3 edition of Isotopic biogeochemistry found in the catalog.
John M. Hayes
|Statement||J.M. Hayes, principal investigator.|
|Series||NASA contractor report -- NASA CR-176128.|
|Contributions||United States. National Aeronautics and Space Administration., Indiana University Foundation.|
|The Physical Object|
Methods in Biogeochemistry of Wetlands R.D. DeLaune, K.R. Reddy, C.J. Richardson, and J.P. Megonigal, editors Book and Multimedia Publishing Committee April Ulery, Chair Warren Dick, ASA Editor-in-Chief E. Charles Brummer, CSSA Editor-in-Chief Andrew Sharpley, SSSA Editor-in-Chief Lajpat Ahuja Michael Casler David Clay Kimberly Cook David FangFile Size: KB. Isotopic Tracers in Biology: An Introduction to Tracer Methodology, Third Edition focuses on stable isotopes, structures, composition, and reactions of nitrogen and oxygen, and radioactive tracers. The book first takes a look at atomic nuclei, radioactivity, and the production of radioactive isotopes and radiation characteristics of tracer atoms. Furthermore, no studies have addressed the isotopic biogeochemistry of seabird guano from an agricultural or horticultural standpoint. The purpose of this study, therefore, is to assess the isotopic and vital effects of Peruvian seabird guano fertilization on maize (Zea mays) under controlled by:
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Isotope Geochemistry | Wiley. This book provides a comprehensive introduction to radiogenic and stable isotope geochemistry. Beginning with a brief overview of nuclear physics and nuclear origins, it then reviews radioactive decay schemes and their use in geochronology. A following chapter covers the closely related techniques such as fission-track and carbon dating.
Book Condition: May have some highlighting or book has been loved by someone. Binding is tight, pages are clean. Overall book in GOOD condition. Clean crisp pages with a tight binding. Ships directly from Amazon and is eligible for prime or super saver (free) 5/5(1). This book contains an exceptional list of literature references for additional study on specific topics.
Hoefs’ book is a very valuable reference for individuals and companies engaged in isotopic studies and is very reasonably priced." (Robert F. Ehinger, American Association of Manufacturer: Springer. The Handbook of Environmental Isotope Geochemistry comprises a series of books, each focussing on a selected environment, presenting in-depth reviews of all relevant studies and results obtained in specific research areas.
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 : Springer-Verlag Berlin Heidelberg.
Isotopic analysis of clay minerals for hydrogen and oxygen isotope analysis of clay minerals have been established and yield satisfactory results for most minerals with a precision.
Additionally, it includes the isotope analysis of pore waters and associated non-clay minerals in clay-rich rocks. tracers of the solutes in the water: solute isotope biogeochemistry.
These classifications are by no means universal but they are conceptually useful and often eliminate confusion when comparing results using different tracers. This book uses this classification for dividing chapters into Part III (Chapters 10 - 14) and Part IV (Chapters 15 - 20).
Biogeochemistry—winner of a Textbook Excellence Award (Texty) from the Text and Academic Authors Association—considers how the basic chemical conditions of the Earth, from atmosphere to soil to seawater, have been and are being affected by the existence of life. Human activities in particular, from the rapid consumption of resources to the destruction of the rainforests and the expansion of smog.
White Geochemistry Chapter 9: Stable Isotopes The Fractionation Factor The fractionation factor, α, is the ratio of isotope ratios in two phases: α A−B ≡ R A R B The fractionation of isotopes between two phases is also often reported as ∆File Size: 1MB.
PD Dr. Hans-Hermann Richnow. He is a geochemist and Head of the Department of Isotope Biogeochemistry at the UFZ. His expertise is in developing concepts for applying isotope techniques to environmental monitoring (claims, historical contamination, remedial work on historical contamination) and the behaviour of chemicals in the environment.
Geochemistry - Books and Journals These Springer books, book series, and journals introduce you to the world of geochemistry. Geochemistry is a natural science discipline that combines geosciences and chemistry.
