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林业科学 ›› 2022, Vol. 58 ›› Issue (2): 49-57.doi: 10.11707/j.1001-7488.20220206

• 前沿与重点: 森林碳汇专题 • 上一篇    下一篇

我国森林土壤微生物生物量碳的纬度分布特征及影响因子

周莎1,马寰菲1,王洁莹1,任成杰2,郭垚鑫3,王俊1,4,*,赵发珠1   

  1. 1. 西北大学城市与环境学院 陕西省地表系统与环境承载力重点实验室 西安 710127
    2. 西北农林科技大学农学院 杨凌 712100
    3. 西北大学生命科学学院 西安 710127
    4. 中国科学院水利部水土保持研究所 杨凌 712100
  • 收稿日期:2021-05-31 出版日期:2022-02-25 发布日期:2022-04-26
  • 通讯作者: 王俊
  • 基金资助:
    中国科学院西部之光"西部引进人才"项目

Latitudinal Distribution of Forest Soil Microbial Biomass Carbon and Its Affecting Factors in China

Sha Zhou1,Huanfei Ma1,Jieying Wang1,Chengjie Ren2,Yaoxin Guo3,Jun Wang1,4,*,Fazhu Zhao1   

  1. 1. Key Laboratory of Surface System and Environmental Carrying Capacity of Shaanxi Province College of Urban and Environmental Sciences, Northwest University Xi'an 710127
    2. College of Agronomy, Northwest Agriculture and Forestry University Yangling 712100
    3. College of Life Science, Northwest University Xi'an 710127
    4. Institute of Soil and Water Conservation, Chinese Academy of Sciences and Ministry of Water Resources Yangling 712100
  • Received:2021-05-31 Online:2022-02-25 Published:2022-04-26
  • Contact: Jun Wang

摘要:

目的: 探讨土壤微生物生物量碳(MBC)含量的纬度变化规律及驱动因子, 以期揭示我国沿纬度分布的森林生态系统中土壤MBC含量变化的效应和机制, 为气候变暖条件下阐明土壤MBC周转和固持提供理论依据。方法: 在我国沿纬度选取10个典型森林生态系统, 测定0~10 cm土层的MBC含量, 并与各非生物因素(气候条件和土壤理化性质指标)进行相关性分析。结果: 森林土壤MBC含量变化范围为(200.57±13.99)~(913.32±39.62) mg·kg-1, 随纬度降低而降低。MBC含量与土壤的有机碳含量(r=0.64, P < 0.01)、砂砾含量(r=0.48, P < 0.01)、水解酶活性(r=0.48, P < 0.01)、全磷含量(r=0.47, P < 0.01)、pH值(r=0.43, P < 0.01)、全氮含量(r=0.31, P < 0.01)和土壤有机碳化学结构组分中烷基碳含量(r=0.21, P < 0.01)极显著正相关, 与土壤粉粒含量(r=0.15, P < 0.05)和氧化酶活性(r=0.15, P < 0.05)显著正相关; 还与年均气温(MAT, r=0.31, P < 0.01)极显著正相关。结论: 森林土壤的MBC含量随纬度降低而降低, 主要影响因素为土壤质地、土壤营养、土壤酶活性和土壤烷基碳含量, 其次为年均气温。

关键词: 森林土壤, 微生物生物量碳, 纬度梯度, 土壤理化性质, 气候条件, 烷基碳

Abstract:

Objective: The study aims to investigate the patterns of latitudinal variation of soil microbial biomass carbon (MBC) and its driving forces, further to reveal the effect and mechanism of soil MBC content across forest ecosystems along the latitudinal gradients in China, providing a theoretical basis for understanding forest soil carbon turnover and sequestration in the context of global warming. Method: Ten typical forest ecosystems along the latitude gradients in China were selected to measure soil microbial biomass carbon (MBC) contents at 0-10 cm soil layer, and the correlation between MBC and abiotic factors (climate factors, soil physical and chemical properties) were conducted. Result: The MBC content of the forest soil decreased with decreasing latitude, ranging from (200.57 ± 13.99) mg·kg-1 to (913.32 ± 39.62) mg·kg-1. The soil MBC content and soil physical and chemical properties were positively correlated (r=0.51, P < 0.01). Highly significant positive correlation with the soil MBC content were identified in soil organic carbon content (r=0.64, P < 0.01), soil sand content (r=0.48, P < 0.01), soil hydrolase activity (r=0.48, P < 0.01), soil total phosphorus content (r=0.47, P < 0.01), pH value (r=0.43, P < 0.01) and soil total nitrogen content (r=0.31, P < 0.01). While silt content (r=0.15, P < 0.05) and soil oxidase activity (r=0.15, P < 0.05) were significantly positively correlated with MBC content. Both the mean annual temperature (r=0.31, P < 0.01), and the alkyl carbon content (r=0.21, P < 0.01) in the chemical structure of soil organic carbon were highly positively correlated with MBC content. Conclusion: Our results demonstrated a prominent decrease of MBC content along the latitude, with the main affecting factors being soil texture, soil nutrient, soil enzyme activities, and soil alkyl carbon content, followed by mean annual temperature.

Key words: forest soil, microbial biomass carbon, latitudinal gradient, soil physicochemical properties, climate factors, alkyl carbon

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