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Books on the topic 'Isotopic model'

Author: Grafiati
Published: 10 March 2023

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1

Thorstenson, Donald C. Calculation of individual isotope equilibrium constants for implementation in geochemical models. Denver, Colo: U.S. Dept. of the Interior, U.S. Geological Survey, 2002.

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2

Poli͡achenko, A. L. Chislennye metody v i͡adernoĭ geofizike. Moskva: Ėnergoatomizdat, 1987.

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3

Okazaki, Atsushi. Development of stable water isotope incorporated atmosphere-land coupled model and comparison with climate proxies. Tokyo]: Division of Climate System Research, Atmosphere and Ocean Research Institute, The University of Tokyo, 2018.

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4

1948-, Bassett R. L., Woodhouse E. G, and U.S. Nuclear Regulatory Commission. Office of Nuclear Regulatory Research. Division of Regulatory Applications., eds. Field studies at the Apache Leap Research Site in support of alternative conceptual models. Washington, D.C: Division of Regulatory Applications, Office of Nuclear Regulatory Research, U.S. Nuclear Regulatory Commission, 1997.

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5

Hirose, Akira. Anomalous electron thermal diffusivity, anomalous particle pinch and isotope effect due to the skin size electromagnetic drift mode. Saskatoon, Sask: University of Saskatchewan, Plasma Physics Laboratory, 1990.

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6

Sedimentation rate through environmental radioactivity: Models and applications. Hamilton, Ont: Environmental Research & Publications, 2002.

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7

Duffield, Wendell A. A model to help explain Sr-isotope disequilibrium between feldspar phenocrysts and melt in large-volume silicic magma systems. [Menlo Park, Calif.?]: U.S. Dept. of the Interior, U.S. Geological Survey, 1994.

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8

Kelly, Brian P. Ground-water flow simulation and chemical and isotopic mixing equation analysis to determine source contributions to the Missouri River alluvial aquifer in the vicinity of the Independence, Missouri, well field. Rolla, Mo: U.S. Dept. of the Interior, U.S. Geological Survey, 2002.

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9

Kelly, Brian P. Ground-water flow simulation and chemical and isotopic mixing equation analysis to determine source contributions to the Missouri River alluvial aquifer in the vicinity of the Independence, Missouri, well field. Rolla, Mo: U.S. Dept. of the Interior, U.S. Geological Survey, 2002.

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10

Kelly, Brian P. Ground-water flow simulation and chemical and isotopic mixing equation analysis to determine source contributions to the Missouri River alluvial aquifer in the vicinity of the Independence, Missouri, well field. Rolla, Mo: U.S. Dept. of the Interior, U.S. Geological Survey, 2002.

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11

Kelly, Brian P. Ground-water flow simulation and chemical and isotopic mixing equation analysis to determine source contributions to the Missouri River alluvial aquifer in the vicinity of the Independence, Missouri, well field. Rolla, Mo: U.S. Dept. of the Interior, U.S. Geological Survey, 2002.

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12

Kelly, Brian P. Ground-water flow simulation and chemical and isotopic mixing equation analysis to determine source contributions to the Missouri River alluvial aquifer in the vicinity of the Independence, Missouri, well field. Rolla, Mo: U.S. Dept. of the Interior, U.S. Geological Survey, 2002.

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13

Koerner, Terry. Using kinetic isotope effects to model the transition states for the sn2 reactions between sodium borohydride and para-substituted benzyl chlorides. Sudbury, Ont: Laurentian University Press, 1996.

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14

Zakrzewska-Trznadel, Grażyna. Procesy membranowe w technologiach jądrowych: Wybrane zagadnienia modelowania transportu masy oraz projektowania systemów rozdzielania. Warszawa: Instytut Chemii i Techniki Jądrowej, 2006.

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15

Zakrzewska-Trznadel, Grażyna. Procesy membranowe w technologiach jądrowych: Wybrane zagadnienia modelowania transportu masy oraz projektowania systemów rozdzielania. Warszawa: Instytut Chemii i Techniki Jądrowej, 2006.

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16

F, Badavi F., Tripathi Ram K, and United States. National Aeronautics and Space Administration., eds. Shielding from space radiations: Annual technical report : period, December 1, 1992 through June 1, 1993. Newport News, Va: Christopher Newport University, 1993.

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17

Shukla, Bhagwan S. Diffusion coefficient and mixing depth through environmental radioactivity (models and applications). Hamilton, Ont: Environmental Research & Publications, 2010.

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18

Measurements, National Council on Radiation Protection and. Some aspects of strontium radiobiology. Bethesda, MD: The Council, 1991.

