit im vergangenen Jahrzehnt. Dabei begibt sie sich auf die Spuren des Wandels im Leitbild wissenschaftlicher Bibliotheken. Gemeinsam mit Partnern aus der Wissenschaft wurden zahlreiche, wegweisende Projekte auf dem Gebiet der digitalen Forschung vorangebracht. Dieser Pionierarbeit in der deutschen Bibliothekslandschaft wird in 19 Aufsätzen von über 30 Autorinnen und Autoren nachgegangen.

Description / Table of Contents: Provides detailed advice about how to land a good scientist job, win funding, and shape the public debate. This title argues that marketing is a critical component of the modern scientific endeavour, not only advancing personal careers but also society's knowledge. It approaches marketing as a science in itself.It's a tough time to be a scientist: universities are shutting science departments, funding organisations are facing flat budgets, and many newspapers have dropped their science sections altogether. But according to Marc Kuchner, this anti-science climate doesn't have to equal a career death knell - it just means scientists have to be savvier about promoting their work and themselves. In "Marketing for Scientists", he provides clear, detailed advice about how to land a good job, win funding, and shape the public debate. As an astrophysicist at NASA, Kuchner knows that "marketing" can seem like a superficial distraction, whether your daily work is searching for new planets or seeking a cure for cancer. In fact, he argues, it's a critical component of the modern scientific endeavour, not only advancing personal careers but also society's knowledge. Kuchner approaches marketing as a science in itself. He translates theories about human interaction and sense of self into methods for building relationships - one of the most critical skills in any profession.And he explains how to brand yourself effectively - how to get articles published, give compelling presentations, use social media like Facebook and Twitter, and impress potential employers and funders.

Description / Table of Contents: Contents: Foreword 1. Spatial Science and Its Traditions 2. Literature Reviews 3. Research Questions 4. Data and Methods in Spatial Science 5. Graduate Degree Proposals 6. Grants and Grant Writing 7. Disseminating Research 8. Reflections on Proposal Writing in Spatial Science 9. Model Proposals 10. Thesis I: Human Systems 11. Thesis II: Human Systems-Mixed Methods 12. Dissertation I: Human-Environment Interactions 13. Dissertation II: Geo-Techniques 14. Dissertation III: Physical Systems 15. Extramural Grant I: Collaborative Research and Outreach 16. Extramural Grant II: Instrumentation 17. Extramural III: Doctoral Dissertation Research Improvement Grant 18. Intramural Grants Index

Description / Table of Contents: An essential guide for succeeding in today's competitive environment, this book provides beginning scientists and experienced researchers with practical advice on writing about their work and getting published. This new, updated edition discusses the latest print and Internet resources. Preparing, submitting and publishing scientific papers is now largely electronic, and the book has been revised to reflect this. New material includes more information on including supplementary material online, using reference management software, and preparing tables and figures; expanded sections on structuring a discussion section and the strengths and limitations of the research; and additional material on international aspects of scientific writing. The book guides readers through the processes involved in writing and publishing for scientific journals, from choosing a suitable journal to presenting results and citing references. It covers ethical issues in scientific publishing; explains rights and permissions; and discusses writing grant proposals, giving presentations and writing for general audiences.

Description / Table of Contents: Nicht erst seit Beginn des 21. Jahrhunderts stehen Neue Technologien im Fokus der Öffentlichkeit. Von der Kernenergie über die Mikroelektronik bis hin zur Bio- und Nanotechnologie und dem Internet scheinen sie die Möglichkeitshorizonte moderner Gesellschaften zu definieren.Die Debatten um Neue Technologien erlauben deshalb Einblick in zentrale gesellschaftliche Interessenlagen, Konfliktlinien und Entwicklungsdynamiken. Anhand konkreter Beispiele beleuchtet dieser Band den meist in forschungs- und innovationspolitischen Kontexten verwendeten Begriff Neue Technologien in soziologischer und historischer Perspektive.

