地学前缘 ›› 2024, Vol. 31 ›› Issue (3): 432-442.DOI: 10.13745/j.esf.sf.2023.3.1

• 地质环境与地质工程 • 上一篇    下一篇

有机污染场地原位修复过程的地球物理动态监测与分析

夏腾1(), 张家铭2, 李书鹏2, 郭丽莉2, 王祺2, 毛德强1,*()   

  1. 1.山东大学 土建与水利学院, 山东 济南 250061
    2.北京建工环境修复股份有限公司, 北京 100015
  • 收稿日期:2022-12-03 修回日期:2023-02-11 出版日期:2024-05-25 发布日期:2024-05-25
  • 通信作者: *毛德强(1981—),男,博士,教授,博士生导师,研究方向为地下水科学与工程、水文地球物理、地下水污染物探监测及反演模型研究。E-mail: maodeqiang@sdu.edu.cn
  • 作者简介:夏腾(1993—),男,博士,岩土工程专业,研究方向为水文地球物理、地下污染介质精细刻画与动态监测研究。E-mail: Tengxiasdu@163.com
  • 基金资助:
    国家重点研发计划“场地土壤污染成因与治理技术”重点专项(2019YFC1804900);国家自然科学基金项目(42177056)

Geophysical dynamic monitoring and analysis of in-situ remediation process at organic contaminated sites

XIA Teng1(), ZHANG Jiaming2, LI Shupeng2, GUO Lili2, WANG Qi2, MAO Deqiang1,*()   

  1. 1. School of Civil Engineering, Shandong University, Jinan 250061, China
    2. Beijing Construction Engineering Environmental Remediation Co., Ltd., Beijing 100015, China
  • Received:2022-12-03 Revised:2023-02-11 Online:2024-05-25 Published:2024-05-25

摘要:

有机污染场地原位修复过程的动态监测是评估修复进程和效果的重要环节,监测方法的选择直接影响修复效率及费用。本研究利用高密度电阻率法,结合常规监测井数据,全面刻画了原位热强化氧化耦合修复过程。结果显示,场地内电阻率与水化学、地下水位、污染物含量和温度数据相互验证,实现了点面信息结合。研究发现,在原位热修复过程中,场地内地层电阻率会随温度升高而降低。基于温度与电阻率的经验关系,本文提出了污染物含量变化对电阻率的影响系数,得出影响系数随污染物含量的不断减小而增加。本研究还推算出原位热修复过程中温度及污染物含量的分布,即浓度随温度的不断升高而降低。针对原位氧化修复过程,电阻率变化有效刻画了原位氧化修复中过硫酸钠及水的动态注入过程。研究充分体现了地球物理方法在原位修复监测中的优势,可为有机污染场地原位修复过程精准、高效及低成本的动态监测提供重要参考。

关键词: 地球物理, 有机污染场地, 原位热修复, 原位化学氧化, 动态监测

Abstract:

Real-time monitoring of in-situ remediation processes is crucial for evaluating the progress and effectiveness of addressing organic contamination at sites. Electrical resistivity tomography, in conjunction with sampling analysis, is utilized to monitor in-situ thermal oxidation remediation procedures. The findings demonstrate that changes in resistivity align with variations in hydrochemistry, groundwater levels, contaminant concentrations, and temperature. Specifically, resistivity decreases as temperature rises during in-situ thermal remediation. By establishing an empirical link between temperature and resistivity, an influence coefficient of concentration on resistivity is proposed, with the coefficient increasing as contamination concentration decreases. Furthermore, the distributions of temperature and contaminant concentrations during the heating phase are inferred, showing a decrease in concentration with increasing temperature. Additionally, variations in resistivity effectively map out the dynamic injection process of persulfate and water during in-situ chemical oxidation remediation. In summary, geophysical methods offer an effective means to dynamically monitor in-situ remediation processes at organic contaminated sites.

Key words: geophysics, organic contaminated site, in-situ thermal desorption, in-situ chemical oxidation, dynamic monitoring

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