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Books on the topic 'Volatile elements'

Author: Grafiati

Published: 4 June 2021

Last updated: 25 May 2024

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1

Kallenbach, R., T. Encrenaz, J. Geiss, K. Mauersberger, T. C. Owen, and F. Robert, eds. Solar System History from Isotopic Signatures of Volatile Elements. Dordrecht: Springer Netherlands, 2003. http://dx.doi.org/10.1007/978-94-010-0145-8.

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2

B, McConnell James, United States. Dept. of the Army., US Army Signal Center and Fort Gordon. Environmental and Natural Resources Management Office., and Geological Survey (U.S.), eds. Trace elements and semi-volatile organic compounds in bed sediments from streams and impoundments at Fort Gordon, Georgia. Atlanta, Ga: U.S. Dept. of the Interior, U.S. Geological Survey, 2000.

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3

B, McConnell James, United States. Dept. of the Army, US Army Signal Center and Fort Gordon. Environmental and Natural Resources Management Office, and Geological Survey (U.S.), eds. Trace elements and semi-volatile organic compounds in bed sediments from streams and impoundments at Fort Gordon, Georgia. Atlanta, Ga: U.S. Dept. of the Interior, U.S. Geological Survey, 2000.

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4

B, McConnell James, United States. Dept. of the Army, US Army Signal Center and Fort Gordon. Environmental and Natural Resources Management Office, and Geological Survey (U.S.), eds. Trace elements and semi-volatile organic compounds in bed sediments from streams and impoundments at Fort Gordon, Georgia. Atlanta, Ga: U.S. Dept. of the Interior, U.S. Geological Survey, 2000.

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5

B, McConnell James, United States. Dept. of the Army, US Army Signal Center and Fort Gordon. Environmental and Natural Resources Management Office, and Geological Survey (U.S.), eds. Trace elements and semi-volatile organic compounds in bed sediments from streams and impoundments at Fort Gordon, Georgia. Atlanta, Ga: U.S. Dept. of the Interior, U.S. Geological Survey, 2000.

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6

B, McConnell James, United States. Dept. of the Army., US Army Signal Center and Fort Gordon. Environmental and Natural Resources Management Office., and Geological Survey (U.S.), eds. Trace elements and semi-volatile organic compounds in bed sediments from streams and impoundments at Fort Gordon, Georgia. Atlanta, Ga: U.S. Dept. of the Interior, U.S. Geological Survey, 2000.

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7

Mesko, Thomas O. Occurrence of pesticides, nitrate, volatile organic compounds, and trace elements in ground water and streams, southeastern Missouri, 1986-87. [Denver, Colo: Dept. of the Interior, U.S. Geological Survey, 1988.

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8

Mesko, Thomas O. Occurrence of pesticides, nitrate, volatile organic compounds, and trace elements in ground water and streams, southeastern Missouri, 1986-87. [Denver, Colo: Dept. of the Interior, U.S. Geological Survey, 1988.

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9

M, Carlson Gale, Missouri. Dept. of Health, Missouri. Dept. of Natural Resources, and Geological Survey (U.S.), eds. Occurrence of pesticides, nitrate, volatile organic compounds, and trace elements in ground water and streams, southeastern Missouri, 1986-87. [Denver, Colo: Dept. of the Interior, U.S. Geological Survey, 1988.

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10

Detra, D. E. A modification of the U.S. Geological Survey one-sixth order semiquantitative spectrographic method for the analysis of geologic materials that improves limits of determination of some volatile to moderately volatile elements. Denver, CO: U.S. Geological Survey, 1988.

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11

United States Geological Survey. A modification of the U.S. Geological Survey one-sixth order semiquantitative spectrographic method for the analysis of geologic materials that improves limits of determination of some volatile to moderately volatile elements. S.l: s.n, 1988.

