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美国加利福尼亚州内华达山脉帕利塞德冰川积雪层中 4-壬基酚光解转化为 4-壬基儿茶酚。

The photolytic conversion of 4-nonylphenol to 4-nonylcatechol within snowpack of the Palisade Glacier, Sierra Nevada, CA, USA.

机构信息

University of Redlands, 1200 E Colton Ave., Redlands, CA 92373, United States of America.

University of Redlands, 1200 E Colton Ave., Redlands, CA 92373, United States of America.

出版信息

Sci Total Environ. 2023 Jun 10;876:162835. doi: 10.1016/j.scitotenv.2023.162835. Epub 2023 Mar 15.

Abstract

4-Nonylphenol (4-NP), an environmental pollutant with potent ecotoxicological effects, has been discovered in significant quantities in glacial ice and snow of the Sierra Nevada Mountain Range, CA. Photolysis of 4-NP is suspected to be a major, if not the sole, breakdown pathway in snow. However, the photolysis process has yet to be characterized in detail for this unique environment. This study therefore seeks to (1) confirm the presence of the major photolysis product within snowpack and snowmelt samples from the Palisade Glacier, CA, (2) determine key photolysis parameters through laboratory assays in snow analogs, and (3) compute environmentally relevant photolysis rates in snowpack via a spectral solar irradiance model parameterized for the Palisade Glacier. The primary photooxidation product of 4-NP, 4-nonylcatechol (4-NC), was synthesized and characterized by NMR and GC-MS for use as a reference standard in the detection of 4-NC in environmental samples. 4-NP was detected in all snowpack (n = 4) and snowmelt (n = 5) samples, with concentrations of 1.05 (± 0.11) μg L and 1.28 (± 0.12) μg L, respectively. 4-NC was detected in all snowmelt outflow samples and all but one snow samples (88 % detection frequency) but was below the limit of quantification for the given method. All samples were collected during a sampling regime at the Palisade Glacier in August of 2021. Quantum yields of photolysis at the 277 nm absorption band were determined to be 0.36 (±0.06) and 0.21 (±0.06) in ultrapure water and liquid snow, respectively. Under clear sky conditions at the Palisade Glacier, half-lives for 4-NP are estimated to range from 235 to 251 h (9.8-10.5 days) based on assays conducted in liquid snowmelt and irradiance modeling. These results suggest that the photolysis of 4-NP, and hence the production of 4-NC, is occurring at significant rates within the snowpack where 4-NC is inevitably released to downstream catchment areas via snowmelt. 4-NC is significantly more toxic than its precursor, thereby raising amplified concerns for downstream human and wildlife populations. Furthermore, the ubiquity of 4-NP among the Earth's environments presents this as an issue of potentially global concern.

摘要

4-壬基酚(4-NP)是一种具有强烈生态毒理学效应的环境污染物,已在加利福尼亚内华达山脉的冰川冰和雪中大量发现。光解被怀疑是雪中主要的(如果不是唯一的)分解途径。然而,这个独特环境中的光解过程尚未得到详细描述。因此,本研究旨在:(1)确认加利福尼亚州帕利塞德冰川的雪堆和融雪中存在主要光解产物,(2)通过实验室模拟在雪样中确定关键光解参数,以及(3)通过为帕利塞德冰川参数化的光谱太阳辐照度模型来计算雪堆中的环境相关光解速率。4-NP 的主要光氧化产物 4-壬基儿茶酚(4-NC)通过 NMR 和 GC-MS 进行了合成和表征,用作环境样品中 4-NC 检测的参考标准。在所有雪堆(n=4)和融雪(n=5)样本中都检测到了 4-NP,浓度分别为 1.05(±0.11)μg/L 和 1.28(±0.12)μg/L。在所有融雪流出样本和除一个雪样本外的所有样本中都检测到了 4-NC(88%的检测频率),但低于该方法的定量下限。所有样本均于 2021 年 8 月在帕利塞德冰川的采样制度下收集。在 277nm 吸收带处的光解量子产率分别确定为超纯水和液态雪中的 0.36(±0.06)和 0.21(±0.06)。根据在液态融雪中进行的测定和辐照度建模,在内华达山脉帕利塞德冰川的晴朗天空条件下,4-NP 的半衰期估计范围为 235 至 251 小时(9.8-10.5 天)。这些结果表明,4-NP 的光解,因此 4-NC 的生成,在雪堆中以很高的速率发生,在雪堆中,4-NC 不可避免地通过融雪释放到下游集水区。4-NC 的毒性比其前体显著更高,从而对下游人类和野生动物种群产生了放大的担忧。此外,4-NP 在地球环境中的普遍存在使其成为一个潜在的全球性问题。

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