Soil respiration in tropical seasonal rain forest in Xishuangbanna, SW China

作     者：SHA Liqing, ZHENG Zheng, TANG Jianwei, WANG Yinghong, ZHANG Yiping, CAO Min, WANG Rui, LIU Guangren, WANG Yuesi & SUN Yang Xishuangbanna Tropical Botanical Garden, Chinese Academy of Sciences, Kunming 650223, China Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China Graduate School of Chinese Academy of Sciences, Beijing 100039, China 

作者机构：Xishuangbanna Tropical Botanical Garden Chinese Academy of Sciences Kunming 650223 China Graduate School of Chinese Academy of Sciences Beijing 100039 China Xishuangbanna Tropical Botanical Garden Chinese Academy of Sciences Kunming 650223 China Institute of Atmospheric Physics Chinese Academy of Sciences Beijing 100029 China 

出 版 物：《Science China Earth Sciences》 (中国科学（地球科学英文版）)

年 卷 期：2005年第48卷第Z1期

页      面：189-197页

学科分类：09[农学] 0903[农学-农业资源与环境] 090301[农学-土壤学] 

基　　金：This work was supported by the Knowledge Innovation Program of the Chinese Academy of Sciences(Grant No.KZCX1-SW-01) the Basic Science Development Program of China(Grant No.2002CB412501) the National Natural Science Foundation of China(Grant No.40173039) 

主　　题：seasonal rain forest, soil respiration, CO2 efflux, Q10, Xishuangbanna. 

摘      要：With the static opaque chamber and gas chromatography technique, from January 2003 to January 2004 soil respiration was investigated in a tropical seasonal rain forest in Xishuangbanna, SW China. In this study three treatments were applied, each with three replicates: A (bare soil), B (soil+litter), and C (soil+litter+seedling). The results showed that soil respiration varied seasonally, low from December 2003 to February 2004, and high from June to July 2004. The annual average values of CO2 efflux from soil respiration differed among the treatments at 1 % level, with the rank of C (14642 mgCO2 · m-2 · h-1)B (12807 mgCO2 · m-2 · h-1) A (9532 mgCO2·m-2 · h-1). Diurnal variation in soil respiration was not apparent due to little diurnal temperate change in Xishuangbanna. There was a parabola relationship between soil respiration and soil moisture at 1% level. Soil respiration rates were higher when soil moisture ranged from 35% to 45%. There was an exponential relationship between soil respiration and soil temperature (at a depth of 5cm in mineral soil) at 1% level. The calculated Q10 values in this study, ranging from 2.03 to 2.36, were very near to those of tropical soil reported. The CO2 efflux in 2003 was 5.34 kgCO2 · m-2 · a-1 from soil plus litter plus seedling, of them 3.48 kgCO2 · m-2 · a-1 from soil (accounting for 62.5%), 1.19 kgCO2 · m-2 · a-1 from litter (22.3%) and 0.67 kgCO2 · m-2 · a-1 from seedling (12.5%).