地下水开采——重要的CO<sub>2</sub>排放源

贾国东; 段光杰; 钟佐燊

Volume 27 Issue 2

Mar. 2002

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JIA Guo-dong, DUAN Guang-jie, ZHONG Zuo-shen, 2002. Groundwater Exploitation: An Important CO_2 Source. Earth Science, 27(2): 153-156.

Citation:

JIA Guo-dong, DUAN Guang-jie, ZHONG Zuo-shen, 2002. Groundwater Exploitation: An Important CO_2 Source. Earth Science, 27(2): 153-156.

JIA Guo-dong, DUAN Guang-jie, ZHONG Zuo-shen, 2002. Groundwater Exploitation: An Important CO_2 Source. Earth Science, 27(2): 153-156.

Citation:

JIA Guo-dong, DUAN Guang-jie, ZHONG Zuo-shen, 2002. Groundwater Exploitation: An Important CO_2 Source. Earth Science, 27(2): 153-156.

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Groundwater Exploitation: An Important CO_2 Source

1.
Guangzhou Institute of Geochemistry, Chinese Academy of Science, Guangzhou 510640, China
2.
Department of Water Resources and Environmental Engineering, China University ofGeosciences, Beijing 100083, China

Received Date: 2001-11-12
Publish Date: 2002-03-25

Abstract

Abstract

Partial CO₂pressure(p(CO₂))of groundwater from Qijia water supply base and mass transfers after the groundwater being pumped out to equilibrate with atmospheric CO₂are calculated by hydrogeochemical modeling. The results show that the groundwater p(CO₂)is pronounced higher than atmospheric p(CO₂), and that 11.15 mmol/kg CO₂will be emitted to the atmosphere when the groundwater reaches the surface. Further discussion has revealed that different lithologic aquifers usually contain higher groundwater p(CO₂).Consequently, groundwater exploitation hasbecome a man-made CO₂source and should arouse our attention.
- hydrogeochemical modeling,
- groundwater exploitation,
- CO₂ emission

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References(13)