Description / Table of Contents: Contents: Chapter 1. Metabolic Synthesis Chapter 2. Chemical Biomarker Applications to Ecology and Paleoecology Chapter 3. Stable Isotopes and Radiocarbon Chapter 4. Analytical Chemical Methods and Instrumentation Chapter 5. Carbohydrates: Neutral and Minor Sugars Chapter 6. Proteins: Amino Acids and Amines Chapter 7. Nucleic Acids and Molecular Tools Chapter 8. Lipids: Fatty Acids Chapter 9. Isoprenoid Lipids: Steroids, Hopanoids, and Triterpenoids Chapter 10. Lipids: Hydrocarbons Chapter 11. Lipids: Alkenones, Polar Lipids, and Ether Lipids Chapter 12. Photosynthetic Pigments: Chlorophylls, Carotenoids, and Phycobilins Chapter 13. Lignins, Cutins, and Suberins Chapter 14. Anthropogenic Markers Appendix I. Atomic Weights of Elements Appendix II. Useful SI Units and Conversion Factors Appendix III. Physical and Chemical Constants Glossary Bibliography

Description / Table of Contents: Scientific Writing and Communication: Papers, Proposals, and Presentations covers all the areas of scientific communication that a scientist needs to know and to master to successfully promote his or her research and career. This unique "all-in-one" handbook begins with a discussion of the basics of scientific writing style and composition and then applies these principles to writing research papers, review articles, grant proposals, research statements, and resumes as well as to preparing academic presentations and posters. FEATURES: A practical presentation carefully introduces such basic writing mechanics as word choice and word location, sentence structure, and paragraph organization before moving into manuscript planning and organizational strategies. Extensive hands-on guidance for composing scientific documents and presentations then follows. Relevant and multi-disciplinary examples taken from real research papers and grant proposals by writers ranging from students to Nobel Laureates illustrate clear technical writing as well as common mistakes that one should avoid.Examples are drawn from a broad range of scientific disciplines including medicine, molecular biology, biochemistry, ecology, geology, chemistry, engineering, and physics. Extensive end-of-chapter exercise sets provide the opportunity to review style and composition principles and encourage readers to apply them to their own writing. Writing guidelines and revision checklists warn scientists against common pitfalls and equip them with the most successful techniques to revise a scientific paper, review article, or grant proposal. Annotated text passages bring the writing principles and guidelines to life by applying them to real-world, relevant, and multidisciplinary examples. Clear, easy-to-follow writing style is understandable to both native and non-native English speakers; special ESL features address problems faced by non-native English speakers. Eight chapters on grant writing demonstrate how to write successful grant applications and how to avoid the most common application mistakes.Covering all the facets of communication that scientists need to master, Scientific Writing and Communication: Papers, Proposals, and Presentations is ideal for a wide range of readers--from upper-level undergraduates and graduate students to postdoctoral fellows, faculty, and professional researchers--in the life sciences, medicine, psychology, chemistry, and engineering.

Description / Table of Contents: "This is a hands-on guide for graduate students and other young researchers wishing to perfect the practical skills that are needed for a successful career in research. By teaching junior scientists to develop effective research habits, the book helps make the experience of graduate study a more efficient, effective and rewarding one. Many graduate students learn these skills "on the job", often by doing them poorly at first, with the result that much valuable time can be lost; this book will help prevent that. The authors have taught a graduate course on the topics covered in this book for many years, and provide a sample curriculum for instructors in graduate schools who wish to teach a similar course. ... The wealth of advice offered in this book is invaluable to students, junior researchers and their mentors in all fields of science, engineering and the humanities."

Description / Table of Contents: Stable Isotope Geochemistry is an introduction to the use of stable isotopes in the geosciences. It is subdivided into three parts: theoretical and experimental principles; fractionation processes of light and heavy elements; the natural variations of geologically important reservoirs. Since the application of stable isotopes to earth sciences has grown in the last few years, a new edition appears necessary. Recent progress in analysing the rare isotopes of certain elements for instance allow the distinction between mass-dependent and mass-independent fractionations. Special emphasis has been given to the growing field of heavy elements. Many new references have been added, which will enable quick access to recent literature. For students and scientists alike the book will be a primary source of information with regard to how and where stable isotopes can be used to solve geological problems.

