首页> 外文会议>American Society For Engineering Education Annual Conference and Exposition >USING EITHER HYDROGEN OR DITHIONITE AS REDUCTANT IN URANIUM CONTAMINATED GROUNDWATER AT POSTLEACH URANIUM MINING SITES, SOUTH TEXAS
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USING EITHER HYDROGEN OR DITHIONITE AS REDUCTANT IN URANIUM CONTAMINATED GROUNDWATER AT POSTLEACH URANIUM MINING SITES, SOUTH TEXAS

机译:在南德克萨斯州的后冻结地区铀污染地下水中使用氢气或二硫代硫酸盐作为还原剂。

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This paper summarizes the results of a summer research project conducted by a public high school teacher. The project focused on the impacts of in situ recovery (ISR) uranium mining on groundwater quality in South Texas. Uranium is a major groundwater constituent at ISR mining sites and there is need for more effective post-mining restoration strategies. One promising approach is to add reductants to reduce soluble U(VI) species to insoluble U(IV) species that are permanently immobilized within the aquifer formation. In this research a hydrogeochemical computer program from USGS (PHREEQC) was used to simulate how two different reductants, hydrogen gas (H_2) and sodium dithionite (Na_2S_2O_4), induce reduction of U(VI) to U(IV) and groundwater and associated changes in the hydrogeochemistry. The modeling simulation performed with H_2 as the reductant showed that significant reduction of uranium, iron and sulfate was achieved, resulting in very strong reducing conditions. In contrast, the modeling simulation with sodium dithionite as the reductant showed reduction of uranium and iron only. These results have significant implications with respect to the potential effectiveness of H_2 and dithionite as chemical reductants for restoring groundwater quality at uranium ISR mining sites. In particular, while addition of H_2 should achieve stronger reducing conditions near the injection point, the addition of dithionite will likely have a larger zone of influence because it will not be consumed via sulfate reduction reactions. A learning module based on the legacy cycle concept was developed that challenges the students to think through the processes and steps to determine the level of contamination and the amount of restoration required to return groundwater to safe levels. This learning module will be introduced into high school mathematics and science classes during spring semester 2011-2012 school year. A subsequent assessment of the students' performance will be carried out and reported.
机译:本文总结了公立高中教师进行了暑期研究项目的结果。该项目侧重于在原位恢复(ISR)铀矿开采对南得克萨斯地下水水质的影响。铀是在ISR采矿点的主要地下水成分,也需要更有效的采矿后恢复策略。一个有希望的方法是添加还原剂以降低可溶性U(VI)物质的不溶性U(IV),其永久地固定在含水层地层内的物种。在本研究中使用从美国地质调查局一个水文计算机程序(PHREEQC)来模拟两个不同的还原剂,氢气(H_2)和连二亚硫酸钠(Na_2S_2O_4)如何,诱导还原U(Ⅵ)的对U(Ⅳ)和地下水和相关的变化在水文。建模仿真与H_2作为还原剂显示达到了铀,铁和硫酸的那显著减少,导致非常强的还原条件下进行。相比之下,建模仿真与连二亚硫酸钠作为还原剂还原表现出铀和仅铁。这些结果相对于H_2的潜在效益和连二亚硫酸钠作为在铀ISR采矿点恢复地下水水质化学还原剂显著影响。特别是,虽然除了H_2的应达到注射点附近强还原条件下,在加入连二亚硫酸盐将可能具有的影响力较大的区域,因为它不会通过硫酸盐还原反应被消耗掉。基于传统周期概念的学习模块的开发,挑战学生通过流程和步骤,以确定污染和恢复量的水平认为地下水恢复到安全水平所需。该学习模块将春季学期2011-2012学年期间被引入到高中的数学和科学课。学生成绩的后续评估将进行并报告。

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