Hydrological aspects of electromagnetic surveys.

B. Williams, John W. Anderson
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引用次数: 0

Abstract

Interpreting Electromagnetic (EM) surveys - Electromagnetic induction techniques have now largely replaced previous descriptive, and largely subjective, techniques used for soil salinity surveys. The question then is a matter of how to interpret the EM data. A very clear linkage exists between Apparent Electrical Conductivity (ECa) and the total soluble salts in the upper soil profile. This, in turn, can be interpreted as reflecting the degree of vertical/ lateral leaching of soluble salts, or of salt accumulation in the profile. Topography, depth to groundwater and groundwater salinity also appear to affect ECa, although they are not suited to rapid survey techniques and do not necessarily have a direct relationship with either the total salt content of the upper soil profile or the ECa values. The interpretation of isoconductivity maps in terms of the degree of leaching of the soil profile from point to point provides an added hydrological management perspective to EM soil salinity surveys.
水文方面的电磁调查。
解释电磁(EM)调查-电磁感应技术现在已经在很大程度上取代了以前用于土壤盐度调查的描述性和主观性的技术。接下来的问题是如何解读新兴市场数据。表观电导率(ECa)与上层土壤剖面中总可溶性盐之间存在非常明显的联系。反过来,这可以解释为反映可溶性盐的垂直/侧向淋滤程度,或盐在剖面中的积累程度。地形、地下水深度和地下水盐度似乎也影响非洲经委会,尽管它们不适合快速调查技术,也不一定与上层土壤剖面的总含盐量或非洲经委会值有直接关系。根据土壤剖面逐点淋滤程度对等导电性图进行解释,为EM土壤盐度调查提供了额外的水文管理视角。
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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