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12

Detra, D. E. A modification of the U.S. Geological Survey one-sixth order semiquantitative spectrographic method for the analysis of geologic materials that improves limits of determination of some volatile to moderately volatile elements. Washington, DC: U.S. Dept. of the Interior, 1988.

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13

Houghton, Robert L. Volatile trace-element concentrations in snowmelt contributions to streams monitored by hydrologic bench-mark network stations in the conterminous United States where average annual snowfall exceeds 12 inches. Bismarck, N.D: U.S. Dept. of the Interior, Geological Survey, 1985.

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14

ISSI Workshop (2002 Bern, Switzerland). Solar system history from isotopic signatures of volatile elements: Volume resulting from an ISSI workshop, 14-18 January 2002, Bern, Switzerland. Dordrecht: Kluwer Academic Publishers, 2003.

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15

A, Colman John, Geological Survey (U.S.), and National Water-Quality Assessment Program (U.S.), eds. Surface-water-quality assessment of the Upper Illinois River basin in Illinois, Indiana, and Wisconsin: Data on manmade nonagricultural volatile and semivolatile organic chemicals in water, May 1988 through March 1990. [Urbana, IL]: U.S. Dept. of the Interior, U.S. Geological Survey, 1993.

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16

A, Colman John, Geological Survey (U.S.), and National Water Quality Assessment Program (U.S.), eds. Surface-water-quality assessment of the Upper Illinois River basin in Illinois, Indiana, and Wisconsin: Data on manmade nonagricultural volatile and semivolatile organic chemicals in water, May 1988 through March 1990. [Urbana, IL]: U.S. Dept. of the Interior, U.S. Geological Survey, 1993.

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17

A, Colman John, Geological Survey (U.S.), and National Water Quality Assessment Program (U.S.), eds. Surface-water-quality assessment of the Upper Illinois River basin in Illinois, Indiana, and Wisconsin: Data on manmade nonagricultural volatile and semivolatile organic chemicals in water, May 1988 through March 1990. [Urbana, IL]: U.S. Dept. of the Interior, U.S. Geological Survey, 1993.

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18

A, Colman John, Geological Survey (U.S.), and National Water Quality Assessment Program (U.S.), eds. Surface-water-quality assessment of the Upper Illinois River basin in Illinois, Indiana, and Wisconsin: Data on manmade nonagricultural volatile and semivolatile organic chemicals in water, May 1988 through March 1990. [Urbana, IL]: U.S. Dept. of the Interior, U.S. Geological Survey, 1993.

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19

B, Lowenstern Jacob, and Geological Survey (U.S.), eds. Major-element, trace-element, and volatile concentrations in silicate melt inclusions from the tuff of Pine Grove, Wah Wah Mountains, Utah. [Menlo Park, Calif.?]: U.S. Dept. of the Interior, U.S. Geological Survey, 1994.

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20

B, Lowenstern Jacob, and Geological Survey (U.S.), eds. Major-element, trace-element, and volatile concentrations in silicate melt inclusions from the tuff of Pine Grove, Wah Wah Mountains, Utah. [Menlo Park, Calif.?]: U.S. Dept. of the Interior, U.S. Geological Survey, 1994.

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21

B, Lowenstern Jacob, and Geological Survey (U.S.), eds. Major-element, trace-element, and volatile concentrations in silicate melt inclusions from the tuff of Pine Grove, Wah Wah Mountains, Utah. [Menlo Park, Calif.?]: U.S. Dept. of the Interior, U.S. Geological Survey, 1994.

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22

B, Lowenstern Jacob, and Geological Survey (U.S.), eds. Major-element, trace-element, and volatile concentrations in silicate melt inclusions from the tuff of Pine Grove, Wah Wah Mountains, Utah. [Menlo Park, Calif.?]: U.S. Dept. of the Interior, U.S. Geological Survey, 1994.

