Loáiciga Hugo A
Department of Geography, University of California, Santa Barbara, CA 93106.
Ground Water. 2017 May;55(3):334-345. doi: 10.1111/gwat.12481. Epub 2016 Oct 25.
Methods for calculating the safe yield are evaluated in this paper using a high-quality and long historical data set of groundwater recharge, discharge, extraction, and precipitation in a karst aquifer. Consideration is given to the role that climatic variability has on the determination of a climatically representative period with which to evaluate the safe yield. The methods employed to estimate the safe yield are consistent with its definition as a long-term average extraction rate that avoids adverse impacts on groundwater. The safe yield is a useful baseline for groundwater planning; yet, it is herein shown that it is not an operational rule that works well under all climatic conditions. This paper shows that due to the nature of dynamic groundwater processes it may be most appropriate to use an adaptive groundwater management strategy that links groundwater extraction rates to groundwater discharge rates, thus achieving a safe yield that represents an estimated long-term sustainable yield. An example of the calculation of the safe yield of the Edwards Aquifer (Texas) demonstrates that it is about one-half of the average annual recharge.
本文利用喀斯特含水层中高质量的长期地下水补给、排泄、抽取及降水历史数据集,对安全开采量的计算方法进行了评估。考虑了气候变率在确定用于评估安全开采量的气候代表性时期方面所起的作用。用于估算安全开采量的方法与其作为避免对地下水产生不利影响的长期平均抽取率的定义相一致。安全开采量是地下水规划的一个有用基线;然而,本文表明它并非在所有气候条件下都能良好运行的操作规则。本文表明,由于动态地下水过程的性质,采用将地下水抽取率与地下水排泄率相联系的适应性地下水管理策略可能最为合适,从而实现代表估计长期可持续开采量的安全开采量。对爱德华兹含水层(德克萨斯州)安全开采量的计算示例表明,其约为年平均补给量的一半。