钒污染土壤地下水的修复技术研究进展  

Research Progress on Remediation Technology of Vanadium Contaminated Soil and Groundwater

作　　者：谷倩 刘欢[1] 张宝刚[1] 梁帅 Gu Qian;Liu Huan;Zhang Baogang;Liang Shuai(Key Laboratory of Ministry of Education of Groundwater Circulation and Environmental Evolution,School of Water Resources and Environment,China University of Geosciences,Beijing 100083,China)

机构地区：[1]中国地质大学水资源与环境学院地下水循环与环境演化教育部重点实验室,北京100083

出　　处：《地球科学》2018年第A01期84-96,共13页Earth Science

基　　金：国家自然科学基金项目(No.41672237);北京市"科技新星计划"项目(No.Z171100001117082)

摘　　要：钒是典型的氧化还原敏感元素,其在地壳中储量丰富,又是现代工业中性能优异的催化剂.由于地质风化作用及密集的开采、冶炼、应用等人类活动,导致土壤地下水钒污染日益严重,引起研究者的广泛关注.从物理法、化学法和生物法3个方面,综述了土壤地下水钒污染修复技术的最新研究进展.物理法主要包括改土法和电解法,化学法主要包括化学淋洗、化学吸附及化学还原固定,生物法主要包括植物修复和微生物修复.同时展望了钒污染土壤地下水修复技术的发展趋势,为后续研究提供参考.Vanadium is a typical redox-sensitive element that is abundant in the crust and is a superior catalyst in modern industry. Due to the geological weathering and intensive human activities such as mining, smelting and applications, vanadium pollution in soil and groundwater is becoming more and more serious, arousing widespread concern of researchers. This article reviews the latest research progress of remediation of vanadium contamination in soil and groundwater from three aspects： physical methods, chemical methods and biological methods. Physical methods include soil replacement and electrolysis. Chemical methods include chemical leaching, chemical adsorption and chemical reduction immobilization. Biological methods include phytoremediation and microbial remediation. Meanwhile, the trend of the development in remediation technology of vanadium contaminated soil and groundwater is also forecasted, which will provide reference for subsequent researches.

关 键 词：钒 修复 土壤 地下水 环境地质 

分 类 号：P641.7[天文地球—地质矿产勘探]