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首页> 外文期刊>Journal of Hydrology: Regional Studies >Estimating impact of forest land on groundwater recharge in a humid subtropical watershed of the Lower Mississippi River Alluvial Valley
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Estimating impact of forest land on groundwater recharge in a humid subtropical watershed of the Lower Mississippi River Alluvial Valley

机译:估算密西西比河下游冲积河谷湿润的亚热带流域中林地对地下水补给的影响

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摘要

Study regionLower Mississippi River Alluvial Valley (LMRAV) is located in the humid subtropical region of mid-south USA, and Lower Yazoo River Watershed (LYRW) in Mississippi is within the LMRAV.Study focusGroundwater depletion due to anthropogenic activities is an issue of water resource concern in the LMRAV. Some studies suggested that forest lands reduce water recharge from land surface into aquifers as compared to agricultural lands. However, very few efforts have been devoted to investigating the relationship of water recharge and land use in the LMRAV. This study was designed to meet this need.New hydrological insights for the regionUsing the HSPF (Hydrological Simulation Program-FORTRAN) model along with the LYRW, we found that the annual average water recharge from the land surface into the deep aquifer over the 10-year simulation period for the three land uses was: agriculture?
机译:研究区域下密西西比河冲积河谷(LMRAV)位于美国中南部潮湿的亚热带地区,密西西比州的下亚佐河流域(LYRW)在LMRAV范围内。关注LMRAV。一些研究表明,与农业用地相比,林地减少了从地表到含水层的补给水。但是,很少有工作致力于调查LMRAV中的补水与土地利用之间的关系。这项研究旨在满足这一需求。该地区的新水文见解使用HSPF(水文模拟计划-FORTRAN)模型和LYRW模型,我们发现从地表到深层含水层的年平均补给量在10-这三种土地利用的年度模拟期为:农业-<森林> <湿地。来自农业,森林和湿地的沉淀水分别只有1.1%,1.2%和1.4%补给了LYRW中的深层含水层。结果表明,与农地相比,林地从地表到地下水的补给量略有增加而不是减少。这些发现可能会改变关于森林如何影响全球湿润的亚热带地区的地下水补给水的传统科学观点。

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