模拟研究了三江平原典型草甸小叶章湿地及人工林地土壤有机碳(SOC)矿化在4种C/N(Ⅰ: 9-10,Ⅱ:11-12,Ⅲ: 13-16,Ⅳ: 16-22)处理下的变化特征,分析了SOC矿化对C/N的响应。结果表明:在36天的培养期内,高C/N处理下两种土壤的SOC累积矿化量分别是低C/N时的2.78和2.68倍,两种土壤SOC矿化量对C/N变化的响应不存在显著差异;不同C/N处理下,两种土壤SOC的矿化速率均在前期(0~4天)较高,随着培养时间的延长逐渐降低,并趋于稳定;一级动力学方程能较好的描述两种土壤的SOC矿化动态,其C0和C0/SOC值均随C/N的增加而增加;回归分析表明,试验C/N(9-22)范围内湿草甸土和林地土的SOC累积矿化量及矿化速率分别与C/N呈显著的线性和二次曲线关系,C/N是影响湿地土壤有机碳富集程度的关键因素。
An incubation expericment with typical Deyeuxia angustifolia meadow soil and artificial forest soil in the Sanjiang plain was conducted under different soil C/N (Ⅰ: 9-10, Ⅱ:11-12, Ⅲ: 13-16, Ⅳ: 16-22) to examine the responses of soil organic carbon (SOC) mineralization to C/N changes. The result showed that during the period of 36d incubation, the SOC accumulative losses of two kinds of soils under high C/N treatment were about 2.78 and 2.68 times as much as that under low C/N, respectively. SOC mineralization rates for both the two kinds of soils were higher in the first 4 days of incubation, and became stable as the time prolonged. The dynamics of SOC mineralization of two kinds of soil preferably followed the first-order kinetics, and the C0 and C0/SOC values increased exponentially with the increasing of C/N. The regression analysis also found that there were significant linear or conic relationships between the accumulative loss and mineralization rate of SOC and C/N, which explained that C/N was the key factor in affecting the sequestration of SOC in wetland.
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