河北平原第四系深层地下水<sup>36</sup>Cl同位素年龄的研究

董悦安; 何明; 蒋崧生; 武绍勇; 姜山

Volume 27 Issue 1

Jan. 2002

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Article Navigation > Earth Science > 2002 > 27(1): 105-109

DONG Yue-an, HE Ming, JIANG Song-sheng, WU Shao-yong, JIANG Shan, 2002. Chlorine-36 Age Study for Deep Groundwater of Quaternary Sediments, Hebei Plain. Earth Science, 27(1): 105-109.

Citation:

DONG Yue-an, HE Ming, JIANG Song-sheng, WU Shao-yong, JIANG Shan, 2002. Chlorine-36 Age Study for Deep Groundwater of Quaternary Sediments, Hebei Plain. Earth Science, 27(1): 105-109.

DONG Yue-an, HE Ming, JIANG Song-sheng, WU Shao-yong, JIANG Shan, 2002. Chlorine-36 Age Study for Deep Groundwater of Quaternary Sediments, Hebei Plain. Earth Science, 27(1): 105-109.

Citation:

DONG Yue-an, HE Ming, JIANG Song-sheng, WU Shao-yong, JIANG Shan, 2002. Chlorine-36 Age Study for Deep Groundwater of Quaternary Sediments, Hebei Plain. Earth Science, 27(1): 105-109.

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Chlorine-36 Age Study for Deep Groundwater of Quaternary Sediments, Hebei Plain

1.
Institute of Low Energy Nuclear Physics, Beijing Normal University, Beijing 100875, China
2.
Beijing Radiation Center, Beijing 100875, China
3.
Radiation Beams and Material Engineering Laboratory of Education Ministry, Beijing 100875, China
4.
Institute of Nuclear Physics, China Institute of Atomic Energy, Beijing 102413, China

Received Date: 2001-03-28
Publish Date: 2002-01-25

Abstract

Abstract

For the study of the groundwater age in the deep formation of Quaternary sediments of Hebei plain, the N(³⁶Cl)/N(Cl) ratio of groundwater samples were determined by tandem accelerator mass spectrometry. The chlorine 36 ages were compared with hydrodynamic ages. The groundwater of the third and fourth aquifers of Quaternary sediments in the Baoding district of Hebei plain was found young, that of the third aquifer in the east of Baoding district and the west of Cangzhou district being less than 50 thousand years and that of the fourth aquifer, perhaps more than 100 thousand years. While the groundwater age of the third aquifer in Cangzhou city and Qingxian county was 80-90 thousand years and that in Dongguang county was 260 thousand years, that of the fourth aquifer in Cangzhou city was 330 thousand years and that in Dongguang county was 770 thousand years.
- chlorine 36 age,
- accelerator mass spectrometry,
- Hebei plain

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References(18)

References

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