Spatial Distribution of Organic and Inorganic Carbon in Sediments of Tai Lake, China

N. Xu, Feng Wei, Hongying Liu, Hui Yang
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Abstract

The sediment in lakes is the pools of material and energy, and the composition and content of organic and inorganic carbon in sediments constrain carbon cycling. This paper conducts research of spatial distribution of organic and inorganic carbon contents in sediments of Tai lake in China based on the data of geochemical survey in the early 2000s. Results show that the organic, inorganic carbon contents in surface sediments (0-20 cm) of the lake are 5.76±4.38, 1.42±1.40 g kg-1 and those in deep sediments (160-180 cm) are 2.30±1.39, 2.30±1.39 g kg-1, respectively. The organic carbon content in deep sediments is close to that in surface sediments, but inorganic carbon content is 1.62 times of that in surface sediments. The ranges and coefficients of variation of carbon contents in deep sediments show lower spatial variability due to limited human activity. This work provides valuable information regarding accurate distribution of organic and inorganic carbon in the surface and deep sediments of Tai lake, which may be useful to evaluate intrinsic pollution in the lake.
太湖沉积物中有机碳和无机碳的空间分布特征
湖泊沉积物是物质和能量的储存库,沉积物中有机碳和无机碳的组成和含量制约着碳循环。基于2000年代初的地球化学调查资料,对中国太湖沉积物中有机碳和无机碳含量的空间分布进行了研究。结果表明:湖泊表层沉积物(0 ~ 20 cm)有机碳、无机碳含量分别为5.76±4.38、1.42±1.40 g kg-1,深层沉积物(160 ~ 180 cm)有机碳、无机碳含量分别为2.30±1.39、2.30±1.39 g kg-1。深层沉积物的有机碳含量与表层沉积物的有机碳含量接近,但无机碳含量是表层沉积物的1.62倍。由于人类活动的限制,深层沉积物碳含量的变异范围和变异系数表现出较低的空间变异性。本研究为太湖表层和深层沉积物中有机碳和无机碳的准确分布提供了有价值的信息,为湖泊内在污染评价提供了依据。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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