Remediation of acidic groundwater by way of permeable reactive barrier

被引:12
|
作者
Indraratna, Buddhima [1 ]
Pathirage, Punyama Udeshini [1 ]
Banasiak, Laura Joan [1 ]
机构
[1] Univ Wollongong, Fac Engn & Informat Sci, Ctr Geomech & Railway Engn, Wollongong, NSW, Australia
来源
ENVIRONMENTAL GEOTECHNICS | 2017年 / 4卷 / 04期
基金
澳大利亚研究理事会;
关键词
geotechnical engineering; groundwater; mathematical modelling; ZERO-VALENT IRON; SULFATE SOIL; MINERAL PRECIPITATION; TRANSPORT; PERFORMANCE; DISSOLUTION; FLOODPLAIN;
D O I
10.1680/envgeo.14.00014
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
A permeable reactive barrier (PRB) was installed in the Shoalhaven Floodplain about 100 km south of Sydney (Australia), where acidic groundwater generation from pyritic soil poses a severe environmental and socioeconomic problem. Recycled concrete aggregates were a promising source of alkalinity-generating material and adopted as the reactive media for this PRB. The current study simulates the performance of the PRB through coupling geochemical reactions involved with recycled concrete and acidic groundwater with geohydraulics (transient groundwater flows). This is the first such attempt made for time-dependent modelling and performance verification of a PRB located in acid sulfate soil (ASS) terrain. The developed model describes the chemical clogging due to mineral precipitates and the associated reductions in porosity and hydraulic conductivity of the reactive medium. The governing equations of the model were incorporated into commercial software, MODFLOW and RT3D. The field results are in favourable agreement with the model predictions, confirming that the reduction in hydraulic conductivity due to mineral precipitation occurs predominantly at the entrance zone of the PRB and insignificantly in the middle and exit zones after 7 years of operation. Mineralogical analysis undertaken on sample specimens from the PRB also confirms that clogging is minimal at the entrance zone.
引用
收藏
页码:284 / 298
页数:15
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