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开采堪萨斯州高平原含水层中用于农业生产的不可持续地下水储量,预测到 2110 年。

Tapping unsustainable groundwater stores for agricultural production in the High Plains Aquifer of Kansas, projections to 2110.

机构信息

Department of Civil Engineering, Kansas State University, Manhattan, KS 66506.

出版信息

Proc Natl Acad Sci U S A. 2013 Sep 10;110(37):E3477-86. doi: 10.1073/pnas.1220351110. Epub 2013 Aug 26.

Abstract

Groundwater provides a reliable tap to sustain agricultural production, yet persistent aquifer depletion threatens future sustainability. The High Plains Aquifer supplies 30% of the nation's irrigated groundwater, and the Kansas portion supports the congressional district with the highest market value for agriculture in the nation. We project groundwater declines to assess when the study area might run out of water, and comprehensively forecast the impacts of reduced pumping on corn and cattle production. So far, 30% of the groundwater has been pumped and another 39% will be depleted over the next 50 y given existing trends. Recharge supplies 15% of current pumping and would take an average of 500-1,300 y to completely refill a depleted aquifer. Significant declines in the region's pumping rates will occur over the next 15-20 y given current trends, yet irrigated agricultural production might increase through 2040 because of projected increases in water use efficiencies in corn production. Water use reductions of 20% today would cut agricultural production to the levels of 15-20 y ago, the time of peak agricultural production would extend to the 2070s, and production beyond 2070 would significantly exceed that projected without reduced pumping. Scenarios evaluate incremental reductions of current pumping by 20-80%, the latter rate approaching natural recharge. Findings substantiate that saving more water today would result in increased net production due to projected future increases in crop water use efficiencies. Society has an opportunity now to make changes with tremendous implications for future sustainability and livability.

摘要

地下水是维持农业生产的可靠水源,但含水层的持续枯竭威胁着未来的可持续性。大平原含水层为全国 30%的灌溉地下水提供了供应,堪萨斯州的部分地区为全国农业市场价值最高的国会选区提供了支持。我们预测地下水下降情况,以评估研究区域何时可能耗尽水资源,并全面预测减少抽水量对玉米和牛肉生产的影响。到目前为止,地下水已经开采了 30%,在未来 50 年内,按照现有趋势,还将消耗另外 39%的地下水。补给量供应了当前抽水量的 15%,要完全填补一个枯竭的含水层,平均需要 500-1300 年的时间。鉴于目前的趋势,未来 15-20 年内,该地区的抽水率将大幅下降,但由于预计玉米生产中的用水效率会提高,到 2040 年,灌溉农业的产量可能会增加。如果今天减少 20%的用水量,农业生产将减少到 15-20 年前的水平,农业生产的高峰期将延长到 2070 年代以后,到 2070 年以后的产量将远远超过没有减少抽水的预测产量。情景评估了当前抽水率减少 20-80%的增量,后者接近自然补给率。研究结果证实,今天节约更多的水将导致由于未来作物用水效率的提高而导致净产量增加。社会现在有机会做出改变,这对未来的可持续性和宜居性具有巨大影响。

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