摘要
根据大气降水化学成分和岩溶水化学成分的分析，认识到了陕西镇安、旬阳地区夏秋季岩溶水 Ｈ＋ 与 Ｈ Ｃ Ｏ－３ 含量高，岩溶作用活跃，冬春季的变化相反。根据该区及南桂林等地现代岩溶作用强弱变化规律，提出了补充的岩溶作用的物理化学模式。
According to the analysis of the chemical composition of rainwater and karst ground water in Zhenan and Xunyang areas in Shaanxi province, we know that the content of H + and HCO - 3 is more in summer and autumn during which karst process is intense than in winter and spring On the basis of change laws of karst process in different seasons in the areas and Guilin areas, supplementary physical chemical model in karst process is put forward in this paper
出处
《西安工程学院学报》
1999年第3期24-27,共4页
Journal of Xi'an Engineering University
