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季铵盐类化合物在河水中的光化学行为。

Photochemical fate of quaternary ammonium compounds in river water.

机构信息

Department of Civil, Environmental, and Geo- Engineering, University of Minnesota - Twin Cities, 500 Pillsbury Drive SE, Minneapolis, Minnesota 55455, USA.

出版信息

Environ Sci Process Impacts. 2020 Jun 24;22(6):1368-1381. doi: 10.1039/d0em00086h.

Abstract

Quaternary ammonium compounds (QACs) are not completely removed during wastewater treatment and are frequently detected in surface waters and sediments. The photochemical transformation of QACs has not been thoroughly investigated as a potential degradation pathway affecting their fate in the environment. Kinetic studies of common QACs with and without aromatic groups under simulated and natural sunlight conditions were performed with model sensitizers and dissolved organic matter to estimate photochemical half-lives in the aquatic environment. All QACs investigated react with hydroxyl radicals at diffusion-controlled rates (∼2.9 × 109 to 1.2 × 1010 M-1 s-1). Benzethonium reacted via direct photolysis (ΦBZT,outdoor = 1.7 × 10-2 (mol Ei-1)). Benzethonium also reacted with the triplet excited state model sensitizer 2-acetylnaphthalene, but evidence suggests this reaction pathway is unimportant in natural waters due to faster quenching of the triplet 2-acetylnapthalene by oxygen. Reactivity with singlet oxygen for the QACs was minimal. Overall, reactions with hydroxyl radicals will dominate over direct photolysis due to limited spectral overlap of sunlight emission and QAC absorbance. Photolysis half-lives are predicted to be 12 to 94 days, indicating slow abiotic degradation in surface water.

摘要

季铵化合物(QACs)在废水处理过程中不能被完全去除,经常在地表水和沉积物中被检测到。作为影响其在环境中归宿的潜在降解途径,QACs 的光化学转化尚未得到充分研究。在模拟和自然阳光条件下,使用模型敏化剂和溶解有机物对具有和不具有芳环基团的常见 QACs 进行了动力学研究,以估计在水生环境中的光化学半衰期。所有研究的 QACs 均以扩散控制速率(∼2.9×109 至 1.2×1010 M-1 s-1)与羟基自由基反应。苯扎氯铵通过直接光解(ΦBZT,outdoor = 1.7×10-2(mol Ei-1))反应。苯扎氯铵还与三重态激发态模型敏化剂 2-乙酰萘反应,但有证据表明,由于氧气对 2-乙酰萘三重态的快速猝灭,该反应途径在天然水中并不重要。QAC 与单线态氧的反应性最小。总的来说,由于阳光发射和 QAC 吸收的光谱重叠有限,与羟基自由基的反应将主导直接光解。光解半衰期预计为 12 至 94 天,表明地表水的非生物降解速度较慢。

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