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23

B, Lowenstern Jacob, and Geological Survey (U.S.), eds. Major-element, trace-element, and volatile concentrations in silicate melt inclusions from the tuff of Pine Grove, Wah Wah Mountains, Utah. [Menlo Park, Calif.?]: U.S. Dept. of the Interior, U.S. Geological Survey, 1994.

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24

Illustrated Elements of Essential Oils (Illustrated Elements Of...). Element Books Ltd., 2002.

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25

Solar System History from Isotopic Signatures of Volatile Elements (Space Sciences Series of ISSI). Springer, 2003.

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26

Trace elements and semi-volatile organic compounds in bed sediments from streams and impoundments at Fort Gordon, Georgia. Atlanta, Ga: U.S. Dept. of the Interior, U.S. Geological Survey, 2000.

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27

Trace elements and semi-volatile organic compounds in bed sediments from streams and impoundments at Fort Gordon, Georgia. Atlanta, Ga: U.S. Dept. of the Interior, U.S. Geological Survey, 2000.

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28

Murphy, Mark A., and Emmett C. Murphy. Leading on the Edge of Chaos: The 10 Critical Elements for Success in Volatile Times. Prentice Hall Press, 2002.

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29

Trace elements and semi-volatile organic compounds in bed sediments from streams and impoundments at Fort Gordon, Georgia. Atlanta, Ga: U.S. Dept. of the Interior, U.S. Geological Survey, 2000.

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30

Trace elements and semi-volatile organic compounds in bed sediments from streams and impoundments at Fort Gordon, Georgia. Atlanta, Ga: U.S. Dept. of the Interior, U.S. Geological Survey, 2000.

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31

Murphy, Mark, and Emmett C. Murphy. Leading on the Edge of Chaos Prepack: The 10 Critical Elements for Success in Volatile Times with Poster. Prentice Hall, 2002.

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32

Solar System History from Isotopic Signatures of Volatile Elements: Volume Resulting from an ISSI Workshop 14-18 January 2002, Bern, Switzerland. Springer, 2012.

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33

Geiss, Johannes, Thérèse Encrenaz, Tobias Owen, R. Kallenbach, and Konrad Mauersberger. Solar System History from Isotopic Signatures of Volatile Elements: Volume Resulting from an ISSI Workshop 14-18 January 2002, Bern, Switzerland. Springer London, Limited, 2012.

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34

Surface-water-quality assessment of the Upper Illinois River basin in Illinois, Indiana, and Wisconsin: Data on manmade nonagricultural volatile and semivolatile organic chemicals in water, May 1988 through March 1990. [Urbana, IL]: U.S. Dept. of the Interior, U.S. Geological Survey, 1993.

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35

Surface-water-quality assessment of the Upper Illinois River basin in Illinois, Indiana, and Wisconsin: Data on manmade nonagricultural volatile and semivolatile organic chemicals in water, May 1988 through March 1990. [Urbana, IL]: U.S. Dept. of the Interior, U.S. Geological Survey, 1993.

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36

Surface-water-quality assessment of the Upper Illinois River basin in Illinois, Indiana, and Wisconsin: Data on manmade nonagricultural volatile and semivolatile organic chemicals in water, May 1988 through March 1990. [Urbana, IL]: U.S. Dept. of the Interior, U.S. Geological Survey, 1993.

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37

U.S. Department of the Interior. Assessment of Energetic Compounds, Semi-volatile Organic Compounds, and Trace Elements in Streambed Sediment and Stream Water from Streams Draining ... and Impact Areas, Fort Riley, Kansas, 2007?08. CreateSpace Independent Publishing Platform, 2014.

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38

Selin, Henrik, and Noelle Eckley Selin. Mercury Stories: Understanding Sustainability Through a Volatile Element. MIT Press, 2020.

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39

Riddle, Nick. The Damned. Liverpool University Press, 2019. http://dx.doi.org/10.3828/liverpool/9781911325529.001.0001.

