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YANG Yun-cheng, HOU Guang-cai, MA Si-jin. The age and origin of groundwater in the Ordos basin[J]. Northwestern Geology, 2004, 37(2): 97-100.
Citation: YANG Yun-cheng, HOU Guang-cai, MA Si-jin. The age and origin of groundwater in the Ordos basin[J]. Northwestern Geology, 2004, 37(2): 97-100.
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The age and origin of groundwater in the Ordos basin

  • Xi'an Institute of Geology and mineral Resourses, Xi'an, 710054, China

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  • Received Date: August 24, 2003
  • Revised Date: January 14, 2004
  • Published Date: June 04, 2004
    Graphical Abstract
    • Abstract
  • Summarizing the compositions of tritium in precipitation since the 1960's,and ba sed on the decay law of isotope,the tracks of tritium evolution in groundwater formed in different terms was described. Comparing the composition of tritium of precipitation in different terms with the evolution of tritium in groundwater formed from precipitation,the authors get conclusion that the rate of decay of tritium in groundwater is slower than that of renew of the tritium in precipitation,and explain the age and orig in of the groundwater in theodos basin,according to the composition of tritium in groundwater in the Ordos basin.
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    • References (5)
  • 刘存富,王恒纯.环境同位素水文地质学基础工业[M].1984,10.
    卫克勤,等.我国天然水中氚含量的分布特征,科学通报,1980,(10).
    Willem G. Mook. Isotope Hydrology Section international Atomic Energy [M].Vienna, UNESCO/IAEA Series on, 2000.
    IAEA database on precipitation isotope, 2003.
    Ian Clark & Peter Fritz, Environmental Isotopes in Hydrogeology, 1998.
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