滕彦国, 左锐, 王金生, 林学钰. 区域地下水演化的地球化学研究进展[J]. 水科学进展, 2010, 21(1): 127-136.
引用本文: 滕彦国, 左锐, 王金生, 林学钰. 区域地下水演化的地球化学研究进展[J]. 水科学进展, 2010, 21(1): 127-136.
TENG Yan-guo, ZUO Rui, WANG Jin-sheng, LIN Xue-yu. Progress in geochemistry of regional groundwater evolution[J]. Advances in Water Science, 2010, 21(1): 127-136.
Citation: TENG Yan-guo, ZUO Rui, WANG Jin-sheng, LIN Xue-yu. Progress in geochemistry of regional groundwater evolution[J]. Advances in Water Science, 2010, 21(1): 127-136.

区域地下水演化的地球化学研究进展

Progress in geochemistry of regional groundwater evolution

  • 摘要: 由于区域地质特征、水文地质条件、气候影响和人类活动的差异性,导致区域地下水演化的地球化学过程复杂、影响因素众多.在总结近年来国内外区域地下水化学演化研究大量成果的基础上,综述了地下水演化的地球化学系统分析方法,地下水演化研究的水文地球化学方法、同位素地球化学和元素地球化学方法和技术以及地下水演化的地球化学模拟方法和技术及常用软件.指出在今后的一段时期内,区域地下水自然演化与人类活动的复合作用、地下水与地表水的相互作用、微生物-水-岩相互作用将是区域地下水地球化学研究的热点领域,其中物理、化学、生物的耦合作用将是区域地下水演化的地球化学研究的重点领域.

     

    Abstract: Due to the differences in the regional geological and the hydrogeological conditions and the impacts of human activities and climate changes,the process of regional groundwater geochemistry evolution is complex,and controlled by lots of factors.On the basis of the summary of the current major research achievements,this paper gives some reviews about:(1) the principles and methods of analyzing geochemistry system of groundwater;(2) the hydrogeological,isotopic,element analysis methods and applied techniques in the study of groundwater evolution;(3) the geochemical models and the well-known software of simulating groundwater evolution.And in the future,the complex action of natural evolution and human activity,the interaction of groundwater and surface water,the interaction of microbe-water-rock are the hotspots and developing tendencies.In which,the coupling of the physical,chemical and biological actions would be the significant filed in the regional groundwater evolution.

     

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