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Thermodynamics and the role of hydro...
~
Hoehler, Tori Michael.
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Thermodynamics and the role of hydrogen in anoxic sediments.
紀錄類型:
書目-電子資源 : Monograph/item
正題名/作者:
Thermodynamics and the role of hydrogen in anoxic sediments./
作者:
Hoehler, Tori Michael.
面頁冊數:
193 p.
附註:
Source: Dissertation Abstracts International, Volume: 59-07, Section: B, page: 3297.
Contained By:
Dissertation Abstracts International59-07B.
標題:
Biogeochemistry. -
電子資源:
http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=9840926
ISBN:
0591948672
Thermodynamics and the role of hydrogen in anoxic sediments.
Hoehler, Tori Michael.
Thermodynamics and the role of hydrogen in anoxic sediments.
- 193 p.
Source: Dissertation Abstracts International, Volume: 59-07, Section: B, page: 3297.
Thesis (Ph.D.)--The University of North Carolina at Chapel Hill, 1998.
The redox chemistry of the oceans and atmosphere is driven in large part by the biogeochemical cycling that occurs in anoxic environments. This cycling is mediated by communities of anaerobic bacteria that utilize molecular hydrogen as the primary carrier of electrons. Using a framework of thermodynamics, this volume examines the bacterial processes that control and are controlled by H
ISBN: 0591948672Subjects--Topical Terms:
545717
Biogeochemistry.
Thermodynamics and the role of hydrogen in anoxic sediments.
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Thermodynamics and the role of hydrogen in anoxic sediments.
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193 p.
500
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Source: Dissertation Abstracts International, Volume: 59-07, Section: B, page: 3297.
500
$a
Adviser: Marc J. Alperin.
502
$a
Thesis (Ph.D.)--The University of North Carolina at Chapel Hill, 1998.
520
$a
The redox chemistry of the oceans and atmosphere is driven in large part by the biogeochemical cycling that occurs in anoxic environments. This cycling is mediated by communities of anaerobic bacteria that utilize molecular hydrogen as the primary carrier of electrons. Using a framework of thermodynamics, this volume examines the bacterial processes that control and are controlled by H
$\
sb2
$
concentrations in anoxic sediments from the White Oak River and Cape Lookout Bight, North Carolina.
520
$a
In a series of laboratory experiments, temperature, terminal electron acceptor, sulfate concentration, and pH were found to exhibit thermodynamic control over steady-state porewater H
$\
sb2
$
concentrations. Changes in these parameters alter the free energy yield of bacterially-mediated H
$\
sb2
$-
consuming reactions; the response of H
$\
sb2
$
concentrations in each case tended to offset whatever energetic change had been induced. In the case of temperature and sulfate concentration, the change in H
$\
sb2
$
concentrations was exactly sufficient to maintain a constant energy yield (
$\
Delta
$\
sb2
$-
consuming reaction. In field studies, the observed down-core, seasonal, and inter-environmental variations in H
$\
sb2
$
concentrations compare favorably with the laboratory-determined dependencies for the four controls. This thermodynamic control likely results from a competition-induced necessity for terminal bacteria to maintain H
$\
sb2
$
concentrations at a minimum level set by bioenergetic considerations.
520
$a
The ability of H
$\
sb2
$
concentrations to exert thermodynamic control on bacterially-mediated processes was examined in two cases. First, a series of field and laboratory experiments suggest that anaerobic methane oxidation in Cape Lookout Bight sediments represents a reversal of methanogenic CO
$\
sb2
$
reduction. It is shown that variations in H
$\
sb2
$
concentrations provide a thermodynamic basis for this reversal. Second, the dynamics of acetate-H
$\
sb2
$/
CO
$\
sb2
$
interconversion were examined. Tracer studies indicate the directionality of this process is controlled by H
$\
sb2
$
concentrations. In one instance, acetogenesis from H
$\
sb2
$\
sb2
$
was the major H
$\
sb2
$-
consuming process and consequently the primary control on H
$\
sb2
$
concentrations.
590
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School code: 0153.
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http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=9840926
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