Kinetics of methanethiol oxidation by oxygen under aqueous conditions

IF 4.5 1区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS
Irina Zweig, Alexey Kamyshny Jr.
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Abstract

Methanethiol is one of the most abundant volatile organic sulfur compounds in natural aquatic systems and one of the main products of dimethylsulfoniopropionate decomposition. This study focuses on the kinetic parameters of the reaction of methanethiol and its deprotonated form, methanethiolate, with dissolved oxygen in aqueous solutions at various reactant concentrations, pH, and temperatures. The reaction proceeds through two distinct pathways: a slow reaction between protonated methanethiol and oxygen under acidic to neutral conditions, and a fast reaction between methanethiolate and oxygen under basic conditions. At the environmentally relevant pH and concentrations, the reaction order with respect to methanethiol is 2.2 ± 0.4 for the protonated form and 1.6 ± 0.2 for the deprotonated form, while in both cases it is 1.0 ± 0.3 with respect to oxygen. Dimethyl disulfide was the only product detected in both reaction pathways. The ratio between the consumption rates of oxygen and methanethiolate was approximately 1:4, while the ratio of oxygen to methanethiol consumption rates was close to 1:2. This implies that dimethyl disulfide is not the only product of methanethiol oxidation. The half-life of methanethiol in oxic water column at 25 °C and typical marine methanethiol concentrations of 0.02–2 nM was estimated to be 80 to 1200 years. Rates of chemical oxidation of MT in the surface waters are lower than the rates of its photooxidation and degassing. Thus, the contribution of the chemical oxidation of MT in marine systems to its budget is negligible but should be considered for the MT-rich aphotic hydrothermal and limnic waters. In systems with methanethiol concentrations exceeding 1 mM, such as bioreactors, chemical oxidation rather than microbial decomposition is likely the primary mechanism for methanethiol removal, even at low oxygen levels. Under fully oxic conditions, the rate of chemical oxidation of methanethiol is expected to surpass the rate of microbial degradation observed under anoxic conditions typically utilized in these reactors.
水条件下甲硫醇被氧氧化的动力学
甲硫醇是天然水生系统中含量最丰富的挥发性有机硫化合物之一,是二甲基磺酰丙酸分解的主要产物之一。本研究的重点是甲硫醇及其去质子化形式甲硫醇与溶解氧在不同反应物浓度、pH和温度下的反应动力学参数。反应通过两种不同的途径进行:在酸性到中性条件下质子化的甲硫醇和氧之间的缓慢反应,以及在碱性条件下甲硫醇和氧之间的快速反应。在与环境相关的pH和浓度下,甲基硫醇的质子化反应级数为2.2 ± 0.4,去质子化反应级数为1.6 ± 0.2,而两种情况下对氧的反应级数均为1.0 ± 0.3。二甲基二硫是两种反应途径中唯一检测到的产物。氧与甲硫醇的消耗率之比约为1:4,而氧与甲硫醇的消耗率之比接近1:2。这意味着二甲二硫不是甲硫醇氧化的唯一产物。在25 °C和典型海洋甲烷硫醇浓度为0.02-2 nM的氧化水柱中,甲烷硫醇的半衰期估计为80 ~ 1200 年。地表水中MT的化学氧化速率低于其光氧化和脱气速率。因此,海洋系统中MT的化学氧化对其预算的贡献可以忽略不计,但对于富含MT的光热液和石灰水应予以考虑。在甲硫醇浓度超过1 mM的系统中,如生物反应器,即使在低氧水平下,化学氧化而不是微生物分解可能是甲硫醇去除的主要机制。在全氧条件下,甲硫醇的化学氧化速率预计将超过在这些反应器中通常使用的缺氧条件下观察到的微生物降解速率。
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来源期刊
Geochimica et Cosmochimica Acta
Geochimica et Cosmochimica Acta 地学-地球化学与地球物理
CiteScore
9.60
自引率
14.00%
发文量
437
审稿时长
6 months
期刊介绍: Geochimica et Cosmochimica Acta publishes research papers in a wide range of subjects in terrestrial geochemistry, meteoritics, and planetary geochemistry. The scope of the journal includes: 1). Physical chemistry of gases, aqueous solutions, glasses, and crystalline solids 2). Igneous and metamorphic petrology 3). Chemical processes in the atmosphere, hydrosphere, biosphere, and lithosphere of the Earth 4). Organic geochemistry 5). Isotope geochemistry 6). Meteoritics and meteorite impacts 7). Lunar science; and 8). Planetary geochemistry.
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