Description / Table of Contents: Contents: 1. Isotopes and radioactivity; 2. The principles o radioactive dating; 3. Radiometric dating methods; 4. Dating by cosmogenic isotopes; 5. Uncertainties and results of radiometric dating; 6. Radiogenic isotope geochemistry; 7. Stable isotope geochemistry; 8. Isotope geology and dynamic reservoir analysis

Description / Table of Contents: Hydrogen may be the most abundant element in the universe, but in science and in nature oxygen has an importance that is disproportionate to its abundance. Human beings tend to take it for granted because it is all around us and we breathe it, but consider the fact that oxygen is so reactive that in a planetary setting it is largely unstable in its elemental state. Were it not for the constant activity of photosynthetic plants and a minor amount of photo dissociation in the upper atmosphere, we would not have an oxygen-bearing atmosphere and we would not be here. Equally, the most important compound of oxygen is water, without which life (in the sense that we know it) could not exist. The role of water in virtually all geologic processes is profound, from formation of ore deposits to igneous petrogenesis to metamorphism to erosion and sedimentation. In planetary science, oxygen has a dual importance. First and foremost is its critical role in so many fundamental Solar System processes. The very nature of the terrestrial planets in our own Solar System would be much different had the oxygen to carbon ratio in the early solar nebula been somewhat lower than it was, because elements such as calcium and iron and titanium would have been locked up during condensation as carbides, sulfides and nitrides and even (in the case of silicon) partly as metals rather than silicates and oxides. Equally, the role of water ice in the evolution of our Solar System is important in the early accretion and growth of the giant planets and especially Jupiter, which exerted a major control over how most of the other planets formed. On a smaller scale, oxygen plays a critical role in the diverse kinds of physical evolution of large rocky planets, because the internal oxidation state strongly influences the formation and evolution of the core, mantle and crust of differentiated planets such as the Earth. Consider that basaltic volcanism may be a nearly universal phenomenon among the evolved terrestrial planets, yet there are basalts and basalts. The basalts of Earth (mostly), Earth's Moon, Vesta (as represented by the HED meteorites) and Mars are all broadly tholeiitic and yet very different from one another, and one of the primary differences is in their relative oxidation states (for that matter, consider the differences between tholeiitic and calc-alkaline magma series on Earth). But there is another way that oxygen has proven to be hugely important in planetary science, and that is as a critical scientific clue to processes and conditions and even sources of materials. Understanding the formation and evolution of our Solar System involves reconstructing processes and events that occurred more than 4.5 Ga ago, and for which the only contemporary examples are occurring hundreds of light years away. It is a detective story in which most of the clues come from the laboratory analysis of the products of those ancient processes and events, especially those that have been preserved nearly unchanged since their formation at the Solar System's birth: meteorites; comets; and interplanetary dust particles. For example, the oxidation state of diverse early Solar System materials ranges from highly oxidized (ferric iron) to so reducing that some silicon exists in the metallic state and refractory lithophile elements such as calcium exist occur in sulfides rather than in silicates or carbonates. These variations reflect highly different environments that existed in different places and at different times. Even more crucial has been the use of oxygen 3-isotope variations, which began almost accidentally in 1973 with an attempt to do oxygen isotope thermometry on high-temperature solar nebula grains (Ca-, Al-rich inclusions) but ended with the remarkable discovery of non-mass-dependent oxygen isotope variations in high-temperature materials from the earliest Solar System. The presolar nebula was found to be very heterogeneous in its isotopic composition, and virtually every different planet and asteroid for which we have samples has a unique oxygen-isotopic fingerprint. The idea for this book originated with Jim Papike, who suggested the idea of a study initiative (and, ultimately, a published volume) focused on the element that is so critically important in so many ways to planetary science. He recognized that oxygen is such a constant theme through all aspects of planetary science that the proposed initiative would serve to bring together scientists from a wide range of disciplines for the kind of cross-cutting dialogue that occurs all too rarely these days. In this sense the Oxygen Initiative is modeled on the Basaltic Volcanism Study Project, which culminated in what remains to this day a hugely important reference volume (Basaltic Volcanism Study Project 1981). After obtaining community input and feedback, primarily through the Curation and Analysis Planning Team for Extraterrestrial Materials (CAPTEM) and the Management Operations Working Group for NASA's Cosmochemistry Program, a team of scientists was assembled who would serve as chapter writing leads, and the initiative was formally proposed to and accepted by the Lunar and Planetary Institute (LPI; Dr. Stephen Mackwell, Director) for sponsorship. A formal proposal was then submitted to and approved by the Mineralogical Society of America to publish the resulting volume in the Reviews in Mineralogy and Geochemistry (RiMG) series. Three open workshops were held as preludes to the book: Oxygen in the Terrestrial Planets, held in Santa Fe, NM July 20-23, 2004; Oxygen in Asteroids and Meteorites, held in Flagstaff, AZ June 2-3, 2005; and Oxygen in Earliest Solar System Materials and Processes (and including the outer planets and comets), held in Gatlinburg, TN September 19-22, 2005. The workshops were each organized around a small number of sessions (typically 4-6), each focusing on a particular topic and consisting of invited talks, shorter contributed talks, and ample time for discussion after each talk. In all of the meetings, the extended discussion periods were lively and animated, often bubbling over into the breaks and later social events. As a consequence of the cross-cutting approach, the final book spans a wide range of fields relating to oxygen, from the stellar nucleosynthesis of oxygen, to its occurrence in the interstellar medium, to the oxidation and isotopic record preserved in 4.56 Ga grains formed at the Solar System's birth, to its abundance and speciation in planets large and small, to its role in the petrologic and physical evolution of the terrestrial planets.

