成土母质及土壤类型作用下土壤有机碳分布特征

    Distribution characteristics of soil organic carbon under the influence of parent material and soil type

    • 摘要: 土壤有机碳是陆地生态系统碳库的重要组成部分,对农田土壤的碳循环过程以及耕地质量发挥着重要作用,影响土壤有机碳空间分布特征的因素众多,其中成土母质和土壤类型直接影响着土壤有机碳的分布。以吉林省延边州中部偏东地区的延吉鸠巢平原为例,通过系统分层取样,对研究区典型土壤剖面的土壤有机碳的分布特征及影响因素进行分析研究。结果表明: 延吉鸠巢平原土壤有机碳平均含量为48.68×10-3,含量丰富,在垂向上随着土壤深度的增加而逐渐降低,0, 20 cm表层土壤有机碳的含量明显高于深层土壤,具有表聚性; 延吉鸠巢平原的成土母质主要为中生代砂岩类风化物和第四系河湖相冲积物,对比发现,第四系河湖相冲积物发育的土壤有机碳富集能力低于中生代砂岩类风化物发育的土壤有机碳富集能力,且有机碳整体损失率较高,分散性较大; 延吉鸠巢平原主要发育土壤类型为暗棕壤和水稻土,不同土壤分层条件下,不同土壤类型有机碳含量与各土层深度存在显著负相关性, 同一土层对比发现,水稻土土壤有机碳含量沿剖面垂向损失更明显,相较于暗棕壤土壤有机碳具有高度变异性。研究结果可为评价延吉鸠巢平原土壤有机碳的碳源碳汇提供基础数据,可为东北地区土壤有机碳空间分布、深层土壤有机碳变化提供参考依据。

       

      Abstract: Soil organic carbon is an important component of the terrestrial ecosystem carbon pool, playing an important role in the carbon cycling process of farmland soil and the quality of farmland. The spatial distribution characteristics of soil organic carbon are affected by many factors, among which parent material and soil type directly affect the distribution of soil organic carbon. The authors in this study took Yanji Jiuchao Plain in the central eastern region of Yanbian Prefecture in Jilin Province as an example to analyze and study the distribution characteristics and influencing factors of soil organic carbon in typical soil profiles in the area through systematic stratified sampling. The results showed that the average organic carbon content in the soil of Jiuchao Plain in Yanji was 48.68×10-3, which was generally rich. And the organic carbon content gradually decreased with the increase of profile depth in vertical direction. Besides, the content of the surface organic carbon(0, 20 cm) was significantly higher than that of the deep soil, showing surface aggregation. The main types of parent material in Jiuchao Plain of Yanji were Mesozoic sandstone weathering materials and Quaternary loose deposits. The soil organic carbon enrichment ability developed by Quaternary loose deposits was lower than that developed by Mesozoic sandstone weathering products, with higher loss rate and variability. The main soil type developed in Yanji Jiuchao Plain was dark brown soil and paddy soil. The organic carbon content of soil with different types had a significant negative relationship with the soil depth. Compared with dark brown soil in the same soil layer, paddy soil had high variability and significant loss along the depth profile. The research results could provide basic data for evaluating the carbon sources and sinks of soil organic carbon in Yanji Jiuchao Plain, and could provide references for the spatial distribution of soil organic carbon and changes in deep soil organic carbon in Northeast China.

       

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