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Fluorescence: Absorption coefficient ratio — Tracing photochemical and microbial degradation processes affecting coloured dissolved organic matter in a coastal system

机译:荧光:吸收系数比-跟踪影响沿海系统中有色溶解有机物的光化学和微生物降解过程

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摘要

The optical properties of coloured dissolved organic matter (CDOM) – absorption coefficient, induced fluorescence, and fluorescence quantum yield – were determined in the coastal eutrophic system of the Ría de Vigo (NW Spain) under two contrasting situations: a downwelling event in September 2006 and an upwelling event in June 2007. Significantly different optical properties were recorded in the shelf surface (higher absorption coefficient and lower quantum yield) and bottom (lower absorption coefficient and higher quantum yield) waters that entered the embayment during downwelling and upwelling conditions, respectively. Continental waters presented distinctly high CDOM levels. The spatial and temporal variability of the induced fluorescence to absorption coefficient ratio during the mixing of shelf and continental waters was used to quantify the relative importance of photochemical and microbial processes under these contrasting hydrographic conditions. Photochemical processes were dominant during the downwelling episode: 86% of the variability of CDOM can be explained by photochemical degradation. On the contrary, microbial processes prevailed during the upwelling event: 77% of the total variability of CDOM was explained by microbial respiration.
机译:在两个相反的情况下,测定了维加(西班牙西北部)沿海富营养化系统中有色溶解有机物(CDOM)的光学特性(吸收系数,诱导的荧光和荧光量子产率):2006年9月的一次下沉事件以及2007年6月发生的上升流事件。分别在下降流和上升流条件下进入排架的架子表面(较高的吸收系数和较低的量子产率)和底部(较低的吸收系数和较高的量子产率)水记录了明显不同的光学特性。 。大陆水域的CDOM含量明显较高。在陆架水和大陆水混合的过程中,诱导的荧光与吸收系数之比的时空变化被用来量化在这些相反的水文条件下光化学和微生物过程的相对重要性。光化学过程在下降过程中占主导地位:CDOM变异的86%可以通过光化学降解来解释。相反,在上升事件中微生物过程占主导地位:CDOM总变异性的77%由微生物呼吸作用解释。

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