• ISSN 1008-505X
  • CN 11-3996/S

玉米间作田菁通过增加亚耕层植物残体碳驱动黑土有机碳积累

Maize−Sesbania cannabina Intercropping drives black soil organic carbon accumulation by increasing subsoil plant residue carbon

  • 摘要:
    目的 绿肥(也称覆盖作物)具有扼制黑土退化、培肥并提升黑土固碳潜力等多样化功能。本研究从微生物碳泵和有机碳组分角度探究了玉米间作豆科绿肥体系下黑土耕层和亚耕层土壤的固碳效应及机制。
    方法 田间定位试验于2021年起在黑龙江哈尔滨进行,设置玉米单作(MM)和玉米−田菁(Sesbania cannabina)间作(MG)两个处理。2025年在玉米拔节期分别采集0—20 cm和20—40 cm土壤样品,比较两个体系下土壤基本理化性质、土壤有机碳(SOC)及物理组分、微生物源与植物源残体碳累积等指标的差异。
    结果 与MM处理相比,MG处理耕层SOC无明显变化,但亚耕层SOC、微生物生物量碳(MBC)和可溶性有机氮(DON)分别增加了14.43%、135.02%和88.27%,矿物结合态有机碳(MAOC)和颗粒态有机碳(POC)含量分别增加了32.89%和40.75%,且亚耕层MAOC和POC含量与SOC含量呈显著正相关;MG处理亚耕层土壤微生物碳利用效率显著提高19.57%,碳、氮、磷循环相关水解酶(β-葡萄糖苷酶、β-纤维二糖酶、N-乙酰氨基葡萄糖苷酶、磷酸酶)活性增加86.9%~145.0%,土壤中植物残体碳含量(PRC)显著增加31.1%,微生物残体碳含量无显著变化,因而微生物残体碳积累系数下降56.1%;耕层和亚耕层土壤丁香基酚类酸醛比(Ad/Al)s不变,而香草基酚类酸醛比 (Ad/Al)v分别降低69.2%和33.6%,肉桂基/香草基酚类比值(C/V)分别降低26.3%和19.5%。Mantel分析结果显示,POC、MAOC和SOC均与PRC显著相关,表明亚耕层土壤PRC增加是SOC积累的关键因素。
    结论 豆科绿肥田菁属深根系作物,显著增加了亚耕层的根系残体碳量,其较低的C/N比促进了微生物对碳的利用,增加了亚耕层土壤碳氮磷相关水解酶活性。土壤微生物水解酶活性的增加能够加速微生物碳泵中微生物的“体外修饰”过程,促进土壤中植物残体碳中木质素的氧化,以及向POC和MAOC的转化,最终表现为亚耕层土壤有机碳的积累。因此,亚土层中植物性残体碳含量的增加是玉米间作田菁提升黑土耕地有机碳含量的关键驱动因子。

     

    Abstract:
    Objectives Green manure (cover crops) can curb the degradation of black soil and simultaneously sequester carbon and improve soil fertility. This study aimed to clarify the carbon sequestration effects and underlying mechanisms in topsoil (0−20 cm) and subsoil (20−40 cm) under a maize-sesbania (Sesbania cannabina) intercropping system, from the perspectives of the microbial carbon pump and organic carbon fractions.
    Methods A field experiment was established in Harbin since 2021. Maize monoculture (MM) and maize-sesbania intercropping (MG) treatments were included in the experiment. At the maize jointing stage in 2025, soils were sampled from 0−20 cm and 20−40 cm layers. Basic physicochemical properties, soil organic carbon (SOC) and its physical fractions, and the accumulation of microbial- and plant-derived necromass carbon were compared between the two systems.
    Results Compared to the MM treatment, the MG treatment showed no significant change in topsoil SOC, but subsoil SOC, microbial biomass carbon (MBC), and dissolved organic nitrogen (DON) increased by 14.43%, 135.02%, and 88.27%, respectively. The subsoil mineral-associated organic carbon (MAOC) and particulate organic carbon (POC) contents increased by 32.89% and 40.75%, respectively, and both MAOC and POC contents exhibited a significant positive correlation with SOC content. Subsoil soil microbial carbon use efficiency significantly increased by 19.57%, and the activities of carbon-, nitrogen-, and phosphorus-cycling-related hydrolases (β-glucosidase, β-cellobiosidase, N-acetylglucosaminidase, phosphatase) increased by 86.9% to 145.0%. The plant residue carbon (PRC) content in subsoil significantly increased by 31.1%, while microbial necromass carbon content showed no significant change, leading to a 56.1% decrease in the microbial necromass carbon accumulation coefficient. The syringyl phenol acid-to-aldehyde ratio (Ad/Al)s in both topsoil and subsoil remained unchanged, while the vanillyl phenol acid-to-aldehyde ratio (Ad/Al)v decreased by 69.2% and 33.6%, respectively, and the cinnamyl-to-vanillyl phenol ratio (C/V) decreased by 26.3% and 19.5%, respectively. Mantel analysis revealed that POC, MAOC, and SOC were all significantly correlated with PRC, indicating that subsoil PRC is a key factor in SOC accumulation.
    Conclusions Leguminous green manure, Sesbania cannabina, is a deep-rooted crop that significantly increases root residue carbon in the subsoil. Its low C/N ratio promotes microbial carbon utilization and enhances the activity of carbon-, nitrogen- and phosphorus-related hydrolases in the subsoil. The increase in soil microbial hydrolase activity accelerates the "extracellular modification" process in the microbial carbon pump, promoting the oxidation of lignin in plant residue carbon and its transformation into POC and MAOC. This ultimately leads to the accumulation of soil organic carbon in the subsoil. Therefore, plant residue carbon enrichment in subsoil drives SOC accumulation in maize-sesbania intercropping on black soil.

     

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