长期施肥对黄泥田土壤有机碳化学结构与固碳细菌群落结构的影响OA
Effects of Long-Term Fertilization on Soil Organic Carbon Structure and Carbon-Fixing Bacterial Community Structure in Yellow-Mud Paddy Soil
[目的]土壤有机碳(SOC)稳定性受官能团组成和固碳微生物的影响,通过比较长期不同施肥对黄泥田土壤有机碳结构和固碳细菌cbbL基因群落结构影响的差异,全面认识黄泥田土壤固碳潜力及其机制.[方法]基于农业农村部福建耕地保育科学观测实验站长期定位稻田,设不施肥(CK)、化肥(NPK)、化肥+稻草还田(NPKS)和化肥+牛粪(NPKM)处理,利用13C 核磁共振和傅里叶技术测定土壤有机碳结构,及利用高通量测序技术测定固碳细菌群落结构.[结果]化肥配施有机肥(NPKS和NPKM处理)显著提高了黄泥田土壤有机碳含量,土壤有机碳含量随土层加深而降低.矿质结合态有机碳的含量、颗粒态有机碳的含量及颗粒态有机碳占土壤有机碳的比例均随土层加深而降低,而矿质结合态有机碳占土壤有机碳比例则随土层加深而增加.NPKS和NPKM处理增加了SOC中烷烃及芳香碳化合物含量,提高了土壤有机碳的稳定性及复杂程度,亚表层土壤有机碳稳定性高于表层.土壤固碳细菌α多样性指数分析结果显示,施肥显著提高了黄泥田土壤固碳细菌多样性指数,其中NPKM处理表现最好.土壤优势菌纲为β-变形菌纲,施肥不同程度地提高β-变形菌纲的相对丰度.Sulfuricaulis和Sulfuritortus为优势菌属.亚表层土壤相较于表层土壤降低了光自养微生物相对丰度,而提高了化能自养微生相对丰度.[结论]稻草、牛粪与化肥配施不仅促进了黄泥田土壤有机碳的稳定性,而且显著增加了土壤固碳细菌的多样性和丰度,改变了土壤固碳细菌群落的结构.其中,牛粪配施化肥更有利于黄泥田土壤有机碳结构稳定和固碳细菌群落的多样性.
[Objective]Soil organic carbon(SOC)stability is significantly influenced by the functional group composition and carbon-fixing microorganisms.This study compared the differences in soil organic carbon structure and cbbL bacterial community structure under long-term fertilization regimes,so as to provide an understanding of the carbon sequestration potential and mechanisms of yellow-mud paddy soil.[Method]In this study,the effects of no fertilization(CK),chemical fertilizer(NPK),chemical fertilizer+rice straw returning(NPKS)and chemical fertilizer+organic manure(NPKM)treatments on the characteristics of organic carbon functional groups and the community structure of carbon sequestration bacteria were studied by using 13C nuclear magnetic resonance(NMR)and Fourier transform technology to determine the organic carbon structure and the community structure of carbon-fixing bacteria by high-throughput sequencing technology,respectively.[Result]The co-chemical fertilizer and manure application(NPKS and NPKM)significantly increased the total SOC content in yellow-mud paddy soil,while the SOC content decreased with increasing soil depth.The contents of MOC and POC,as well as the POC/SOC ratio,decreased with soil depth,while the MOC/SOC ratio showed the opposite trend.NPKS and NPKM treatments also increased the content of aliphatic and aromatic carbon compounds,then enhancing the stability and complexity of soil organic carbon,with subsoil organic carbon being more stable than surface soil.Analysis of the α-diversity index of carbon-fixing bacteria in the soil revealed that fertilization significantly increased the diversity index of carbon-fixing bacteria,with the NPKM treatment showing the best results.The dominant bacterial phylum in paddy soil was Proteobacteria,and fertilization increased the relative abundance of this phylum to varying extents.The dominant genera were Sulfuricaulis and Sulfuritortus.In the subsoil,compared with the surface soil,the relative abundance of photoautotrophic microorganisms was reduced,while the relative abundance of chemo lithotrophic microorganisms was increased.[Conclusion]Therefore,combined organic amendments(straw or manure)with chemical fertilizers not only enhanced SOC stability but also increased the diversity and abundance of carbon-fixing bacteria,restructuring their communities.NPKM was the most effective in stabilizing SOC and promoting microbial diversity,highlighting its role in sustainable yellow-mud paddy soil management.
魏圆慧;余益辉;李子钧;丁文杰;涂文龙;毛艳玲
福建农林大学资源与环境学院,福州 350002||土壤生态系统健康与调控福建省高校重点实验室,福州 350002福建农林大学资源与环境学院,福州 350002||土壤生态系统健康与调控福建省高校重点实验室,福州 350002福建农林大学资源与环境学院,福州 350002||土壤生态系统健康与调控福建省高校重点实验室,福州 350002福建农林大学资源与环境学院,福州 350002||土壤生态系统健康与调控福建省高校重点实验室,福州 350002福建农林大学资源与环境学院,福州 350002||土壤生态系统健康与调控福建省高校重点实验室,福州 350002福建农林大学资源与环境学院,福州 350002||土壤生态系统健康与调控福建省高校重点实验室,福州 350002||自然生物资源保育利用福建省高校工程研究中心,福州 350002
黄泥田土壤长期施肥有机无机肥配施土壤有机碳结构固碳细菌
yellow-mud paddy soillong-term fertilizationco-chemical fertilizer and manure applicationsoil organic carbon structurecarbon-fixing bacteria
《中国农业科学》 2026 (5)
1020-1033,14
福建省财政厅项目(KKY22005XA)、福建农林大学科技创新专项基金项目(KFB24124A)
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