松嫩平原玉米带农田土壤有机碳时空格局

    Spatial and temporal changes of organic carbon in agricultural soils of Songnen Plain maize belt

    • 摘要: 该文基于吉林省第二次全国土壤普查省数据、县级土壤剖面资料和2003-2006年实测数据,估算了不同土壤类型农田表层土壤有机碳密度和储量,并对近25年来土壤有机碳时空变化特征及其原因进行分析。结果表明,总体上松嫩平原玉米带农田土壤有机碳密度和储量呈增加趋势。其中,碱土、暗棕壤、黑土和草甸土的土壤有机碳密度增幅分别达33%(4.16 kg/m2),23.05%(3.79 kg/m2)、16.51%(3.74 kg/m2)和12.20%(3.77 kg/m2);相反,黑钙土有机碳密度下降幅度达30.79%(2.18 kg/m2)。两时期土壤有机碳密度的空间分布格局基本一致,呈中部高、边缘低的趋势,但25年间土壤有机碳含量变化与1980年初始含量呈显著负相关(r=-0.615**,P<0.01),且4.04 kg/m2是土壤有机碳上升或下降的临界值。根据West等提出的土壤碳汇潜力估算方法,如果保持1980年土地利用方式和传统的栽培耕作措施不变的情况下,松嫩平原玉米带农田土壤有机碳的碳汇潜力为0.33 Tg/a。

       

      Abstract: In this paper, a database of soil organic carbon in topsoil (0-20 cm) of Songnen Plain maize belt was obtained from the second national soil survey in Jilin Province and its four counties in 1980, and from field measurements in 2003-2006. The density and storage of organic carbon in agricultural topsoil was estimated from different soil types, and then the spatial and temporal variations of soil organic carbon in the past 25 years were analyzed. The results showed that the area-weighted average organic carbon density and storage in agricultural soils had an increasing trend. The significant carbon gains were 33% (4.16 kg/m2), 23.05% (3.79 kg/m2), 16.51% (3.74 kg/m2), and 12.20% (3.77 kg/m2) for Solonetzs, Dark-brown earths, Black soils and Meadow soils, respectively. On the contrary, the soil organic carbon density decreased by 30.79% (2.18 kg/m2) in the chernozems. The spatial distributions of soil organic carbon density were the same for two periods, which was higher in centre and lower in the edge region. There was a significant negative relationship (r=-0.615**, P<0.01) for the carbon changes in the past 25 years to its original contents in 1980, and the turning point of soil organic carbon was at 4.04 kg/m2. Under the current land use patterns and traditional cultivation and tillage, the soil organic carbon sequestration potential would be 0.33Tg/a in Songnen Plain maize belt.

       

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