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首页> 外文期刊>Chilean Journal of Agricultural Research >Assessment of current and potential yield of hand-dug wells in a semi-arid zone in south-central Chile using an analytical methodology
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Assessment of current and potential yield of hand-dug wells in a semi-arid zone in south-central Chile using an analytical methodology

机译:使用分析方法评估智利中南部半干旱地区手挖井的当前和潜在产量

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The semi-arid interior dryland region in south-central Chile is characterized by shrink-swell granitic soils and a semi-arid Mediterranean climate, which together cause scarce dry-season surface water supplies. Historically, the lack of easily accessible water has limited the region's economic development. In most of the region's rural communities, the only local water supplies for drinking and small-scale irrigation are shallow, hand-dug wells. The objectives of this study, conducted in the San José catchment in the Biobío Region (36°24' S, 72°30' W), were to demonstrate the usefulness of a simple aquifer characterization methodology to assess the likelihood of additional extraction of groundwater in this area with existing wells, estimate potential increases in productivity through increases in well depth, and present the spatial distribution of aquifer properties in this area. Hydraulic conductivity values (Ks) were measured from analyses of recovery rates of hand-dug wells. Values of Ks ranged between 0.04 and 5.1 m d-1 (mean = 1.07 m d-1; standard deviation = 1.36 m d-1), which resulted in a low yield from the shallow wells. These Ks values were used to estimate the potential groundwater yield which could be extracted from hand-dug wells in the region in their current condition with increased pumping and, where feasible, if wells were deepened by 0.5 m. Results suggested that existing wells could produce up to 0.008 m yr-1 and up to 0.02 m yr-1 by deepening them. Since current water usage has been estimated as 0.002 m yr-1, these results suggest that additional groundwater supplies could be exploited.
机译:智利中南部的半干旱内陆干旱地区以花岗岩膨胀土壤和半干旱地中海气候为特征,两者共同导致旱季地表水供应稀缺。从历史上看,缺乏容易获得的水限制了该地区的经济发展。在该地区的大多数农村社区中,仅有的用于饮用水和小规模灌溉的本地供水是浅井,手工挖井。这项研究的目标是在比奥比奥地区(36°24'S,72°30'W)的SanJosé流域进行的研究,目的是证明一种简单的含水层表征方法对评估额外开采地下水的可能性的有效性。在已有井的区域,通过增加井深来估计生产力的潜在增长,并显示该区域含水层性质的空间分布。水力传导率值(Ks)是通过分析手挖井的回收率来测量的。 Ks值介于0.04和5.1 m d-1之间(平均值= 1.07 m d-1;标准偏差= 1.36 m d-1),这导致浅井的产量较低。这些Ks值用于估计潜在的地下水产量,可以在当前条件下通过增加抽水量从该地区的手挖井中抽取水,并且在可行的情况下,如果将井加深0.5 m。结果表明,现有的油井通过加深,最多可产生0.008 m yr-1和0.02 m yr-1。由于目前的用水量估计为0.002 m yr-1,这些结果表明可以开发更多的地下水供应。

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