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提高对混合土地利用流域悬移质泥沙规律的认识:通过高频采样的机理进展。

Improving understanding of mixed-land-use watershed suspended sediment regimes: Mechanistic progress through high-frequency sampling.

机构信息

University of Missouri, School of Natural Resources, 203 ABNR Building, Columbia, MO 65211, USA; West Virginia University, Institute of Water Security and Science, Davis College, Schools of Agriculture and Food, and Natural Resources. 3107 Agricultural Sciences Building, Morgantown, WV 26506, USA.

West Virginia University, Institute of Water Security and Science, 3109 Agricultural Sciences Building, Morgantown, WV 26506, USA; West Virginia University, Davis College, Schools of Agriculture and Food, and Natural Resources. 3109 Agricultural Sciences Building, Morgantown, WV 26506, USA.

出版信息

Sci Total Environ. 2017 Nov 15;598:228-238. doi: 10.1016/j.scitotenv.2017.04.052. Epub 2017 Apr 22.

Abstract

Given the importance of suspended sediment to biogeochemical functioning of aquatic ecosystems, and the increasing concern of mixed-land-use effects on pollutant loading, there is an urgent need for research that quantitatively characterizes spatiotemporal variation of suspended sediment dynamics in contemporary watersheds. A study was conducted in a representative watershed of the central United States utilizing a nested-scale experimental watershed design, including five gauging sites (n=5) partitioning the catchment into five sub-watersheds. Hydroclimate stations at gauging sites were used to monitor air temperature, precipitation, and stream stage at 30-min intervals during the study (Oct. 2009-Feb. 2014). Streamwater grab samples were collected four times per week, at each site, for the duration of the study (Oct. 2009-Feb. 2014). Water samples were analyzed for suspended sediment using laser particle diffraction. Results showed significant differences (p<0.05) between monitoring sites for total suspended sediment concentration, mean particle size, and silt volume. Total concentration and silt volume showed a decreasing trend from the primarily agricultural upper watershed to the urban mid-watershed, and a subsequent increasing trend to the more suburban lower watershed. Conversely, mean particle size showed an opposite spatial trend. Results are explained by a combination of land use (e.g. urban stormwater dilution) and surficial geology (e.g. supply-controlled spatial variation of particle size). Correlation analyses indicated weak relationships with both hydroclimate and land use, indicating non-linear sediment dynamics. Suspended sediment parameters displayed consistent seasonality during the study, with total concentration decreasing through the growing season and mean particle size inversely tracking air temperature. Likely explanations include vegetation influences and climate-driven weathering cycles. Results reflect unique observations of spatiotemporal variation of suspended sediment particle size class. Such information is crucial for land and water resource managers working to mitigate aquatic ecosystem degradation and improve water resource sustainability in mixed-land-use watersheds globally.

摘要

鉴于悬浮泥沙对水生生态系统生物地球化学功能的重要性,以及混合土地利用对污染物负荷的影响日益受到关注,因此迫切需要研究定量描述当代流域悬浮泥沙动态的时空变化。本研究在美国中部一个具有代表性的流域中进行,利用嵌套尺度实验流域设计,包括五个测量点(n=5),将流域划分为五个子流域。测量点的水文气候站用于在研究期间(2009 年 10 月至 2014 年 2 月)每 30 分钟监测一次空气温度、降水和河流水位。在整个研究期间(2009 年 10 月至 2014 年 2 月),每周在每个站点采集四次河流地表水样本。水样采用激光颗粒衍射法分析悬浮泥沙。结果表明,总悬浮泥沙浓度、平均粒径和粉土体积在监测点之间存在显著差异(p<0.05)。总浓度和粉土体积从主要农业上游流域到城市中游流域呈下降趋势,然后到更郊区的下游流域呈上升趋势。相反,平均粒径表现出相反的空间趋势。结果可以用土地利用(如城市雨水稀释)和地表地质(如粒径空间控制供应变化)的组合来解释。相关分析表明与水文气候和土地利用的关系较弱,表明泥沙动态呈非线性。悬浮泥沙参数在整个研究期间表现出一致的季节性,总浓度在生长季节下降,平均粒径与空气温度呈反向关系。可能的解释包括植被影响和气候驱动的风化循环。结果反映了悬浮泥沙粒径类别的时空变化的独特观测。此类信息对于在全球混合土地利用流域中努力减轻水生生态系统退化和提高水资源可持续性的土地和水资源管理者来说至关重要。

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