珠江口虎门淡水端溶解有机碳变化的机制——基于三端元混合模型的结果

The mechanism of the variation of DOC concentration in the freshwater end-member in Humen outlet of Pearl River Estuary-based on a three-component model analysis

  • 摘要: 采用高温燃烧法测定了夏季珠江口的溶解有机碳(dissolved organic carbon,DOC)浓度,结果表明,DOC浓度在夏季珠江口虎门上游不同来源的淡水水体间存在较大差异,广州段水体DOC浓度高达479 μmol/L,在广州-虎门约70 km干流中DOC浓度呈快速降低趋势。东江三条支流在广州-虎门汇入干流中,东江各支流平均DOC浓度约为227 μmol/L,东江DOC浓度相对较低水体的汇入稀释了干流中的DOC,再加上DOC的去除效应,至虎门时干流中DOC浓度只有139 μmol/L,即干流中DOC下降的浓度为340 μmol/L。建立三端元混合模型定量讨论去除效应和稀释效应各自的贡献,结果表明去除效应和稀释效应的贡献分别为228 μmol/L(占比约67%)和112 μmol/L(占比约33%),DOC浓度在珠江广州-虎门快速下降主要由去除效应造成,但东江对干流的稀释效应也不可忽略。

     

    Abstract: Dissolved organic carbon (DOC) concentrationin the Pearl River Estuary in summer was observed by high temperature combustion method, the result showed that a great difference of the DOC concentration among the different sources freshwater bodies in the upper reaches of Humen outlet.While the highest DOC (479 μmol/L) was observed in Guangzhou section, it decreased drastically in a 70 km voyage from Guangzhou to Humen outlet.Three tributaries of the Dongjiang River flow into the main stream, bringing an average 227 μmol/L DOC concentration freshwater, the remittance of the relatively low DOC in Dongjiang River and the removal effect of DOC reduced the DOC in the main stream, DOC was only 139 μmol/L in Humen outlet, i.e., the concentration of DOC decreased totally 340 μmol/L in the main stream from Guangzhou to Humen outlet.A three-component model was used to discuss the respective contribution of removal and dilution effects, the running results showed that the removal and dilution effects were 228 μmol/L (accounting for 67%) and 112 μmol/L (accounting for 33%), respectively, the removal effect was the dominant process while the dilution effect can not be neglected.

     

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