Description / Table of Contents: The idea for this book was conceived in early June, 2005 at a paleoaltimetry workshop held at Lehigh University, Lehigh, Pennsyalvania and organized by Dork Sahagian. The workshop was funded by the tectonics program at NSF, and was designed to bring together researchers in paleoaltimetry to discuss different techniques and focus the community on ways of improving paleoelevation estimates and consequent interpretations of geodynamics and tectonics. At this meeting, some commented that a comprehensive volume describing the different methods could help advance the field. I offered to contact the Mineralogical Society of America and the Geochemical Society about publishing a RiMG volume on paleoaltimetry. Because many of the techniques used to infer paleoelevations are geochemically-based or deal with thermodynamic principles, the GS and MSA agreed to the project. Two years and roughly 1000 e-mails later, our book has arrived. The book is organized into 4 sections: Geodynamic and geomorphologic rationale (Clark). This chapter provides the broad rationale behind paleoaltimetry, i.e., why we study it. Stable isotope proxies. These 4 chapters cover theory of stable isotopes in precipitation and their response to altitudinal gradients (Rowley), and stable isotopes sytematics in paleosols (Quade, Garzione and Eiler), silicates (Mulch and Chamberlain) and fossils (Kohn and Dettman). Proxies of atmospheric properties. These 4 chapters cover temperature lapse rates (Meyer), entropy (Forest), and atmospheric pressure proxies, including total atmospheric pressure from gas bubbles in basalt (Sahagian and Proussevitch), and the partial pressure of CO2 (Kouwenberg, Kürshner, and McElwain). Note that clumped isotope thermometry (Quade, Garzione and Eiler) also provides direct estimates of temperature. Radiogenic and cosmogenic nuclides. These 2 chapters cover low-temperature thermochronologic approaches (Reiners) and cosmogenic isotopes (Riihimaki and Libarkin). Some chapters overlap in general content (e.g., basic principles of stable isotopes in precipitation are covered to different degrees in all stable isotope chapters), but no attempt was made to limit authors' discussion of principles, or somehow attempt to arrive at a "consensus view" on any specific topic. Because science advances by critical discussion of concepts, such restrictions were viewed as counterproductive. This does mean that different chapters may present different views on reliability of paleoelevation estimates, and readers are advised to read other chapters in the book on related topics – they may be more closely linked than they might at first appear! I hope readers of this book will discover and appreciate the synergy among paleoaltimetry, climate change, and tectonic geomorphology. These interrelationships create a complex, yet rich field of scientific enquiry that in turn offers insights into climate and geodynamics.

