供稿: 周廷强;林健旺;高宝珠;王心义 | 时间: 2019-05-31 | 次数: |
作者单位:焦作工学院资源与环境工程系;天津地热勘查开发设计院
摘要:放射性同位素14C的半衰期为5730±40a,在地热研究中是一个其他同位素所不能替代的测年工具.天津地热田各热储层在空间上的不连续性导致了地热水的年龄差异.因此,本文利用放射性同位素14C实测的地热水年龄,分析了天津深部地热水的运移机制,为地热水的进一步开发利用提供了科学依据.
基金:河南省自然科学基金(0211060200);焦作工学院博士基金资助.;
分类号:P314.1
Application of radioisotope14C to geothermal analysis
Abstract:The radioisotope14C, an irreplaceable dating tool in thermal analysis, has an half?life value of5?730±40 years.In the space of the discontinuity of the reservoirs in Tianjin geothermal field, this leads to the age difference of geothermal water.Based on the measuremeant of the age of14C, the paper analyses the migratory mechanism of deep geothermal water, which provides scientific basis for its further exploiting and utilization.