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The effects of changing precipitation patterns on soil microbial communities and nitrogen cycling in the New Jersey PinelandsLandesman, William Joel, January 2009 (has links)
Thesis (Ph. D.)--Rutgers University, 2009. / "Graduate Program in Ecology and Evolution." Includes bibliographical references.
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Patterns of nitrogen fluxes in watersheds of the H.J. Andrews Experimental Forest, OR /Vanderbilt, Kristin Lynn, January 1900 (has links)
Thesis (Ph. D.)--Oregon State University, 2001. / Typescript (photocopy). Includes bibliographical references (leaves 99-110). Also available on the World Wide Web.
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The chemistry of acidic soils in humid, temperate forested watersheds with emphasis on phosphorus, aluminum and iron /SanClements, Michael, January 2009 (has links)
Thesis (Ph.D.) in Ecology and Environmental Science--University of Maine, 2009. / Includes vita. Includes bibliographical references (leaves 147-157).
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Molecular analysis of anammox, AOA and AOB in high nitrogen sediment and wetlandsLee, Kwok-ho., 李國豪. January 2010 (has links)
published_or_final_version / Biological Sciences / Master / Master of Philosophy
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Relationships between microbial physiological status and nitrogen availability in forest soilsAu, William R. January 1998 (has links)
Although the physiological nitrogen demand of the soil microbial biomass is a major determinant of N mineralization in forest soils, the exact nature of the relationship is unclear. This study investigated the relationships between a respiration-based indicator of microbial physiological N demand (NIR) and N availability in forest soils. NIR was found to correlate significantly with net mineralized N in the field and annual foliar litterfall N fluxes. In a laboratory incubation, NIR was shown to be sensitive to changes in soil available C and N pools. These results demonstrated that microbial physiological N demand is determined by relative availabilities of labile C and N, and that it is significantly related to N cycling in forest soils. Results from a seasonal study of a forested watershed suggest that nutrient availability determined tree production and soil C availability, which in turn determined microbial physiological N demand and nitrogen dynamics in the forest.
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Nitrogen cycling in the northern hardwood forest soil, plant, and atmospheric processes /Nave, Lucas Emil, January 2007 (has links)
Thesis (Ph. D.)--Ohio State University, 2007. / Title from first page of PDF file. Includes bibliographical references (p. 78-89).
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Nitrogen dynamics across silvicultural canopy gaps in young forests of western Oregon /Thiel, Aaron L. January 1900 (has links)
Thesis (M.S.)--Oregon State University, 2008. / Printout. Includes bibliographical references (leaves 45-51). Also available on the World Wide Web.
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Studies on the nitrogen cycle under systems of crop rotation /Jeevarnatnam, Appapillai Jacob. January 1956 (has links) (PDF)
Thesis (M.Ag.Sc)--University of Adelaide, Faculty of Agricultural Science, 1956. / Typewritten. Includes bibliographical references.
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Studies on nitrogen cycling processes in Lake Illawarra, New South Wales, AustraliaQu, Wenchuan. January 2004 (has links)
Thesis (Ph.D.)--University of Wollongong, 2004. / Typescript. Includes bibliographical references: leaf 178-199.
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Decomposition and nitrogen dynamics of red alder and Douglas-fir leaf litter in Oregon Coast Range riparian forests /Matkins, Joselin. January 1900 (has links)
Thesis (M.S.)--Oregon State University, 2009. / Printout. Includes bibliographical references (leaves 99-104). Also available on the World Wide Web.
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