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生态学杂志 ›› 2021, Vol. 40 ›› Issue (11): 3531-3542.doi: 10.13292/j.1000-4890.202110.019

• 研究报告 • 上一篇    下一篇

文山自然保护区典型植被土壤碳氮储量变化特征

李聪1,吕晶花1,陆梅1*,杨志东1,刘攀1,任玉连3,杜凡2   

  1. 1西南林业大学生态与环境学院, 昆明 650224;2西南林业大学林学院, 昆明 650224; 3贵州大学生命科学学院, 贵阳 550025)
  • 出版日期:2021-11-10 发布日期:2022-05-10

Variation of soil carbon and nitrogen storage under typical vegetations in Wenshan Nature Reserve.

LI Cong1, LYU Jing-hua1, LU Mei1*, YANG Zhi-dong1, LIU Pan1, REN Yu-lian3, DU Fan2   

  1. (1College of Ecology and Environment, Southwest Forestry University, Kunming 650224, China; 2College of Forestry, Southwest Forestry University, Kunming 650224, China; 3College of Life Sciences, Guizhou University, Guiyang 550025, China).
  • Online:2021-11-10 Published:2022-05-10

摘要: 探究文山自然保护区土壤有机碳和全氮储量沿海拔的变化特征及其与环境因子的耦合关系,为评估保护区植被碳氮固定潜力提供数据支撑。选取保护区沿海拔分布的3种典型植被类型为对象,研究土壤有机碳和全氮储量沿海拔和土层的分布规律,并采用主成分降维分析方法探讨环境因子(微气候、植被与土壤)沿海拔变化对土壤碳氮储量的影响。结果表明:不同植被类型土壤碳氮储量沿海拔升高呈显著增加趋势(P<0.05),最大值出现在高海拔中山湿性常绿阔叶林,相较于低海拔亚热带季风常绿阔叶林,其增幅分别达82.81%和80.98%。土壤碳氮储量随土层加深呈显著减小趋势(P<0.05),相较于0~10 cm土层,40~50 cm土层的降幅分别为54.82%和55.38%;凋落物厚度、Simpson指数、土壤总孔隙度、毛管孔隙度、含水量、全钾沿海拔上升呈增加趋势,全磷则先减后增;相较于低海拔亚热带季风常绿阔叶林,上述指标在高海拔中山湿性常绿阔叶林的增幅为53.29%~666.67%;而Margalef指数、Shannon指数、Pielou指数、土壤非毛管孔隙度、土壤容重、温度、pH、机械组成沿海拔梯度呈减小趋势,这些指标在高海拔中山湿性常绿阔叶林的降幅为15.97%~59.71%;环境因子沿海拔的变化对碳氮储量具有极显著的共线性影响(P<0.05),凋落物厚度、年均降水量、土壤总孔隙度、毛管孔隙度、含水量、全钾沿海拔的增加对碳氮储量存在极显著的正效应(P<0.01),植物多样性沿海拔的减小对碳氮储量存在显著的正效应(P<0.01)。综上,文山保护区土壤碳氮储量沿海拔升高呈现显著增加趋势,其中,微气候、土壤理化性质、凋落物厚度沿海拔的垂直分布是调控碳氮储量的关键因子。

关键词: 植被, 海拔, 土壤有机碳储量, 土壤氮储量, 环境因子

Abstract: We explored the changes of soil organic carbon (C) and total nitrogen (N) storage along an altitudinal gradient and its coupling relationship with environmental factors in Wenshan Nature Reserve, to provide basic data for estimating ecosystem C and N fixation potential. Three typical vegetation types along an altitude gradient were selected to examine the distribution of C and N storage along the altitude gradient and soil profile. The principal component reduction analysis was used to explore the impacts of environmental factors (microclimate, vegetation, and soil) on C and N storage along the altitude gradient. The results showed that soil carbon and nitrogen storage of different vegetation types showed a significant increase along the altitude (P<0.05). The storage of C and N peaked in middle-montane humid evergreen broad-leaved forest of high altitude, which increased by 82.81% and 80.98% compared with monsoon evergreen broad-leaved forest in the low altitude. Soil C and N storage decreased with the deepening of soil layers (P<0.05). Compared with 0-10 cm layer, C and N storage in 40-50 cm layer decreased by 54.82% and 55.38%, respectively. Litter  thickness, Simpson index, soil total porosity, capillary porosity, moisture content, and total potassium increased along the altitude, while total phosphorus decreased first and then increased. The values of the above-mentioned variables were 53.29%-666.67% higher in middle-montane humid evergreen broad-leaved forest of higher altitude than that in the monsoon evergreen broad-leaved forest of low altitude. The Margalef index, Shannon index, Pielou index, soil non-capillary porosity, bulk density, temperature, pH and mechanical composition decreased along the altitude, the values of which were 15.97%-59.71% lower in the middle-montane humid evergreen broad-leaved forest of high altitude than in the monsoon evergreen broad-leaved forest of low altitude. Changes of environmental factors along the altitude significantly affected C and N storage (P<0.05). The increases of litter amount, annual precipitation, soil total porosity, capillary porosity, moisture content and total potassium along altitudes had a significant positive effect on C and N storage, while the decreases of plant diversity along the altitude had an extremely significant positive effect on C and N storage. In conclusion, soil C and N storage increased along the altitude in Wenshan Nature Reserve. The vertical distributions of microclimate, soil physicochemical properties and litter  thickness along the altitude are the key factors controlling C and N storage.

Key words: vegetation, altitude, soil organic carbon storage, soil total nitrogen storage, environmental factor.