Description / Table of Contents: Contents: The peer-review process - how to get going. Manuscript submission and initial checks on completeness and suitability. The full review process. The decision-making process for reviewed manuscripts. Moving to online submission and review. Reviewers: a precious resource. The obligations and responsibilities of the people involved in peer review. Misconduct in scientific research and publishing - what it is and how to deal with it.The Golden Rules and the Peer Review Good Practice Checklist. Other models of peer review.

Description / Table of Contents: Over 25 years ago, Volume 9 of Reviews in Mineralogy: Amphiboles and Other Hydrous Pyriboles seemed to contain all that was possible to know about this group of fascinating minerals. The subsequent twenty-five years have shown that this assessment was wrong: Nature was keeping a lot in reserve, and has since revealed considerable new complexity in the constitution and behavior of amphiboles. Some of the advances in knowledge have been due to the use of new experimental techniques, some have been due to the investigation of hitherto neglected rock-types, and some have been due to the development of new ideas. The identification and systematic investigation of variable LLE (Light Lithophile Elements), particularly Li and H, led to the identification of several new amphibole species and the recognition that variable Li and H play an important role in chemical variations in amphiboles from both igneous and metamorphic parageneses. In turn, this work drove the development of microbeam SIMS to analyze LLE in amphiboles. Detailed mineralogical work on metasyenites showed hitherto unexpected solid-solution between Na and Li at the M(4) site in monoclinic amphiboles, a discovery that has upset the current scheme of amphibole classification and nomenclature and initiated new efforts in this direction. Systematic and well-planned synthesis of amphiboles, combined with careful spectroscopy, has greatly furthered our understanding of cation and anion order in amphiboles. The use of bond-valence theory to predict patterns of SRO (Short-Range Order) in amphiboles, and use of these predictions to understand the infrared spectra of well-characterized synthetic-amphibole solid-solutions, has shown that SRO is a major feature of the amphibole structure, and has resulted in major advances in our understanding of SRO in minerals. There has been significant progress relating changes in amphibole composition and cation ordering to petrogenetic conditions and trace-element behavior. Work on the nature of fibrous amphiboles and their toxicity and persistence in living organisms has emphasized the importance of accurate mineralogical characterization in environmental and health-related problems. The current volume has taken a different approach from previous volumes concerned with major groups of rock-forming minerals. Some of the contents have previously been organized by the investigative technique or groups of similar techniques: crystal-structure refinement, spectroscopy, TEM etc. Here, we have taken an approach that focuses on aspects of amphiboles rather than experimental techniques: crystal chemistry, new compositions, long-range order, short-range order etc., and all experimental results germane to these topics are discussed in each chapter. The intent of this approach is to focus on amphiboles, and to emphasize that many techniques are necessary to fully understand each aspect of the amphiboles and their behavior in both natural and industrial processes.

Description / Table of Contents: Contents: 1. Why we should care: the impact of anthropogenic carbon dioxide on the carbon cycle.2. The thermodynamic background.3. Carbon dioxide and CO2-H2O mixtures.4. The aqueous electrolytic solution.5. The product solid phases.6. The kinetics of mineral carbonation.7. Reaction path modeling of geological CO2 sequestration.

Description / Table of Contents: Contents: Extracting Salient Structures.- Graph Drawing Algorithms.- Systems and Applications.- Knowledge Domain Visualization.- Empirical Studies of Information Visualization.- Virtual Environments.- Detecting Abrupt Changes and Emerging Trends.

Description / Table of Contents: This book brings together the essential theory required to understand the behaviour of trace elements in magmas, and magma-derived rocks.

