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Books on the topic 'Isotopen'

Author: Grafiati

Published: 4 June 2021

Last updated: 31 January 2023

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1

Christoph, Gernot. Beiträge zur Theorie der Isotopen- und Elementgeochemie. Zentralinstitut für Isotopen- und Strahlenforschung, Akademie der Wissenschaften der DDR, 1988.

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2

Arnikar, Hari Jeevan. Isotopes in the atomic age. Wiley Eastern, 1989.

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3

Isotopes in the atomic age. Wiley, 1989.

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4

Segschneider, Hans-Josef. Untersuchungen zur Aufnahme und zum Einbau von anthropogenen Stickoxiden (NOx) durch Sonnenblumen und Mais mittels 15N-Isotopen-Markierung. Forschungszentrum Jülich GmbH, Zentralbibliothek, 1994.

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5

Stable isotope geochemistry. 5th ed. Springer, 2004.

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6

Faure, Gunter. Principles of isotope geology. 2nd ed. Wiley, 1986.

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7

Stable isotope geochemistry. 3rd ed. Springer-Verlag, 1987.

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8

W, Valley John, Cole David R, and Mineralogical Society of America, eds. Stable isotope geochemistry. Mineralogical Society of America, 2001.

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9

Principles of isotope geology. 2nd ed. Wiley, 1986.

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10

Stable isotope geochemistry. 4th ed. Springer, 1997.

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11

Spivack, Arthur J. Boron isotope geochemistry. Woods Hole Oceanographic Institution, 1986.

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12

Symons, E. A. Lithium isotope separation: A review of possible techniques. CFFTP, 1985.

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13

M, Johnson Clark, Beard Brian L, Albarède Francis, American Geophysical Union Meeting, and Canadian Geophysical Union Meeting, eds. Geochemistry of non-traditional stable isotopes. Mineralogical Society of America, 2004.

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14

Krämer, Hans Georg. Uranisotopentrennung in Zentrifugen. Deutsches Atomforum, 1985.

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15

Attendorn, H. G. Radioactive and stable isotope geology. Chapman & Hall, 1997.

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16

Kashcheev, N. A. Ėlektromagnitnoe razdelenie izotopov i izotopnyĭ analiz. Ėnergoatomizdat, 1989.

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17

Niebler, Hans-Stefan. Rekonstruktionionen von Paläo-Umweltparametern anhand von stabilen Isotopen und Faunen-Vergesellschaftlungen planktischer Foraminiferen im Südatlantik =: Reconstruction of paleo-environmental parameters using stable isotopes and faunal assemblages of planktonic foraminifera in the South Atlantic Ocean. Alfred-Wegener-Institut für Polar- und Meeresforschung, 1995.

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18

Introduction to isotope hydrology: Stable and radioactive isotopes of hydrogen, oxygen and carbon. Taylor & Francis, 2006.

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19

Godwin, Colin I. Leadtable: A galena lead isotope data base for the Canadian Cordillera, with a guide to its use by explorationists. Mineral Resources Division, Geological Survey Branch, 1988.

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20

Tian ran qi tan qing tong wei su fen liu dong li xue ji qi ying yong. Shi you gong ye chu ban she, 2010.

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21

1938-, Coleman David C., and Fry Brian, eds. Carbon isotope techniques. Academic Press, 1991.

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22

Godwin, Colin I. Leadtable: A galena lead isotope data base for the Canadian Cordillera, with a guide to its use by explorationists. Ministry of Energy, Mines and Petroleum Resources, 1988.

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23

Japan-CIS Workshop on Interactions of Fuel Particles with Fusion Materials (1st 1992 University of Tokyo). Proceedings of Japan-CIS Workshop on Interactions of Fuel Particles with Fusion Materials (IFPFM), at University of Tokyo, Tokyo, Japan, on December 1-4, 1992. Edited by Yamawaki M, Nihon Genshiryoku Gakkai, and Tōkyō Daigaku. Genshiryoku Kōgaku Kenkyū Shisetsu. The Laboratory, 1993.

