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某石油污染含水层降解能力地球化学评估
引用本文:宁卓,郭彩娟,蔡萍萍,张敏,陈宗宇,何泽. 某石油污染含水层降解能力地球化学评估[J]. 中国环境科学, 2018, 38(11): 4068-4074
作者姓名:宁卓  郭彩娟  蔡萍萍  张敏  陈宗宇  何泽
作者单位:1. 中国地质科学院水文地质环境地质研究所, 河北 石家庄 050061;2. 中国地质大学(北京)中国地质科学院, 北京 100083;3. 河北省地下水污染机理与修复重点实验室, 河北 石家庄 050061;4. 合肥工业大学资源与环境工程学院, 安徽 合肥 230009
基金项目:国家自然科学基金资助项目(41602261);中国地质科学院基本科研业务费专项经费资助(SK201702,SK201604,SK201614);河北省自然科学基金资助项目(D2016504021)
摘    要:含水层降解能力是石油类污染场地监控自然衰减需获取的重要参数.通过测定某石油污染场地地下水电子供体(苯系物、化学耗氧量)和电子受体/产物(DO、NO3-、Mn2+、Fe2+、SO42-和HCO3-)等地球化学指标,分析了电子供受体分布规律,确定了电子受体背景值,采用传统地球化学评估法,计算了所有单井降解能力;在此基础上,引入累积概率曲线法,更科学的评估了场地含水层降解能力,结合地下水更新能力,估算了污染物降解速率;同时,划分了含水层降解能力强弱区.结果显示:该场地单井降解能力为36.49~70.05mg/L,其累积概率拟合曲线符合F(x)=0.008e0.07x指数模型,以此评估含水层降解能力为57.83mg/L.以径流量132m3/d估算地下水更新能力,估算污染物降解速率为2790kg/a;强降解能力区位于下游源区,面积约为5100m2,占场地总面积的5.3%;地下水中硫酸盐、硝酸盐消耗严重,强化硫酸盐还原和反硝化作用可能是该场地管理修复的一个有效方法.

关 键 词:石油污染  降解能力  电子受体  累积概率曲线法  地球化学评估  
收稿时间:2018-04-18

Geochemical evaluation of biodegradation capacity in a petroleum contaminated aquifer
NING Zhuo,GUO Cai-juan,CAI Ping-ping,ZHANG Ming,CHEN Zong-yu,HE Ze. Geochemical evaluation of biodegradation capacity in a petroleum contaminated aquifer[J]. China Environmental Science, 2018, 38(11): 4068-4074
Authors:NING Zhuo  GUO Cai-juan  CAI Ping-ping  ZHANG Ming  CHEN Zong-yu  HE Ze
Affiliation:1. Institute of Hydrogeology and Environmental Geology, Chinese Academy of Geological Sciences, Shijiazhuang 050061, China;2. Chinese Academy of Geological Sciences, China University of Geosciences in Beijing, Beijing 100083, China;3. Key Laboratory of Groundwater Remediation of Hebei Province, Shijiazhuang 050061, China;4. School of Resources and Enviromental Engineering, HeFei University of Technology, Hefei 230009, China
Abstract:It is essential to determine the biodegradation capacity when monitoring or enhancing natural attenuation of petroleum in contaminated aquifers. Here, the concentrations of typical electron donorcontaminants (benzene, toluene, ethylbenzene, and xylene, and chemical oxygen demand) and electron acceptors and byproducts (dissolved oxygen, NO3-, Mn2+, Fe2+, SO42- and HCO3-) in a petroleum-contaminated aquifer were determined. The background electron acceptor/byproduct concentrations were determined from the electron donor concentrations, and the acceptor/byproduct distributions were characterized. The biodegradation capacity at each well was estimated using a general geochemical evaluation method. The cumulative probability curve method was used withthe general method to evaluate the biodegradation capacities in the aquifer. The biodegradation rates were determined from the biodegradation capacities and groundwater renewal rates, and different biodegradation zones were identified from the biodegradation rates. The biodegradation capacities of the wells were 36.49~70.05mg/L, and the biodegradation capacity cumulative probability curve for each well fitted the exponential equation F(x)=0.008e0.07x. The whole-aquifer biodegradation capacity (determined using the probabilities for the different aquifer parts) was 57.83mg/L and the whole-aquifer biodegradation rate (calculated defining the groundwater renewal rate as the groundwater runoff rate, 132m3/d) was 2790kg/a. The downstream source zone was found to have a strong biodegradation capacity. It was concluded that petroleumcontaminants were mainly degraded by the electron acceptors SO42- and NO3- reduction. Enhancing SO42- and NO3- reduction may be a promising way of managing and remediating the study site.
Keywords:petroleum contamination  biodegradation capacity  electron acceptors  cumulative probability curve method  geochemical evaluation  
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