摘要
分析了娘子关泉域岩溶地下水SO2-4,Ca2+,Mg2+等组分含量增多的原因,并定量地探讨了SO2-4,Ca2+,Mg2+的各种来源比例。研究表明,含水层中石膏溶解及硫化物氧化是造成SO2-4,Ca2+,Mg2+高含量的主要原因,控制硫化物氧化水进入含水层,对水质改良有显著效果。
The causes of high concentration of SO 2- 4,Ca 2+ and Mg 2+ in karst water in Niangziguan spring area are analyzed,and the mixing proportions of SO 2- 4,Ca 2+ and Mg 2+ from different sources are quantitatively discussed.The research shows that the high concentration of SO 2- 4,Ca 2+ and Mg 2+ is mainly caused by gypsum dissolving and sulfide oxidation in aquifer bed.Preventing sulfide oxidation water from seeping into ground water will remedy water quality efficiently
出处
《地质科技情报》
CAS
CSCD
北大核心
1998年第A02期111-114,共4页
Geological Science and Technology Information
基金
国家自然科学基金