Characteristics and Assessment of Groundwater

N. Akhtar, M. Syakir, M. T. Anees, A. Qadir, M. S. Yusuff
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引用次数: 5

Abstract

Groundwater system is very vital to humanity and the ecosystem. Aquifers are determined based on the absence or presence of water table positioning, that is, confined, unconfined, leaky aquifers and fractured aquifers. The objective of this chapter is to discuss the characteristic and assessment of groundwater within the scope of vertical distribution of GW, types of the aquifer system, types of SW-GW interface, and SW-GW interaction at both local and regional scales. The properties of the aquifer depend on the physical characteristics of the materials (porosity, permeability, specific yield, specific storage, and hydraulic conductivities) which are determined by techniques like resistivity surveys and pumping tests followed by remote sensing and geographic information system for better information on the groundwater system. Furthermore, understanding the SW-GW interactions through available methods (seepage meter, heat tracer, and environmental tracer) is useful in watershed management, that is, risk management and assessment of the aquifer system.
地下水特征与评价
地下水系统对人类和生态系统至关重要。含水层是根据有无地下水位定位来确定的,即承压含水层、非承压含水层、渗漏含水层和裂缝含水层。本章的目的是在局地和区域尺度上,讨论GW垂直分布范围内的地下水特征和评价、含水层系统类型、SW-GW界面类型以及SW-GW相互作用。含水层的性质取决于材料的物理特性(孔隙度、渗透率、比产量、比储水量和水力导电性),这些特性由诸如电阻率调查和抽水试验等技术确定,然后是遥感和地理信息系统,以便更好地了解地下水系统。此外,通过可用的方法(渗透计、热示踪剂和环境示踪剂)了解SW-GW相互作用有助于流域管理,即含水层系统的风险管理和评估。
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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