首页> 外文期刊>Environmental Geology >Major ions in typical subterranean rivers and their anthropogenic impacts in southwest karst areas, China
【24h】

Major ions in typical subterranean rivers and their anthropogenic impacts in southwest karst areas, China

机译:中国西南喀斯特地区典型地下河中的主要离子及其人为影响

获取原文
获取原文并翻译 | 示例
           

摘要

Subterranean rivers contain much of the groundwater in karst and supply many local people in southwest China. The quality of groundwater in subterranean rivers is of concern because of its sensitivity to anthropogenic activity. Groundwater samples in a rural catchment were collected at the discharge point, and the concentrations of major ions including potassium, sodium, calcium, magnesium, chloride, sulfate, nitrate and bicarbonate were analyzed in this study. Rainfall and discharge were also observed at the same time. It could be concluded from the data that the concentrations of sulfate and nitrate had a peak in the rainy season when the concentrations of sodium, calcium, magnesium and bicarbonate were low. The concentrations of potassium and chloride changed randomly throughout the year. The concentration of major ions in flood process was not completely controlled by discharge. Only the concentrations of nitrate and sulfate had obviously increased during the past two decades. It was believed that dilution, eluviation, karst erosion and anthropogenic activity can explain the ion variations and hence this study helps to understand environmental problem in karst.
机译:地下河流蕴藏着喀斯特的大部分地下水,并为中国西南部的许多当地居民提供了水。地下河的地下水质量因其对人为活动的敏感性而受到关注。在该排放点收集了一个农村集水区的地下水样品,并分析了包括钾,钠,钙,镁,氯,硫酸根,硝酸根和碳酸氢根在内的主要离子的浓度。同时也观察到降雨和排放。从数据可以得出结论,在雨季,当钠,钙,镁和碳酸氢盐的浓度较低时,硫酸盐和硝酸盐的浓度达到峰值。全年中钾和氯的浓度随机变化。洪水过程中主要离子的浓度不能完全由放电控制。在过去的二十年中,只有硝酸盐和硫酸盐的浓度明显增加。据认为,稀释,淋洗,岩溶侵蚀和人为活动可以解释离子的变化,因此,这项研究有助于了解岩溶的环境问题。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号