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Changes in stable carbon isotopes of methane along a salinity gradient in a hypersaline microbial mat systemPotter, Elyn. January 2007 (has links)
Thesis (M.S.)--University of Missouri-Columbia, 2007. / The entire dissertation/thesis text is included in the research.pdf file; the official abstract appears in the short.pdf file (which also appears in the research.pdf); a non-technical general description, or public abstract, appears in the public.pdf file. Title from title screen of research.pdf file (viewed on November 1, 2007) Includes bibliographical references.
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Dating the paleobeaches of Pampa Mejillones, northern Chile, by cosmogenic chlorine-36Almasi, Peter Ferenc. January 2001 (has links) (PDF)
Thesis (M.S. - Hydrology and Water Resources)--University of Arizona. / Includes bibliographical references (leaves 119-128).
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The use of ostracoda in the palaeoenvironmental reconstruction of the Gulf of Carpentaria, Australia, from the last interglacial to presentReeves, Jessica Marie. January 2004 (has links)
Thesis (Ph.D.)--University of Wollongong, 2004. / Typescript. Includes bibliographical references: p. 366-393.
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Mudgases geochemistry and factors controlling their variabilityVlad, Daniela. January 2010 (has links)
Thesis (Ph.D.)--University of Alberta, 2010. / Title from PDF file main screen (viewed on Apr. 13, 2010). A thesis submitted to the Faculty of Graduate Studies and Research in partial fulfillment of the requirements for the degree of Doctor of Philosophy, Department of Earth and Atmospheric Sciences, University of Alberta. Includes bibliographical references.
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The production of high specific activity radionuclides for radiotherapy application /Jia, Wei, January 1996 (has links)
Thesis (Ph. D.)--University of Missouri-Columbia, 1996. / Typescript. Vita. Includes bibliographical references (leaves 120-126). Also available on the Internet.
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The production of high specific activity radionuclides for radiotherapy applicationJia, Wei, January 1996 (has links)
Thesis (Ph. D.)--University of Missouri-Columbia, 1996. / Typescript. Vita. Includes bibliographical references (leaves 120-126). Also available on the Internet.
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Etude du probleme de l'origine des carbonatites au moyen des isotopes du carbone et de l'oxygenePineau, Françoise. January 1900 (has links)
Thesis (doctoral)--Faculté des sciences de Paris, (197-?). / Includes bibliographical references (leaves [43]-[46]).
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Assessing the effects of LXR agonists in cholesterol handling: stable isotope tracer studies /Aravindhan, Karpagam. Jucker, Beat M. DiNardo, N. John. January 2005 (has links)
Thesis (Ph. D.)--Drexel University, 2005. / Includes abstract and vita. Includes bibliographical references (leaves 191-199).
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Comparison of four trace element extractants by isotope dilution analysisVale, Rui Ramos do. January 1982 (has links)
Thesis (M.S.)--University of Wisconsin--Madison, 1982. / Typescript. eContent provider-neutral record in process. Description based on print version record. Includes bibliographical references (leaves 112-116).
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Nitrogen Transport and Connectivity in two Wetland-Rich Boreal sites in the Athabasca Oil Sands Region, CanadaCherry, Mikaela 13 January 2016 (has links)
Development of the Athabasca Oil Sands Region (AOSR) has increased atmospheric
nitrogen emissions, a trend which is expected to increase in the future. The area
surrounding development is comprised of Boreal upland forests and peatlands. Improved
understanding of the hydrological connectivity between Boreal peatlands and uplands is
needed to predict the fate and transport of atmospheric N deposited across the region. Two
field sites: Jack Pine High (JPH, located 45 km north of Fort McMurray) and Mariana
Lakes (ML, located 100 km south of Fort McMurray) were instrumented with piezometers
nests and water table wells for this study (n= 108 sampling locations). The wells were
placed along transects that cover target landscape units (bog, fen, upland). Wells were
sampled for water isotopes and geochemical parameters during the summers of 2011-2014
to characterize the baseline geochemistry of groundwater in the different landscape units.
Inorganic (nitrate, ammonium) and organic forms of nitrogen (dissolved organic nitrogen),
major and minor ions and water isotope tracers (18O, 2H and 3H) were measured to
identify the various forms of nitrogen in the different landscape units, as well as to assess
connectivity and potential for nitrogen transport between the different units. At JPH
surface and groundwater flow is from the uplands to the fen. There was little (<0.1-1.5
mg/L) nitrate, ammonium, or dissolved organic nitrate (DON) found throughout JPH. At
ML nitrogen concentrations were higher (<0.1-30 mg/l) and concentrations of ammonium
and DON increased at depths throughout ML. The distribution of 3H with depth within the
peatland reveals limited connectivity between the peat and underlying mineral soils.
Tritium sampling at ML indicates that at some locations the wetland residence time is
greater than 50 years. Nitrogen movement out of peatlands may take longer due to
conversions and storage. At ML nitrogen (NH4 and DON) is produced and stored at depth
in the wetlands. At JPH higher nitrogen concentrations are found in the shallow
groundwater of the fen. Increases in nitrogen inputs to JPH and ML are likely to be utilized
by plants, but dramatic changes to the peatland may cause stored nitrogen to become
mobile. / Graduate
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