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Mapping infiltration rates in Dane County, Wisconsin.

机译:绘制威斯康星州戴恩县的入渗率。

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摘要

Dane County, Wisconsin has experienced rapid population growth and development over the last 40 years. Groundwater pumping and loss of recharge associated with development have contributed to significant groundwater drawdown---up to 20m compared to predevelopment conditions. Infiltrating stormwater is a practice that may minimize recharge loss in developed areas, especially if the stormwater is directed to high-infiltration soils. The saturated hydraulic conductivity (Ksat), which is a measure of how easily a soil transmits water, can be used to compare the infiltration potential of different soils. Most Ksat estimates are based on measurements in which water flow is primarily through micropores, rather than macropores. However, macropore flow can dominate the infiltration rate when the soil is saturated, as it is likely to be in areas receiving stormwater runoff.;The objective of this study was to produce a relative infiltration map for Dane. County that is based on local infiltration measurements that do include macropore flow. Infiltration measurements were taken (50 sites, 124 measurements) and soil samples collected for a wide variety of soils and land uses across Dane County. Multiple regression analysis was done to examine relationships between Ksat and soil and non-soil properties (landcover and topography). Percent sand and bulk density of the surface horizon were the two best soil property predictors of Ksat. Landcover was the best non-soil Ksat predictor. These relationships were used to develop a relative infiltration map for Dane County from existing geospatial data layers for soils, landcover and topography. Including landcover as a predictor of Ksat improves the accuracy of the regression model compared to the model based on soil properties alone (percent sand and bulk density) and also increases the spatial resolution of the relative infiltration map. This map is designed for use in township or watershed-scale land use planning. Local land use planners can use this information to identify the suitability of potential development areas for infiltration-based stormwater management.
机译:威斯康星州丹恩县在过去40年中经历了快速的人口增长和发展。与开发相关的地下水抽取和补给的损失导致了地下水的大量流失-与开发前的条件相比,长达20m。渗入雨水的做法可以使发达地区的补给损失降到最低,特别是如果雨水直接流向高渗入土壤的情况下。饱和水力传导率(Ksat)是衡量土壤传输水的容易程度的一种度量,可以用来比较不同土壤的渗透潜力。大多数Ksat估计都是基于测量,其中水的流动主要通过微孔而不是大孔。然而,当土壤饱和时,大孔流量可以控制入渗率,因为它很可能在接受雨水径流的地区。这项研究的目的是为戴恩绘制一个相对的入渗图。基于包含大孔流量的局部入渗测量结果的县。进行了入渗测量(50个地点,共124个测量值),并收集了丹讷县范围内各种土壤和土地用途的土壤样品。进行了多元回归分析,以检查Ksat与土壤和非土壤属性(土地覆盖和地形)之间的关系。地表水平的沙子百分比和堆密度是Ksat的两个最佳土壤属性预测指标。 Landcover是最好的非土壤Ksat预报器。这些关系被用来从现有的土壤,土地覆盖物和地形地理空间数据层为戴恩县开发一个相对入渗图。与仅基于土壤特性(沙子和堆积密度的百分比)的模型相比,将土地覆盖物作为Ksat的预测因子可以提高回归模型的准确性,还可以提高相对入渗图的空间分辨率。该地图旨在用于城镇或流域规模的土地使用规划。当地土地使用规划人员可以使用此信息来确定潜在开发区域是否适合基于渗透的雨水管理。

著录项

  • 作者

    Arrington, Kathleen E.;

  • 作者单位

    The University of Wisconsin - Madison.;

  • 授予单位 The University of Wisconsin - Madison.;
  • 学科 Agriculture Soil Science.;Water Resource Management.;Land Use Planning.
  • 学位 Ph.D.
  • 年度 2009
  • 页码 125 p.
  • 总页数 125
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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