地下水补给、循环和混合作用的氦同位素证据─&mdash;以石羊河、黑河流域为例

史基安; 王先彬; 王琪; 赵兴东; 李春园; 孙明良

ISSN 1000-0550 CN 62-1038/P

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地下水补给、循环和混合作用的氦同位素证据─—以石羊河、黑河流域为例

史基安, 王先彬, 王琪, 赵兴东, 李春园, 孙明良

文章导航 > 沉积学报 > 1999 > 17(S1): 815-819

史基安, 王先彬, 王琪, 赵兴东, 李春园, 孙明良. 地下水补给、循环和混合作用的氦同位素证据─—以石羊河、黑河流域为例[J]. 沉积学报, 1999, 17(S1): 815-819.

引用本文:

SHI Ji-an, WANG Xian-bin, WANG Qi, ZHAO Xing-dong, LI Chun-yuan, SUN Ming-liang. Evidences from Helium Isotope for Groundwater Supplement,Circul ation and Mixing—Taking the Shiyanghe and Heihe river basins as an example[J]. Acta Sedimentologica Sinica, 1999, 17(S1): 815-819.

Citation:

SHI Ji-an, WANG Xian-bin, WANG Qi, ZHAO Xing-dong, LI Chun-yuan, SUN Ming-liang. Evidences from Helium Isotope for Groundwater Supplement,Circul ation and Mixing—Taking the Shiyanghe and Heihe river basins as an example[J]. Acta Sedimentologica Sinica, 1999, 17(S1): 815-819.

引用本文:

Citation:

SHI Ji-an, WANG Xian-bin, WANG Qi, ZHAO Xing-dong, LI Chun-yuan, SUN Ming-liang. Evidences from Helium Isotope for Groundwater Supplement,Circul ation and Mixing—Taking the Shiyanghe and Heihe river basins as an example[J]. Acta Sedimentologica Sinica, 1999, 17(S1): 815-819.

地下水补给、循环和混合作用的氦同位素证据─—以石羊河、黑河流域为例

中国科学院兰州地质研究所,气体地球化学国家重点实验室,兰州 730000

基金项目: 国家科学技术部特别资助;中国科学院重点和西部之光资助

详细信息

作者简介:
史基安，男，1958年出生，研究员，沉积学。

中图分类号: P597

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文章访问数: 489
HTML全文浏览量: 20
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被引次数: 0

Evidences from Helium Isotope for Groundwater Supplement,Circul ation and Mixing—Taking the Shiyanghe and Heihe river basins as an example

Lanzhou Institute of Geology,Chinese Academy of Sciences Lanzhou 730000

摘要

摘要: 石羊河、黑河流域地下水氦同位素组成的研究表明，大部分样品的³He/⁴He具有大气降水特征，部分地区地下水⁴He同位素的过剩是基岩裂隙水和卤水的混合作用所致，祁连山前深大断裂带附近地下水的氮同位素具有明显的馒源氦特征，说明该断层的活动仍未停止。
- 石羊河流域 /
- 地下水 /
- 氦同位素 /
- 混合作用
Abstract: Shiyanghe and Heihe rivers,situated in the east part of Hexi Corridor,Gansu province,are two typical rivers in the arid and semi-arid area. According to the groundwateic helium isotope composition,most samples collected from these two river basins are of meteoric characteristics. Theirδ³He values range from -93.8%-181.4%, but most of them are close to the atmosphere helium with δ³He ranging between-20-+200%³He/²⁰Ne distribute in the range of 4.65×10^-7-7.43×10^-7, which is slightly higher than that of the air, indicating that their origin is mainly from the meteoric water. In the northwest of Wuwei basin,Shiyanghe river the He³/He⁴ values of groundwater is lower than atmosphere helium in 1-2 magnitude of orders,implying that the mixing of radiogenic helium from adjacent granite bodies in which abundant minerals containing U and Th are observed. The decay of U and Th can produce a large amount of ⁴He resulting in the excess of helium in the groundwater. The eminent accumulation of radiogenic helium shows that the circulation period of groundwater in this area could be 1000 years. Along the hidden fault in the front of the Qilian Mountains can observe the much higher ³He/⁴He values with δ³He ranging from 70%-180 %, indicating that the eminent contribution of mantle helium which implies that the Fault is still active.
- Shiyanghe river basin /
- groundwater /
- helium isotope /
- mixing

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参考文献(1)

[1]

1 王先彬编著.稀有气体同位素地球化学和宇亩化学[M].北京:科学出版社，1989

2 Kamensky I L. Tnkarev I V, Tolstikhin I N. ³H一³He dating: A case for nuxmg of young and old groundwaters[J]. Geochim. Cosmoclum. Acta,1991, 55:2895-2899

3 王先彬，陈践发，徐胜等.地震区温泉气体的地球化学特征[J].中国科学，1992,8(84):9-854

4 Tolstinkhin I. Lehmann B E,Loosli H H,Gautschi A. Helium and argon isotopes in rocks，minerals, and related groundwaters: A case study in northern Switzerland[J].Geochim. Cosmochim. Acta, 1996,60:1497-1514

