林业科学
林業科學
임업과학
SCIENTIA SILVAE SINICAE
2014年
11期
182-187
,共6页
韩海燕%张涛%王鹏程%雷静品%曾立雄%黄志霖%肖文发
韓海燕%張濤%王鵬程%雷靜品%曾立雄%黃誌霖%肖文髮
한해연%장도%왕붕정%뢰정품%증립웅%황지림%초문발
土壤呼吸%根呼吸%凋落物分解%土壤有机质分解%温度敏感性
土壤呼吸%根呼吸%凋落物分解%土壤有機質分解%溫度敏感性
토양호흡%근호흡%조락물분해%토양유궤질분해%온도민감성
soil respiration%root respiration%litter decomposition%soil organic matter decomposition%temperature sensitivity
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 ( R total ) ,root respiration ( R root ) ,aboveground litter decomposition ( R lit er ) 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,Rliter andRSOMwere 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 Q10of Rtotal,Rroot,Rliter and RSOMwere 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 ) .