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Characteristics and sources of chromophoric dissolved organic matter in lakes of the Yungui Plateau, China, differing in trophic state and altitude

机译:不同营养状态和海拔的中国云贵高原湖泊发色溶解性有机物的特征和来源

摘要

The high-mountain lakes on the Yungui Plateau in China are exposed to high-intensity ultraviolet radiation, and contain low concentrations of chromophoric dissolved organic matter (CDOM). We determined CDOM absorption, fluorescence, composition, and source in 38 lakes on the Yungui Plateau at altitudes of 1516 to 4591 m above sea level. Total nitrogen (TN), total phosphorus (TP), and chlorophyll a (Chl a) concentrations significantly increased with increasing trophic state, and decreased with altitude. The CDOMabsorption coefficient aCDOM(280) significantly increased with increasing trophic state, but not with altitude. There were significant and negative correlations between altitude and TN, TP, Chl a concentrations, and aCDOM(280). Parallel factor analysis identified two humic-like and two protein-like fluorescent components. Humic-like component 1 was terrestrially derived and positively correlated to CDOM absorption. Component 2 was similar to a marine humic-like substance originating from biological degradation of phytoplankton. Components 3 and 4 were autochthonous tryptophanlike and tyrosine-like fluorophores.CDOMwas, thus, a mixture of material from the catchment and autochthonous material produced by biota in the lake. CDOM fluorescence characteristics of oligotrophic and mesotrophic lakes were dominated by the spectral signatures of protein-like components, but marine and terrestrial humic-like components dominated in eutrophic lakes. The fluorescence indices FI255, FI310, and FI370 were useful tools for readily defining and classifying CDOM characteristics in the Yungui Plateau lake waters.
机译:中国云贵高原的高山湖泊暴露于高强度紫外线辐射,并且含有低浓度的发色溶解有机物(CDOM)。我们确定了云贵高原海拔1516至4591 m的38个湖泊中CDOM的吸收,荧光,组成和来源。总氮(TN),总磷(TP)和叶绿素a(Chl a)的浓度随着营养状态的增加而显着增加,而随着海拔的升高而降低。 CDOM吸收系数aCDOM(280)随营养状态的增加而显着增加,但不随高度的增加而增加。海拔高度与TN,TP,Chla浓度和aCDOM之间存在显着和负相关(280)。平行因素分析确定了两个腐殖质样和两个蛋白质样荧光成分。腐殖质样成分1来源于地面,与CDOM吸收呈正相关。成分2与浮游植物的生物降解产生的海洋腐殖质类似。组分3和4是土生色氨酸和酪氨酸样荧光团.CDOM是流域的物质和湖中生物群产生的土生物质的混合物。贫营养湖和中营养湖的CDOM荧光特征主要由蛋白质样成分的光谱特征决定,而富营养化湖泊中海洋和陆地腐殖质样成分占主导。荧光指数FI255,FI310和FI370是用于在云归高原湖水中轻松定义和分类CDOM特征的有用工具。

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