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The Damned (1963) is the most intriguing of director Joseph Losey's British “journeyman” films. A sci-fi film by a director who hated sci-fi; a Hammer production that sat on the shelf for over two years before being released with almost no publicity as the second half of a double bill. Losey was a director vocal in his dislike of depictions of physical violence, but he often made films that radiate an energy produced by a violent clash of elements. The Damned catches a series of collisions — some of them inadvertent — and traps them as if in amber. Its volatile elements include Losey, the blacklisted director; Hammer, the erratic British studio, Oliver Reed, the 'dangerous' young actor, and radioactive children. This book concentrates on historical and cultural context, place, genre, and other themes in order to try to make sense of a fascinating, underappreciated film.

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40

Haines, David W., and Karen Rosenblum. Illegal Immigration in America. Greenwood Publishing Group, Inc., 1999. http://dx.doi.org/10.5040/9798400668326.

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Few issues have provoked as much controversy over the last decade as illegal immigration. While some argue for the need to seal America's borders and withdraw all forms of social and governmental support for illegal migrants and their children, others argue for humanitarian treatment—including legalization—for people who fill widely acknowledged needs in American industry and agriculture and have left home-country situations of economic hardship or political persecution. The study of illegal immigration necessarily confronts a broad range of migrants—from the familiar border crossers to those who enter illegally and overstay their visas, to the many unrecognized refugees who enter the country to seek protection under U.S. asylum law. The subject also demands attention to American society's responses to these newcomers—responses that often focus on limited elements of a complex issue. A comprehensive, up-to-date review of this volatile subject, this book provides an accessible, balanced introduction to the subject. Covering the full range of illegal immigrants from Mexican border crossers to Central American refugees, illegal Europeans, and smuggled Chinese, the book considers the kind of work the migrants do and the public response to them. The work is divided into four parts: Concepts, Policies, and Numbers; The Migrants and Their Work; The Responses; and Illegal Immigration in Perspective.

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41

Taliaferro, Jeffrey W. Defending Frenemies. Oxford University Press, 2019. http://dx.doi.org/10.1093/oso/9780190939304.001.0001.

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Defending Frenemies examines the nonproliferation strategies that the United States pursued toward vulnerable and often obstreperous allies in three volatile regions of the globe, the Middle East, South Asia, and East Asia, from the early 1960s to the early 1990s. It presents a historical and comparative analysis of how successive US presidential administrations (those of John F. Kennedy to George H. W. Bush) employed inducements and coercive diplomacy toward Israel, Pakistan, South Korea, and Taiwan over nuclear proliferation. Building upon neoclassical realism, Jeffrey W. Taliaferro argues that regional power dynamics and US domestic politics shaped the types of nonproliferation strategies pursued. The overriding goals of successive administrations were to contain the growth of the Soviet Union’s influence in the Middle East and South Asia, as well as to enlist China as an ally of convenience against the Soviets in East Asia. Weaker allies’ nuclear proliferation could facilitate or complicate the realization of those goals. When policymakers perceived an unfavorable regional power distribution and short-time horizons for emerging threats to US interests, they were inclined to pursue accommodative strategies toward an ally. Conversely, when they perceived a favorable regional power distribution and longer time horizons for threats, they were inclined to pursue coercive nonproliferation strategies toward an ally. However, congressional opposition to certain arms transfers and to nonproliferation legislation sometimes led administrations to pursue hybrid strategies—combining coercive and accommodating elements—toward nuclear proliferating allies.

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42

Drelichman, Mauricio, and Hans-Joachim Voth. Taxes, Debts, and Institutions. Princeton University Press, 2017. http://dx.doi.org/10.23943/princeton/9780691151496.003.0004.

