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SEASONAL CHANGES OF DISSOLVED AND PARTICULATE ORGANIC CARBON IN DONGHU LAKE, CHINA

机译:东湖湖泊溶解性和颗粒状有机碳的季节变化

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摘要

Concentrations of dissolved and particulate organic carbon (DOC and POC) were documented in 1996-1997 at 4 different trophic state stations in Donghu Lake, a typical shallow eutrophic lake along the Changjiang River's middle reaches. The mean concentrations of DOC were 15.11±3.26, 15.19±4.24, 14.27±3.43, and 13.31±3.30 mg/L in Station I, II, III, and IV, respectively. The DOC concentrations of the studied area were very similar to that in other lakes along the Changjiang River's middle reaches. The POC mean of the whole lake was 5.01 mg/L due to the large amount of organic detritus of both allochthonous and autochthonous origin. Significant linear relationship was found between POC and chlorophyll a at all 4 stations, which presumably reflect that phytoplankton, its exudates and its metabolic products were the main contributors to the POC pool in the water column. The slope of such linear relationship at Station IV was significantly steeper than that at Station I, II and III. In addition, the DOC/POC ratios (mean value: 4.40) indicated that the organic detritus was the most important component of the particulate organic matter; in other words, next to organic detritus, phytoplankton dominated the particulate organic matter in Donghu Lake.
机译:1996年至1997年,东湖是长江中游地区的典型浅水富营养化湖,在4个不同的营养状态站记录了溶解态碳和颗粒有机碳(DOC和POC)的浓度。 I,II,III和IV站的DOC平均浓度分别为15.11±3.26、15.19±4.24、14.27±3.43和13.31±3.30 mg / L。研究区的DOC浓度与长江中游沿岸其他湖泊的DOC浓度非常相似。整个湖泊的POC平均值为5.01 mg / L,这是由于大量的异源和本地有机碎屑所致。在所有四个站上,POC和叶绿素a之间都存在显着的线性关系,这大概反映出浮游植物,其渗出物和代谢产物是水柱中POC池的主要贡献者。 IV站的这种线性关系的斜率比I,II和III站的陡峭得多。此外,DOC / POC比(平均值:4.40)表明,有机碎屑是颗粒状有机物的最重要组成部分。换句话说,在东湖中,浮游植物以有机碎屑为主要成分。

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