Description / Table of Contents: In situ-produced cosmogenic nuclides can provide chronologies of environmental change over the past few thousand to several millions of years and may be used to quantify a wide range of weathering and sediment transport processes. These nuclides are thus now used across a broad spectrum of earth science disciplines, including paleoclimatology, geomorphology, and active tectonics. This book is organized around sections that focus on specific aspects of the utilization of cosmogenic nuclides in earth sciences: (1) development of new methods for application of in situ-produced cosmogenic nuclides (burial dating methods, extending their utilization to carbonate-rich and mafic environments); (2) glacial geology (Laurentide Ice Sheet, northern Alps); (3) active tectonics, focusing on applications to constrain slip rates of active faults in Asia (Tibet and Mongolian Gobi-Altay); and (4) landscape development (quantifying sediment production or erosion rates and processes and application of exposure dating to landslides in Hong Kong).

Description / Table of Contents: The IUGS/IAGC Global Geochemical Baselines Programme aims to establish a global geochemical reference baseline for 〉60 determinants in a range of media for environmental and other applications. The European contribution to the programme has been carried out by government institutions from 26 countries under the auspices of the Forum of European Geological Surveys (FOREGS) The main objectives of this European survey were: 1) to apply standardised methods of sampling, chemical analysis and data management to prepare a geochemical baseline across Europe; and 2) to use this reference network to level national baseline datasets. Samples of stream water, stream sediment and three types of soil (organic top layer, minerogenic top and sub soil) have been collected at 900 stations, each representing a catchment area of 100 km2, corresponding to a sampling density of about one sample per 4700 km2. In addition, the uppermost 25 cm of floodplain sediment was sampled from 790 sites each representing a catchment area of 1000 km2. All soil and sediment samples were prepared at the same laboratory, and all samples of particular sample types were analysed by the same method at the same laboratory. More than 50 elements, both total and aqua regia extractable concentrations, and other parameters (such as pH and grain size) were determined on the 〈2 mm grain size fraction of minerogenic samples, and total concentrations of organic soil samples were measured after using a strong acid digestion. Nine laboratories of European geological surveys carried out the analytical work. Altogether, 360 geochemical maps showing the distribution of elements across Europe have been prepared. All the results and field observations are organised in a common database and the maps are published as a Geochemical Atlas of Europe. All the sampling sites were photographed and this photo archive is also available. Samples have been archived in the Slovak Republic for possible future use. Initial results show that the distribution patterns of both water and solid samples are related to such factors as large-scale tectonic provinces, geochemical variation of large lithological units, extension of the Weichselian glaciation, and contamination reflecting industrialized areas and regions of intensive agriculture. Key words (GeoRef Thesaurus, AGI): geochemical surveys, baseline studies, soils, sediments, stream water, sampling, sample preparation, chemical analysis, geochemical maps, atlas, areal geology, Europe

Description / Table of Contents: Contents: The Focused Ion Beam Instrument. Ion,Solid Interactions. Focused Ion Beam Gases for Deposition and Enhanced Etch. Three-Dimensional Nanofabrication Using Focused Ion Beams. Device Edits and Modifications. The Uses of Dual Beam FIB in Microelectronic Failure Analysis. High Resolution Live Imaging of FIB Milling Processes for Optimum Accuracy. FIB for Materials Science Applications. Practical Aspects of FIB TEM Specimen Preparation. FIB LiftOut Specimen Preparation Techniques. A FIB MicroSampling Technique and a Site Specific TEM Specimen Preparation Method. DualBeam (FIBSEM) Systems. Focused Ion Beam Secondary Ion Mass Spectrometry (FIBSIMS). Quantitative Three Dimensional Analysis Using Focused Ion Beam Microscopy. Applications of FIB in Combination with Auger Electron Spectroscopy.

