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首页> 外文期刊>International Journal of Mineral Processing >In situ bioremediation of soils contaminated with radioactive elements and toxic heavy metals
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In situ bioremediation of soils contaminated with radioactive elements and toxic heavy metals

机译:对被放射性元素和有毒重金属污染的土壤进行原位生物修复

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摘要

Two experimental plots of an agricultural and contaminated with radioactive elements (uranium, radium thorium) and toxic heavy metals (copper, zinc, cadmium) were treated by two different biotechnological in situ methods. The soil in this land was characterized by a negative net neutralization potential, and the soil pH was in a slightly acidic pH range (from 4 to 5). The contaminants were located mainly in the upper soil layers (mainly in the horizon A).Both methods were connected with the initial solubilization of the contaminants. Water acidified with sulphuric acid was used as a leach solution. The solubilization was mainly a result of the activity of the indigenous soil microflora. This activity was enhanced by suitable changes in the levels of some essential environmental factors, such as water, oxygen and nutrient content of the soil. The first method was then connected with the removal of the dissolved contaminants from the soil through the soil effluents. The second method was based on the transfer of the contaminants into the deeply located soil horizon B_2, where they were immobilized mainly as a result of the activity of the indigenous sulphate-reducing bacteria. Their activity was enhanced by injecting water solutions of organic compounds into the horizon B_2 through boreholes located in the relevant experimental plot.
机译:用两种不同的生物技术原位方法处理了两个农业用地和放射性元素(铀,镭th)和有毒重金属(铜,锌,镉)污染的试验区。该土地上的土壤的特征在于净中和电位为负,土壤的pH值处于弱酸性pH范围(4至5)。污染物主要位于上层土壤层(主要位于地平线A),这两种方法都与污染物的初始溶解有关。用硫酸酸化的水用作浸出溶液。增溶作用主要是土著土壤微生物群落活动的结果。通过适当改变一些基本环境因素(例如土壤中的水,氧气和养分含量)的水平,可以增强这项活动。然后,第一种方法与通过土壤流出物从土壤中去除溶解的污染物有关。第二种方法是基于将污染物转移到位置较深的土壤层B_2中的,这些污染物在土壤层中被固定化的主要原因是本地还原硫酸盐的细菌的活性。通过将有机化合物的水溶液通过位于相关实验区的钻孔注入到地平线B_2中,可以增强其活性。

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