This discipline focuses on the material structure, distribution, stability and circulation of chemical elements and their isotopes in. Organic Geochemistry serves as the only dedicated medium for the publication of peer-reviewed research on all phases of geochemistry in which organic compounds play a major role.
The Editors welcome contributions covering a wide spectrum of subjects in the geosciences broadly based on organic chemistry (including molecular and isotopic geochemistry), and involving geology, biogeochemistry.
Principles of Stable Isotope Geochemistry is written as a textbook to accompany a one semester course in Stable Isotope Geochemistry.
There are 13 chapters, each dealing with a Cited by: He continued this interest up to his latest days. He wrote a fundamental essay, ‘The geologic history of seawater,’ on the subject in the Treatise on Geochemistry () for which he and I acted as executive editors.
We were close to completing the second edition of the treatise. Isotope geochemistry is an aspect of geology based upon the study of natural variations in the relative abundances of isotopes of various elements.
Variations in isotopic abundance are measured by isotope ratio mass spectrometry, and can reveal information about the ages and origins of rock, air or water bodies, or processes of mixing between them.
Over the past decade the number of ecological studies using stable isotopes has grown exponentially and research focused on marine mammals is no exception ().Stable isotope values of carbon, nitrogen, hydrogen, and oxygen are now used routinely to study foraging ecology and trophic status, habitat use, migration, population connectivity, and by: Stable Isotopes in Ecology and Environmental Science, Second Edition.
Editor(s): Stable Isotopes in Ecology and Environmental Science is an ideal resource for both ecologists who are new to isotopic in the Department of Botany and Plant Pathology at Oregon State University and the Editor-in-Chief of Biogeochemistry.
She is a terrestrial. Isotope Geochemistry by William M White (author) and a great selection of related books, art and collectibles available now at Abstract. Inin his classical paper on the thermodynamic properties of isotopic substances, H.
Urey  laid the foundation of modern isotope geochemistry. At the same time, A. Nier  designed a new mass spectrometer which allowed the measurement of small differences in isotope abundance ratios.
A modification in the Nier-type mass spectrometer and a refinement in instrumentation Cited by: Organic carbon dissolved in the ocean, suspended as particles or cells, and accumulating in sediments together constitute the other significant fractions of marine carbon, with organic carbon in the water column similar in quantity to the current atmospheric inventory of carbon dioxide.
Isotopic partitioning among various inorganic and organic Cited by: Table of Contents. Editors: Alicia R. Ventresca Miller and Cheryl Makarewicz; Chapter 1: Isotopic Approaches to Pastoralism in Prehistory: Diet, Mobility, and Isotopic Reference Sets; Chapter 2: Understanding ephemeral pastoralist settlement sites in eastern Africa: the potential of isotopes in cattle tooth enamel; Chapter 3: Investigating seasonal changes of cattle diet in terrestrial C 3.
Biology & Biogeochemistry Isotopic signatures in a wide variety of complex organic compounds can reveal unique insights in biological and biogeochemical process. This is true as chemical and physical processes lead to changes in the natural isotope composition of organic compounds.
Principles of Stable Isotope Geochemistry About this book Abundances of the Rare Isotopes of Light Elements 7 Characteristics of Elements That Undergo Significant Isotopic Fractionation 7 Applications in the Earth Sciences 9 Isotope Effects 10 Kinetic Isotope Effects 10 Equilibrium Isotope Effects Another branch of biogeochemistry is concerned with the chemistry of mineralized products of ancient organisms.
The three chemical attributes of mineralized fossils that have received the most intensive study are mineral composition, trace chemistry, and isotopic composition. The factors controlling these three properties may often be a complex.
A preliminary study of the carbon and nitrogen isotopic biogeochemistry of lacustrine sedimentary rocks from the Green River Formation Chapter (PDF Available) January with Reads. (). Contribution of isotopic biogeochemistry (13C, 15N, 18O) to the paleoecology of mammoths (mammuthus primigenius).