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24

Fachtagung, Kammer der Technik. Rechentechnik in der Isotopen- und Strahlenforschung: Ausgewählte Vorträge der KdT-Fachtagung, Gerode, 29.10-1.11. 1985. Verbesserung der Informationsversorgung der Forschung durch Datenaustausch zwischen grossen und kleinen Informationsfonds. Akademie der Wissenschaften der DDR, Zentralinstitut für Isotopen- und Strahlenforschung, 1986.

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25

Marschall, Horst, and Gavin Foster, eds. Boron Isotopes. Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-64666-4.

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26

Menkhoff, Herbert. Raumgewichtsbestimmung Mit Radioaktiven Isotopen. VS Verlag fur Sozialwissenschaften GmbH, 2013.

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27

Ellam, Rob. 4. Measuring isotopes. Oxford University Press, 2016. http://dx.doi.org/10.1093/actrade/9780198723622.003.0004.

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‘Measuring isotopes: counting the atoms’ explores how isotopes are measured. For stable isotopes, atoms of each isotope are counted using a mass spectrometer. This turns atoms into charged ions and separates them into the different isotopic species using a mass filter. Precise measurements of isotopic abundance can be achieved in a few minutes or hours. Mass spectrometry could be used for radioactive isotopes, but for short-lived isotopes, their low abundance often makes them difficult to detect. The alternative is to use nuclear spectroscopy or counting methods to detect the characteristic en

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28

Neue Ergebnisse zur Isotopen- und Strahlenforschung. Das Institut, 1986.

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29

Opitz, Herwart. Standzeituntersuchungen und Verschleißmessungen Mit Radioaktiven Isotopen. VS Verlag fur Sozialwissenschaften GmbH, 2013.

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30

Rauschenbach, P., R. Tykva, Simon H, and H. L. Schmidt. Messung Von Radioaktiven und Stabilen Isotopen. Springer London, Limited, 2013.

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31

Wenzel, M., P. Rauschenbach, H. L. Schmidt, R. Tykva, and Simon H. Messung von radioaktiven und stabilen Isotopen. Springer, 2011.

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32

Nuclear Development Beneficial Uses and Production of Isotopes: 2004 Update (Nuclear Development). Nuclear Energy Agency, 2005.

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33

Agency, OECD Nuclear Energy, and Organisation for Economic Co-operation and Development., eds. Beneficial uses and production of isotopes: 2004 update. Nuclear Energy Agency, Organisation for Economic Co-operation and Development, 2005.

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34

Kauw, Gisela. Untersuchungen an Angereicherten Isotopen Auf Natürliche Alphastrahlung. VS Verlag fur Sozialwissenschaften GmbH, 2013.

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35

Melville, Harry W. Die Anwendung Von Radioaktiven Isotopen und Hoher Energiestrahlung in der Polymeren Chemie. VS Verlag fur Sozialwissenschaften GmbH, 2013.

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36

Ellam, Rob. 6. Measuring isotopes. Oxford University Press, 2016. http://dx.doi.org/10.1093/actrade/9780198723622.003.0006.

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Mass spectrometers have become routine laboratory instruments in many disciplines. ‘Measuring isotopes: mass spectrometers’ concentrates on those used to quantify the abundance of different isotopes—gas source isotope ratio, thermal ionization, inductively coupled plasma, and secondary ion mass spectrometers. A mass spectrometer can be used to quantify the concentration of a particular element by monitoring an isotope of that element not overlapped by isotopes of other elements. All mass spectrometers have three essential components: an ion source, a mass filter, and a detector. There are two

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37

Ellam, Rob. Isotopes. Oxford University Press, 2016. http://dx.doi.org/10.1093/actrade/9780198723622.001.0001.

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An isotope is a variant form of a chemical element, containing a different number of neutrons in its nucleus. Most elements exist as several isotopes. Many are stable, others are radioactive, and some may only exist fleetingly before decaying into other elements. The study of isotope ratios has become central to many areas of science, and used to probe the age and history of the Earth and the origins of the Solar System. Radioactive isotopes find wide applications, from nuclear power to medicine and carbon dating. Isotopes: A Very Short Introduction provides an overview of the nature of stable

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38

Ellam, Rob. 8. Scratching the surface with cosmogenic isotopes. Oxford University Press, 2016. http://dx.doi.org/10.1093/actrade/9780198723622.003.0008.

