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TRANSIENT RESPONSE FUNCTIONS FOR CONJUNCTIVE WATER MANAGEMENT IN THE SNAKE RIVER PLAIN, IDAHO

机译:爱达荷州蛇河平原连续水管理中的瞬态响应函数

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摘要

Increasing demands on western water are causing a mounting need for the conjunctive management of surface water and ground water resources. Under western water law, the senior water rights holder has priority over the junior water rights holder in times of water shortage. Water managers have been reluctant to conjunctively manage surface water and ground water resources because of the difficulty of quantification of the impacts to surface water resources from ground water stresses. Impacts from ground , water use can take years to propagate through an aquifer system. Prediction of the degree of impact to surface water resources over time and the spatial distribution of impacts is very difficult. Response functions mathematically describe the relationship between a unit ground water stress applied at a specific location and stream depletion or aquifer water level change elsewhere in the system. Response functions can be used to help quantify the spatial and temporal impacts to surface water resources caused by ground water pumping. This paper describes the theory of response functions and presents an application of transient response functions in the Snake River Plain, Idaho. Transient response functions can be used to facilitate the conjunctive management of surface and ground water not only in the eastern Snake River Plain basin, but also in similar basins throughout the western United States.
机译:对西方水的需求不断增加,因此越来越需要对地表水和地下水资源进行综合管理。根据西方水法,在缺水时,高级水权所有人比初级水权所有人优先。由于难以量化地下水压力对地表水资源的影响,水管理者一直不愿联合管理地表水和地下水资源。地面的影响,水的使用可能需要数年时间才能通过含水层系统传播。预测随时间推移对地表水资源的影响程度以及影响的空间分布非常困难。响应函数用数学方法描述了在特定位置施加的单位地下水压力与系统其他位置的河流枯竭或含水层水位变化之间的关系。响应函数可用于帮助量化地下水抽取对地表水资源的时空影响。本文描述了响应函数的理论,并提出了瞬态响应函数在爱达荷州蛇河平原的应用。瞬态响应功能不仅可用于在Snake River Plain盆地东部,而且可用于美国西部类似盆地的地表水和地下水的联合管理。

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