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尽管采取了农业土壤保持措施,流域泥沙仍加速向湖泊输送。

Watershed sediment losses to lakes accelerating despite agricultural soil conservation efforts.

机构信息

Department of Ecology, Evolution, and Organismal Biology, Iowa State University, Ames, Iowa, United States of America.

出版信息

PLoS One. 2013;8(1):e53554. doi: 10.1371/journal.pone.0053554. Epub 2013 Jan 9.

DOI:10.1371/journal.pone.0053554
PMID:23326454
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC3541183/
Abstract

Agricultural soil loss and deposition in aquatic ecosystems is a problem that impairs water quality worldwide and is costly to agriculture and food supplies. In the US, for example, billions of dollars have subsidized soil and water conservation practices in agricultural landscapes over the past decades. We used paleolimnological methods to reconstruct trends in sedimentation related to human-induced landscape change in 32 lakes in the intensively agricultural region of the Midwestern United States. Despite erosion control efforts, we found accelerating increases in sediment deposition from erosion; median erosion loss since 1800 has been 15.4 tons ha(-1). Sediment deposition from erosion increased >6-fold, from 149 g m(-2) yr(-1) in 1850 to 986 g m(-2) yr(-1) by 2010. Average time to accumulate one mm of sediment decreased from 631 days before European settlement (ca. 1850) to 59 days mm(-1) at present. Most of this sediment was deposited in the last 50 years and is related to agricultural intensification rather than land clearance or predominance of agricultural lands. In the face of these intensive agricultural practices, traditional soil conservation programs have not decelerated downstream losses. Despite large erosion control subsidies, erosion and declining water quality continue, thus new approaches are needed to mitigate erosion and water degradation.

摘要

农业土壤流失和沉积对水生生态系统造成了影响,这是一个全球性的问题,不仅损害了水质,还给农业和粮食供应带来了巨大的经济损失。例如,在美国,过去几十年,数十亿美元的资金用于补贴农业景观中的水土保持措施。我们使用古湖泊学方法重建了与人类引起的景观变化有关的沉积趋势,研究对象为美国中西部高度集约化农业地区的 32 个湖泊。尽管采取了侵蚀控制措施,但我们发现由于侵蚀导致的沉积物沉积仍在加速增加;自 1800 年以来,平均每年的侵蚀损失为 15.4 吨/公顷。自 1850 年以来,由于侵蚀导致的沉积物沉积增加了 6 倍以上,从 149 克/平方米/年增加到 2010 年的 986 克/平方米/年。从欧洲殖民前(约 1850 年)到现在平均每积累 1 毫米的沉积物所需的时间从 631 天减少到 59 天/毫米。这些沉积物中的大部分是在过去 50 年中沉积的,与农业集约化而非土地开垦或农业用地为主有关。面对这些集约化的农业实践,传统的土壤保持计划并没有减缓下游的损失。尽管有大量的侵蚀控制补贴,但侵蚀和水质下降仍在继续,因此需要采取新的方法来减轻侵蚀和水退化。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2dfe/3541183/01851e1bfcf9/pone.0053554.g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2dfe/3541183/b93318668a3b/pone.0053554.g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2dfe/3541183/01851e1bfcf9/pone.0053554.g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2dfe/3541183/b93318668a3b/pone.0053554.g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2dfe/3541183/01851e1bfcf9/pone.0053554.g002.jpg

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