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美国东北部和大西洋中部地区营养物质向受纳水体的来源与输送

Source and Delivery of Nutrients to Receiving Waters in the Northeastern and Mid-Atlantic Regions of the United States.

作者信息

Moore Richard B, Johnston Craig M, Smith Richard A, Milstead Bryan

出版信息

J Am Water Resour Assoc. 2011 Oct;47(5):965-990. doi: 10.1111/j.1752-1688.2011.00582.x.

DOI:10.1111/j.1752-1688.2011.00582.x
PMID:22457578
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC3307627/
Abstract

This study investigates nutrient sources and transport to receiving waters, in order to provide spatially detailed information to aid water-resources managers concerned with eutrophication and nutrient management strategies. SPAtially Referenced Regressions On Watershed attributes (SPARROW) nutrient models were developed for the Northeastern and Mid-Atlantic (NE US) regions of the United States to represent source conditions for the year 2002. The model developed to examine the source and delivery of nitrogen to the estuaries of nine large rivers along the NE US Seaboard indicated that agricultural sources contribute the largest percentage (37%) of the total nitrogen load delivered to the estuaries. Point sources account for 28% while atmospheric deposition accounts for 20%. A second SPARROW model was used to examine the sources and delivery of phosphorus to lakes and reservoirs throughout the NE US. The greatest attenuation of phosphorus occurred in lakes that were large relative to the size of their watershed. Model results show that, within the NE US, aquatic decay of nutrients is quite limited on an annual basis and that we especially cannot rely on natural attenuation to remove nutrients within the larger rivers nor within lakes with large watersheds relative to the size of the lake.

摘要

本研究调查营养物质来源及其向受纳水体的输送情况,以便提供空间详细信息,帮助关注富营养化和营养管理策略的水资源管理者。针对美国东北部和大西洋中部(美国东北部)地区,开发了基于流域属性的空间参考回归(SPARROW)营养模型,以呈现2002年的源状况。为研究氮素向美国东北部沿海九条大河河口的来源和输送情况而开发的模型表明,农业源对输送至河口的总氮负荷贡献比例最大(37%)。点源占28%,而大气沉降占20%。第二个SPARROW模型用于研究美国东北部湖泊和水库中磷的来源和输送情况。磷的最大衰减发生在相对于其流域面积而言较大的湖泊中。模型结果表明,在美国东北部,营养物质的水生衰减在年度基础上相当有限,而且我们尤其不能依靠自然衰减来去除较大河流以及相对于湖泊面积而言流域面积较大的湖泊中的营养物质。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/28fd/3307627/2a794f390142/jawr0047-0965-f9.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/28fd/3307627/db14fbdadd6c/jawr0047-0965-f1.jpg
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https://cdn.ncbi.nlm.nih.gov/pmc/blobs/28fd/3307627/13d2e3379d35/jawr0047-0965-f5.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/28fd/3307627/b18ae027c93e/jawr0047-0965-f6.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/28fd/3307627/0a6c5d69383b/jawr0047-0965-f7.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/28fd/3307627/fde641e731cf/jawr0047-0965-f8.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/28fd/3307627/2a794f390142/jawr0047-0965-f9.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/28fd/3307627/db14fbdadd6c/jawr0047-0965-f1.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/28fd/3307627/2393ed8717a5/jawr0047-0965-f2.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/28fd/3307627/569abe758cf1/jawr0047-0965-f3.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/28fd/3307627/6691dd4567c6/jawr0047-0965-f4.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/28fd/3307627/13d2e3379d35/jawr0047-0965-f5.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/28fd/3307627/b18ae027c93e/jawr0047-0965-f6.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/28fd/3307627/0a6c5d69383b/jawr0047-0965-f7.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/28fd/3307627/fde641e731cf/jawr0047-0965-f8.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/28fd/3307627/2a794f390142/jawr0047-0965-f9.jpg

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