水化学揭示的弱透水层孔隙水演化特征及其古气候指示意义

李静; 梁杏; 毛绪美; 王聪; 柳富田

doi:10.3799/dqkx.2012.070

Volume 37 Issue 3

May 2012

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Article Navigation > Earth Science > 2012 > 37(3): 612-620

LI Jing, LIANG Xing, MAO Xu-mei, WANG Cong, LIU Fu-tian, 2012. Hydro-Geochemistry Implications of Evolution of Pore Water in Low-Penetrability Aquifer and Significance of Paleoclimate. Earth Science, 37(3): 612-620. doi: 10.3799/dqkx.2012.070

Citation:

LI Jing, LIANG Xing, MAO Xu-mei, WANG Cong, LIU Fu-tian, 2012. Hydro-Geochemistry Implications of Evolution of Pore Water in Low-Penetrability Aquifer and Significance of Paleoclimate. Earth Science, 37(3): 612-620. doi: 10.3799/dqkx.2012.070

Citation:

LI Jing, LIANG Xing, MAO Xu-mei, WANG Cong, LIU Fu-tian, 2012. Hydro-Geochemistry Implications of Evolution of Pore Water in Low-Penetrability Aquifer and Significance of Paleoclimate. Earth Science, 37(3): 612-620. doi: 10.3799/dqkx.2012.070

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Hydro-Geochemistry Implications of Evolution of Pore Water in Low-Penetrability Aquifer and Significance of Paleoclimate

doi: 10.3799/dqkx.2012.070

1.
School of Environmental Studies, China University of Geosciences, Wuhan 430074, China
2.
State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430074, China
3.
Tianjin Center of Geological Survey, Tianjin 300170, China

Received Date: 2011-05-15
Available Online: 2021-11-09
Publish Date: 2012-05-01

Abstract

Abstract

The low-penetrability aquifer plays an important role in hydrogeology and engineering geology activities, including groundwater exploitation, porewater release from aquitard, migration and transformation of pollutants, and reposition of high radioactive waste. For understanding the low-penetrability aquifer, it's important to investigate the evolution of pore water. In this paper, pore water was extracted by mechanical squeeze in a bore of Caofeidian with a depth of 0-100 m. The analysis of porewater indicates that the pore water is alkaline, and the total dissolved solid is between 7.26 and 26.89 g/L, decreasing with depth; and Cl/Br in continental sediment tends to infinity, while that in marine sediment is 279-280. It can be concluded that the pore water is sedimentary water revealing the freshwater and seawater characteristics in continental and marine sediment respectively with no clear signs of modern seawater intrusion. The trend of Cl^-, Na⁺ is dominated by evaporation; SO₄^2- is controlled both by sulfate reduction and gypsum dissolution; cation exchange and adsorption mainly influence Ca²⁺, K⁺ and Na⁺. The reconstruction of Late Pleistocene temperature is 5.21-5.81 ℃ using δ¹⁸O, with much higher temperatures calculated by shallow data within 40 m attributed to mixing and diffusion of modern pore water.
- low-penetrability aquifer,
- pore water,
- geochemistry,
- oxygen and hydrogen isotope,
- hydrogeology

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References(60)

References

An, F.T., Gao, S.M., Li, Y.F., 1982. A research on depositional environment of delta by analyzed method of trace elements in Luanhe River. Transactions of Oceanology and Limnology, 2: 24-31 (in Chinese with English abstract). http://en.cnki.com.cn/article_en/cjfdtotal-hyfb198202004.htm

An, Z. S, Wu, X.H., Lu, Y.C., et al., 1990. A preliminary study on the paleoenvironment change of China during the last 20 000 years. In: Liu, D.S., ed., Quaternary geology and global change. Science Press, Beijing, 1-26 (in Chinese).

Bufflap, S.E., Allen, H.E., 1995. Sediment pore water collection methods for metal analysis: a review. Wat. Res., 29(1): 165-177. doi: 10.1016/0043-1354(94)E0105-F.

