Dissolution and sorption of hexahydro-1,3,5-trinitro-1,3,5-triazine (RDX) and 2,4,6-trinitrotoluene (TNT) residues from detonated mineral surfaces

被引:13
|
作者
Jaramillo, Ashley M. [1 ,2 ]
Douglas, Thomas A. [1 ]
Walsh, Marianne E. [3 ]
Trainor, Thomas P. [2 ]
机构
[1] Cold Reg Res & Engn Lab, Ft Wainwright, AK 99703 USA
[2] Univ Alaska Fairbanks, Dept Chem & Biochem, Fairbanks, AK 99775 USA
[3] USA, Cold Reg Res & Engn Lab, Hanover, NH 03755 USA
关键词
Dissolution; Sorption; Explosive residue; TNT; RDX; NITROAROMATIC EXPLOSIVES; COMPOSITION-B; SOIL; SOLUBILITY; TRANSPORT; WATER; OCTAHYDRO-1,3,5,7-TETRANITRO-1,3,5,7-TETRAZOCINE; METABOLITES; NITRAMINE; SEDIMENTS;
D O I
10.1016/j.chemosphere.2011.04.066
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Composition B (Comp B) is a commonly used military formulation composed of the toxic explosive compounds 2,4,6-trinitrotoluene (TNT), and hexahydro-1,3,5-trinitro-1,3,5-triazine (RDX). Numerous studies of the temporal fate of explosive compounds in soils, surface water and laboratory batch reactors have been conducted. However, most of these investigations relied on the application of explosive compounds to the media via aqueous addition and thus these studies do not provide information on the real world loading of explosive residues during detonation events. To address this we investigated the dissolution and sorption of TNT and RDX from Comp B residues loaded to pure mineral phases through controlled detonation. Mineral phases included nontronite, vermiculite, biotite and Ottawa sand (quartz with minor calcite). High Performance Liquid Chromatography and Attenuated Total Reflectance Fourier Transform Infrared spectroscopy were used to investigate the dissolution and sorption of TNT and RDX residues loaded onto the mineral surfaces. Detonation resulted in heterogeneous loading of TNT and RDX onto the mineral surfaces. Explosive compound residues dissolved rapidly (within 9 h) in all samples but maximum concentrations for TNT and RDX were not consistent over time due to precipitation from solution, sorption onto mineral surfaces, and/or chemical reactions between explosive compounds and mineral surfaces. We provide a conceptual model of the physical and chemical processes governing the fate of explosive compound residues in soil minerals controlled by sorption-desorption processes. Published by Elsevier Ltd.
引用
收藏
页码:1058 / 1065
页数:8
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