水稻土和旱地土有机碳积累及微生物残体碳贡献特征与驱动机制
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1.闽江大学地理与海洋学院;2.福建师范大学

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S154.36

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The characteristics and driving mechanism of organic carbon accumulation and microbial necromass carbon contribution in paddy soils and upland soils
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1.College of Geography and Oceanography,Minjiang University;2.School of Geographical Sciences,Fujian Normal University

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    摘要:

    土地利用方式通过改变土壤水分条件、碳输入途径及微生物代谢环境,深刻影响土壤有机碳(SOC)的积累与稳定。然而,不同土地利用方式下微生物残体碳(MNC)积累及其对SOC贡献的差异机制仍缺乏系统认识。本研究以江西省余江、吉水、信丰和宜丰4个典型农业区域的配对水稻土和旱地土为研究对象,测定土壤理化性质、SOC含量及基于氨基糖表征的微生物残体碳,系统比较不同土地利用方式下土壤碳库组成特征及其环境驱动因子。结果表明,四个区域水稻土SOC含量均显著高于旱地土,分别是旱地土的1.5~3.0倍;同时,水稻土MNC、真菌残体碳(FNC)和细菌残体碳(BNC)含量均显著高于旱地土,表明长期淹水环境和较高有机碳输入促进了微生物残体积累。然而,MNC对SOC的贡献率在旱地土中(21.55%~46.06%)整体高于水稻土(23.36%~30.81%),表明微生物残体碳在低碳环境下对维持土壤碳库具有更高的相对贡献。不同土地利用方式中,FNC含量及其对SOC的贡献均显著高于BNC,真菌残体是亚热带农田土壤MNC积累的主要组分。随机森林分析表明,土壤总氮(TN)是驱动SOC及MNC、FNC和BNC积累的关键环境因子,TN与各碳组分均呈显著正相关,而NO3?、pH和有效磷(AP)与其呈负相关。综上,土地利用方式通过改变土壤碳氮资源状况及微生物残体形成与保存过程,调控农田土壤碳库数量及组成特征;水稻土具有更高的SOC和MNC积累能力,而旱地土壤MNC对SOC的相对贡献更高。

    Abstract:

    Land use has a profound impact on the accumulation and stability of soil organic carbon (SOC) by changing soil moisture conditions, carbon input pathways and microbial metabolic environment. However, there is still a lack of systematic understanding of the accumulation characteristics of microbial residual carbon (MNC) and the different mechanisms of its contribution to SOC under different land use types. In this study, the paired paddy soils and upland soils in four typical agricultural areas of Yujiang, Jishui, Xinfeng and Yifeng in Jiangxi Province were used as the research objects to determine the soil physicochemical properties, SOC content and microbial necromass carbon based on amino sugar index. The composition characteristics of soil carbon pool and its environmental driving factors under different land use types were systematically compared. The results showed that the SOC content of paddy soils was significantly higher than that of upland soils in the four regions, which was 1.5~3.0 times higher than that of upland soils. At the same time, the contents of MNC, fungal necromass carbon (FNC) and bacterial necromass carbon (BNC) in paddy soils were significantly higher than those in upland soils, indicating that long-term flooding environment and high organic carbon input promoted the accumulation of microbial necromass. However, the contribution of MNC to SOC in upland soils (21.55%~46.06%) was higher than that in paddy soils (23.36%~30.81%), indicating that microbial necromass carbon had a higher relative contribution to maintaining soil carbon pool under low carbon input environment. In different land use types, FNC content and its contribution to SOC were significantly higher than BNC, and fungal debris was the main component of microbial carbon accumulation in subtropical farmland soils. Random forest analysis showed that soil total nitrogen (TN) was the key environmental factor driving the accumulation of SOC, MNC, FNC and BNC.TN was significantly positively correlated with each carbon component, while NO3?, pH and available phosphorus (AP) were negatively correlated with it. In summary, land use patterns regulate the quantity and composition of farmland soil carbon pool by changing the status of soil carbon and nitrogen resources and the formation and preservation process of microbial necromass. Paddy soils had higher SOC and MNC accumulation capacity, while the relative contribution of microbial necromass carbon to SOC was higher in upland soils.

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  • 收稿日期:2026-07-11
  • 最后修改日期:2026-09-08
  • 录用日期:2026-09-14
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