Description / Table of Contents: Contents: The Earth's Aggregate Physical and Chemical State. Introduction to Thermodynamics. Mixture and Simple Phase Relations. Mineral Chemistry. Aqueous Solutions. Chemistry of Natural Waters. Chemistry of Igneous Rocks. Chemical Controls on Soil Formation, Diagenesis, Metamorphism, and Hydrothermal Ore Deposition . Radioactive Isotope Geochemistry. Stable Isotope Geochemistry. Surface Sorption Geochemistry. Chemical Kinetics. Oxidation and Reduction. Organic Geochemistry. Atmospheric Chemistry

Description / Table of Contents: As geomicrobiologists, we seek to understand how some of nature's most complex systems work, yet the very complexity we seek to understand has placed many of the insights out of reach. Recent advances in cultivation methodologies, the development of ultrahigh throughput DNA sequencing capabilities, and new methods to assay gene expression and protein function open the way for rapid progress. In the eight years since the first Geomicrobiology volume (Geomicrobiology: Interactions between microbes and minerals; volume 35 in this series) we have transformed into scientists working hand in hand with biochemists, molecular biologists, genome scientists, analytical chemists, and even physicists to reveal the most fundamental molecular-scale underpinnings of biogeochemical systems. Through synthesis achieved by integration of diverse perspectives, skills, and interests, we have begun to learn how organisms mediate chemical transformations, the ways in which the environment determines the architecture of microbial communities, and the interplay between evolution and selection that shapes the biodiversity of the planet. This volume presents chapters written by leaders in the rapidly maturing field we refer to as molecular geomicrobiology. Most of them are relatively young researchers who share their approaches and insights and provide pointers to exciting areas ripe for new advances. This volume ties together themes common to environmental microbiology, earth science, and astrobiology. The resesarch presented here, the associated short course, and the volume production were supported by funding from many sources, notably the Mineralogical Society of America, the Geochemical Society, the US Department of Energy Chemical Sciences Program and the NASA Astrobiology Institute.

Description / Table of Contents: Contents: Terrestrial craters: Structure, geophysics and cratering motions. - Terrestrial craters: Ejecta studies. - Shock metamorphism. - The planetary perspective.

Description / Table of Contents: Contents: Knowledge visualization. - Information visualization. - Visualizing knowledge and information for fostering learning and instruction. - Knowledge-oriented organization of information for fostering information use.

Description / Table of Contents: Contents: 1. The Discovery of Silicate Melts. An Industrial and Geological Perspective. 2. Glass Versus Melt. 3. Glasses and Melts vs. Crystals. 4. Melt and Glass Structure - Basic Concepts. 5. Silica - A Deceitful Simplicity. 6. Binary Metal Oxide-Silica Systems I. Physical Properties.7. Binary Metal Oxide-Silica Systems II. Structure. 8. Aluminosilicate Systems I. Physical Properties. 9. Aluminosilicate Systems II. Structure. 10. Iron-bearing Melts I. Physical Properties. 11. Iron-bearing Melts II. Structure. 12. The Titanium Anomalies. 13. Phosphorus. 14. Water - An Elusive Component. 15. Volatiles I. The System C-O-H-S. 16. Volatiles II. Noble Gases and Halogens. 17. Natural Melts.

Description / Table of Contents: Contents: Carbon, the Earth and life. Chemical composition of biogenic matter. Production, preservation and degradation of organic matter. Long-term fate of organic matter in the geosphere. Chemical stratigraphy. The carbon cycle and climate. Anthropogenic carbon and the environment.

Description / Table of Contents: Part I: Introduction. - Part II: Environmental Chemist's Toolbox. - Part III: The Atmosphere. - Part IV: The Chemistry Of Continental Solids. - Part V: The Chemistry Of Continental Waters. - Part VI: The Oceans. - Part VII: Global Change

