地表水中硝酸盐和亚硝酸盐作为*OH源相对作用的季节和水柱变化趋势

Davide Vione, Claudio Minero, Valter Maurino, Ezio Pelizzetti
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引用次数: 13

摘要

基于阳光光谱、光解量子产率和吸收光谱的文献数据,评价了亚硝酸根和硝酸盐作为*OH源在地表水中的相对作用,并研究了亚硝酸根和硝酸盐作为*OH源对季节和水柱深度的依赖性。在大多数地表水样本(河流、湖泊和海水)中,尽管亚硝酸盐的[NO2-]值通常较低,但与硝酸盐相比,亚硝酸盐作为*OH源的作用预计更重要。有趣的是,在硝酸盐和亚硝酸盐浓度比例恒定的假设下(稍后根据给定样品中的实际浓度比例进行修正),亚硝酸盐与硝酸盐相比的相对作用在夏季中午在自然水体的表层中最小。在自然环境中可以经历的任何阳光强度的降低(不同于夏季的季节、水柱吸收、一天中不同于正午的时间),以及它对阳光光谱的相关影响,将增加亚硝酸盐相对于硝酸盐的作用。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Seasonal and Water Column Trends of the Relative Role of Nitrate and Nitrite as *OH Sources in Surface Waters

Based on literature data of sunlight spectrum, photolysis quantum yields, and absorption spectra, the relative role of nitrite and nitrate as *OH sources in surface waters was assessed, and its dependence on the season and the depth of the water column studied. In the majority of surface water samples (river, lake and seawater) nitrite is expected to play a more important role as *OH source compared to nitrate, in spite of the usually lower [NO2-] values. Interestingly, under the hypothesis of a constant ratio of the concentrations of nitrate and nitrite (to be corrected later on for the actual concentration ratio in a given sample), the relative role of nitrite compared to nitrate would be minimum in summer, at noon, in the surface layer of natural waters. Any decrease in the sunlight intensity that can be experienced in the natural environment (different season than summer, water column absorption, time of the day other than the solar noon), with its associated influence on the sunlight spectrum, would increase the relative role of nitrite compared to nitrate.

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