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林业科学 ›› 2014, Vol. 50 ›› Issue (11): 182-187.doi: 10.11707/j.1001-7488.20141124

• 研究简报 • 上一篇    下一篇

三峡库区兰陵溪小流域3种林分类型土壤呼吸特征

韩海燕1, 张涛2, 王鹏程3, 雷静品4, 曾立雄5, 黄志霖5, 肖文发5   

  1. 1. 中国林业科学研究院荒漠化研究所 北京 100091;
    2. 恩施自治州林业调查规划设计院 恩施 445000;
    3. 华中农业大学园艺林学学院 武汉 430070;
    4. 中国林业科学研究院林业研究所 北京 100091;
    5. 中国林业科学研究院森林生态环境与保护研究所 北京 100091
  • 收稿日期:2013-07-13 修回日期:2014-09-22 出版日期:2014-11-25 发布日期:2014-12-04
  • 通讯作者: 王鹏程
  • 基金资助:

    国家"十二五"科技支撑项目"长江流域防护林体系整体优化及调控技术研究"(2011BAD38B04);林业公益性行业科研专项"典型森林土壤碳储量分布格局及变化规律研究"(201104008).

Characteristics of Soil Respiration in Three Types of Stands in Lanlingxi Small Watershed in Three Gorges Reservoir Area

Han Haiyan1, Zhang Tao2, Wang Pengcheng3, Lei Jingpin4, Zeng Lixiong5, Huang Zhilin5, Xiao Wenfa5   

  1. 1. Institute of Desertification Studies, CAF Beijing 100091;
    2. Institute of Forestry Survey and Design of Enshi Enshi 445000;
    3. College of Horticulture and Forestry, Huazhong Agricultural University Wuhan 430070;
    4. Research Institute of Foresty, CAF Beijing 100091;
    5. Research Institute of Forest Environment and Protection, CAF Beijing 100091
  • Received:2013-07-13 Revised:2014-09-22 Online:2014-11-25 Published:2014-12-04

关键词: 土壤呼吸, 根呼吸, 凋落物分解, 土壤有机质分解, 温度敏感性

Abstract:

In this study, the trenching method and infrared gas exchange analyzer were used to research the characteristics of soil respiration in 3 different types of stands including coniferous forest, broad-leaved forest and conifer-broadleaved forest in Lanlingxi small watershed in Three Gorges Reservoir Area of China. The results indicated that the annual total soil respiration (Rtotal), root respiration (Rroot), aboveground litter decomposition (Rlitter) and soil organic matter (SOM) decomposition (RSOM) of coniferous forest were 1.61, 0.47, 0.38, 0.76 μmol·m-2 s-1, respectively. The annual Rtotal,Rroot,Rlitter and RSOM were 1.47,0.35,0.16,0.96 μmol·m-2 s-1 for broad-leaved forest and 2.04,0.76,0.48,0.80 μmol·m-2 s-1 for conifer-broadleaved forest, respectively. The respiration rates of soil and its components displayed obvious seasonal dynamics with maximum rate in summer and minimum rate in winter. Soil temperature was the main factor that affected soil and its components respiration rates, and there were significant positive exponential relationships between them (P<0.05). The annual Q10 of Rtotal,Rroot,Rlitter and RSOM were 2.01,1.52,2.73 and 3.03 for coniferous forest,2.51,1.42,3.46,3.08 for broad-leaved forest and 1.86,1.14,3.00,2.32 for conifer-broadleaved forest, respectively. These results suggested that the annual Q10 value of Rroot in the three types of stands was significantly lower than that of the total soil respiration and its other components respiration (P<0.05).

Key words: soil respiration, root respiration, litter decomposition, soil organic matter decomposition, temperature sensitivity

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