张晓堂, 田昆, 袁杰, 岳海涛, 张昆. 积水条件对若尔盖典型高寒沼泽碳氮垂直分布的影响[J]. 西南林业大学学报, 2017, 37(2): 116-121. DOI: 10.11929/j.issn.2095-1914.2017.02.019
引用本文: 张晓堂, 田昆, 袁杰, 岳海涛, 张昆. 积水条件对若尔盖典型高寒沼泽碳氮垂直分布的影响[J]. 西南林业大学学报, 2017, 37(2): 116-121. DOI: 10.11929/j.issn.2095-1914.2017.02.019
Xiaotang Zhang, Kun Tian, Jie Yuan, Haitao Yue, Kun Zhang. Effect of Hydrological Conditions on Carbon, Nitrogen Vertical Distribution of Typical Alpine Marsh in Zoige[J]. Journal of Southwest Forestry University, 2017, 37(2): 116-121. DOI: 10.11929/j.issn.2095-1914.2017.02.019
Citation: Xiaotang Zhang, Kun Tian, Jie Yuan, Haitao Yue, Kun Zhang. Effect of Hydrological Conditions on Carbon, Nitrogen Vertical Distribution of Typical Alpine Marsh in Zoige[J]. Journal of Southwest Forestry University, 2017, 37(2): 116-121. DOI: 10.11929/j.issn.2095-1914.2017.02.019

积水条件对若尔盖典型高寒沼泽碳氮垂直分布的影响

Effect of Hydrological Conditions on Carbon, Nitrogen Vertical Distribution of Typical Alpine Marsh in Zoige

  • 摘要: 通过野外样品采集和室内测定分析, 对若尔盖季节性积水和常年积水沼泽土壤有机碳与氮含量的垂直分布进行研究。结果表明:在0~200 cm土层内, 常年积水沼泽的有机碳含量为270.174 g/kg, 氮含量为11.963 g/kg; 季节性积水沼泽碳含量为212.066 g/kg, 氮含量为10.824 g/kg; 季节性积水沼泽的平均碳、氮含量均低于常年积水沼泽。在0~60 cm土层, 2种沼泽的各层次有机碳含量无显著差异, 均表现为下降趋势; 在60~110 cm土层, 2种沼泽的有机碳含量呈现不同程度的增加, 但常年积水沼泽有机碳含量增加幅度与速率均明显大于季节性积水沼泽; 在110~200 cm土层, 含碳量变化趋于相对稳定, 但同等深度下常年积水沼泽的含碳量明显高于季节性积水沼泽。在泥炭表、中层(0~110 cm), 季节性积水沼泽氮含量 < 常年积水沼泽; 而在泥炭底层(110~200 cm), 季节性积水沼泽氮含量>常年积水沼泽。有机碳和氮含量数据表明, 在常年积水沼泽向季节性积水沼泽演变过程中, 有机碳含量呈现一定趋势的减小, 湿地的碳汇功能发生了变化。

     

    Abstract: Vertical distribution of soil organic carbon and nitrogen content of seasonal water marsh and perennial water marsh in Zoige was studied with field sampling and laboratory analysis.The results showed that within the range of 0-200 cm soil layer, organic carbon content of perennial water marsh was 270.174 g·kg-1, and the nitrogen content was 11.963 g·kg-1.Carbon content of seasonal water marsh was 212.066 g·kg-1, and the nitrogen content was 10.824 g·kg-1.Carbon and nitrogen content of seasonal water marsh were less than that of perennial water marsh.In the range of 0-60 cm soil layer, the organic carbon content of 2 kinds of marsh appeared different degree of increase, but the increase amplitude and increase rate of organic carbon content of perennial water marsh was significantly higher than that of seasonal water marsh.In the range of 110-200 cm soil layer, the change of carbon content tends to be stable, but the carbon content of perennial water marsh was obviously higher than that of seasonal water marsh at the same depth.In the surface and middle layer of peat (0-110 cm), the nitrogen content of seasonal water marsh was greater than that of the perennial water marsh.And at the bottom layer of peat (110-200 cm), the nitrogen content of seasonal water marsh was greater than that of the perennial water marsh.The above data demonstrated that the content of organic carbon was decreased in the evolution process from the perennial water marsh to the seasonal water marsh, the carbon sinks function of wetlands has changed.

     

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