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‘Scratching the surface with cosmogenic isotopes’ explains spallation—when a high energy cosmic ray particle removes several nucleons from an atom. Spallation produces 10Be from 16O in the atmosphere and rock surfaces, while spallation of silicon produces another cosmogenic isotope, 26Al. Cosmogenic isotope production is about four times greater at the poles than at the equator and is also greater at higher altitudes. To calculate a cosmogenic isotope exposure age, the latitude and altitude at which the sample was exposed needs to be known. Using ‘exposure’ and ‘burial’ methodologies, cosmogen

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39

Ellam, Rob. 3. You are what you eat … plus a few per mil. Oxford University Press, 2016. http://dx.doi.org/10.1093/actrade/9780198723622.003.0003.

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‘You are what you eat … plus a few per mil’ explains delta notation and organic isotopic fractionation. An isotopic balance has to be maintained, so the isotopic fractionation into a mineral crystallizing from a fluid will be balanced by a change in the isotopic composition of the remaining fluid. Carbon, nitrogen, oxygen, and strontium isotope values can be measured through the food chain and in animal and human bones. There is also a geographical oxygen isotope zonation, but this is disrupted by major changes in topography. Isotopic measurements helped in identifying King Richard III’s bones

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40

H. P., Jr. Taylor (Editor), ed. Stable Isotopes in High Temperature Geological Processes (Reviews in Mineralogy, Vol 16). Mineralogical Society of America, 1986.

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41

(Editor), S. A. Abrams, and W. W. Wong (Editor), eds. Stable Isotopes in Human Nutrition: Laboratory Methods and Research Applications (Life Sciences). CABI, 2003.

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42

M, Andreev B., ed. Separation of isotopes of biogenic elements in two-phase systems. Elsevier, 2007.

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43

Ellam, Rob. 2. Isotopic clocks. Oxford University Press, 2016. http://dx.doi.org/10.1093/actrade/9780198723622.003.0002.

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About one in a trillion atoms of carbon is the radioactive isotope 14C. It is a ‘cosmogenic isotope’ produced by the interaction between atmospheric nitrogen (N) and cosmic rays. The half-life of 14C is 5,730 years, so every 5,730 years the ratio of 14C to 12C will halve. ‘Isotopic clocks: the persistence of carbon’ describes how scientists Willard Libby, Hessel de Vries, Hans Seuss, and their contemporaries established the radiocarbon dating technique. Radiocarbon has become one of the most valuable isotopic tools available to scientists looking to date materials formed over the past 50,000 y

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44

Ellam, Rob. 11. Cosmic stopped clocks. Oxford University Press, 2016. http://dx.doi.org/10.1093/actrade/9780198723622.003.0011.

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‘Cosmic stopped clocks’ explains how, using isotopes that are the daughters of isotopes that no longer exist, isotope geochemistry has been able to assemble a chronology for the formation and growth of the Solar System and the Earth. Our Solar System began around 4.5 billion years ago. Within a few million years, the earliest solid minerals crystallized. After about ten million years, small astronomical bodies had formed and, within 100 million years, the planets had not only formed but had differentiated into bodies fundamentally similar to the Earth we live on.

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45

Hoefs, Jochen. Stable Isotope Geochemistry. Springer, 2015.

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46

Hoefs, Jochen. Stable Isotope Geochemistry. Springer London, Limited, 2015.

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47

Hoefs, Jochen. Stable Isotope Geochemistry. Springer, 2010.

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48

Allègre, Claude J., and Christopher Sutcliffe. Isotope Geology. Cambridge University Press, 2012.

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49

(Translator), Christopher Sutcliffe, ed. Isotope Geology. Cambridge University Press, 2008.

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50

Hoefs, Jochen. Stable Isotope Geochemistry. Springer London, Limited, 2013.

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