Historical Biology: Vol. 7, No. 3, pp. Cited by: Dartmouth Earth Sciences is well equipped for geochemical research. Here, we have several multiple inductively coupled plasma-mass spectrometers and optical emission spectrometers for elemental and isotopic analyses, facilities for isotope-ratio mass spectrometry, liquid and gas chromatographs for chemical separation and speciation, facilities for mineral/petrographic spectroscopy, and a.
Biogeochemistry—winner of a Textbook Excellence Award (Texty) from the Text and Academic Authors Association—considers how the basic chemical conditions of the Earth, from atmosphere to soil to seawater, have been and are being affected by the existence of life.
Human activities in particular, from the rapid consumption of resources to the destruction of the rainforests 5/5(2).
“Isotopic Biogeochemistry of Rivers, Lakes and Watersheds: From the source to the estuary”– One of the major challenges of current research on the functioning of the continental ecosphere is the development of approaches integrating source and process information on local, landscape, regional and global scales.
The isotopic composition of. This section contains free e-books and guides on BioChemistry, some of the resources in this section can be viewed online and some of them can be downloaded.
Graduate Biochemistry Lecture Notes This note covers the following topics: Kinetics, Molecular Graphics, Chemical Kinetics Simulator, Chemical Thermodynamics, Chemical Equilibrium, Mystery. Today viewed from a year perspective, these findings on isotopic variation in plants are both simplistic and profound because they highlight biological variations that capture the big trends.
In fact, data like these are fundamental to understanding isotope biogeochemistry of. Geology - Geology - Isotopic geochemistry: Isotopic geochemistry has several principal roles in geology. One is concerned with the enrichment or impoverishment of certain isotopic species that results from the influence of differences in mass of molecules containing different isotopes.
Measurements of the proportions of various isotopic species can be used as a form of geologic thermometer. Natural variation in plant/soil δ15N. The purpose of this paper is not to provide a detailed overview of the various processes influencing the N isotopic composition of plants and soils; for these purposes the reader is referred to many of the comprehensive reviews and syntheses that have already been published on this topic (Nadelhoffer and Fry, ; Handley and Scrimgeour, ; Högberg Cited by: Silicon (Si) is the second most abundant element in the Earth's crust and is an important nutrient in the ocean.
The global Si cycle plays a critical role in regulating primary productivity and carbon cycling on the continents and in the oceans. Development of the analytical tools used to study the sources, sinks, and fluxes of the global Si cycle (e.g., elemental and stable isotope ratio data Cited by: Books shelved as biochemistry: Principles of Biochemistry by Albert L.
Lehninger, Biochemistry by Jeremy M. Berg, Lippincott's Illustrated Reviews: Bioch. Research on the oceanic biogeochemistry of Si at ETH Zurich focuses on analysing the stable isotope composition of silicon dissolved in seawater, in order to: resolve data ambiguities regarding the marine silicon isotope distribution, especially the isotopic composition of dissolved silicon.
For the past 4 billion years, the chemistry of the Earth's surface, where all life exists, has changed remarkably. Historically, these changes have occurred slowly enough to allow life to adapt and evolve. In more recent times, the chemistry of the Earth is being altered at a staggering rate, fueled by industrialization and an ever-growing human population.
The founder of biogeochemistry was Russian and Ukrainian scientist Vladimir Vernadsky whose book The Biosphere, in the tradition of Mendeleev, formulated a physics of the earth as a living sky distinguished three spheres, where a sphere was a concept similar to the concept of a observed that each sphere had its own laws of evolution, and that the higher spheres.Books; Move navigation right Ocean biogeochemistry Main content.
The oceans are the ultimate repository of the products of chemical weathering of the continents. This large chemical reservoir dominates many surface Earth biogeochemical cycles, such as that of carbon.
We use culturing and isotopic approaches to understand and quantify.Results in Geochemistry is an international open-access peer reviewed journal that publishes a wide range of original research papers on isotopic and elemental geochemistry, both organic and inorganic.
The journal focuses on geochemical processes in the hydrosphere, biosphere, and lithosphere of the Earth, including but not restricted to igneous, metamorphic, and sedimentary petrology, low.