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Diffusion of explosives through frozen and unfrozen sand

机译:炸药通过冷冻和未冷冻的沙子扩散

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Areas subject to military conflict or military training sometimes contain unexploded ordinance and/or explosives residues resulting from detonations. A variety of past field and modeling studies have investigated the behavior of explosives in soils in warm climates, but the behavior in cold climates, including frozen soil and snow, has been less studied. In northern areas of military conflict, and at Army military training grounds in cold regions, winter weather exists for many months of the year. The impact of temperature and moisture changes in the soil, due to changing weather conditions, can have a large effect on the fate and transport of the explosives. The basic transport parameters for the behavior of the contaminant in frozen soil are unknown, yet these parameters are needed for problem assessment both for simple estimates and full numerical studies. In this paper we discuss sample results of controlled laboratory experiments performed to investigate the diffusion of 2,4-DNT through sand, under two conditions each of temperature and moisture. Based on the experimental data we present preliminary effective diffusion coefficients for the conditions. The concentrations show clear transport of the contaminant due to vapor diffusion and sorption. Sorption is a controlling feature of diffusion of explosives in sand. Diffusion rates and concentration on the particles increase with temperature. In both frozen and unfrozen sand, higher moisture content causes faster diffusion rates but lower particle concentration levels than in the corresponding dry cases.
机译:遭受军事冲突或军事训练的区域有时会包含爆炸引起的未爆炸条例和/或爆炸物残留。过去的各种领域和模型研究都对温暖气候下土壤中炸药的行为进行了研究,但对寒冷气候下(包括冻土和积雪)的行为进行了较少的研究。在军事冲突的北部地区以及寒冷地区的陆军军事训练场,一年中的许多月份都存在冬季天气。由于天气条件的变化,土壤中温度和水分变化的影响可能对炸药的命运和运输产生重大影响。冻土中污染物行为的基本运输参数尚不清楚,但是对于简单的估计和完整的数值研究,问题评估都需要这些参数。在本文中,我们讨论了在温度和湿度两个条件下进行的受控实验室实验的样本结果,这些实验用于研究2,4-DNT在沙子中的扩散。根据实验数据,我们给出了这些条件的初步有效扩散系数。由于蒸汽的扩散和吸附,浓度显示出污染物的清晰运输。吸附是炸药在沙子中扩散的控制特征。扩散速率和颗粒上的浓度随温度而增加。在冷冻和未冷冻的沙子中,与相应的干燥情况相比,较高的水分含量导致更快的扩散速度,但颗粒浓度较低。

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