Description / Table of Contents: Until only a few years ago, I would never have imagined that a volume on the stable isotope geochemistry of elements like Mg, Fe or Cu would be written. In fact, a comic book of blank pages entitled The Stable Isotope Geochemistry of Fluorine would have been a more likely prospect. In volume 16 of this series, published in 1986, I wrote: Isotopic variations have been looked for but not found for heavy elements like Cu, Sn, and Fe .... Natural variations in isotopic ratios of terrestrial materials have been reported for other light elements like Mg and K, but such variations usually turn out to be laboratory artifacts. I am about ready to eat those words. We have known for many years that large isotopic fractionations of heavy elements like Pb develop in the source regions of TIMS machines. Nonetheless, most of us held fast to the conventional wisdom that no significant mass-dependent isotopic fractionations were likely to occur in natural or laboratory systems for elements that are either heavy or engaged in bonds with a dominant ionic character. With the relatively recent appearance of new instrumentation like MC-ICP-MS and heroic methods development in TIMS analyses, it became possible to make very precise measurements of the isotopic ratios of some of these non-traditional elements, particularly if they comprise three or more isotopes. It was eminently reasonable to reexamine these systems in this new light. Perhaps atomic weights could be refined, or maybe there were some unexpected isotopic variations to discover. There were around the turn of the present century, reports began appearing of biological fractionations of about 2-3 per mil for heavy elements like Fe and Cr and attempts were made to determine the magnitude of equilibrium isotope effects in these systems, both by experiment and semi-empirical calculations. Interest emerged in applying these effects to the study of environmental problems. Even the most recalcitrant skeptic now accepts the fact that measurable and meaningful variations in the isotopic ratios of heavy elements occur as a result of chemical, biological and physical processes. Most of the work discussed in this volume was published after the year 2000 and thus the chapters are more like progress reports rather than reviews. Skepticism now focuses on whether isotopic variations as small as 0.1 per mil are indeed as meaningful as some think, and the fact that measured isotopic fractionations of these non-traditional elements are frequently much smaller than predicted from theoretical considerations. In fact the large fractionations suggested by the calculations provide much of the stimulus for working in this discipline. Clearly some carefully designed experiments could shed light on some of the ambiguity. My optimism for the future of this burgeoning new field remains high because it is in very good hands indeed. Approximately three-quarters of the elements in the Periodic Table have two or more isotopes. RiM 16 and RiMG 43 were devoted to H, C, 0, and S isotope variations, and B isotope variations were discussed in RiM 33. The importance of these elements to geochemistry may be illustrated by a GeoRef search of 0 isotope publications, which yields over 25,000 papers, theses, and abstracts spanning over five decades. Isotopic variations of the remaining 56 elements that have two or more isotopes, however, remains relatively little explored, but is gaining rapid attention, in part driven by advances in analytical instrumentation in the last 5-10 years. Our goal for this volume was to bring together a summary of the isotope geochemistry of non-traditional stable isotope systems as is known through 2003 for those elements that have been studied in some detail, and which have a variety of geochemical properties. In addition, recognizing that many of these elements are of interest to workers who are outside the traditional stable isotope fields, we felt it was important to include discussions on the broad isotopic variations that occur in the solar system, theoretical approaches to calculating isotopic fractionations, and the variety of analytical methods that are in use. We hope, therefore, that this volume proves to be useful to not only the isotope specialist, but to others who are interested in the contributions that these non-traditional stable isotopes may make toward understanding geochemical and biological cycles.

Description / Table of Contents: Contents: General Significance of Geochemical Models of Hydrothermal Systems.- Concepts, Classification and Chemistry of Geothermal Systems.- Theory of Chemical Modeling.- Specific Features of Coupled Fluid Flow and Chemical Reaction.- Fossil Hydrothermal Systems.- Recent Hydrothermal Systems.- Reservoir Management.

Description / Table of Contents: Contents: Physical properties of water. Near-critical behavior of aqueous systems.Aqueous solubility of volatile nonelectrolytes. Calculation of standard thermodynamic properties of aqueous electrolytes and nonelectrolytes.Hydrothermal solution structure: experiments and computer. Vapor-liquid equilibrium involving aqueous, binary nonelectrolytes. Binary homogeneous nucleation in selected aqueous vapor mixtures. Solute concentration effects on reaction thermodynamics in steam cycle fluids. Stable isotope partitioning in aqueous and hydrothermal systems to elevated temperatures. Transport properties in high temperature and pressure ionic solutions. Electrochemical processes in high-temperature aqueous solutions. Partitioning of electrolytes to steam and their solubilities in steam. Dissociation equilibria of weak acids and bases. Solubility and surface adsorption characteristics of metal oxides. Phase equilibria of water-salt systems at high temperatures and pressures. Kinetics and mechanisms of hydrothermal organic reactions. Water chemistry in commercial water-steam cycles. Hydrothermal synthesis of ceramic materials.