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Deyun Chena,b, Zhiyun Luc, Yanping Wangd, Chunyu Houa, Jianping Wua*
aState Key Laboratory of Vegetation Structure, Function and Construction (VegLab), Yunnan Key Laboratory of Plant Reproductive Adaptation and Evolutionary Ecology/Institute of Biodiversity, School of Ecology and Environmental Science, Yunnan University, Kunming 650500, China
bNational Plateau Wetlands Research Center, College of Ecology and Environment, Southwest Forestry University, Kunming 650224, China
cAilaoshan Station of Subtropical Forest Ecosystem Studies, Xishuangbanna Tropical Botanical Garden, Chinese Academy of Sciences, Jingdong 676209, China
dSchool of Environmental Engineering, Yunnan Forestry Technological College, Kunming 650224, China
*Correspondence: Jianping Wu, E-mail: jianping.wu@ynu.edu.cn, Tel: +86-871-65939546, Fax: +86-871-65031317
摘要: 土壤呼吸释放到大气中的CO2是陆地生态系统与大气之间的第二大碳通量。已有大量研究聚焦于表层土壤,但针对深层土壤的CO2排放模式及其驱动因素的探索还存在不足。本研究选择原始森林土壤剖面作为研究对象,利用静态箱法对6个不同深度(10 cm、50 cm、100 cm、200cm、300 cm和400 cm)的土壤CO2排放进行了测量,并分析了土壤理化性质、微生物多样性、群落结构和功能的潜在变化,探讨了土壤CO2排放的动态及驱动因子。结果表明,土壤养分以及真菌和细菌多样性总体上随土层加深而递减。土壤CO2排放量也随深度增加显著降低,其主要驱动因素包括真菌和细菌α多样性等生物因子,以及铵态氮和有效磷等非生物因子。这些发现将为揭示森林生态系统深层土壤碳循环机制提供了新的见解。