5 Savchenko V P. The problem of geochemistry of helium[J]. Natural Gases,1935,9:53-197

6 Weiss R F. Solubility of Helium and neon in water and sea water [J]. Jour.Chem.Eng. Data,1971,16,235-241

7 Schlosser P,Stute M,Sonntag C,Munnich KO. Tritiogenic ³He in shallow groundwater[J]. Earth and Planetary Science Letters,1989,94:245-256

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地下水补给、循环和混合作用的氦同位素证据─—以石羊河、黑河流域为例

中国科学院兰州地质研究所,气体地球化学国家重点实验室,兰州 730000

基金项目: 国家科学技术部特别资助;中国科学院重点和西部之光资助

作者简介:
史基安，男，1958年出生，研究员，沉积学。

收稿日期: 1999-12-04
修回日期: 1999-02-05
刊出日期: 1999-12-10

中图分类号: P597

关键词:

石羊河流域 /

地下水 /

氦同位素 /

混合作用

摘要: 石羊河、黑河流域地下水氦同位素组成的研究表明，大部分样品的³He/⁴He具有大气降水特征，部分地区地下水⁴He同位素的过剩是基岩裂隙水和卤水的混合作用所致，祁连山前深大断裂带附近地下水的氮同位素具有明显的馒源氦特征，说明该断层的活动仍未停止。

English Abstract

Evidences from Helium Isotope for Groundwater Supplement,Circul ation and Mixing—Taking the Shiyanghe and Heihe river basins as an example

Lanzhou Institute of Geology,Chinese Academy of Sciences Lanzhou 730000

Received Date: 1999-12-04
Rev Recd Date: 1999-02-05
Publish Date: 1999-12-10

Keywords:

Abstract: Shiyanghe and Heihe rivers,situated in the east part of Hexi Corridor,Gansu province,are two typical rivers in the arid and semi-arid area. According to the groundwateic helium isotope composition,most samples collected from these two river basins are of meteoric characteristics. Theirδ³He values range from -93.8%-181.4%, but most of them are close to the atmosphere helium with δ³He ranging between-20-+200%³He/²⁰Ne distribute in the range of 4.65×10^-7-7.43×10^-7, which is slightly higher than that of the air, indicating that their origin is mainly from the meteoric water. In the northwest of Wuwei basin,Shiyanghe river the He³/He⁴ values of groundwater is lower than atmosphere helium in 1-2 magnitude of orders,implying that the mixing of radiogenic helium from adjacent granite bodies in which abundant minerals containing U and Th are observed. The decay of U and Th can produce a large amount of ⁴He resulting in the excess of helium in the groundwater. The eminent accumulation of radiogenic helium shows that the circulation period of groundwater in this area could be 1000 years. Along the hidden fault in the front of the Qilian Mountains can observe the much higher ³He/⁴He values with δ³He ranging from 70%-180 %, indicating that the eminent contribution of mantle helium which implies that the Fault is still active.

引用本文:

Citation:

SHI Ji-an, WANG Xian-bin, WANG Qi, ZHAO Xing-dong, LI Chun-yuan, SUN Ming-liang. Evidences from Helium Isotope for Groundwater Supplement,Circul ation and Mixing—Taking the Shiyanghe and Heihe river basins as an example[J]. Acta Sedimentologica Sinica, 1999, 17(S1): 815-819.

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地下水补给、循环和混合作用的氦同位素证据─—以石羊河、黑河流域为例

作者简介:
史基安，男，1958年出生，研究员，沉积学。

计量

Evidences from Helium Isotope for Groundwater Supplement,Circul ation and Mixing—Taking the Shiyanghe and Heihe river basins as an example

计量

目录

地下水补给、循环和混合作用的氦同位素证据─—以石羊河、黑河流域为例

中国科学院兰州地质研究所,气体地球化学国家重点实验室,兰州 730000

作者简介:
史基安，男，1958年出生，研究员，沉积学。

English Abstract

Evidences from Helium Isotope for Groundwater Supplement,Circul ation and Mixing—Taking the Shiyanghe and Heihe river basins as an example

Lanzhou Institute of Geology,Chinese Academy of Sciences Lanzhou 730000

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地下水补给、循环和混合作用的氦同位素证据─—以石羊河、黑河流域为例

作者简介: 史基安，男，1958年出生，研究员，沉积学。

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Evidences from Helium Isotope for Groundwater Supplement,Circul ation and Mixing—Taking the Shiyanghe and Heihe river basins as an example

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出版历程

目录

地下水补给、循环和混合作用的氦同位素证据─—以石羊河、黑河流域为例

中国科学院兰州地质研究所,气体地球化学国家重点实验室,兰州 730000

作者简介: 史基安，男，1958年出生，研究员，沉积学。

English Abstract

Evidences from Helium Isotope for Groundwater Supplement,Circul ation and Mixing—Taking the Shiyanghe and Heihe river basins as an example

Lanzhou Institute of Geology,Chinese Academy of Sciences Lanzhou 730000

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期刊在线

联系我们

作者简介:
史基安，男，1958年出生，研究员，沉积学。

作者简介:
史基安，男，1958年出生，研究员，沉积学。