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Hillslope hydrologic connectivity controls riparian groundwater turnover: Implications of catchment structure for riparian buffering and stream water sources

机译:山坡水文连通性控制河岸地下水周转:流域结构对河岸缓冲和溪流水源的影响

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摘要

Hydrologic connectivity between catchment upland and near stream areas is essential for the transmission of water, solutes, and nutrients to streams. However, our current understanding of the role of riparian zones in mediating landscape hydrologic connectivity and the catchment scale export of water and solutes is limited. We tested the relationship between the duration of hillslope-riparian-stream (HRS) hydrologic connectivity and the rate and degree of riparian shallow groundwater turnover along four HRS well transects within a Sci of nested mountain catchments (Tenderfoot Creek Experimental Forest, MT). Transect HRS water table connectivity ranged from 9 to 123 days during the annual snowmelt hydrograph. Hillslope water was always characterized by low specific conductance (~27 μS cm~(-1)). In transects with transient hillslope water tables, riparian groundwater specific conductance was elevated during base flow conditions ~27 μS cm~(-1)) but shifted toward hillslope signatures once a HRS groundwater connection was established. The degree of riparian groundwater turnover was proportional to the duration of HRS connectivity and inversely related to the riparian: hillslope area ratios (buffer ratio; r~2 = 0.95). We applied this relationship to the stream network in seven subcatchments within the Tenderfoot Creek Experimental Forest and compared their turnover distributions to source water contributions measured at each catchment outlet. The amount of riparian groundwater exiting each of the seven catchments was linearly related (r~2 = 0.92) to their median riparian turnover time. Our observations suggest that the size and spatial arrangement of hillslope and riparian zones along a stream network and the timing and duration of groundwater connectivity between them is a first-order control on the magnitude and timing of water and solutes observed at the catchment outlet.
机译:集水区高地和附近溪流地区之间的水文连通性对于将水,溶质和养分传输到溪流至关重要。然而,我们目前对河岸带在介导景观水文连通性和流域规模水和溶质出口方面的作用的理解是有限的。我们测试了山坡-河岸流(HRS)的水文连通性的持续时间与巢山流域Sci中的四个HRS井样断面的河岸浅层地下水周转率和程度之间的关系(Tenderfoot Creek实验森林,MT)。在年度融雪水文期间,横断面HRS地下水位的连通性范围为9到123天。斜坡水总是以低的电导率(〜27μScm〜(-1))为特征。在具有临时坡地地下水位的样带中,在基流条件下(〜27μScm〜(-1)),河岸地下水的比电导率会升高,但一旦建立了HRS地下水连接,河岸地下水的电导率就会向坡地标志移动。河岸地下水周转的程度与HRS连通的持续时间成正比,与河岸:山坡面积比(缓冲比; r〜2 = 0.95)成反比。我们将此关系应用于Tenderfoot Creek实验森林内七个子集水区的河流网络,并将它们的周转分布与每个集水区出口处的水源贡献进行了比较。七个集水区中每个流域的河岸地下水量与河岸中位周转时间线性相关(r〜2 = 0.92)。我们的观察结果表明,沿河网的坡地和河岸带的大小和空间布置以及它们之间的地下水连通时间和持续时间是对流域出口处水和溶质的量和时间的一级控制。

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  • 来源
    《Water resources research》 |2010年第10期|p.W10524.1-W10524.18|共18页
  • 作者单位

    Department of Land Resources and Environmental Sciences, Montana State University, Bozeman, MT 59717, USA;

    Department of Land Resources and Environmental Sciences, Montana State University, Bozeman, MT 59717, USA;

    Civil Environmental Engineering Department, Penn State University, 212 Sackett Bldg., University Park, PA 16802, USA;

    U.S. Geological Survey, 345 Middlefteld Road, Menlo Park, CA 94025, USA;

    U.S. Forest Service, Pacific Northwest Research Station Olympia Forestry Sciences Lab, Olympia, WA 98512, USA;

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  • 入库时间 2022-08-18 03:39:04

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