Fate and transport of 2,4,6-trinitrotoluene in loams at a former explosives factory

被引:16
|
作者
Robertson, Timothy James
Martel, Richard [1 ]
Quan, Doan Minh
Ampleman, Guy
Thiboutot, Sonia
Jenkins, Thomas
Provatas, Arthur
机构
[1] Univ Quebec, INRS, ETE, Quebec City, PQ, Canada
[2] Univ Melbourne, Sch Earth Sci, Parkville, Vic 3052, Australia
[3] Civil Aviat Adm Vietnam, Air Navigat Dept, Hanoi, Vietnam
[4] DRDC Valcartier, Dept Def, Val Belair, PQ, Canada
[5] Ctr Res Dev & Engn, Cold Reg Res & Engn Lab, Hanover, NH USA
[6] DSTO, Dept Def, Weapons Syst Div, Edinburgh, SA, Australia
来源
SOIL & SEDIMENT CONTAMINATION | 2007年 / 16卷 / 02期
关键词
TNT; adsorption; biodegradation; explosives; loam; ATRANS20; TNT; TRANSFORMATION; ADSORPTION; HEXAHYDRO-1,3,5-TRINITRO-1,3,5-TRIAZINE; MUTAGENICITY; METABOLITES; REDUCTION; TOXICITY; MODEL; IRON;
D O I
10.1080/15320380601166462
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Natural attenuation processes affecting 2,4,6-trinitrotoluene (TNT) were determined within loams for two study areas at the former Explosives Factory Maribyrnong, Australia. TNT fate and transport was investigated through spectrophotometric/High Performance Liquid Chromatography (HPLC) analyses of soil and groundwater, adsorption and microcosm testwork. A five tonne crystalline TNT source zone delineated within near surface soils at the base of a TNT process waste lagoon was found to be supplying aqueous TNT loading (7 ppm) to subsurface soils and groundwater. The resultant plume was localized within the loam aquitard due to a combination of natural attenuation processes and hydrogeological constraints, including low hydraulic conductivity and upward hydraulic gradients. Freundlich described sorptive partitioning was the main TNT sink (K-F = 29 mL/g), while transformation rates were model-ate (1.01 x 10(-4) h(-1)) under the aerobic conditions. Increasing 2-amino-4,6-dinitrotoluene predominance over 4-amino-2.6-dinitrotoluene was discovered with depth (in situ) and time (microcosms). Simplified dissolution rate calculations indicate that without mitigation of the TNT source, contaminant persistence within the vadose zone may approach 2000 years, while ATRANS20 simulations demonstrate that the TNT plume propagates very slowly along the flow path within the aquitard.
引用
收藏
页码:159 / 179
页数:21
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