摘要
应用热力学原理对平顶山煤矿八矿地层中的长石、石英、高岭土及碳酸锶在该区热力学条件下溶解的可能性进行了计算。结果表明,该区矿泉水中的可溶性硅主要来自随温度升高溶解度增大的石英,锶来源于灰岩中碳酸锶的溶解。
he authors discuss the dissolubility of feldspar, quartz, kaolin and strontium carbonate in the area of No8 pit, Pingdingshan mine by using thermodynamic method. The result shows that the soluable silicon in mineral water mainly comes from the enlargement of quartz's solubility which was caused by the increasment of temperature. It also shows that the strontium comes from the solution of strontium carbonate.
出处
《现代地质》
CAS
CSCD
北大核心
1998年第2期249-252,共4页
Geoscience
关键词
煤矿
矿泉水
可溶性硅
锶
自由能
Pingdingshan mine, mineral water, soluable silicon, strontium, Gibbs free energy