摘要
在山东省德州市首次探明国内稀有含碘饮用天然矿泉水──“中华碘泉”。研究表明,矿泉水是在新生代断陷盆地发育的构造背景和弱碱氧化的水文地球化学环境条件下,地下水与含水介质长期水-岩反应中经溶滤形成的;矿泉水水量丰富,水质优良,为含碘小苏打型矿泉水,但氟含量偏高,为合理开发这一宝贵资源,可选用电渗析、倾析方法以降低氟含量,并将其作为规模化含碘矿泉水生产的技术工艺。
This is the first work to verity the rare iodine-bearing natural drinking mineralwater named 'Sino iodine-bearing mineralwater'. The study shows that this mineralwater was formed in a Cenozoic fault-bounded basin with weakly basic and oxidizing hydrogeochemical condition.It is the product of the reaction between the groundwater and the continental clastic sediments. The high-quality water belongs to the iodine-bearing soda type mineralwater with slightly higher concentration of fluorine.In order to exploit the water reasonably,the electronic percolation technique is suggested to be used to reduce the fluorine during large-scale production.
出处
《高校地质学报》
CAS
CSCD
1995年第1期97-100,共4页
Geological Journal of China Universities
关键词
中华碘泉
矿泉水
德州市
开发利用
Sino iodine-bearing mineralwater,mineralwater,exploitation, Dezhou city