| 北京平原区永定河冲洪积扇地下水水化学特征与演化规律 |
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| 引用本文： | 郇环,王金生,翟远征,郑洁琼.北京平原区永定河冲洪积扇地下水水化学特征与演化规律[J].地球学报,2011,32(3):357-366. |
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| 作者姓名： | 郇环 王金生 翟远征 郑洁琼 |
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| 作者单位： | 北京师范大学水科学研究院; 地下水污染控制与修复教育部工程研究中心;北京师范大学水科学研究院; 地下水污染控制与修复教育部工程研究中心;北京师范大学水科学研究院; 地下水污染控制与修复教育部工程研究中心;北京师范大学水科学研究院; 地下水污染控制与修复教育部工程研究中心 |
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| 基金项目： | 北京市重大科技项目(编号: D07050601510000) |
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| 摘 要： | 本文以北京市平原区永定河冲洪积扇地下水化学场的演化机理及地下水水循环规律为研究目的,根据水化学特征的水平分布及典型剖面上的演化过程研究,得到以下结论:1)从永定河冲洪积扇顶部补给区到扇缘排泄区,地下水水化学类型呈现水平分带性,潜水水化学类型由Ca-HCO3过渡到Ca·Mg-HCO3、Mg·Na-SO4,局部因人类活动影...
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| 关 键 词： | 永定河冲洪积扇 地下水水化学类型分带 水-岩相互作用 |
Chemical Characteristics and Evolution of Groundwater in the Yongding River Alluvial Fan of Beijing Plain |
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| HUAN Huan,WANG Jin-sheng,ZHAI Yuan-zheng and ZHENG Jie-qiong.Chemical Characteristics and Evolution of Groundwater in the Yongding River Alluvial Fan of Beijing Plain[J].Acta Geoscientia Sinica,2011,32(3):357-366. |
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| Authors: | HUAN Huan WANG Jin-sheng ZHAI Yuan-zheng and ZHENG Jie-qiong |
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| Institution: | College of Water Sciences, Beijing Normal University; Engineering Research Center for Groundwater Pollution Control and Remediation, Ministry of Education;College of Water Sciences, Beijing Normal University; Engineering Research Center for Groundwater Pollution Control and Remediation, Ministry of Education;College of Water Sciences, Beijing Normal University; Engineering Research Center for Groundwater Pollution Control and Remediation, Ministry of Education;College of Water Sciences, Beijing Normal University; Engineering Research Center for Groundwater Pollution Control and Remediation, Ministry of Education |
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| Abstract: | This study intends to find out the evolutionary mechanism of groundwater geochemical field and groundwater cycle in the Yongding River alluvial fan of Beijing.Based on the horizontal distribution of geochemical characteristics and groundwater evolutionary process in typical profiles,the authors have reached the following conclusions:1) From the recharge area to the discharge area of Yongding River alluvial fan,different zones of groundwater chemical types can be recognized.The chemical type of phreatic groundwater changes from Ca-HCO3 to Ca·Mg-HCO3 and Mg·Na-SO4 while the type of deep groundwater changes from Ca·Mg·Na-HCO3 and Ca·Na-HCO3 to Na-HCO3 and Na-HCO3·SO4.Groundwater with chemical types of Ca·Na-HCO3·SO4,Na·Ca-Cl or Ca·Mg-SO4 in the recharge area have been affected by human activities.In general,the distribution of groundwater chemical zones is consistent with that of groundwater flow zones,especially in the unconfined and moderate-deep confined aquifer.2) The groundwater chemical field in different depths is affected by water-rock interaction,which includes the dissolution/deposition of sulfate,silicate,carbonate and halite and the cation exchange of Ca-Na and Ca-Mg.3) From the recharge areas to the downstream discharge areas of the Yongding River alluvial fan,the groundwater velocity decreases gradually while the amount of dissolution/deposition for silicate,carbonate,sulfate and halite grows gradually.Therefore,the renewable velocity of groundwater decreases. |
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| Keywords: | Yongding River alluvial fan zones of groundwater chemical types water-rock interaction |
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