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19

Surkova, Galina. Atmospheric chemistry. ru: INFRA-M Academic Publishing LLC., 2021. http://dx.doi.org/10.12737/1079840.

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The textbook contains material corresponding to the course of lectures on atmospheric chemistry prepared for students studying meteorology and climatology. The basic concepts of atmospheric chemistry are given, its gaseous components, as well as aerosols and chemical processes related to their life cycles, which are important from the point of view of the formation of the radiation, temperature and dynamic regime of the atmosphere, as well as its pollution, are considered. The main regularities of the transport of impurities in the atmosphere and the role of processes of different spatial and temporal scales in this process are presented. The concept of approaches of varying degrees of complexity used to model the transport of matter in the atmosphere, taking into account its chemical transformations, is presented. The processes in the gaseous and liquid phases that affect the chemical composition and acidity of clouds and precipitation are described. Modern methods of using information about the concentration and state of chemical compounds, including their radioactive and stable isotopes, to obtain information about the meteorological regime of the atmosphere in the present and past are considered. Meets the requirements of the federal state educational standards of higher education of the latest generation. For students of higher educational institutions studying in the field of training "Hydrometeorology".
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20

Kolář, Miroslav. Near-field mass transport from a point source (instantaneously failed container) located in a disposal room. Pinawa, Man: Whiteshell Laboratories, 1995.

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21

Miroslav, Kolár, LeNeveu Dennis M, and Atomic Energy of Canada Limited., eds. Near-field mass transport from a point source (instantaneously failed container) located in a disposal room. Chalk River, Ont: Chalk River Nuclear Laboratories, 1995.

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22

Pham, Thuy Van. Using isotope effects to model transition states for carbocation-nucleophile combination reactions. U of Toronto, 1999.

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23

Eckardt, Hella, and Gundula Müldner. Mobility, Migration, and Diasporas in Roman Britain. Edited by Martin Millett, Louise Revell, and Alison Moore. Oxford University Press, 2014. http://dx.doi.org/10.1093/oxfordhb/9780199697731.013.012.

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This chapter examines the main sources of evidence for mobility in the Roman period, focusing on epigraphy, material culture, and new scientific techniques, specifically isotopic analysis, evaluating strengths and weaknesses of each approach. Employing diaspora theory and hybridization models, it also asks broader questions of how interactions and relationships between incomers and locals can be modelled. Finally, and acknowledging that there is now an increased awareness of the political context in which research on emotive themes such as migration is conceived and conducted, we review some recently developed educational resources and their potential impact on public perceptions of mobility in the past.
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24

Higgins, John Andrew. The global carbon cycle on geologic timescales: Insights from magnesium isotopes and numerical models. 2009.

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25

Tuolumne Meadows quadrangle, California -- analytic data: Modal, chemical, and isotopic data for the granitic rocks of the Tuolumne Meadows quadrangle. Washington: U.S. G.P.O., 1988.

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26

Testing of environmental transfer models using data from the atmospheric release of iodine-131 from the Hanford Site, USA, in 1963: Report ; theme 2. Vienna, Austria: International Atomic Energy Agency, 2003.

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27

Assessment, Biosphere Modelling and. Testing of Environmental Transfer Models Using Data from the Atmospheric Release of Iodine-131 from the Hanford Site, USA, in 1963 (IAEA-Biomass). International Atomic Energy Agency, 2003.

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28

Raghunathan, Karthik, and Andrew Shaw. Crystalloids in critical illness. Oxford University Press, 2016. http://dx.doi.org/10.1093/med/9780199600830.003.0057.

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‘Crystalloid’ refers to solutions of crystalline substances that can pass through a semipermeable membrane and are distributed widely in body fluid compartments. The conventional Starling model predicts transvascular exchange based on the net balance of opposing hydrostatic and oncotic forces. Based on this model, colloids might be considered superior resuscitative fluids. However, observations of fluid behaviour during critical illness are not consistent with such predictions. Large randomized controlled studies have consistently found that colloids offer no survival advantage relative to crystalloids in critically-ill patients. A revised Starling model describes a central role for the endothelial glycocalyx in determining fluid disposition. This model supports crystalloid utilization in most critical care settings where the endothelial surface layer is disrupted and lower capillary pressures (hypovolaemia) make volume expansion with crystalloids effective, since transvascular filtration decreases, intravascular retention increases and clearance is significantly reduced. There are important negative consequences of both inadequate and excessive crystalloid resuscitation. Precise dosing may be titrated based on functional measures of preload responsiveness like pulse pressure variation or responses to manoeuvres such as passive leg raising. Crystalloids have variable electrolyte concentrations, volumes of distribution, and, consequently variable effects on plasma pH. Choosing balanced crystalloid solutions for resuscitation may be potentially advantageous versus ‘normal’ (isotonic, 0.9%) saline solutions. When used as the primary fluid for resuscitation, saline solutions may have adverse effects in critically-ill patients secondary to a reduction in the strong ion difference and hyperchloraemic, metabolic acidosis. Significant negative effects on immune and renal function may result as well.
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29

Bethke, Craig M. Geochemical Reaction Modeling. Oxford University Press, 1996. http://dx.doi.org/10.1093/oso/9780195094756.001.0001.

