Springer Geochemistry – serie

This book explores water geothermometry, a highly relevant topic in the exploration and exploitation of geothermal energy. Presenting theoretical geothermometers and indicators of CO2 fugacity, it describes a rigorous new approach entirely based on thermodynamics. The book will appeal to geothermal geoscientists, especially those working in research institutions and companies around the globe. It is also of interest to students on advanced courses in applied geochemistry, water–rock interaction and other related areas.

This book explores water geothermometry, a highly relevant topic in the exploration and exploitation of geothermal energy. Presenting theoretical geothermometers and indicators of CO2 fugacity, it describes a rigorous new approach entirely based on thermodynamics. The book will appeal to geothermal geoscientists, especially those working in research institutions and companies around the globe. It is also of interest to students on advanced courses in applied geochemistry, water–rock interaction and other related areas.

This book summarizes recent impressive improvements in the application of Quantum Mechanics, coupled with the significant increase in both speed and storage capabilities of modern computers, that allow to depict the energy and reactive properties of chemically complex materials through first principles and destroy the dogmatic assumption that the natural complexity cannot be modeled. It presents methods of Quantum Chemistry applied to various fields of geoscience. The book aims to convey to the audience, methods and procedures apt to obtain sound thermodynamic and thermo-physical data for earth’s materials under various aggregation states. The attention of this book focusses on the applicative aspects of the various procedures, with reference to the underlying theory.

This book summarizes recent impressive improvements in the application of Quantum Mechanics, coupled with the significant increase in both speed and storage capabilities of modern computers, that allow to depict the energy and reactive properties of chemically complex materials through first principles and destroy the dogmatic assumption that the natural complexity cannot be modeled. It presents methods of Quantum Chemistry applied to various fields of geoscience. The book aims to convey to the audience, methods and procedures apt to obtain sound thermodynamic and thermo-physical data for earth’s materials under various aggregation states. The attention of this book focusses on the applicative aspects of the various procedures, with reference to the underlying theory.

This book compiles a compendium of the current knowledge on the distribution, speciation and behavior of sulfur in the atmosphere, surface, crust, mantle, and core of the Earth as well as the other bodies of the solar system, including the terrestrial planets, dwarf planets, asteroids, moons, and the gas giants. It brings together a diverse group of geoscientists with broad interests, knowledge, and expertise regarding the behavior of sulfur in a variety of natural processes. This diversity of knowledge and experience allowed them to contribute to a comprehensive and coherent series of review chapters, which outline and expand upon the basis of our current understanding regarding how sulfur contributes to the origin, evolution, and functioning of the Earth as well as the other bodies of the solar system.With a plethora of oxidation states (from ‐2 to +6), a cosmic element abundance rank of ten, a fascinating redox‐, pH‐, and radical‐dependent chemistry, a strong chemical affinity for many metals, and a large fractionation among its four stable isotopes, sulfur is a key player and a powerful tracer element in the various physical and chemical processes occurring in the atmosphere, surface, crust, mantle, and core of the Earth as well as in the other bodies of the solar system. On Earth, as a key component of aqueous fluids, sulfur is a powerful complexing agent for a series of metals, which allows for their transfer across the lithosphere and subsequent concentration as ore deposits. As sulfur dioxide and sulfate, sulfur can act as an oxidizing agent, whereas as hydrogen sulfide and polysulfides, it can act as a reducing agent and a strong binder for metals, over a wide range of pressures and temperatures in the crust, upper mantle, and during subduction processes. Sulfur controls the partitioning of a many metals between silicate melts, gaseous and aqueous fluids, and mineral phases, thereby playing a major role in the formation of magmatic‐hydrothermal and metamorphic ore deposits that supply strategic metal resources to our society. In the atmospheres of both the terrestrial worlds and the gas giants, sulfur plays a diverse and important role shaping their physical, chemical and biological evolution.

This book reviews all the major research accomplishments and summarizes the different applications of radon. It serves as a solid reference book for researchers who are interested in the U-series radionuclides and noble gases as tracers and chronometers. Radon has been widely utilized as a powerful tracer to quantify a number of processes that include gas exchange rates between air and water, submarine groundwater discharge in coastal waters, water exchange between rivers and lakes, ocean circulation, hydrocarbon and uranium exploration. It is also used as an atmospheric tracer for the identification and quantification of air masses and as a tool for earthquake prediction, etc. A significant portion of the book presents state-of-the knowledge on indoor-radon-related health issues. Applications of the decay-series of Rn-222 are presented in a chapter. It serves as a reference and a state-of-the-art resource for researchers who want to learn the different applications of radon in Earth systems.

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.

This book reviews all the major research accomplishments and summarizes the different applications of radon. It serves as a solid reference book for researchers who are interested in the U-series radionuclides and noble gases as tracers and chronometers. Radon has been widely utilized as a powerful tracer to quantify a number of processes that include gas exchange rates between air and water, submarine groundwater discharge in coastal waters, water exchange between rivers and lakes, ocean circulation, hydrocarbon and uranium exploration. It is also used as an atmospheric tracer for the identification and quantification of air masses and as a tool for earthquake prediction, etc. A significant portion of the book presents state-of-the knowledge on indoor-radon-related health issues. Applications of the decay-series of Rn-222 are presented in a chapter. It serves as a reference and a state-of-the-art resource for researchers who want to learn the different applications of radon in Earth systems.

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.

The aim of this book is to unlock the power of the freeware R language to advanced university students and researchers dealing with whole-rock geochemistry of (meta-) igneous rocks. The first part covers data input/output, calculation of commonly used indexes and plotting in R. The core of the book then focusses on the presentation and practical implementations of modelling techniques used for fingerprinting processes such as partial melting, fractional crystallization, binary mixing or AFC using major-, trace-element and radiogenic isotope data. The reader will be given a firm theoretical basis for forward/reverse modelling, followed by exercises dealing with typical problems likely to be encountered in real life, and their solutions using R. The concluding sections demonstrate, using practical examples, how a researcher can proceed in developing a realistic model simulating natural systems. The appendices outline the fundamentals of the R language and provide a quick introductionto the open-source R-package GCDkit for interpretation of whole-rock geochemical data from igneous and metamorphic rocks.