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Treatise on Geochemistry, Ten Volume Set
 
 
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Treatise on Geochemistry, Ten Volume Set [Hardcover]

K.K. Turekian (Editor), H.D. Holland (Editor)
5.0 out of 5 stars  See all reviews (1 customer review)

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Book Description

0080437516 978-0080437514 December 18, 2003 1
The Treatise on Geochemistry is the first work providing a comprehensive, integrated summarry of the present state of geochemistry. It deals with all the major subjects in the field, ranging from the chemistry of the solar system to environmental geochemistry. The Treatise on Geochemistry has drawn on the expertise of outstanding scientists throughout the world, creating the reference work in geochemistry for the next decade.

Each volume consists of fifteen to twenty-five chapters written by recognized authorities in their fields, and chosen by the Volume Editors in consultation with the Executive Editors. Particular emphasis has been placed on integrating the subject matter of the individual chapters and volumes.

Elsevier also offers the Treatise on Geochemistry in electronic format via the online platform ScienceDirect®, the most comprehensive database of academic research on the Internet today, enhanced by a suite of sophisticated linking, searching and retrieval tools.

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Editorial Reviews

About the Author

622551turekianeditor.jpg

Radioactive, radiogenic and isotope measurements in Earth materials provide useful approaches to the study of terrestrial and cosmic processes. Our laboratory has used these tools to address problems as diverse as the circulation of Long Island Sound and the cosmic dust flux to our planet. A few of the projects are listed:

1. Air samples and atmospheric precipitation are analyzed for 222Rn(radon) daughters such as 210Pb and 214Pb as well as cosmogenically produced 7Be and 35S to determine: (a) the residence times of aerosols in different layers of the troposphere via 214Pb, 210Pb and 7Be, (b) the sources of ozone found in the troposphere based on correlations with 7Be and 210Pb, and (c) the oxidation and precipitation kinetics (including dry deposition) of SO2 based on cosmogenic 35S measurements.

2. The radioactive decay of 187Re (half-life ca. 4.6x1010 years) produces 187Os. The ratio of 187Os to non-radiogenic Os (nominally represented by 186Os) in rocks undergoing weathering is determined by the Re/Os of the rock and its age. The variation in the relative sources of weathered material (high 187Os/186Os from continental crust, low 187Os/186Os from mantle-derived rocks) is sensed by contemporary sea water osmium and ultimately recorded in accumulating marine sediments. The tectonic history of the past 100 million years is inferred from Os isotope measurements in deep-sea deposits.

3. The measurement of 222Rn(3.4 d), 226Ra(1620 y), 228Ra(5.7 y) and 224Ra(3.6 d) in Long Island Sound water profiles provides information on the mean residence time of water in the Sound as well as the flux of nutrient-rich water from the New York City area. The radium isotop

622551hollandeditor.jpg

My research is focused on two problems: the long-term evolution of the atmosphere and the long-term evolution of seawater. Emphasis in the first problem area is on the Great Oxidation Event between ca. 2.3 and 2.0 Ga, in particular the change from an atmosphere that probably contained a significant amount of methane to one that contained a significant amount of oxygen. During the next few years we hope to define the cause of this change and to refine its timing.

The past several years have shown that the composition of seawater changed very significantly during the course of the Phanerozoic. However, the actual course of the chemistry of seawater is still poorly defined. The causes are clearly related to tectonism, marine biology, and the flooding of the continents, but a coherent theory relating these processes to the history of seawater remains to be constructed. We hope to contribute materially to this enterprise.

E-mail: holland@eps.harvard.edu


Product Details

  • Hardcover: 7800 pages
  • Publisher: Elsevier Science; 1 edition (December 18, 2003)
  • Language: English
  • ISBN-10: 0080437516
  • ISBN-13: 978-0080437514
  • Product Dimensions: 16.1 x 12.5 x 8.5 inches
  • Shipping Weight: 35.9 pounds (View shipping rates and policies)
  • Average Customer Review: 5.0 out of 5 stars  See all reviews (1 customer review)
  • Amazon Best Sellers Rank: #5,940,832 in Books (See Top 100 in Books)

 

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0 of 4 people found the following review helpful:
5.0 out of 5 stars Treatise on Geochemistry, July 8, 2004
By A Customer
This review is from: Treatise on Geochemistry, Ten Volume Set (Hardcover)
"This landmark 10-volume publication is a comprehensive review of the many-faceted field of geochemistry. (...)
The Treatise will be an indispensable reference not only to academics but to contamination cleanup professionals, resource managers, and environmental regulators as well."
David W. Morganwalp, U.S. Geological Survey, Reston, VA, USA
(...)

"This publication is - without a doubt - a must have for researchers, teachers and students in Japan and also for scientists in geophysics, rocks- mineralogy-science of ore deposits, geology, natural geography and so on."
Prof. Dr. Naotatsu Shikazono, Dep. of Applied Chemistry, Environmental Geochemistry, Keio University, Japan

"This first volume of Treatise on Geochemistry provides the reader a summary of high-quality reviews on the current status of geochemical exploration of our solar system. It is recommended to researchers and students for a concise up-to-date overview of the field."
Dr. Heike Rauer, Institute of Planetary Research, DLR, German Aerospace Center, Berlin, Germany
(on Volume 1 of Treatise on Geochemistry)

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Inside This Book (learn more)
First Sentence:
Jenny (1941) applied principles from the physical sciences to the study of soil formation. Read the first page
Key Phrases - Statistically Improbable Phrases (SIPs): (learn more)
solute isotopes, global meteoric waterline, crystalline rock environments, weathering velocity, dicarboxylic acid anions, natural weathering rates, total hydrolyzable amino acids, proglacial zone, biomass triangle, dissolution plateau, hydrolyzable sugars, basinal waters, forsterite dissolution, geological membranes, stable chlorine isotopes, weathering gradient, large vascular plants, hydrolytic weathering, sedimentary basin brines, mole balancing, plagioclase weathering, solute evolution, reactive organic species, alkali feldspar dissolution, chemical erosion rates
Key Phrases - Capitalized Phrases (CAPs): (learn more)
New York, Water Resour, Earth Planet, United States, Mineralogical Society of America, Kluwer Academic, Gulf Coast, American Chemical Society, American Geophysical Union, Gulf of Mexico, North America, Sierra Nevada, Soil Sci, Black Creek, Academic Press, Great Plains, Paris Basin, Great Artesian Basin, Cambridge University Press, Geological Society of America, Special Paper, Dead Sea, Great Basin, Boca Raton, Caspian Sea
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