多种稳定同位素(C, N, Cl)对除草剂阿特拉津和异丙草胺光降解的见解。

Chemosphere Pub Date : 2025-02-01 Epub Date: 2024-12-24 DOI:10.1016/j.chemosphere.2024.144010
Matias Levesque-Vargas, Leanne Ohlund, Lekha Sleno, Yves Gélinas, Patrick Höhener, Violaine Ponsin
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引用次数: 0

摘要

许多过程可有助于减少地表水中经常检测到的有毒除草剂阿特拉津和异丙甲草胺,包括光降解。多元素化合物特异性同位素分析有可能破译这些不同的降解途径,因为Cl是一种很有前途的途径识别工具,也是阿特拉津和异丙草胺降解的敏感指标。本研究分别在缓冲溶液(直接光降解)和硝酸盐溶液(OH自由基间接光降解)下进行了模拟阳光下阿特拉津和异丙甲草胺的光降解实验,测定了动力学、转化产物和C、N的同位素分异,并首次测定了Cl。对于异甲草胺,C-Cl双同位素斜率(ΛC/Cl = 0.46±0.19)与之前报道的土壤中水解和生物降解的值相同,表明相同的反应机制(SN2亲核取代破坏C-Cl键)。对于阿特拉嗪,直接和间接光降解均导致氯的同位素反作用(εCl = 6.9±3.3‰,εCl = 2.3±1.2‰),导致特征双同位素斜率(ΛC/Cl = -0.49±0.17,ΛC/Cl = -0.31±0.10)。这些值不同于之前报道的地表水中相关的非生物水解、生物水解和氧化脱烷基过程,为未来的实地研究开辟了途径识别的道路。
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Insights from multiple stable isotopes (C, N, Cl) into the photodegradation of herbicides atrazine and metolachlor.

Many processes can contribute to the attenuation of the frequently detected and toxic herbicides atrazine and metolachlor in surface water, including photodegradation. Multi-element compound-specific isotope analysis has the potential to decipher between these different degradation pathways as Cl is a promising tool for both pathway identification and a sensitive indicator of degradation for both atrazine and metolachlor. In this study, photodegradation experiments of atrazine and metolachlor were conducted under simulated sunlight in buffered solutions (direct photodegradation) and with nitrate (indirect photodegradation by OH radicals) to determine kinetics, transformation products and isotope fractionation for C, N and for the first time Cl. For metolachlor, the C-Cl dual isotope slope (ΛC/Cl = 0.46 ± 0.19) is identical to previously reported values for hydrolysis and biodegradation in soils, suggesting the same reaction mechanism (C-Cl bond breakage by SN2 nucleophilic substitution). For atrazine, both direct and indirect photodegradation resulted in a pronounced inverse isotope effect for chlorine (εCl = 6.9 ± 3.3 ‰, and εCl = 2.3 ± 1.2 ‰, respectively), leading to characteristic dual isotope slopes (ΛC/Cl = -0.49 ± 0.17 and ΛC/Cl = -0.31 ± 0.10, respectively). These values are distinct from those previously reported for abiotic hydrolysis, biotic hydrolysis and oxidative dealkylation which are all relevant processes in surface water, opening the path for pathway identification in future field studies.

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