Geophysical characterization of near-surface formations in the La Villa River catchment (Los Santos, Panama)

F. Rejiba, A. Mojica, M. Schmutz, A. Ruiz, M.G. Castrellón, J. L. D. Guevara, S. Saavedra, J. Fábrega, C. Finco, C. Schamper, L. C. Fraga, M. Llubes
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引用次数: 3

Abstract

Summary The central Pacific Region (Panama) is known to suffer from water scarcity during periods of extended drought. The groundwater/surface water interactions and dynamics, provided by conceptual or numerical models are crucial for water resource management. At the regional scale, such models generally lack of structural information concerning the internal variability of the near surface formations. The spatialization of the direct observations from sparse boreholes can only achieved by geophysical investigations. The aim of this work is to characterize, in the La Villa groundwater basin, the near surface aquifer located in the lateritic horizon using electrical resistivity imaging (ERI), vertical electrical soundings (VES) and time domain electromagnetic soundings (TDEM). This case study illustrates the relevance of the use coupled ERI, TDEM and VES to describe the near surface variability due to the leaching of the lateritic horizon as well as the level of the water table.
La Villa河流域(Los Santos, Panama)近地表地层的地球物理特征
众所周知,中太平洋地区(巴拿马)在长期干旱期间缺水。概念或数值模型提供的地下水/地表水相互作用和动态对水资源管理至关重要。在区域尺度上,这种模式通常缺乏关于近地表地层内部变率的结构信息。稀疏钻孔直接观测的空间化只能通过地球物理调查来实现。这项工作的目的是利用电阻率成像(ERI)、垂直电测深(VES)和时域电磁测深(TDEM)对La Villa地下水盆地位于红土层的近地表含水层进行表征。本案例研究说明了耦合使用ERI、TDEM和VES来描述由于红土层浸出和地下水位引起的近地表变化的相关性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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