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Richard C. Foltz 《Journal of Agricultural and Environmental Ethics》2007,20(6):533-542
283.
Biodiversity and Disease Risk: the Case of Lyme Disease 总被引:14,自引:0,他引:14
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Incorporating Geological Effects in Modeling of Revegetation Strategies for Salt-Affected Landscapes 总被引:1,自引:0,他引:1
Christopher J. Clarke Richard W. Bell Richard J. Hobbs Richard J. George 《Environmental management》1999,24(1):99-109
The work highlights the difficulties of using standard sampling and statistical techniques to investigate regional phenomena
and presents an integrated approach combining small-scale sampling with broad-scale observations to provide input into a modeling
exercise. It is suggested that such approaches are vital if landscape- and regional-scale processes are to be understood and
managed. The way in which the problem is perceived (holistically or piecemeal) affects the way treatments are designed and
their effectiveness: past approaches have failed to integrate the various scales and processes involved. Effective solutions
require an integrated holistic response. 相似文献
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Richard B. Alexander Elizabeth W. Boyer Richard A. Smith Gregory E. Schwarz Richard B. Moore 《Journal of the American Water Resources Association》2007,43(1):41-59
Abstract: Knowledge of headwater influences on the water‐quality and flow conditions of downstream waters is essential to water‐resource management at all governmental levels; this includes recent court decisions on the jurisdiction of the Federal Clean Water Act (CWA) over upland areas that contribute to larger downstream water bodies. We review current watershed research and use a water‐quality model to investigate headwater influences on downstream receiving waters. Our evaluations demonstrate the intrinsic connections of headwaters to landscape processes and downstream waters through their influence on the supply, transport, and fate of water and solutes in watersheds. Hydrological processes in headwater catchments control the recharge of subsurface water stores, flow paths, and residence times of water throughout landscapes. The dynamic coupling of hydrological and biogeochemical processes in upland streams further controls the chemical form, timing, and longitudinal distances of solute transport to downstream waters. We apply the spatially explicit, mass‐balance watershed model SPARROW to consider transport and transformations of water and nutrients throughout stream networks in the northeastern United States. We simulate fluxes of nitrogen, a primary nutrient that is a water‐quality concern for acidification of streams and lakes and eutrophication of coastal waters, and refine the model structure to include literature observations of nitrogen removal in streams and lakes. We quantify nitrogen transport from headwaters to downstream navigable waters, where headwaters are defined within the model as first‐order, perennial streams that include flow and nitrogen contributions from smaller, intermittent and ephemeral streams. We find that first‐order headwaters contribute approximately 70% of the mean‐annual water volume and 65% of the nitrogen flux in second‐order streams. Their contributions to mean water volume and nitrogen flux decline only marginally to about 55% and 40% in fourth‐ and higher‐order rivers that include navigable waters and their tributaries. These results underscore the profound influence that headwater areas have on shaping downstream water quantity and water quality. The results have relevance to water‐resource management and regulatory decisions and potentially broaden understanding of the spatial extent of Federal CWA jurisdiction in U.S. waters. 相似文献
288.
An Integrated Model of Two Fire Regimes 总被引:1,自引:0,他引:1
Richard A. Minnich 《Conservation biology》2001,15(6):1549-1553
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