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一、研究意义及现状研究喀斯特水的形成及其运动动态规律,既是阐明喀斯特发育规律的基础,也是定性和定量评价喀斯特发育程度及其水文地质条件的基础。因而阐明这一问题,不仅具有重要理论意义,而且有极大的实际价值。在文献中,过去将有关这一问题的研究称为喀斯特水形学(或译水文地理学)。近来,由于其所涉及的问题和服务的对象主要是属于水文地质方面的,因此大多数学者趋向于将其归入喀斯特水文地质学范畴之内,仅某些地理学者(如H.A.格沃兹杰茨基1954)仍沿用这一术语。在所谓喀斯特水形学中所讨论的问题,通常包括以下几个方面:1)喀斯特含水介质的特性及由其所决定的喀斯特水的埋藏条件;2).喀斯特水的循环及水动力带的划分;
First, the research significance and current situation The formation of karst water and its dynamic laws of motion are not only the basis for clarifying the law of karst development, but also the basis for qualitatively and quantitatively evaluating the degree of karst development and its hydrogeological conditions. Therefore, clarifying this issue not only has important theoretical significance, but also has great practical value. In the literature, research on this subject was referred to as Karst (or hydrogeography) in the past. Recently, most of the scholars tend to include them in the category of karst hydrogeology due to the fact that the objects and services they deal with are mainly of hydrogeology. Only some geographers Czki 1954) still use the term. The problems discussed in the so-called Karst hydrology usually include the following aspects: 1) the characteristics of karst aquifer and the burial conditions of karst water determined by them; 2) the karst water circulation and hydrodynamic band Divide