Introductory Chapter: Aquifers Today and Tomorrow

Muhammad Salik Javaid, S. Khan
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Abstract

As defined in many scientific texts “An aquifer is an underground layer of water bearing permeable rock, rock fractures or unconsolidated material from which groundwater can be extracted using water well” [1]. Related terms used are aquitard, which is a bed of low permeability along an aquifer, and aquiclude, which is a solid, impermeable area underlying or overlying an aquifer, making an aquifer confined or unconfined. Aquifer system is a series of two or more aquifers hydraulically connected with each other. If an aquifer or an aquifer system spans more than one state, it is called transboundary aquifer [2]. An aquifer is therefore the combination of both; an underground rock structure, and water mass existing in the pores and voids. Aquifers contain by far the largest volume of unfrozen fresh water on earth thus making it an enormously important natural resource, entrusted to us by the Mother Nature for equitable use and safe custody for the next generations to come. Because of the fact that aquifer is hidden to the eye, therefore till today they are poorly known and understood by the common masses and decision makers alike.
导论章:含水层的今天和明天
正如许多科学文献所定义的那样,“含水层是地下一层含水的可渗透岩石、岩石裂缝或松散物质,可以利用水井从中提取地下水”[1]。相关术语有aquitard和aquiclude, aquitard指的是沿含水层的低渗透率地层,aquiclude指的是含水层下面或上面的不透水的固体区域,使含水层承压或无承压。含水层系统是由两个或两个以上的含水层通过水力相互连接而成的一系列含水层。如果一个含水层或含水层系统跨越一个以上的州,则称为跨界含水层[2]。因此,含水层是两者的结合;一种地下岩石结构,存在于孔隙和空隙中的水团。含水层含有迄今为止地球上最大数量的未冻淡水,因此使其成为一种极其重要的自然资源,大自然母亲委托我们为下一代公平利用和安全保管。由于含水层隐藏在肉眼看不到的地方,因此直到今天,普通大众和决策者都对含水层知之甚少。
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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