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heng yang hong ceng rong kong shui tan suan gai xi chu de fan ying ji li fen xi
Author(s): 
Pages: 32-34
Year: Issue:  1
Journal: Hydrogeology and Engineering Geology

Keyword:  溶孔碳酸钙沉淀地下水红色泥岩红层机理分析硫酸盐矿物水空间方解石水-岩作用;
Abstract: <正> 衡阳红色泥岩含水层中含有比较丰富的溶孔水,含水空间是由大量的溶孔及裂隙组成。大量的溶孔层是地下水溶解硫酸盐矿物造成的。另一方面,大量微小裂缝及溶孔均有一定量的碳酸钙沉淀充填。含水层处于地表浅部,埋深一般在百米之内,水-岩作用
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