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    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
    shu

    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
    • 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; SO42- 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.

       

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    • 致谢: 本研究受到国家重点基础研究发展计划“973”项目基金及国家自然科学青年基金项目“深层地下水惰性气体法同时定量恢复气温和降雨量研究”基金资助；试验原状土样由天津地质调查中心提供；水样的检测由中国地质大学(武汉)生物地质与环境地质重点实验室完成，岩土矿物的检测由中国地质大学(武汉)地质过程与矿产资源国家重点实验完成.在此对上述提供资助和帮助的单位表示衷心的感谢.
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