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林业科学 ›› 2008, Vol. 44 ›› Issue (9): 142-145.doi: 10.11707/j.1001-7488.20080925

• 论文 • 上一篇    下一篇

寒温带兴安落叶松林土壤呼吸特征

张慧东1,2 周梅1 赵鹏武1 包青春1 海龙1   

  1. 1.内蒙古农业大学,呼和浩特010019;2.辽宁省林业科学研究院沈阳110032
  • 收稿日期:2007-01-26 修回日期:1900-01-01 出版日期:2008-09-25 发布日期:2008-09-25
  • 通讯作者: 周梅

Soil Respiration of Larix gmelinii Forest in Cool Temperate Zone

Zhang Huidong1,2,Zhou Mei1,Zhao Pengwu1,Bao Qingchun1,Hai Long1   

  1. 1.Inner Mongolia Agricultural University Huhhot 010019;2.Liaoning Academy of Forest Science Shenyang 110032
  • Received:2007-01-26 Revised:1900-01-01 Online:2008-09-25 Published:2008-09-25

关键词: 土壤呼吸, 土壤温度, 兴安落叶松林, 大兴安岭

Abstract: The soil respiration rate was measured with an IRGA in the natural Larix gmelinii forest of the Northern Great Xing'anling Mountain in the cool temperate zone.The environmental factors were recorded using the weather equipment.The soil respiration showed obvious diurnal variation and a total 706 gC·m-2 was released during the plant growth period(May.1th~Oct.31th).The soil respiration rate was influenced significantly by soil tempeture in this zone,and a significant postive correlation was found between soil respiration rates and soil tempetures in 10 cm depth(r=0.879 5).However the soil respiration was not significantly influenced by the soil moisture.Furthmore,there was a negative relationship between the soil respiration rate and air CO2 contiontration of the air in forest(r=-0.426 1).The results from the experiment can provide the basical materials for the calculation of carbon flux in the northern cool temperate zone of China.

Key words: soil respiration rate, soil temperature, Larix gmelinii forest, the Great Xing'anling Mountain