FAN Wei1, YANG Yuesuo1,2, LU Ying1, DU Xinqiang1, ZHANG Jiashuang1, SONG Xiaoming1" /> 层间地下水污染曝气修复的影响带

CIESC Journal

• 能源和环境工程 • 上一篇    下一篇

层间地下水污染曝气修复的影响带

范伟1,杨悦锁1,2,路莹1,杜新强1,张加双1,宋晓明1   

  1. 1吉林大学环境与资源学院,吉林 长春130026;2英国卡迪夫大学地球与海洋科学学院,卡迪夫 CF10 3YE
  • 出版日期:2011-09-05 发布日期:2011-09-05

Zone of influence of air sparging in interlayer groundwater system

FAN Wei1, YANG Yuesuo1,2, LU Ying1, DU Xinqiang1, ZHANG Jiashuang1, SONG Xiaoming1   

  • Online:2011-09-05 Published:2011-09-05

摘要:

影响带是开展曝气修复机理研究和工程设计的重要基础,不同场地条件下影响带的型态与形成机制不同。以我国东北地区典型层间地下水污染场地为例,在阐明污染水文地质特征的基础上,开展曝气修复的运行、监测与分析,利用地下水水位、溶解氧、温度等参数的动态变化来反映曝气修复对地下环境的影响,并以之指示曝气影响带的空间分布。进而通过对影响带地下水动态特征的分析,阐明曝气驱替过程中的水流运动过程,量化分析该层间水曝气模式下的水流运动规律。结果表明,在该曝气模式下,影响半径可达9 m,影响区呈倒圆锥状,其中赋存地下水362.04 m3,受曝气驱替作用,影响带内地下水以一定流量向四周流散,该流量随时间递减,连续运行6 h累积流散量为0.97 m3,表明该曝气修复模式下地下水的侧向流散并不显著。

Abstract:

As a cost-efficient enhanced technique, air sparging is used to address subsurface contamination worldwide.It involves the injection of contaminant-free air into the saturated aquifer in an attempt to enhance aerobic biodegradation and induce mass transfer of volatile contaminants into vapor phase.The zone of influence(ZOI)of air sparging(AS)is a critical parameter for the mechanism studies and project designs, which varies with site characterizations.A case study in northeast China featured by a typical interlayer groundwater system contaminated by hydrocarbons was conducted.Air sparging with soil vapor extraction for remediation was performed based on site characterizations.Groundwater level, temperature and dissolved oxygen in groundwater were monitored in field scale during the air sparging running.The spatial and temporal responses of air sparging to the above parameters were analyzed to reflect the environmental effects of remediation activities, and indicate the ZOI.Mathematical methods, including the least square method and double integral were used to determine the theoretical boundary and volume of the ZOI.In addition, a mathematic model was set up to quantify the water inter-flow in the ZOI on the basis of the understanding of groundwater displacement by sparged air.The results showed that the radius of influence in this case was up to 9 m, and the ZOI presented an inverted cone with 362.04 m3 groundwater in it before AS.Groundwater was up-lifted to the top of the aquifer and then overflowed to the surrounding area, while the flux rate descended with time and the cumulative flux reached 0.97 m3 in 6 h.It could be safely concluded that the lateral groundwater movement was not significant in this case.The knowledge from the comprehensive study could provide useful insight into the design efficiency of in situ air sparging and assist in developing and controlling the sparging system, and even tell the fate and transport of the water-air interaction.