Chen, S.Q., Lu, Q.G., 1995. The development and application of the squeezing instrument for sampling soil water. Eco-Agriculture Research, 3(4): 67-69 (in Chinese with English abstract). http://www.jourlib.org/paper/1505793

Chen, Z.Y., 2001. Groundwater resources evolution based on paleoenvironmental information from groundwater system in the North China plain (Dissertation). Jilin University, Changchun (in Chinese).

Chen, Z.Y., Zhang, G.H., Nie, Z.L., et al., 2002. Groundwater isotopic stratification and its implications in northern China. Earth Science—Journal of China University of Geosciences, 27(1): 97-104 (in Chinese with English abstract). http://www.researchgate.net/publication/284470683_Groundwater_isotopic_stratification_and_its_implications_in_Northern_China

Cheng, S.H., Lu, H.F., 2005. Techniques for marine sediment pore-water sampling. Rock and Mineral Analysis, 24(2): 102-104 (in Chinese with English abstract). http://www.researchgate.net/publication/305375438_Techniques_for_marine_sediment_pore-water_sampling

Dansgaard, W., 1964. Stable isotopes in precipitation. Tellus, 16: 436-468.

Edwards, T.W.D., Wolfe, B.B., MacDonald, G.M., 1996. Influence of changing atmospheric circulation on precipitation delta ¹⁸O-temperature relations in Canada during the Holocene. Quaternary Research, 46(3): 211-218. doi: 10.1006/qres.1996.0061

Ha, C.Y., Wang, R.J., 1996. The information of about sea level changes inferred from groundwater. Earth Science Frontiers, 3(1-2): 177-181 (in Chinese with English abstract).

Han, Y.S., Meng, G.L., Wang, S.Q., et al., 1996. Quaternary brine along the coast of northern China. Science Press, Beijing (in Chinese).

Hendry, M.J., Wassenaar, L.I., 1999. Implications of the distribution of δD in pore waters for groundwater flow and the timing of geologic events in a thick aquitard system. Water Resources Research, 35(6): 1751-1760. doi: 10.1029/1999WR900046

Hendry, M.J., Woodbury, A.D., 2007. Clay Aquitards as archives of Holocene paleoclimate: δ¹⁸O and thermal profiling. Groundwater, 45(6): 683-691. doi: 10.1111/j.1745-6584.2007.00354_x

Hendry, M.J., Wassenaar, L.I., 2000. Controls on the distribution of major ions in pore waters of a thick surficial aquitard. Water Resources Research, 36(2): 503-513. doi: 10.1029/1999WR900310

Kelln, C.J., Wassenaar, L.I., Hendry, M.J., 2001. Stable isotopes (δ¹⁸O, δ²H) of pore water in clay-rich aquitards: a comparison and evaluation of measurement techniques. Ground Water Monitoring & Remediation, 21(2): 108-116 doi: 10.1111/j.1745-6592.2001.tb00306_x

Langmuir, D., 1997. Aqueous environmental geochemistry. Prentice-Hall, Englewood Cliffs, N.J.

Li, L., Li, C.C., 2008. Analysis on regional geological environment in Caofeidian industrial area of Tangshan. Resources and Industries, 10(1): 25-27 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-ZIYU200801009.htm

Liao, X.G., Zhang, X.J., 1984. Geochemistry of interstitial water in Bohai bay. Acta Oceanological Sinica. 5(6): 615-625 (in Chinese with English abstract).

Liu, S.M., Zhang, J., 1999. Several sampling techniques for sediment porewater. Marine Environmental Science, 18(2): 61-66 (in Chinese with English abstract).

Lopes, I., Ribeiro, R., 2005. Optimization of a pressurization methodology for extracting pore-water. Chemosphere, 61(10): 1505-1511. doi: 10.1016/j.chemosphere.2005.04.041

Ma, L., Yu, H.J., Wang, S.K., et al., 2006. Late Quaternary environmental evolution in the Bohai Sea area and formation of Quaternary subsurface brine. Coastal Engineering, 25(4): 1-6 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-HAGC200604000.htm

Oploo, P.V., White, I., Macdonald, B.C.T., et al., 2008. The use of peepers to sample pore water in acid sulphate soils. European Journal of Soil Sciences, 59(4): 762-770. doi: 10.1111/j.1365-2389.2008.01020_x

