智利北部沙漠地区的地下水

Toshio Murashita, Kaneo Kakegawa, T. Tsuchiya
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引用次数: 0

摘要

本文简要介绍了智利北部沙漠地区地下水资源概况。在海拔4000米的Pampa Lirima,含水层处于自流状态,其厚度约为20米。在海拔1500 - 2700米的安第斯山脉前地区,温泉是居民主要的饮用和灌溉水源。在Tamarugal Pampa del Tamarugal,自流水在夏季被河水补充,用于供水和采矿。大部分地下水富含钠和盐酸盐,它们主要来自安第斯山脉的火山。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Ground Water of the Desert Area in Northern Chile
This paper describes a brief outline of ground-water resources in the desert area in the northern part of Chile.
In Pampa Lirima, 4, 000 meters above sea level, the aquifer is under flowing artesian condition, and its thickness is about twenty meters.
In Pre-Andes area, 1, 500-,2, 700 meters above sea level, hot springs are the principal sources of drinking and irrigation for inhabitants.
In Pampa del Tamarugal, the artesian water, replenished with the rive water in the summer, is pumped up for the water supply and mining.
Most of ground water is rich in sodium and salfate, which are derived principally from the Andes volcanos.
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