摘要
临朐山旺泉苏打水赋存于临朐群牛山组蜂窝状玄武岩中,水质优良,开发前景广阔,该文利用高压反应釜模拟实际地层条件下水岩平衡反应,同时辅以同位素分析,矿物X-射线衍射分析等手段,结合当地特殊的水文地质背景,系统性地阐明了苏打水形成机理。
Shanwang spring natural soda water occurred in vesicular basalt rocks in Niushan formation of Linqu group. Its water quanlity is good and has vast exploitable prospect. In this paper,by using high pressure reaction kettle,actual forming conditions of water and rock reaction balance has been simulated. At the same time,with the Isotopic analysis,X-ray diffraction analysis and other means,combining with local special hydrological and geological background,the formation mechanism of soda water has been introduced systematically.
出处
《山东国土资源》
2016年第5期51-54,共4页
Shandong Land and Resources
关键词
天然苏打水
山旺泉
形成环境
水岩平衡
临朐山旺
Natural soda water
forming environment
balance between rock and water
Shanwang spring in Linqu county