哥斯达黎加中部太平洋沿岸含水层Jacó水文地质脆弱性

IF 0.2 Q4 GEOGRAPHY
Alicia Gómez-Cruz, H. Madrigal-Solís, Christian Núñez-Solís, Hazel Calderón-Sánchez, P. Jiménez-Gavilán
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引用次数: 2

摘要

在过去二十年中,哥斯达黎加的中太平洋地区在城市和旅游业发展方面取得了强劲增长。如果不加以管制,这种发展可能对地下水资源造成压力,从而在质量和数量方面构成威胁。本文采用GOD方法绘制了Jacó含水层水文地质脆弱性图。阐述了地质剖面,并进行了现场验证。研究区确定了2个含水层:1)沉积于Jacó冲积平原的碎屑质、多孔性、无承压的海岸含水层;2)位于Nicoya杂岩的玄武质碎裂岩中,在山区无承压,位于中部碎屑地层下方,地下水与碎屑含水层相结合。冲积含水层带的脆弱性指数为中等,山区的脆弱性指数为低。提出了管理建议。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Hydrogeological vulnerability in Jacó coastal aquifers, Central Pacific, Costa Rica
In the last two decades, the Central Pacific of Costa Rica experienced a strong growth in urban and tourism development. If not regulated, this development can result in a pressure to groundwater resources and, therefore, a threat in terms of quality and quantity. In this study, a hydrogeological vulnerability map of Jacó aquifers was performed, by the GOD method. Geological profiles were elaborated, and field verification was performed. It is confirmed that, in the study area, two aquifers are found: a) a detritic, porous, unconfined coastal aquifer, settled in the Jacó alluvial plain and, b) an aquifer in the basaltic fractured rocks of the Nicoya Complex, unconfined in the mountainous zone and underlying the detritic formation in the central area, where the groundwater is integrated to that of the detrital aquifer. The zone of the alluvial aquifer resulted in a medium vulnerability index, whereas the mountainous areas in a low vulnerability. Management recommendations were proposed.
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来源期刊
自引率
25.00%
发文量
15
审稿时长
22 weeks
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