首页> 外文期刊>Hydrological Processes >Evaluation of water-use policies for baseflow recovery during droughts in an agricultural intensive karst watershed: Case study of the lower Apalachicola-Chattahoochee-Flint River Basin, southeastern United States
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Evaluation of water-use policies for baseflow recovery during droughts in an agricultural intensive karst watershed: Case study of the lower Apalachicola-Chattahoochee-Flint River Basin, southeastern United States

机译:农业集约型喀斯特流域干旱期间基流恢复的用水政策评估:美国东南部阿巴拉契科拉-恰塔胡奇-弗林特河盆地下游的案例研究

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摘要

The lower Apalachicola-Chattahoochee-Flint River Basin in the Southeast United States represents a major agricultural area underlain by the highly productive karstic Upper Floridan aquifer (UFA). During El Nino Southern Oscillation-induced droughts, intense groundwater withdrawal for irrigation lowers streamflow in the Flint River due to its hydraulic connectivity with the UFA and threatens the habitat of the federally listed and endangered aquatic biota. This study assessed the compounding hydrologic effects of increased irrigation pumping during drought years (2010-2012) on stream-aquifer water exchange (stream-aquifer flux) between the Flint River and UFA using the United States Geological Survey modular finite element groundwater flow model. Principal component and K-means clustering analyses were used to identify critical stream reaches and tributaries that are adversely affected by irrigation pumping. Additionally, the effectiveness of possible water restriction scenarios on stream-aquifer flux was also analysed. Moreover, a cost-benefit analysis of acreage buyout procedure was conducted for various water restriction scenarios. Results indicate that increased groundwater withdrawal in Water Year 2011 decreased baseflow in the lower Apalachicola-Chattahoochee-Flint River Basin, particularly, in Spring Creek, where irrigation pumping during April, June, and July changed the creek condition from a gaining to losing stream. Results from sensitivity analysis and simulated water restrictions suggest that reducing pumping in selected sensitive areas is more effective in streamflow recovery (approximately 78%) than is reducing irrigation intensity by a prescribed percentage of current pumping rates, such as 15% or 30%, throughout the basin. Moreover, analysis of acreage buyout indicates that restrictions on irrigation withdrawal can have significant impacts on stream-aquifer flux in the Basin, especially in critical watersheds such as Spring and Ichawaynochaway Creeks. The proposed procedure for ranking of stream reaches (sensitivity analysis) in this study can be replicated in other study areas/models. This study provides useful information to policymakers for devising alternate irrigation water withdrawal policies during droughts for maintaining flow levels in the study area.
机译:美国东南部的Apalachicola-Chattahoochee-Flint河下游流域是主要的农业地区,高生产力的岩溶地层的上佛罗里达水层(UFA)是该地区的基础。在厄尔尼诺南方涛动引起的干旱期间,由于与UFA的水力连通性,大量灌溉用水抽取了弗林特河的水流,并威胁了受联邦政府保护和濒临灭绝的水生生物的栖息地。这项研究使用美国地质调查局模块化有限元地下水流模型评估了干旱年份(2010-2012年)增加的灌溉抽水对弗林特河和UFA之间的河流-含水层水交换(河流-含水层通量)的复合水文影响。主成分和K-均值聚类分析用于确定受到灌溉抽水不利影响的关键河段和支流。此外,还分析了可能的水限制方案对水-水流通量的有效性。此外,针对各种用水限制方案进行了土地购买程序的成本效益分析。结果表明,2011年水年度地下水抽取量增加,导致阿巴拉契科拉-查塔胡奇-弗林特河下游盆地的底流量减少,特别是在春溪地区,4月,6月和7月的灌溉抽水使小溪的状况从增加变为减少。敏感性分析和模拟水限制的结果表明,与在指定的百分比下(例如15%或30%)的整个灌溉速率下降低灌溉强度相比,减少选定敏感区域的抽水能更有效地恢复径流(约78%)。盆地。此外,对种植面积买断的分析表明,对灌溉撤出的限制可能会对流域内的含水层通量产生重大影响,特别是在诸如Spring和Ichawaynochaway Creeks等关键流域。在本研究中提出的用于确定河流水位(敏感性分析)的程序可以在其他研究领域/模型中重复使用。这项研究为决策者在干旱期间制定替代灌溉取水政策以维持研究区域的流量水平提供了有用的信息。

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