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Geochemical reaction modeling plays an increasingly vital role in several areas of geoscience, from environmental geochemistry and petroleum geology to the study of geothermal and hydrothermal fluids. This book provides an up-to-date overview of the use of numerical methods to model reaction processes in the Earth's crust and on its surface. Early chapters develop the theoretical foundations of the field, derive a set of governing equations, and show how numerical methods can be used to solve these equations. Other chapters discuss the distribution of species in natural waters; methods for computing activity coefficients in dilute solutions and in brines; the complexation of ions into mineral surfaces; the kinetics of precipitation and dissolution reactions; and the fractionation of stable isotopes. Later chapters provide a large number of fully worked calculation examples and case studies demonstrating the modeling techniques that can be applied to scientific and practical problems. Students in a variety of specialties from low-temperature geochemistry to groundwater hydrology will benefit from the wealth of information and practical applications this book has to offer.
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30

Attardo, Salvatore. The Linguistics of Humor. Oxford University Press, 2020. http://dx.doi.org/10.1093/oso/9780198791270.001.0001.

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This book is the first comprehensive systematic introduction to the linguistics of humor. Assuming no background in humor studies at all, and an elementary knowledge of linguistics, all the terminology and conceptual apparatus of humor studies are introduced, as well as all the linguistic concepts necessary to understand the most up-to-date formulations in the linguistics and applied linguistics of humor. The book is not limited to the theoretical linguistic analyses of humor (for example the General Theory of Verbal humor or the Isotopy Disjunction Model), but has a broad approach encompassing pragmatics, conversation and discourse analysis, ethnomethodology, interactionist and variationist sociolinguistics. Chapters on puns, on the main theories of humor, the semiotics of humor, and on the incongruity-resolution model elucidate the foundations of humor studies, while chapters on the performance of humor, on humor in conversation and discourse, provide the first-ever in-depth discussion and synthesis of the field of the applied linguistics of humor. Chapters on the translation of humor, and on humor in the classroom and in literature broaden the discussion to applications in fields other than linguistics. For the first time ever in a discussion of the linguistics of humor all the fields of linguistics, theoretical and applied alike are given equal treatment and theoretical importance. Thus this book is both a summary of the acquired knowledge about humor and linguistics and a proposal to unify most of the strands of research in a coherent vision.
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31

Walker, James C. G. Numerical Adventures with Geochemical Cycles. Oxford University Press, 1991. http://dx.doi.org/10.1093/oso/9780195045208.001.0001.

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The dynamic, evolving Earth, and the mathematical representation of its geochemical changes are the subject of this timely, helpful handbook. Global warming, changes in the ocean, and the effects of fossil fuel combustion are just a few of the phenomena that make the development of geochemical models critical. But what computational methods will help to accurately carry out this task? This new text teaches the methodology of computational simulation of environmental change. The author presents interesting applications of his methods to describe the response of the ocean and atmosphere to the infusion of pollutants, the effect of evaporation on seawater composition, climate change, and many other aspects of the Earth's evolving ecosystem. He also presents simple approaches for solving non-linear systems, calculating isotope ratios, and dealing with chains of identical reservoirs. With creative programs that can be executed on any personal computer, Walker offers earth scientists the techniques necessary to address the key problems in their field.
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32

Clarke, Andrew. Temperature and its measurement. Oxford University Press, 2017. http://dx.doi.org/10.1093/oso/9780199551668.003.0003.

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Temperature is that property of a body which determines whether it gains or loses energy in a particular environment. In classical thermodynamics temperature is defined by the relationship between energy and entropy. Temperature can be defined only for a body that is in thermodynamic and thermal equilibrium; whilst organisms do not conform to these criteria, the errors in assuming that they do are generally small. The Celsius and Fahrenheit temperature scales are arbitrary because they require two fixed points, one to define the zero and the other to set the scale. The thermodynamic (absolute) scale of temperature has a natural zero (absolute zero) and is defined by the triple point of water. Its unit of temperature is the Kelvin. The Celsius scale is convenient for much ecological and physiological work, but where temperature is included in statistical or deterministic models, only thermodynamic temperature should be used. Past temperatures can only be reconstructed with the use of proxies, the most important of which are based on isotope fractionation.
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