State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430074, PR China.
State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430074, PR China.
Chemosphere. 2017 Jun;176:288-295. doi: 10.1016/j.chemosphere.2017.02.109. Epub 2017 Feb 24.
Although the kinetics and transformation of methyl parathion have been investigated extensively, its abiotic degradation mechanism in anoxic sulfur-containing groundwater system is still not clear. In this work, the abiotic degradation of methyl parathion in anoxic sulfur-containing system mediated by natural organic matter (NOM) was investigated in batch experiments. It was found that the removal of methyl parathion (up to 80.7%) was greatly improved in sulfide containing NOM compared to those in sulfide alone (with 15.5%) and in NOM alone (almost negligible). Various sulfur species presented significant differences in behaviors methyl parathion degradation, but followed by the pseudo-first-order model well. No facilitated degradation of methyl parathion was observed in sulfite (SO) or thiosulfate (SO) containing NOM such as anthraquinone. Although elemental sulfur (S) and cysteine could further improve the degradation rate of methyl parahtion, their impacts was very limited. The removal efficiency of methyl parathion in anoxic sulfur-containing system were related remarkably with NOM concentration and solution pH. Based on the transformation products identified by gas chromatography-mass spectrometer (GC/MS) and liquid chromatography high resolution mass spectrometer (LC/HRMS), both the nitro group reduction and hydrolysis (S@C) processes by sulfide (HS) were further proved to be two predominant reaction mechanisms for the abiotic degradation of methyl parathion in anoxic sulfur-containing system. The results of this study help to understand the natural attenuation of methyl parathion under anoxic sulfide-containing groundwater system mediated by NOM.
尽管已经对甲基对硫磷的动力学和转化进行了广泛研究,但在缺氧含硫地下水系统中其非生物降解机制仍不清楚。在这项工作中,通过批处理实验研究了自然有机物 (NOM) 介导的缺氧含硫系统中甲基对硫磷的非生物降解。结果发现,与单独含硫(去除率为 15.5%)和单独含 NOM(几乎可以忽略不计)相比,含 NOM 的硫化物中甲基对硫磷(高达 80.7%)的去除得到了极大改善。各种硫物种在降解甲基对硫磷的行为上存在显著差异,但都很好地遵循了准一级动力学模型。在含亚硫酸盐 (SO) 或硫代硫酸盐 (SO) 的 NOM(如蒽醌)中未观察到甲基对硫磷的促进降解。尽管元素硫 (S) 和半胱氨酸可以进一步提高甲基对硫磷的降解速率,但它们的影响非常有限。缺氧含硫系统中甲基对硫磷的去除效率与 NOM 浓度和溶液 pH 值密切相关。根据气相色谱-质谱联用仪 (GC/MS) 和液相色谱高分辨质谱仪 (LC/HRMS) 鉴定的转化产物,硫化物 (HS) 的硝基还原和水解 (S@C) 过程均进一步证明是缺氧含硫系统中非生物降解甲基对硫磷的两种主要反应机制。这项研究的结果有助于理解在缺氧含硫化物地下水系统中 NOM 介导的甲基对硫磷的自然衰减。