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DYNAMICS OF HYDROGEN SUPPLY AND DEMAND FOR IN SITU DEHALORESPIRATION

机译:氢气供应动态及对原位除冰料的需求

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The diffusive release of hydrogen (H2) was evaluated as part of a multitechnology pilot program to evaluate the feasibility of various electron donors and delivery methods for reducing chlorinated hydrocarbons in groundwater at a former industrial facility in California. The evaluation was performed as part of a one-year pilot program using separate in-situ test cells designed to intercept treatment-zone groundwater. Groundwater flowing into the two test cells used for this study contained a mixture of chlorinated hydrocarbons, where trichloroethene (TCE) was the most abundant with initial average concentrations exceeding 50 milligrams per liter (mg/L). Sulfate was an important competing electron acceptor, where average pre-test concentrations were approximately 500 mg/L. Waterloo EmittersTM were installed in the test cells to deliver molecular hydrogen (H2) and sulfur hexafluoride (SF6) tracer gas to treatment zone groundwater by a passive, diffusive mechanism. Stoichiometric calculations revealed that the amount of H2 required for reducing TCE and sulfate greatly exceeded its aqueous solubility. Methods to overcome H2 solubility by increasing the H2 utilization rate included adding nutrients and implementing mechanical mixing of groundwater in both test cells. Hydrogen transfer rates were controlled by varying the partial pressure inside the emitters. In both test cells, results were similar, where a 4-fold reduction in TCE, and similar increase in cisdichloroethene (cDCE) concentration was observed over the evaluation period. Hydrogen sulfide increased and sulfate concentrations also decreased. Dissolved H2 concentrations inside both test cells remained below 60 nanomolar for most of the study, although numerical simulations and co-released SF6 tracer concentrations confirmed that the emitters were functioning as designed, and that sufficient H2 was being added to the system to explain the observed changes in TCE and sulfate concentrations. These results suggest that H2 solubility limitations were avoided because of rapid utilization by sulfatereducing and dechlorinating bacteria. More importantly, this work suggests that amendment utilization and supply rates are important considerations when designing insitu systems, and that stoichiometric considerations based on concentration data alone can be misleading when considering in-situ treatment options.
机译:氢气(H2)的扩散释放被评价为多高考试验程序的一部分,以评估各种电子供体和递送方法的可行性,并在加利福尼亚州前工业设施在地下水中还原地下水中的氯化烃的可行性。使用旨在拦截处理区地下水的单独的原位测试单元作为一年试点计划的一部分进行评估。流入用于该研究的两种测试细胞的地下水含有氯化烃的混合物,其中三氯乙烯(TCE)最丰富,初始平均浓度超过每升50毫克(Mg / L)。硫酸盐是一种重要的竞争电子受体,其中平均预测试浓度约为500mg / L. Waterloo Emitterstrs安装在测试细胞中以通过被动的扩散机制将分子氢(H 2)和六氟化硫(SF6)示踪气体输送到处理区地下水。化学计量的计算表明,降低TCE和硫酸盐所需的H 2的量大大超过其水溶性。通过增加加入营养成分的H 2利用率和在两个测试细胞中实施地下水的机械混合来克服H2溶解度。通过改变发射器内的分压来控制氢传递速率。在两个测试细胞中,结果相似,在评价期间观察到TCE的4倍和同样的三氯乙烯(CDCE)浓度的增加。硫化氢增加和硫酸盐浓度也降低。溶解的H2浓度在两个测试细胞中仍然低于60纳摩尔,用于大多数研究,尽管数值模拟和共同释放的SF6示踪剂浓度证实,发射器正在设计,并且加入足够的H2以解释观察到的TCE和硫酸盐浓度的变化。这些结果表明,由于硫酸盐和去氯化细菌快速利用,避免了H2溶解度限制。更重要的是,这项工作表明,在设计Insitu系统时,修正使用和供应率是重要的考虑因素,并且在考虑原位治疗方面时,单独基于浓度数据的化学计量考虑因素可能是误导性的。

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