Racchetti, E., Bartoli, M., Ribaudo, C., et al., 2010. Short term changes in pore water chemistry in river sediments during the early colonization by Vallisneria spiralis. Hydrobiologia, 652(1): 127-137. doi: 10.1007/s10750-010-03246

Sacchi, E., Michelot, J.L., Pitsch, H., et al., 2001. Extraction of water and solutes from argillaceous rocks for geochemical characterisation: methods, processes, and current understanding. Hydrogeology Journal, 9(1): 17-33. doi: 10.1007/s100400000113

Shaw, J.R., Hendry, M.J., 1998. Hydrogeology of a thick clay till and Cretaceous clay sequence, Saskatchewan, Canada. Canadian Geotechnical Journal, 35(6): 1-12. doi: 10.1139/198-060

Shen, Z.L., Zhu, W.H., Zhong, Z.S., 1999. Hydrogeochemical basis (2nd edition). Geological Publishing House, Beijing (in Chinese).

Tang, M.G., Wang, H.J., 1986. The significance and application of soil pore water. Investigation Science and Technology, 5: 1-6 (in Chinese with English abstract).

Tao, C.F., 2008. Research on the characteristics of marine engineering geology and the depth of pile penetration in Caofeidian shoal (Dissertation). Ocean University of China Qingdao (in Chinese).

Waber, H.N., Smellie, J.A.T., 2008. Characterisation of pore water in crystalline rocks. Applied Geochemistry, 23(7): 1834-1861. doi: 10.1016/j.apgeochem.2008.02.007

Wang, H.C., Sun, B., Yin, G., et al., 1991. Introduction to isotope hydrogeology. Geological Publishing House, Beijing (in Chinese).

Wang, Y., 2000. Evolution sequences of palaeovegetation and palaeoclimate in the Caofeidian area since the last stage of the late Pleistocene epoch. Marine Geology and Quaternary Geology, 20(2): 87-92 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-HYDZ200002017.htm

Wang, Y.P., Lin, J.X., Fan, S.Q., et al., 1994. Chemistry of pore water in northern South China Sea and its prospecting significance. Science and Technology Press, Beijing (in Chinese).

Yan, X.X., Huo, J.L., 2007. Analysis for characteristics of physiognomy and sediment in offshore area of Hebei Caofeidian. Journal of Waterway and Harbor, 3(28): 164-168 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-SDGK200703002.htm

Yao, T.D., 1997. Climatic and environmental record in the past about 2000 years from the Guliya ice core. Quaternary Sciences, 1: 52-61 (in Chinese with English abstract). http://www.researchgate.net/publication/285839939_Climatic_and_environmental_record_in_the_past_about_2000_years_from_the_Guliya_ice_core

Zhang, W.J., Sun, X.M., Liu, F.T., et al., 2010. Application of R mode analysis on chemical characters and influential factors of Quaternary groundwater in Caofeidian area. Safety and Environmental Engineering, 17(1): 1-5 (in Chinese with English abstract). http://d.wanfangdata.com.cn/Periodical/dzktaq201001001

Zhang, Z.H., Shi, D.H., Shen, Z.L., et al., 1997. Evolution and development of groundwater environment in North China Plain under human activities. Acta Geoscientia Sinica, 18(4): 337-344 (in Chinese with English abstract).

Zhao, S.L., Yang, G.F., Cang, S.X., et al., 1978. On the marine stratigraphy and coastlines of the western coast of the gulf of Bohai. Oceanologia et Limnologia Sinica, 9(1): 15-25 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-HYFZ197801001.htm

安凤桐, 高善明, 李元芳, 1982. 用微量元素分析法研究滦河三角洲沉积环境. 海洋湖沼通报, 2: 24-31. https://www.cnki.com.cn/Article/CJFDTOTAL-HYFB198202004.htm

安芷生, 吴锡浩, 卢演俦, 等, 1990. 最近2万年中国环境变迁研究. 见: 刘东生主编, 黄土·第四纪地质·全球变化. 北京: 科学出版社, 1-26.

