| 山东临淄地区同位素水文地质研究 |
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| 引用本文： | 陈余道.山东临淄地区同位素水文地质研究[J].桂林工学院学报,1993(3). |
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| 作者姓名： | 陈余道 |
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| 作者单位： | 桂林冶金地质学院水文地质及工程地质系 |
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| 摘 要： | 应用同位素分布特征来解决水文地质问题是一种常用的研究方法。通过对临淄地区稳定同位素~(18)O及D、放射性同位素氚的分布特征的研究,给出了该地区冲积扇首部裂隙岩溶水的补给区,补给高程及补给年龄,并得出了地下水从冲积扇首部迁移到前缘至少需要15年时间的结论,从而为研究区环境质量评价提供了重要依据。
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| 关 键 词： | 稳定同位素 放射性同位素 水文地质 山东 淄博 |
THE STUDY OF ISOTOFE HYDROGEOLOGY IN LINZI AREA |
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| Chen Yudao.THE STUDY OF ISOTOFE HYDROGEOLOGY IN LINZI AREA[J].Journal of Guilin University of Technology,1993(3). |
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| Authors: | Chen Yudao |
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| Abstract: | It is a usual method to study hydrological problems according to isotopic analysis. On the basis of the analysis of the distribution of stable isotopes (~(18)O and D) and radioactive isotope (~3H) in Linzi area, the supply region, height and age of interstitial water in the front of the alluvial cone are given in this paper. The author concludes that it takes 15 years to transport for groundwater from the alluvial cone beginning to the end. This offerrs an important testimony for the environmental assessment over this area. |
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| Keywords: | stable isotope radioactive isotope hydrology Shandong Zibo |
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