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来源和形成过程影响夏季长江流域雨水溶解有机物的化学多样性。

Source and formation process impact the chemodiversity of rainwater dissolved organic matter along the Yangtze River Basin in summer.

机构信息

Institute of Surface-Earth System Science, School of Earth System Science, Tianjin University, Tianjin 300072, China.

School of Urban and Environmental Sciences, Key Laboratory of the Ministry of Education for Earth Surface Processes, Peking University, Beijing 100871, China.

出版信息

Water Res. 2022 Mar 1;211:118024. doi: 10.1016/j.watres.2021.118024. Epub 2021 Dec 30.

Abstract

Rainwater dissolved organic matter (DOM) plays an important role in the biogeochemical cycle and evolution of organic matter in the land-atmosphere interface. To better understand their sources and molecular composition in the atmosphere, rainwater samples were collected at six different locations along the Yangtze River Basin. Based on the application of a combined approach including excitation-emission matrix (EEM) fluorescence and Fourier transform ion cyclotron resonance mass spectrometry (FT-ICR MS), various sources (terrestrial, anthropogenic, and autochthonous sources) of rainwater DOM were revealed. Results show that the derivatives of biogenic volatile organic compounds were widely distributed and contributed to rainwater DOM along the Yangtze River Basin. In the up-river city Batang, rainwater DOM was affected by the long-range atmospheric transport due to the Indian summer monsoon. Lijiang, a city on the southeastern edge of Tibetan plateau, was related to strong local biomass burning. The industrial cities of Panzhihua and Luzhou showed large differences in organic composition due to distinct industrial types. Fuling, a district in Chongqing Municipality, was significantly contributed by aged organics from biomass burning. While rainwater DOM in Shanghai, a coastal megacity, contained a high fraction of sea spray organics. Further, more than 70% of rainwater DOM molecules are associated with 36 typical transformation mechanisms during rainwater-scavenging processes, e.g., oxidation reactions, dealkylation and decarboxylation. Our study demonstrates that local natural and anthropogenic emissions and climatic conditions strongly shaped the chemodiversity and possible precursor-product pairs of rainwater DOM along the Yangtze River Basin, which helps to better understand the biogeochemical cycles of organic matter in a large-scale watershed under the influence of human activities.

摘要

雨水溶解的有机物 (DOM) 在陆地-大气界面的生物地球化学循环和有机物演化中起着重要作用。为了更好地了解它们在大气中的来源和分子组成,在长江流域的六个不同地点采集了雨水样本。基于包括激发-发射矩阵 (EEM) 荧光和傅里叶变换离子回旋共振质谱 (FT-ICR MS) 在内的综合方法的应用,揭示了雨水 DOM 的各种来源(陆地、人为和自生来源)。结果表明,生物挥发性有机化合物的衍生物广泛分布,并为长江流域的雨水 DOM 做出了贡献。在上游城市巴塘,由于印度夏季风的影响,雨水 DOM 受到远距离大气传输的影响。位于青藏高原东南边缘的丽江与强烈的当地生物质燃烧有关。工业城市攀枝花和泸州由于不同的工业类型,其有机组成差异较大。重庆市涪陵区主要受生物质燃烧产生的老化有机物的影响。而沿海特大城市上海的雨水 DOM 含有大量的海雾有机物。此外,超过 70%的雨水 DOM 分子与雨水收集过程中的 36 种典型转化机制有关,例如氧化反应、脱烷基化和脱羧反应。我们的研究表明,当地的自然和人为排放以及气候条件强烈影响了长江流域雨水 DOM 的化学多样性和可能的前体-产物对,这有助于更好地了解在人类活动影响下的大规模流域中有机物的生物地球化学循环。

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