陈世庆, 鲁全国, 1995. 土壤水压榨取样仪的研制及其应用. 生态农业研究, 3(4): 67-69. https://www.cnki.com.cn/Article/CJFDTOTAL-ZGTN199504018.htm

陈宗宇, 2001. 从华北平原地下水系统中古环境信息研究地下水资源演化(博士学位论文). 长春: 吉林大学.

陈宗宇, 张光辉, 聂振龙, 等, 2002. 中国北方第四系地下水同位素分层及其指示意义. 地球科学——中国地质大学学报, 27(1): 97-104. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200201020.htm

程思海, 陆红锋, 2005. 海洋沉积物孔隙水的制备方法. 岩矿测试, 24(2): 102-104. doi: 10.3969/j.issn.0254-5357.2005.02.005

哈承佑, 王瑞久, 1996. 地下水中蕴藏的海平面变化信息. 地学前缘, 3(1-2): 177-181. https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY602.008.htm

韩有松, 孟广兰, 王少青, 1996. 中国北方沿海第四纪地下卤水. 北京: 科学出版社.

李琳, 李昌存, 2008. 唐山曹妃甸工业区区域地质环境分析. 资源与产业, 10(1): 25-27. doi: 10.3969/j.issn.1673-2464.2008.01.008

廖先贵, 张湘君, 1984. 渤海湾间隙水的地球化学特征. 海洋学报, 5(6): 615-625. https://www.cnki.com.cn/Article/CJFDTOTAL-SEAC198405005.htm

刘素美, 张经, 1999. 沉积物间隙水的几种制备方法. 海洋环境科学, 18(2): 61-66. https://www.cnki.com.cn/Article/CJFDTOTAL-HYHJ199902012.htm

马龙, 于洪军, 王树昆, 等, 2006. 渤海地区晚第四纪环境演化与第四纪滨海相地下卤水的形成. 海岸工程, 25(4): 1-6. doi: 10.3969/j.issn.1002-3682.2006.04.001

沈照理, 朱宛华, 钟佐燊, 1999. 水文地球化学基础(第二版). 北京: 地质出版社.

汤鸣皋, 王亨君, 1986. 岩土孔隙溶液成分研究的意义及应用探讨. 勘察科学技术, 5: 1-6. https://www.cnki.com.cn/Article/CJFDTOTAL-KCKX198605000.htm

陶常飞, 2008. 曹妃甸浅滩海洋工程地质特征及插桩深度研究(硕士学位论文). 青岛: 中国海洋大学.

汪蕴璞, 林锦璇, 范时清, 等, 1994. 南海北部海域软泥水化学及其找矿意义. 北京: 北京科学技术出版社.

王恒纯, 孙杉, 尹观, 等, 1991. 同位素水文地质概论. 北京: 地质出版社.

王艳, 2000. 渤海湾曹妃甸晚更新世末期以来古植被与古气候演变序列. 海洋地质与第四纪地质, 20(2): 87-92. https://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ200002017.htm

闫新兴, 霍吉亮, 2007. 河北曹妃甸近海区地貌与沉积特征分析. 水道港口, 3(28): 164-168. https://www.cnki.com.cn/Article/CJFDTOTAL-SDGK200703002.htm

姚檀栋, 1997. 古里雅冰芯近2000年来气候环境变化记录. 第四纪研究, 1: 52-61. doi: 10.3321/j.issn:1001-7410.1997.01.007

张伟敬, 孙晓明, 柳富田, 等, 2010. 曹妃甸地区地下水水化学特征及影响因素的R型因子分析. 安全与环境工程, 17(1): 1-5. doi: 10.3969/j.issn.1671-1556.2010.01.001

张宗祜, 施德鸿, 沈照理, 等, 1997. 人类活动影响下华北平原地下水环境的演化与发展. 地球学报, 18(4): 337-344. https://www.cnki.com.cn/Article/CJFDTOTAL-DQXB704.000.htm

赵松龄, 杨光复, 苍树溪, 等, 1978. 关于渤海湾西岸海相地层与海岸线问题. 海洋与湖沼, 9(1): 15-25. https://www.cnki.com.cn/Article/CJFDTOTAL-HYFZ197801001.htm

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Hydro-Geochemistry Implications of Evolution of Pore Water in Low-Penetrability Aquifer and Significance of Paleoclimate

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