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鼎湖山针阔叶混交林土壤COS和CO_2通量研究
引用本文:易志刚,王新明,张德强,盛国英,傅家谟.鼎湖山针阔叶混交林土壤COS和CO_2通量研究[J].地球与环境,2009,37(3).
作者姓名:易志刚  王新明  张德强  盛国英  傅家谟
作者单位:1. 福建农林大学资源与环境学院,福州,350002;中国科学院广州地球化学研究所有机地球化学国家重点实验室,广州,510640
2. 中国科学院广州地球化学研究所有机地球化学国家重点实验室,广州,510640
3. 中国科学院华南植物园,广州,510650
基金项目:福建省科技计划资助省属高校项目(2008F5013);;国家重点基础研究发展计划(973)课题(2002CB410803)
摘    要:运用静态箱-预浓缩-气相色谱-质谱法和静态箱-色谱法分别测量了南亚热带鼎湖山针阔叶混交林土壤-大气COS和CO2通量。结果表明,土壤吸收COS,凋落物保留样地COS吸收速率显著高于凋落物去除样地,3月土壤COS吸收速率最高。土壤COS吸收速率与大气COS浓度正相关。土壤COS吸收速率与土壤温度、土壤含水量单独未表现出显著相关性,但凋落物保留样地COS吸收速率与土壤温度和含水量两者共同呈二次多项式相关。凋落物保留样地CO2释放速率高于凋落物去除样地。与土壤COS吸收速率相反,土壤CO2释放速率3月最低,7月最高,主要受温度和土壤含水量的影响。土壤CO2释放速率与土壤温度呈指数相关,与土壤含水量直线相关,多元回归分析表明,土壤CO2释放受温度和含水量的共同影响。土壤COS吸收速率随土壤CO2释放速率的增加而增加,表明两者可能受某些共同因素的影响。

关 键 词:鼎湖山  土壤  羰基硫  二氧化碳  通量

COS and CO2 Fluxes Between Soil and Atmosphere in a Coniferous and Broad-leaved Mixed Forest in Dinghushan, China
YI Zhi-gang,WANG Xin-ming,ZHANG De-qiang,SHENG Guo-ying,FU Jia-mo.COS and CO2 Fluxes Between Soil and Atmosphere in a Coniferous and Broad-leaved Mixed Forest in Dinghushan, China[J].Earth and Environment,2009,37(3).
Authors:YI Zhi-gang  WANG Xin-ming  ZHANG De-qiang  SHENG Guo-ying  FU Jia-mo
Affiliation:1.College of Resources and Environment;Fujian Agriculture and Forestry University;Fuzhou 350002;China;2.State Key Laboratory of Organic Geochemistry;Guangzhou Institute of Geochemistry;Chinese Academy of Sciences;Guangzhou 510640;3.South China Botanical Garden;Guangzhou 510650;China
Abstract:Static chamber-preconcentrator-GC-MS and static chamber-GC techniques were applied respectively to measure COS and CO2 flux between soil and atmosphere in a coniferous and broad-leaved mixed forest in Dinghushan Biosphere Reserve in Guangdong province,low-subtropics China.The results showed that soil acted as sink for COS,and COS uptake rates at plots with litter were significantly higher than those without litter.The highest rates were found in March.COS uptake rates were influenced mainly by ambient COS c...
Keywords:Dinghushan  Soil  Carbonyl sulfide(COS)  Carbon dioxide(CO2)  Flux
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