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This chapter describes the fiscal institutions and borrowing instruments available to the Crown. The Castilian portfolio of fiscal and financial instruments was remarkably complete for its time. The revenue technology was a mix of useful adaptations of medieval legacy taxes combined with newer excises and trade duties. On the financing side, the Crown had both long- and short-term debt instruments at its disposal. Although the long-term juros (annuities and perpetuities) were technically nominative, they were widely traded in the secondary market, supplying a key element for the correct pricing of debt. On the short-term front, asientos—which refer to a wide variety of agreements—allowed the Crown to smooth the volatile silver revenues, leverage income outside the purview of the Cortes—Castile's representative assembly—and quickly shift resources throughout the empire.

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43

Trieloff, Mario. Noble Gases. Oxford University Press, 2017. http://dx.doi.org/10.1093/acrefore/9780190647926.013.30.

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This is an advance summary of a forthcoming article in the Oxford Encyclopedia of Planetary Science. Please check back later for the full article.Although the second most abundant element in the cosmos is helium, noble gases are also called rare gases. The reason is that they are not abundant on terrestrial planets like our Earth, which is characterized by orders of magnitude depletion of—particularly light—noble gases when compared to the cosmic element abundance pattern. Indeed, such geochemical depletion and enrichment processes make noble gases so versatile concerning planetary formation and evolution: When our solar system formed, the first small grains started to adsorb small amounts of noble gases from the protosolar nebula, resulting in depletion of light He and Ne when compared to heavy noble gases Ar, Kr, and Xe: the so-called planetary type abundance pattern. Subsequent flash heating of the first small mm to cm-sized objects (chondrules and calcium, aluminum rich inclusions) resulted in further depletion, as well as heating—and occasionally differentiation—on small planetesimals, which were precursors of larger planets and which we still find in the asteroid belt today from where we get rocky fragments in form of meteorites. In most primitive meteorites, we even can find tiny rare grains that are older than our solar system and condensed billions of years ago in circumstellar atmospheres of, for example, red giant stars. These grains are characterized by nucleosynthetic anomalies and particularly identified by noble gases, for example, so-called s-process xenon.While planetesimals acquired a depleted noble gas component strongly fractionated in favor of heavy noble gases, the sun and also gas giants like Jupiter attracted a much larger amount of gas from the protosolar nebula by gravitational capture. This resulted in a cosmic or “solar type” abundance pattern, containing the full complement of light noble gases. Contrary to Jupiter or the sun, terrestrial planets accreted from planetesimals with only minor contributions from the protosolar nebula, which explains their high degree of depletion and basically “planetary” elemental abundance pattern. Indeed this depletion enables another tool to be applied in noble gas geo- and cosmochemistry: ingrowth of radiogenic nuclides. Due to heavy depletion of primordial nuclides like 36Ar and 130Xe, radiogenic ingrowth of 40Ar by 40K decay, 129Xe by 129I decay, or fission Xe from 238U or 244Pu decay are precisely measurable, and allow insight in the chronology of fractionation of lithophile parent nuclides and atmophile noble gas daughters, mainly caused by mantle degassing and formation of the atmosphere.Already the dominance of 40Ar in the terrestrial atmosphere allowed C. F v. Weizsäcker to conclude that most of the terrestrial atmosphere originated by degassing of the solid Earth, which is an ongoing process today at mid ocean ridges, where primordial helium leaves the lithosphere for the first time. Mantle degassing was much more massive in the past; in fact, most of the terrestrial atmosphere formed during the first 100 million years of Earth´s history, and was completed at about the same time when the terrestrial core formed and accretion was terminated by a giant impact that also formed our moon. However, before that time, somehow also tiny amounts of solar noble gases managed to find their way into the mantle, presumably by solar wind irradiation of small planetesimals or dust accreting to Earth. While the moon-forming impact likely dissipated the primordial atmosphere, today´s atmosphere originated by mantle degassing and a late veneer with asteroidal and possibly cometary contributions. As other atmophile elements behave similar to noble gases, they also trace the origin of major volatiles on Earth, for example, water, nitrogen, sulfur, and carbon.

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