J4 ›› 2011, Vol. 41 ›› Issue (4): 1144-1150.

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Comparison of 4He and 14C Dating of Groundwater from Quaternary Confined Aquifers in Hebei Plain

WEI Wen, CHEN Zong-yu, ZHAO Hong-mei, LIU Jun, WANG Ying   

  1. Institute of Hydrogeology and Environmental Geology, Chinese Academy of Geological Sciences, Shijiazhuang050061, China
  • Received:2010-10-21 Online:2011-07-26 Published:2011-07-26

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Abstract:

4He isotope is an ideal tracer for groundwater dating, but it was generally disagreement with 14C dating results due to dating scales and multisources. By taking noble gas samples and 14C samples in the same well from the Quaternary aquifers in Hebei Plain，the results revealed that the concentrations of radiogenic 4Herad components ranged from 5.43×10-8 to 8 994×10-8 cm3·STP/g by using closed-system equilibration (CE) model. Furthermore, it was found that 4He age of groundwater ranged from 8.8 to 55.9 ka and 14C age ranged from 7.7 to 35.2 ka, which indicated that above two results differed slightly and correspondingly we can concluded that the application of 4He dating in Hebei Plain is reasonable.

Key words: Hebei Plain, groundwater, CE model, 4Helium

CLC Number: 

  • P641.7
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