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Soil organic carbon content and storage of raised field wetlands in different functional zones of a typical shallow freshwater lake, China.

机译:典型浅水湖泊,中国不同功能区的土壤有机碳含量和高地湿地的存储。

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摘要

Soil samples were collected in raised-field wetlands of five typical functional zones (inlet zone, water reserve zone, outlet zone, aquaculture zone, industrial zone) in Baiyangdian Lake, China, from a depth of 0-30 cm. The soil organic carbon (SOC) content, density, and storage, and carbon pool index (CPI) were calculated for each typical zone, and spatial distribution of SOC storage in the region was estimated using the ordinary kriging, interpolated value method. Our results showed that the average values of SOC content and storage decreased with depth along the soil profiles. Lowest values of SOC content and storage were observed in the inlet zone, whereas the outlet zone showed the highest SOC content and the water reserve zone showed the highest SOC storage. Surface soils had higher heterogeneity with higher values of SOC content and storage than deeper soils. Storage of SOC was much lower in the south-east of the water reserve zone and the east of the inlet zone than in the north-west of the water reserve zone or in the east of the whole Baiyangdian Lake. Values of CPI followed the order water reserve zone > aquaculture zone > outlet zone > industrial zone > inlet zone. The SOC was positively correlated with water content and negatively correlated with soil bulk density (P<0.01), but had no significant correlation with other soil properties.
机译:在中国白洋淀的五个典型功能区(进水区,蓄水区,出水区,水产养殖区,工业区)的高地湿地上采集土壤样品,深度为0-30厘米。计算每个典型区域的土壤有机碳(SOC)含量,密度和存储量以及碳库指数(CPI),并使用常规克里格插值法估算该区域内SOC的空间分布。我们的研究结果表明,沿着土壤剖面,SOC含量和储存的平均值随深度的增加而降低。进口区的SOC含量和储量最低,而出口区的SOC含量最高,而储水区的SOC储量最高。与深层土壤相比,表层土壤具有更高的异质性,SOC含量和储存值更高。在水储备区的东南部和进水区的东部,SOC的储藏量远低于水储备区的西北部或整个白洋淀的东部。 CPI的值依次为水储备区>水产养殖区>出口区>工业区>入口区。 SOC与含水量呈正相关,与土壤容重呈负相关(P <0.01),但与其他土壤特性无显着相关。

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