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    重庆缙云山 4 种典型林分生长季土壤呼吸特征及其与环境因子的关系

    Soil respiration characteristics and its relationship with environmental factors of four typical forests in Jinyun Mountain, Chongqing

    • 摘要: 2012 年 4—8 月,采用 LI-8100 开路式土壤碳通量测量系统对重庆缙云山 4 种典型林分( 常绿阔叶林、竹林、 针阔混交林和针叶林)的土壤呼吸速率进行测定,并同步测定 5 和 10 cm 土壤温度、湿度及 pH 值,分析 4 种林分土壤呼吸变化特征及其与环境因子的关系。 结果表明:1)4 种典型林分土壤呼吸日变化规律不同,5 月、7 月针阔混交林和针叶林土壤呼吸速率日波动幅度大于常绿阔叶林和竹林;2)各林分土壤呼吸速率均表现出 4—7 月升高而 7— 8 月降低的月变化规律;3)土壤呼吸速率与 5 cm、10 cm 土壤温度均呈指数关系,常绿阔叶林的温度敏感性(5 cm Q10 =2.054,10cmQ10 =2.117)大于其他3种林分;4)常绿阔叶林土壤呼吸速率与土壤湿度无显著相关性,而对其他林分呈二次相关关系;5)常绿阔叶林的土壤呼吸与 5 cm、10 cm 土壤 pH 值显著相关,竹林的土壤呼吸仅与 5 cm 土壤 pH 值显著相关,其他林分未表现出显著相关关系。

       

      Abstract: Soil respiration rates of four typical forest types including evergreen broadleaf forest, bamboo forest, mixed forest and coniferous forest were observed by LI-8100 soil carbon flux measurement system in Jinyun Mountain Nature Reserve of Chongqing during the growing season in 2012 (April to August). Meanwhile, soil temperature and soil moisture, soil pH at 5 and 10 cm depth were measured. Temporal variation of soil respiration rate of the four typical forests and the related environmental factors were analyzed. Results showed that: 1) Diurnal soil respiration rate of four typical forest types were different, the ranges of diurnal soil respiration rate for the mixed forest and coniferous forest in May and July were higher than that of evergreen broadleaf forest and bamboo forest. 2) The monthly soil respiration rate changed regularly, increasing from April to July and decreasing from July to August. 3)At 5 cm and 10 cm soil depth, soil respiration rate had an exponential relationship with soil temperature, and temperature sensibility of evergreen broadleaf forest (5 cm Q10 = 2.054, 10 cm Q10 = 2.117) was higher than others. 4) There was no significant correlation between soil respiration rate and soil moisture in the evergreen broadleaf forest, and the other three types of forests showed a quadratic relationship. 5) For the evergreen broadleaf forest, soil respiration rate and pH showed a significant correlation at 5 cm and 10 cm depth, and bamboo forest only presented a significant correlation at 5 cm depth. There was no significant correlation in the other two types of forests.

       

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