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Fb2 History of the Earth’s Atmosphere ePub

by Michael I. Budyko,Alexander B. Ronov,Alexander L. Yanshin,S.F. Lemeshko,V.G. Yanuta

Category: Engineering
Subcategory: Engineering and Transport
Author: Michael I. Budyko,Alexander B. Ronov,Alexander L. Yanshin,S.F. Lemeshko,V.G. Yanuta
ISBN: 3540172351
ISBN13: 978-3540172352
Language: English
Publisher: Springer; Softcover reprint of the original 1st ed. 1987 edition (April 6, 1987)
Pages: 139
Fb2 eBook: 1332 kb
ePub eBook: 1361 kb
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by Michael I. Budyko (Author), Alexander B. Ronov (Author), Alexander L. Yanshin (Author), . Book Condition: A copy that has been read, but remains in clean condition. All pages are intact, and the cover is intact. The spine may show signs of wear.

by Michael I. Lemeshko (Translator), . Yanuta (Translator) & 2 more. ISBN-13: 978-3540172352. Pages can include limited notes and highlighting, and the copy can include previous owner inscriptions. An ex-library book and may have standard library stamps and/or stickers.

Michael I. Yanshin (author), S. F. Lemeshko (translator), V. . G. Yanuta (translator). The authors of this book have studied the changes in the chemi cal composition of the atmosphere during geological history with regard to its close relationship to the evolution of the Earth's sedimentary shell. Beginning in 1977, the initial results of this study have been published as articles and parts of several monographs.

The authors of this book have studied the changes in the chemi cal composition of the atmosphere during geological history with regard to its close relationship to the evolution of the Earth's sedimentary shell

The authors of this book have studied the changes in the chemi cal composition of the atmosphere during geological history with regard to its close relationship to the evolution of the Earth's sedimentary shell. Since new material clarifying atmospheric evolution have been obtained recently, the necessity has arisen to write a book treating the major results of investigations of the history of the atmosphere

by Michael I. Budyko, Alexander B. Ronov, Alexander L. Yanshin. The authors of this book have studied the changes in the chemi- cal composition of the atmosphere during geological history with regard to its close relationship to the evolution of the Earth's sedimentary shell

by Michael I. The authors of this book have studied the changes in the chemi- cal composition of the atmosphere during geological history with regard to its close relationship to the evolution of the Earth's sedimentary shell.

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Tag - paperback History of the Earth s Atmosphere by Michael I. Budyko. jeudi, février 22 2018. History of the Earth's Atmosphere pdf, epub, mobi. Michael I. Budyko,Alexander B. Ronov,Alexander L. Yanshin,S. Yanuta: History of the Earth's Atmosphere.

Informationen zum Titel History of the Earth's Atmosphere [mit Inhaltsverzeichnis und . Availability is subject to change.

Informationen zum Titel History of the Earth's Atmosphere Availability is subject to change. History of the Earth's Atmosphere Michael I. Yanshin (author) Springer Science+Business Media, 1987 . catalog.

History fo the earth's atmosphere. Budyko, A. B. In the geological past both the chemical composition of the atmosphere and its physical state, . The Heat and Water Balance of the Earth's Surface, the General Theory of Physical Geography and the Problem of the Transformation of Nature. Budyko, I. P. Gerasimov. The question of the chemical composition of the atmosphere of the past is covere. More).

A203410 240 10 Istorii͡a atmosfery. lEnglish 245 10 History of the Earth's atmosphere, c. Yanshin ;. 260 Berlin ;New York : bSpringer-Verlag, cc1987. 300 vi, 139 p. : bill. c24 cm. 500 Translation of: Istorii͡a atmosfery. 504 Bibliography: p. -136. 596 10 650 0 Atmosphere. A995137 650 0 Atmospheric chemistry. A995145 650 0 Climatic changes.

ABSTRACT: The abundant nitrogen in the Earth’s atmosphere can be interpreted as the result of endothermic nuclear transmutation of carbon and oxygen atom pairs in (Ca, D) CO3 or CaCO3 aragonite lattice of Earth’s crust from the Archean era to the present time, by physical catalytic.

ABSTRACT: The abundant nitrogen in the Earth’s atmosphere can be interpreted as the result of endothermic nuclear transmutation of carbon and oxygen atom pairs in (Ca, D) CO3 or CaCO3 aragonite lattice of Earth’s crust from the Archean era to the present time, by physical catalytic help of excited electrons e generated by stick sliding due to plate tectonics. and geoneutrinos ν by the radioactive decay of elements such as uranium and thorium in Earth’s mantle: through a nuclear attraction effect that is due to deuteron catalysis of nitrogen formation.

The authors of this book have studied the changes in the chemi­ cal composition of the atmosphere during geological history with regard to its close relationship to the evolution of the Earth's sedimentary shell. Beginning in 1977, the initial results of this study have been published as articles and parts of several monographs. Since new material clarifying atmospheric evolution have been obtained recently, the necessity has arisen to write a book treating the major results of investigations of the history of the atmosphere. In this book much consideration is given to the interrelation between the evolution of animate nature and changes in atmospheric composition. It proved be necessary to study the history of the two components of atmospheric air: carbon dioxide and oxygen. Attempts have been made to repre­ sent quantitatively the conclusions drawn here, i. e. to determine by calculation the changes in the amount of carbon dioxide and oxygen over much of the history of the atmosphere. These calculations, performed in most detail for the Phanerozoic and to a lesser degree for the Late Precambrian, are supplemented with estimates of changes in the chemical composition of the atmosphere in the Early Precambrian. Comparisons have been drawn between the changes in the chemical composition of the atmosphere and the development of animate nature, a close relationship being found to exist between the stages of the evolution of organisms and variations in the chemical composition of the atmosphere.
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