CAJ | 학술논문

研究我国亚热带地区杉木人工林采伐迹地上营造的19年生米老排人工林和杉木人工林土壤呼吸及其影响因子。结果表明：米老排人工林土壤呼吸速率的年均值为2.95μmolCO2·m -2 s -1，显著高于杉木人工林的2.37μmolCO2·m -2 s -1；米老排人工林土壤呼吸的 Q10值为1.83，显著低于杉木人工林的1.99；2种林分土壤呼吸均呈现明显的季节动态，主要受土壤温度的驱动，土壤温度能分别解释米老排和杉木人工林土壤呼吸速率变化的77.0%和81.6%；回归分析显示，2种林分土壤呼吸速率与凋落物量、细根生物量、土壤有机碳含量、轻组有机碳含量、微生物生物量碳含量和可溶性有机碳含量均显著相关；逐步线性回归分析表明，土壤呼吸速率与凋落物量和土壤微生物生物量碳含量的关系最密切；树种间凋落物量和土壤微生物生物量的差异是导致米老排人工林土壤碳排放速率高于杉木人工林的重要原因。
연구아국아열대지구삼목인공림채벌적지상영조적19년생미로배인공림화삼목인공림토양호흡급기영향인자。결과표명：미로배인공림토양호흡속솔적년균치위2.95μmolCO2·m -2 s -1，현저고우삼목인공림적2.37μmolCO2·m -2 s -1；미로배인공림토양호흡적 Q10치위1.83，현저저우삼목인공림적1.99；2충림분토양호흡균정현명현적계절동태，주요수토양온도적구동，토양온도능분별해석미로배화삼목인공림토양호흡속솔변화적77.0%화81.6%；회귀분석현시，2충림분토양호흡속솔여조락물량、세근생물량、토양유궤탄함량、경조유궤탄함량、미생물생물량탄함량화가용성유궤탄함량균현저상관；축보선성회귀분석표명，토양호흡속솔여조락물량화토양미생물생물량탄함량적관계최밀절；수충간조락물량화토양미생물생물량적차이시도치미로배인공림토양탄배방속솔고우삼목인공림적중요원인。
We investigated monthly soil respiration (Rs) and the affecting factors under 19-year-old Mytilaria laosensis and Cunninghamia lanceolata plantations replanted in a C. lanceolata woodland slash in subtropical China. The results showed that the average annual Rs rates were 2.95 μmolCO2 ·m -2 s -1 under M. laosensis plantations and 2. 37 μmolCO2 · m -2 s -1 under C. lanceolata plantations. The Q10 value was 1. 83 under M. laosensis plantations,which was significantly lower than 1. 99 under C. lanceolata plantations. The Rs rates exhibited distinct seasonal patterns under both M. laosensis plantations and C. lanceolata plantations and were dominantly controlled by the soil temperature,accounting for 77. 0%and 81. 6% of monthly variation,respectively. Linear regression analysis showed that Rs was significantly correlated with annual litter biomass,fine root biomass,soil organic carbon content,light fraction organic carbon content,microbial biomass carbon concentration and dissolved organic carbon concentration ( P<0 . 05 ) . Stepwise regression analysis showed that litter biomass and microbial biomass carbon concentration were the most important affecting factors of Rs. Our results suggest that differences of Rs in different vegetation types may be attributed to the variations in the quantity and quality of litter input and the soil microbial biomass.