Seasonal changes in the contribution of root respiration to total soil respiration in a cool-temperate deciduous forest

被引:273
作者
Lee, MS
Nakane, K
Nakatsubo, T
Koizumi, H
机构
[1] Hiroshima Univ, Grad Sch Biosphere Sci, Dept Environm Studies, Higashihiroshima 7398521, Japan
[2] Hiroshima Univ, Grad Sch Biosphere Sci, Dept Environm Dynam & Management, Hiroshima 730, Japan
[3] Gifu Univ, River Basin Res Ctr, Gifu 5011193, Japan
关键词
carbon; cool-temperature deciduous forest; decomposition rate; root respiration; soil respiration; soil temperature;
D O I
10.1023/A:1026192607512
中图分类号
S3 [农学(农艺学)];
学科分类号
0901 ;
摘要
A trenching method was used to determine the contribution of root respiration to soil respiration. Soil respiration rates in a trenched plot (R-trench) and in a control plot (R-control) were measured from May 2000 to September 2001 by using an open-flow gas exchange system with an infrared gas analyser. The decomposition rate of dead roots (R-D) was estimated by using a root-bag method to correct the soil respiration measured from the trenched plots for the additional decaying root biomass. The soil respiration rates in the control plot increased from May (240-320 mg CO2 m(-2) h(-1)) to August (840-1150 mg CO2 m(-2) h(-1)) and then decreased during autumn (200-650 mg CO2 m(-2) h(-1)). The soil respiration rates in the trenched plot showed a similar pattern of seasonal change, but the rates were lower than in the control plot except during the 2 months following the trenching. Root respiration rate (R-r) and heterotrophic respiration rate (R-h) were estimated from R-control, R-trench, and R-D. We estimated that the contribution of R-r to total soil respiration in the growing season ranged from 27 to 71%. There was a significant relationship between R-h and soil temperature, whereas R-r had no significant correlation with soil temperature. The results suggest that the factors controlling the seasonal change of respiration differ between the two components of soil respiration, R-r and R-h.
引用
收藏
页码:311 / 318
页数:8
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