Factors affecting denitrification in headwater prairie streams

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dc.contributor.author Reisinger, Alexander Joseph
dc.date.accessioned 2010-07-14T19:36:18Z
dc.date.available 2010-07-14T19:36:18Z
dc.date.issued 2010-07-14T19:36:18Z
dc.identifier.uri http://hdl.handle.net/2097/4273
dc.description.abstract Human-induced stressors such as increased nitrogen (N) loadings, altered watershed land-use, and biodiversity losses are a few of the numerous threats to aquatic systems. Prairie streams experience natural disturbances, such as flooding and desiccation, which may alter responses to anthropogenic stressors. Denitrification, the dissimilatory reduction of NO3- to N gas (N2O or N2), is the only permanent form of N removal from terrestrial or aquatic ecosystems, and is important in mitigating N pollution to streams and downstream waters. Little is known about the relationships between denitrification and riparian prairie vegetation or large consumers. In the first chapter, I used outdoor mesocosms to determine the impact of a grazing minnow, Campostoma anomalum, on structural and functional responses of prairie streams to a simulated flood, focusing on denitrification. In terrestrial ecosystems, grazing can stimulate denitrification, but this has not been studied in streams. Ammonium (NH4+) enrichments, used to simulate fish excretion, alleviated N limitations on denitrification. Both fish and NH4+ affected algal biomass accrual, but only fish affected algal filament lengths and particulate organic matter. In a second experiment, I examined the impact of woody vegetation expansion, a primary threat to tallgrass prairie, on riparian and benthic denitrification. Expansion of woody vegetation in these grasslands is due primarily to altered fire regimes, which historically inhibited woody vegetation growth. To determine the effect of woody vegetation expansion on benthic and riparian denitrification, woody vegetation was removed from the riparian zone of a grazed and an ungrazed watershed. Both soil and benthic denitrification rates from this removal buffer were compared to rates in grassy or woody riparian zones. Riparian soil denitrification was highly seasonal, with greatest rates occurring during early spring, and rates being low throughout the remainder of the year. Benthic denitrification was also temporally variable but did not exhibit seasonal trends, suggesting benthic denitrification is driven by factors other than water temperature. Removal of woody vegetation stimulated soil and benthic denitrification rates over rates found in naturally vegetated riparian zones. Elevated N loadings will continue to affect aquatic ecosystems, and these effects may be exacerbated by biodiversity losses or changing riparian vegetation. en_US
dc.description.sponsorship Long Term Ecological Research Network; National Science Foundation; Konza Prairie Biological State; Kansas State University Division of Biology en_US
dc.language.iso en_US en_US
dc.publisher Kansas State University en
dc.subject Denitrification en_US
dc.subject Woody encroachment en_US
dc.subject Prairie streams en_US
dc.subject Nitrogen en_US
dc.subject Biodiversity en_US
dc.subject Ecosystem recovery en_US
dc.title Factors affecting denitrification in headwater prairie streams en_US
dc.type Thesis en_US
dc.description.degree Master of Science en_US
dc.description.level Masters en_US
dc.description.department Department of Biology en_US
dc.description.advisor Walter K. Dodds en_US
dc.subject.umi Biogeochemistry (0425) en_US
dc.subject.umi Biology, Ecology (0329) en_US
dc.subject.umi Biology, Limnology (0793) en_US
dc.date.published 2010 en_US
dc.date.graduationmonth August en_US

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