Removal of ammonium-nitrogen from groundwater using a fully passive permeable reactive barrier with oxygen-releasing compound and clinoptilolite

被引:40
作者
Huang, Guoxin [1 ,2 ]
Liu, Fei [1 ]
Yang, Yingzhao [3 ]
Deng, Wei [4 ]
Li, Shengpin [1 ]
Huang, Yuanying [5 ]
Kong, Xiangke [6 ]
机构
[1] China Univ Geosci, Beijing Key Lab Water Resources & Environm Engn, Beijing 100083, Peoples R China
[2] Beijing Acad Food Sci, China Meat Res Ctr, Beijing 100068, Peoples R China
[3] Hydroengn Team Sichuan Met Geol & Explorat Bur, Chengdu 611730, Peoples R China
[4] Beijing Univ Technol, Coll Environm & Energy Engn, Beijing 100124, Peoples R China
[5] Natl Res Ctr Geoanal, Beijing 100037, Peoples R China
[6] CAGS, Inst Hydrogeol & Environm Geol, Shijiazhuang 050061, Peoples R China
基金
中国博士后科学基金;
关键词
Ammonium-nitrogen; Groundwater; In situ remediation; Permeable reactive barrier; Oxygen-releasing compound; Clinoptilolite; LABORATORY COLUMN EVALUATION; NATURAL AUSTRALIAN ZEOLITE; CONTAMINATED GROUNDWATER; AQUEOUS-SOLUTION; POLYMER MATS; REMEDIATION; NITRIFICATION; COMMUNITY; KINETICS; BIOFILM;
D O I
10.1016/j.jenvman.2015.02.012
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
A novel fully passive permeable reactive barrier (PRB) with oxygen-releasing compound (ORC) and clinoptilolite was proposed for the removal of ammonium-nitrogen from groundwater. The PRB involves a combination of oxygen release, biological nitrification, ion exchange, and bioregeneration. A pilot-scale performance comparison experiment was carried out employing three parallel columns to assess the proposed PRB. The results showed that the PRB achieved nearly complete NH4+ - N depletion (>99%). NH4+ - N of 5.23-10.88 mg/L was removed, and NO2- - N of <1.93 mg/L and NO3- - N of 2.03 -19.67 mg/L were generated. Ion exchange and biological nitrification both contributed to NH4+ - N removal, and the latter played a dominant role under the condition of sufficient oxygen. Biological nitrification favored a delay in sorption saturation and a release of exchange sites. The ORC could sufficiently, efficiently supply oxygen for approximately 120 pore volumes. The clinoptilolite ensured a robust NH4+ - N removal in case of temporary insufficient biological activities. No external alkalinity sources had to be supplied and no inhibition of aerobic metabolism occurred. The ceramicite had a negligible effect on the biomass growth. Based on the research findings, a full-scale continuous wall PRB was installed in Shenyang, China in 2012. (C) 2015 Elsevier Ltd. All rights reserved.
引用
收藏
页码:1 / 7
页数:7
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