References

[1]	张宗祜, 施德鸿, 任福弘, 等. 论华北平原第四系地下水系统之演化[J]. 中国科学(D辑), 1997, 27(2): 168-173. doi: 10.3321/j.issn:1006-9267.1997.02.006 ZHANG Z H, SHI D H, REN F H, et al. Evolution of Quaternary groundwater system in the North China plain[J]. Science in China(Series D), 1997, 27(2): 168-173. doi: 10.3321/j.issn:1006-9267.1997.02.006
[2]	贾国东, 张建立, 秦延君, 等. 地下水水质参数在抽水过程中的不稳定性及其水化学模拟——以大庆市齐家水源地为例[J]. 地球科学——中国地质大学学报, 2000, 25(2): 201-204. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200002017.htm JIA G D, ZHANG J L, QIN Y J, et al. Instability of groundwater quality parameters during pumping and its hydrochemical simulation: example from Qijia water supply base[J]. Earth Science— Journal of China University of Geosciences, 2000, 25(2): 201-204. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200002017.htm
[3]	国家计委能源所能源与环境研究室. 我国矿物燃料燃烧的CO₂排放量及削减对策[J]. 能源政策研究通讯, 1991, (2): 4-6. Institute of Energy and Environment. Amounts of CO₂emission from combustion of mineral fuel and the strategy of decreasing the emission[J]. Energy Policy Research Letter, 1991, (2): 4-6.
[4]	钱天伟, 段长春, 曹玉清. 研究地下水中HCO₃^-来源的稳定碳同位素法[J]. 长春地质学院学报, 1995, 25(2): 178-182. https://www.cnki.com.cn/Article/CJFDTOTAL-CCDZ502.010.htm QIAN T W, DUAN C C, CAO Y Q. Research on the source of HCO₃^- in groundwater by stable isotope method[J]. Journal of Changchun University of Earth Sciences, 1995, 25(2): 178-182. https://www.cnki.com.cn/Article/CJFDTOTAL-CCDZ502.010.htm
[5]	袁道先. 现代岩溶学和全球变化研究[J]. 地学前缘, 1997, 4(1~ 2): 17-25. https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY7Z1.003.htm YUAN D X. Modern karstology and global change study[J]. Earth Science Frontiers, 1997, 4(1-2): 17-25. https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY7Z1.003.htm
[6]	袁道先. 中国岩溶地球化学研究进展[J]. 水文地质工程地质, 1990, (5): 41-42. https://www.cnki.com.cn/Article/CJFDTOTAL-SWDG199005013.htm YUAN D X. Research advance on karst geochemistry in China[J]. Hydrogeology and Engineering Geology, 1990, (5): 41-42. https://www.cnki.com.cn/Article/CJFDTOTAL-SWDG199005013.htm
[7]	沈照理, 朱宛华, 钟佐. 水文地球化学基础[M]. 北京: 地质出版社, 1993. 1-189. SHEN Z L, ZHU W H, ZHONG Z S. Fundamentals of hydrogeochemistry[M]. Beijing: Geological Publishing House, 1993. 1-189.
[8]	李玉军. 西宁市南川水源地水质恶化机制[J]. 青海地质, 1996, 5(2): 43-50. https://www.cnki.com.cn/Article/CJFDTOTAL-GTJL199602006.htm LI Y J. Mechanism of deterioration of groundwater quality in Nanchuan water source site, Xining[J]. Geology of Qinghai, 1996, 5(2): 43-50. https://www.cnki.com.cn/Article/CJFDTOTAL-GTJL199602006.htm
[9]	李中琴. 大同市平原区地下水污染现状分析[J]. 山西地质, 1988, 3(2): 197-205. LI Z Q. Pollution state analysis on groundwater in plain area of Datong[J]. Shanxi Geology, 1988, 3(2): 197205.
[10]	刘金荣, 周玲玲. 岩溶地下水化学组分随降水周期变化的规律性[J]. 广西地质, 1996, 9(3): 53-61. https://www.cnki.com.cn/Article/CJFDTOTAL-GXDZ603.008.htm LIU J R, ZHOU L L. The varying regularity of major chemical compositions of karst water with precipitation cycle[J]. Guangxi Geology, 1996, 9(3): 53-61. https://www.cnki.com.cn/Article/CJFDTOTAL-GXDZ603.008.htm
[11]	陶书华. 渭北岩溶水的化学特征及其地质背景[J]. 陕西地质, 1999, 17(1): 53-57. TAO S H. The chemical characteristics and geological background of karst water in north Weinan, Shaanxi[J]. Geology of Shaanxi, 1999, 17(1): 53-57.
[12]	郭永海, 沈照理, 钟佐. 河北平原地下水化学环境演化的地球化学模拟[J]. 中国科学(D辑), 1997, 27(4): 360-365. doi: 10.3321/j.issn:1006-9267.1997.04.007 GUO Y H, SHEN Z L, ZHONG Z S. Hydrogeochemical modeling of groundwater chemical environmental evolution in Hebei plain[J]. Science in China(Series D), 1997, 27(4): 360-365. doi: 10.3321/j.issn:1006-9267.1997.04.007
[13]	高明, 华致洁, 林玉琴. 江苏省六合、盱眙玄武岩地区含偏硅酸矿泉水形成的水文地球化学机理[J]. 水文地质工程地质, 1992, (3): 39-41. https://www.cnki.com.cn/Article/CJFDTOTAL-SWDG199203015.htm GAO M, HUA Z J, LIN Y Q. The hydrogeochemical mechanism in the formation of metasilicic mineral waterin basaltic area of Liuhe and Xuyi districts, Jiangsu Province[J]. Hydrogeology and Engineering Geology, 1992, (3): 39-41. https://www.cnki.com.cn/Article/CJFDTOTAL-SWDG199203015.htm