The Water Table

Thomas L. Holzer

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The Water Table

机译：地下水位

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The water table is a fundamental concept in hydro-geology, yet it is frequently incorrectly defined. For example, both the NGWA (2003) and AGI (Neuendorf et al. 2005) glossaries define the water table as the atmospheric pressure surface that is coincident with the top of the zone of saturation. This definition is also found occasionally in groundwater textbooks as well as in primers, where it is simply defined as the top of the zone of saturation. This incorrect definition of the water table perpetuates an important conceptual misunderstanding in hydrogeology that the top of the zone of saturation is uniquely related to the water table. This commentary reviews the correct definition of the water table and addresses evidence for unsaturation beneath the water table.

机译：地下水位是水文地质学中的一个基本概念，但经常被错误地定义。例如，NGWA（2003）和AGI（Neuendorf et al。2005）词汇表都将地下水位定义为与饱和区顶部重合的大气压表面。有时在地下水教科书和底漆中也可以找到该定义，只是简单地将其定义为饱和区的顶部。地下水位的这种错误定义在水文地质学中造成了一个重要的概念误解，即饱和区的顶部与地下水位是唯一相关的。本评论评论了地下水位的正确定义，并提出了地下水位以下不饱和的证据。

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《Ground water》 |2010年第2期|171-173|共3页
作者
Thomas L. Holzer;
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U.S. Geological Survey, 345 Middlefield Road, Menlo Park, CA 94025;

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The Water Table

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