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    小兴安岭泥炭藓湿地土壤有机碳分布特征

    Characteristic of soil organic carbon of the Sphagnum spp. wetland in Xiao Hinggan Mountains

    • 摘要: 在小兴安岭林区乌伊岭国家级湿地自然保护区,选择典型泥炭藓湿地进行土壤样品采集,对土壤有机碳(SOC)质量分数、密度及储量进行研究,并分析SOC质量分数与土壤理化性质之间的相关性。结果表明:1)SOC质量分数随土层加深而减少,变化范围在433.89~523.36g/kg之间,平均质量分数为474.27 g/kg;土壤有机碳密度随土层的加深而显著增加,0~60cm土层土壤有机碳储量为166.07t/hm2。2)SOC质量分数与非毛管孔隙度存在极显著的正相关关系,幂函数方程拟合效果显著;SOC质量分数与毛管孔隙度呈极显著负相关,二次曲线拟合效果较好(R2=0.87);SOC质量分数与土壤密度呈极显著负相关,线性方程拟合较好(R2=0.81)。SOC质量分数与全N、全P质量分数呈显著负相关,与有效P质量分数呈极显著正相关,与水解N质量分数相关不显著。研究结果可为我国湿地土壤有机碳储量及碳循环的进一步研究提供帮助。

       

      Abstract: In the Wuyiling National wetland Nature Reserve of the Xiao Hinggan Mountains forest region,the soil samples of typical Sphagnum spp.wetland collected.According to the content of soil organic carbon(SOC),carbon density,carbon reserve,and the relationships between the SOC and the soil physical and chemical properties were analyzed.The results showed that the contents of SOC showed a reduction in a deeper soil stratum which range from 433.89 to 523.36g/kg,and is in a mean content of 474.27g/kg;carbon densities rise in a deeper soil stratum with a soil carbon density of 166.07t/hm2 in the depth of 0-60cm.Secondly,the relation between SOC and soil capillary porosity was significant negative,quadratic curve-fitting results of which was well(R2=0.87);the SOC content is obviously negative correlated with soil bulk density,and the linear equation fitted was well(R2=0.81).The soil organic carbon content were significant negative correlation with total nitrogen and total phosphorus,in a obvious positive correlation with effective phosphorus,And organic carbon and hydrolysis nitrogen were not significantly correlated.The results may help us for further study.on wetland soil carbon storage and carbon cycle.

       

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