生态修复区盐地碱蓬群落碳、氮储量及其影响因素分析——以辽河三角洲大凌河口湿地为例

Study on carbon and nitrogen storage pattern of Suaeda salsa community and its influencing factors in the coastal wetland ——A case study of Dalinghe estuary wetland under Liaohe River Delta

  • 摘要: 为揭示土壤环境变化及植物群落结构对修复初期河口湿地碳汇格局的影响,本文运用方差分解方法测算了群落尺度辽河口湿地生态修复区碳、氮储量分配格局,并定量阐明了盐度、含水率、高程等环境因子对碳、氮储量的影响贡献率。结果表明:(1)春、秋季,土壤碳储量分别为41.93 t/ha和44.72 t/ha,氮储量分别为8.65 t/ha和8.80 t/ha;植物碳储量分别为8.97 kg/ha和180.48 kg/ha,氮储量分别为0.61 kg/ha和16.27 kg/ha。(2)植物碳氮储量与株高、盖度呈显著对数函数关系,与土壤微生物量碳氮及土壤氮的周转速率呈显著负相关性。(3)土壤含水率、群落盖度和高程是影响碳、氮储量的最主要因子,地形高程和含水率能解释幼苗期碳、氮储量分异的45.6%以及成熟期碳、氮储量分异的54.5%。研究结果证明了微地形改造、生态补水等措施对湿地碳汇能力的提升具有重要作用。

     

    Abstract: To reveal the impacts of the soil environmental factors and vegetation community structure on carbon and nitrogen storage pattern of the estuarine wetland at the initial stage of ecological restoration period,this paper studied the carbon and nitrogen storage patterns of the soil-vegetation system in the restoration zone of Liaohe River Delta and clarified the impact contribution rate of the soil environmental factors such as salinity, moisture content, elevation and plant community structures on them based on the analysis of variance decomposition. Results showed that, the average soil carbon and nitrogen storage were 41.93 t/ha, 8.65 t/ha for spring and 44.72 t/ha, 8.80 t/ha for winter respectively. The average plant carbon and nitrogen storage were 8.97 kg/ha, 0.61 kg/ha for spring and 180.48 kg/ha, 16.27 kg/ha for winter respectively. The plant carbon and nitrogen storage had significant logarithmic relationships with plant height and coverage of community, and had significant negative correlations with the turnover rate of soil nitrogen and the microbial biomass C(N). Variance decompose analysis showed that the elevation and moisture content could cumulatively explain 45.6% of the changes in carbon and nitrogen storage patterns at plant seedling stage, and explain 54.5% at the mature stage. The results of this study strongly support that measures of microtopography restoration and water compensation play an important role in improving the blue carbon sequestration of degraded estuarine wetlands.

     

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