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应用生态学报 ›› 2010, Vol. 21 ›› Issue (05): 1097-1104.

• 第六届全国景观生态学学术研讨会会议专栏 • 上一篇    下一篇

长白山阔叶红松林退化生态系统的土壤呼吸作用

梁 宇1,2,3;许嘉巍1**;胡远满2;常 禹2;布仁仓2   

  1. 1东北师范大学城市与环境科学学院,长春 130024;2中国科学院沈阳应用生态研究所,沈阳 110016;3中国科学院研究生院,北京 100049
  • 出版日期:2010-05-20 发布日期:2010-05-20

Soil respiration of degraded Korean pine forest ecosystem in Changbai Mountains.

LIANG Yu1,2,3;XU Jia-wei1;HU Yuan-man2;CHANG Yu2;BU Ren-cang2   

  1. 1College of Urban and Environmental Sciences, Northeast Normal University, Changchun 130024, China;2Institute of Applied Ecology, Chinese Academy of Sciences, Shenyang 110016, China;3Graduate University of Chinese Academy of Sciences, Beijing 100049, China
  • Online:2010-05-20 Published:2010-05-20

摘要: 选择处于全球变化中国东北样带东部典型生态系统的长白山阔叶红松林作为研究区,采用动态气室-CO2红外分析法测定了森林生态系统不同退化阶段的土壤呼吸作用.结果表明:在生长季,长白山阔叶红松林不同退化阶段的土壤呼吸动态变化呈单峰型曲线,在7—8月达到最大值;不同退化阶段林地土壤呼吸大小顺序为:杨桦林>蒙古栎林>阔叶红松林>硬阔叶林>裸地.其中,杨桦林和蒙古栎林样地的碳释放量分别为对照阔叶红松林的1.4和1.3倍,硬阔叶林和裸地的碳释放量分别为对照阔叶红松林的88%和78%.

关键词: 长白山, 阔叶红松林, 退化生态系统, 土壤呼吸, 生物炭, 塿土, 土壤水热特性, 土壤团聚体, 平均质量直径

Abstract: Taking the broad-leaved Korean pine forest area in Changbai Mountains, a typical eastern forest belt of Northeast China for global change as test object, and by using the approaches of trenching-plot and infrared gas exchange analyzer, this paper analyzed the soil respiration in a selected series of degraded Korean pine forest ecosystem, i.e., broad-leaved Korean pine forest (CK), poplarbirch forest (Y), hardwood forest (S), Mongolian oak forest (M), and bare land (L). In the growth season of the forests, soil respiration showed a clear single peak curve, with the maximum in July or August. The soil respiration decreased in the sequence of Y>M>CK>S>L. The amount of CO2 release in Y and M was about 0.4 and 0.3 times higher than that in CK; and that in S and L accounted for 88% and 78% of CK, respectively.

Key words: Changbai Mountains, broad-leaved Korean pine forest, degraded forest ecosystem, soil respiration, biochar, Lou soil, soil water thermal properties, soil aggregate, mean weight diameters.