Nitrogen saturation in streams and forests of the Maryland Piedmont
dc.contributor.advisor | Palmer, Margaret A | en_US |
dc.contributor.author | Craig, Laura Shawn | en_US |
dc.contributor.department | Behavior, Ecology, Evolution and Systematics | en_US |
dc.contributor.publisher | Digital Repository at the University of Maryland | en_US |
dc.contributor.publisher | University of Maryland (College Park, Md.) | en_US |
dc.date.accessioned | 2010-02-19T07:18:24Z | |
dc.date.available | 2010-02-19T07:18:24Z | |
dc.date.issued | 2009 | en_US |
dc.description.abstract | Human activities have dramatically increased nitrogen (N) inputs to the landscape. Consequently, delivery of N to coastal waters, largely as nitrate (NO3-N), has increased, resulting in widespread eutrophication and harmful hypoxic conditions. The ability to mitigate the downstream effects of elevated N inputs requires a clear understanding of the transport and transformation of N in stream ecosystems. Here, I examine N processing in urban and forested watersheds of the Maryland Piedmont. I provide extensive evidence that three high-N streams draining urban and forested watersheds of the Maryland Piedmont are unable to remove NO3-N as a result of both N saturation and phosphorus limitation. My findings illustrate that when elevated NO3-N concentrations occur in the absence of other stressors that stimulate autotrophic activity (e.g. reduced canopy cover, increased nutrients) uptake cannot compensate for increased N loads. A review of the literature indicates that systems that are similarly unable to remove NO3-N vary widely in terms of land use and background N concentrations, highlighting the limitations of our understanding of N saturation in stream ecosystems. I also provide the first documentation of N saturation in both the aquatic and terrestrial components of an un-manipulated forested watershed. Detailed examination of N dynamics within the forested watershed reveals that the forest is severely N-saturated despite receiving atmospheric N inputs that are small relative to other parts of the Northeast and Mid-Atlantic. Because groundwater delivers a disproportionate fraction of the N load to the channel, in-stream N concentrations are elevated when deep groundwater flowpaths dominate, and the watershed is a source of N during dry periods, I hypothesize that hydrogeologic factors that control groundwater susceptibility to NO3-N contamination and promote delivery of NO3-N via subsurface flowpaths may exacerbate N-saturation response. My results suggest that we cannot rely on in-stream processing to reduce N loads even in minimally impacted watersheds. As a result, it is critical that management efforts reduce N loading to streams and take advantage of opportunities for increasing N removal in impaired systems only after other options have been exhausted. | en_US |
dc.identifier.uri | http://hdl.handle.net/1903/10041 | |
dc.subject.pqcontrolled | Biology, Ecology | en_US |
dc.subject.pquncontrolled | Nitrogen | en_US |
dc.subject.pquncontrolled | Piedmont | en_US |
dc.subject.pquncontrolled | saturation | en_US |
dc.subject.pquncontrolled | Stream | en_US |
dc.subject.pquncontrolled | watershed | en_US |
dc.title | Nitrogen saturation in streams and forests of the Maryland Piedmont | en_US |
dc.type | Dissertation | en_US |
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