重金属土壤修复:摩擦擦洗对湿式重力浓缩过程的影响

M. A. Marino, R. M. Brica, C. Neale
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引用次数: 37

摘要

美国军方历来进行的活动直接或间接地造成了环境污染。军事基地的金属污染土壤是由武器生产、小型武器训练活动、金属清洗和金属电镀等活动造成的。洗土是一种利用物理分离和化学分离技术处理污染土壤的有效方法。物理分离方法包括许多不同的单元操作,包括筛分、磨矿、浮选、加氢分级、摩擦洗涤和重力浓缩,如台式和螺旋。本文的主要焦点将是解决摩擦擦洗(高固体环境中磨蚀性土壤颗粒与土壤颗粒相互作用)对重力浓缩过程的影响。来自陆军轻武器训练靶场的土壤,散装土壤中铅污染约为40,000 mg/kg,使用WEMCO®实验室磨损洗涤器与Wilfley®实验室湿摇台一起进行评估。结果表明,摩擦擦洗通过将铅污染物从土体中释放出来,增强了湿式振动台上的物理分离过程,在产生小体积铅富集土的同时获得了大体积的洁净土。实验室测试表明,超过96%的污染可以集中在20%的原始土壤质量上。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Heavy metal soil remediation: The effects of attrition scrubbing on a wet gravity concentration process
The US military has historically conducted activities which have either directly or indirectly contributed to environmental contamination. Metal contaminated soil at military sites has resulted from operations such as weapons production, small arms training activities, metal cleaning, and metal plating activities. Soil washing is an effective approach to the treatment of contaminated soils employing both physical and chemical separation techniques. Physical separation methods encompass many different unit operations including screening, grinding, flotation, hydroclassification, attrition scrubbing and gravity concentration such as tabling and spiraling. The primary focus of this paper will be to address the effects of attrition scrubbing (an abrasive soil particle to soil particle interaction in a high solids environment), on a gravity concentration process. Soil from an Army small arms training range with lead contamination in the bulk soil at approximately 40,000 mg/kg, was evaluated using a WEMCO® Laboratory Attrition Scrubber in conjunction with a Wilfley® Laboratory Wet Shaking Table. Results indicate attrition scrubbing enhanced the physical separation process on the wet shaker table by liberating the Pb contamination from the bulk soil, which resulted in a large volume of clean soil while simultaneously producing a small volume of Pb concentrated soil. Laboratory tests indicate over 96% of the contamination could be concentrated on 20% of the original soil mass.
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