Department of Biology, University of Southern Denmark, Syddanmark 5230, Denmark.
Freshwater Biological Laboratory, Department of Biology, University of Copenhagen, Copenhagen 2100, Denmark.
J Environ Sci (China). 2022 Aug;118:76-86. doi: 10.1016/j.jes.2021.08.027. Epub 2022 Jan 11.
Throughout the freshwater continuum, Dissolved Organic Carbon (DOC) and the colored fraction, Chromophoric Dissolved Organic Material (CDOM), are continuously being added, removed, and transformed, resulting in changes in the chromophoricity and lability of organic matter over time. We examined, experimentally, the effect of increasing irradiation-intensities on the combined photochemical and microbial degradation of CDOM and DOC. This was done by using a simulated mixed water column: aged water from a humic lake was exposed to four irradiation-intensities - representing winter, early and late spring, and summer conditions (0.10, 0.16, 0.36, and 0.58 W/m) - and compared with dark controls over 37 days. We found a linear relationship between CDOM degradation and irradiation-intensities up to 0.36 W/m; the degradation rate saturated at higher intensities, both at specific wavelengths and for broader intervals. After 37 days at high irradiation-intensity, CDOM absorption of irradiation at 340 nm had been reduced by 41%; 48% of DOC had been removed and DOC degradation continued to increase. Aromaticity (SUVA) declined significantly over 37 days at the two lowest but not at the two highest UV- intensities; levels in unexposed control water remained constant. Direct observations of the humic lake showed that CDOM absorption of irradiation (340 nm) declined by 27% from winter to summer. A model based on hydrological CDOM input and CDOM degradation calculated from field measurements of UV-radiation and experimental CDOM degradation with UV-exposure from sunlight accurately predicted the annual course as observed in the lake. With no external CDOM input, 92% of the CDOM could be degraded in a year. The results support the notion that combined photochemical and microbial CDOM degradation can be remarkably higher in lakes than previously thought and that humic lakes retain their color due to light absorption by ongoing CDOM input.
在淡水连续体中,溶解有机碳 (DOC) 和有色部分,发色溶解有机物质 (CDOM),不断被添加、去除和转化,导致有机物质的发色性和不稳定性随时间发生变化。我们通过模拟混合水柱实验研究了增加辐照强度对 CDOM 和 DOC 联合光化学和微生物降解的影响。老化的腐殖质湖水中的水暴露在四个辐照强度下(代表冬季、早春、晚春和夏季条件(0.10、0.16、0.36 和 0.58 W/m)),并与黑暗对照进行了 37 天的比较。我们发现 CDOM 降解与辐照强度之间存在线性关系,直到 0.36 W/m;降解率在更高的强度下饱和,无论是在特定波长还是在更宽的间隔内。在高辐照强度下 37 天后,CDOM 在 340nm 处的辐照吸收率降低了 41%;48%的 DOC 已被去除,DOC 降解仍在继续增加。芳香度(SUVA)在 37 天内两个较低的 UV 强度下显著下降,但在两个较高的 UV 强度下没有下降;未暴露的对照水中的水平保持不变。对腐殖质湖的直接观察表明,CDOM 在 340nm 处的辐照吸收率从冬季到夏季下降了 27%。基于水文 CDOM 输入和基于野外测量的 UV 辐射和实验 CDOM 降解的 CDOM 降解模型,利用阳光中的 UV 暴露准确预测了湖中观察到的年度过程。在没有外部 CDOM 输入的情况下,一年内可降解 92%的 CDOM。结果支持了这样一种观点,即与先前认为的相比,湖泊中联合光化学和微生物 CDOM 降解的速度可能显著提高,并且腐殖质湖由于持续的 CDOM 输入而保持其颜色。