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泥灰岩岩溶裂隙类型及其富水性
引用本文:孙启堂 苗本胜. 泥灰岩岩溶裂隙类型及其富水性[J]. 山东师范大学学报(自然科学版), 1991, 6(1): 69-73
作者姓名:孙启堂 苗本胜
作者单位:沂源县水利局,沂水县水资源办公室
摘    要:目前,在地下水开发工作中,国内不少地区有泥灰岩作为隔水层或弱透水层。作者从近几年来沂蒙山区泥灰岩层地下水开发实践中,总结出泥灰岩的富水条件。根据大量的钻孔资料,将泥灰岩岩溶裂隙型划分为水锤作用、结构成因、组合结构、构造作用和复合作用五种成因类型,并分析了各类型的富水性。

关 键 词:地下水 泥灰岩 岩溶裂隙 富水性

THE TYPE OF MARLITIC KARST FISSURE AND ITS WATER-RICH PROPERTY
Sun Qitang,et al.. THE TYPE OF MARLITIC KARST FISSURE AND ITS WATER-RICH PROPERTY[J]. Journal of Shandong Normal University(Natural Science), 1991, 6(1): 69-73
Authors:Sun Qitang  et al.
Affiliation:Sun Qitang,et al. Water Conservany Bureau,Yishui County,Shandong Province
Abstract:At present, in the work of groundwater exploitation marlite has been regarded asaquiclude or bad permeable stratum in many internal areas in China. In recent years, the au-thor have summed up the water-rich conditions of marlite from the practice of marlitic ground-water exploitation in Yi-Meng mountain area. According to a lot of drillhole information, the type of marlific karst fissure might be divided into five kinds of contributing factor: effect of water hammer, contributing factor of structure, composed structure, tectonic effect and compound effect. And the water-rich property of each type is expounded.
Keywords:karst fissure  marlite  water-rich conditons
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