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Libros sobre el tema "Isotopies"

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Publicado: 11 de marzo de 2023

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1

1959-, Kadeisvili J. V. y Santilli Ruggero Maria 1935-, eds. Isotopies of contemporary mathematical structures. Palermo: Sede della società, 1996.

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2

Kadeisvili, J. V. Santilli's isotopies of contemporary algebras, geometries, and relativities. Palm Harbor, FL, U.S.A: Hadronic Press, 1992.

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3

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

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4

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

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5

Isotopes in the atomic age. New York: Wiley, 1989.

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6

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

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7

W, Valley John, Cole David R y Mineralogical Society of America, eds. Stable isotope geochemistry. Washington, D.C: Mineralogical Society of America, 2001.

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8

Principles of isotope geology. 2a ed. New York: Wiley, 1986.

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9

Stable isotope geochemistry. 4a ed. Berlin: Springer, 1997.

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10

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

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11

Stable isotope geochemistry. 5a ed. Berlin: Springer, 2004.

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12

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

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13

Stable isotope geochemistry. 3a ed. Berlin: Springer-Verlag, 1987.

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14

Faure, Gunter. Principles of isotope geology. 2a ed. New York: Wiley, 1986.

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15

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

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16

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

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17

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

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18

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

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19

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

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20

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

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21

Tom, Edwards, Kull Christoph y Alverson Keith, eds. Stable isotopes. Bern, Switzerland: PAGES International Project Office, 2002.

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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. Victoria, B.C., Canada: Mineral Resources Division, Geological Survey Branch, 1988.

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23

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

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24

1938-, Coleman David C. y Fry Brian, eds. Carbon isotope techniques. San Diego: Academic Press, 1991.

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25

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

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26

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. Editado por Yamawaki M, Nihon Genshiryoku Gakkai y Tōkyō Daigaku. Genshiryoku Kōgaku Kenkyū Shisetsu. Tokyo, Japan: The Laboratory, 1993.

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27

S, Shirley Virginia, ed. Table of isotopes. 8a ed. New York: Wiley, 1996.

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28

William, Walker F., Parrington Josef R, Feiner Frank y General Electric Company, eds. Nuclides and isotopes. San Jose, Calif: General Electric Co., 1989.

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29

Firestone, Richard B. Table of isotopes. Editado por Baglin Coral M. 1939-. 8a ed. New York: Wiley, 1998.

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30

Bowen, Robert. Isotopes and climates. London: Elsevier Applied Science, 1991.

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31

Kadeisvili, J. V. Isotopies of Contemporary Algebras, Geometries, and Relativities. 2a ed. Hadronic Pr, 1997.

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32

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 energy released by the radioactive decay of a particular isotope, but these can be much longer processes.
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33

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 main types of detector: Faraday detectors measure large signals and a variant of photomultiplier tubes measures small isotope signals.
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34

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 and radioactive isotopes, considering their wide range of modern applications.
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35

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, cosmogenic isotopes can be used to address various scientific problems such as recreating the seismic histories of tectonically active areas.
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36

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 and providing background to the life of the 5,000-year-old ‘Ötzi the Iceman’ found in the Ötztal Alps.
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37

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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38

Beard, Brian L., Francis Albarède y Clark M. Johnson. Geochemistry of Non-Traditional Stable Isotopes. de Gruyter GmbH, Walter, 2018.

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39

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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40

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 years or to trace and apportion different sources of carbon.
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41

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

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42

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

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43

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

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44

Allègre, Claude J. y Christopher Sutcliffe. Isotope Geology. Cambridge University Press, 2008.

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45

Allègre, Claude J. y Christopher Sutcliffe. Isotope Geology. Cambridge University Press, 2008.

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46

Stable Isotope Geochemistry. Springer International Publishing AG, 2021.

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47

Hoefs, Jochen. Stable Isotope Geochemistry. Springer, 2019.

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48

Hoefs, Jochen. Stable Isotope Geochemistry. Springer International Publishing AG, 2022.

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49

Hoefs, Jochen. Stable Isotope Geochemistry. Springer, 2018.

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50

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

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