Assessment of Transmissivity of the Weathered Upper Part of Horizontally Layered Bedrock

IF 0.3 Q4 GEOLOGY
A. V. Lekhov
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引用次数: 0

Abstract

The results of flowmeter tests of wells in the upper part of a layered rock massif indicate a model of the permeability medium in the form of separate horizontal thin fracture zones, separated by layers with a thickness of several meters. Pumping was studied with a model in cylindrical coordinates for two thin aquifers. The upper one works with a constant pressure in pumping a well, determined by the position of the zone, and a decreasing rate, and the lower, with an increasing rate, is additional to the pump rate. The filter intervals of the central and the only observation well are the same. Processing of the pumping results with the commonly used Jacob method showed the main features: strong differences in transmissivity in different variants of well locations, unrealistically large values of the storage coefficient, and an ultrasmall calculated radius of the pumping well.

Abstract Image

水平层状基岩风化上部透射率评估
摘要 对层状岩体上部的水井进行流量计测试的结果表明,渗透介质的形式为独立的水平薄断裂带,被厚度为几米的岩层隔开。通过对两个薄含水层的圆柱坐标模型进行抽水研究。上层含水层的抽水井压力恒定,由含水层的位置决定,抽水速率递减;下层含水层的抽水速率递增,是抽水速率的附加值。中央观察井和唯一观察井的过滤间隔相同。用常用的雅各布法处理抽水结果显示了以下主要特征:不同井位的渗透率差异很大,储水系数的数值过大,抽水井的计算半径过小。
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来源期刊
CiteScore
0.60
自引率
25.00%
发文量
43
期刊介绍: Moscow University Geology Bulletin  is the journal that mainly publishes scientific articles, short reports of graduate students, and reviews. Publications made by the members of the Faculty of Geology of the Moscow State University and their collaborators are published. Publications encompass all branches of geology.
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