期刊文献+

神农架海拔梯度上4种典型森林的土壤呼吸组分及其对温度的敏感性 被引量:41

Components of soil respiration and its temperature sensitivity in four types of forests along an elevational gradient in Shennongjia,China
原文传递
导出
摘要 量化森林土壤呼吸及其组分对温度的响应对准确评估未来气候变化背景下陆地生态系统的碳平衡极其重要。该文通过对神农架海拔梯度上常绿阔叶林、常绿落叶阔叶混交林、落叶阔叶林以及亚高山针叶林4种典型森林土壤呼吸的研究发现:4种森林类型的年平均土壤呼吸速率和年平均异养呼吸速率分别为1.63、1.79、1.74、1.35μmolCO2·m-2·s-1和1.13、1.12、1.12、0.80μmolCO2·m-2·s-1。该地区的土壤呼吸及其组分呈现出明显的季节动态,夏季最高,冬季最低。4种森林类型中,阔叶林的土壤呼吸显著高于针叶林,但阔叶林之间的土壤呼吸差异不显著。土壤温度是影响土壤呼吸及其组分的主要因素,二者呈显著的指数关系;土壤含水量与土壤呼吸之间没有显著的相关关系。4种典型森林土壤呼吸的Q10值分别为2.38、2.68、2.99和4.24,随海拔的升高土壤呼吸对温度的敏感性增强,Q10值随海拔的升高而增加。 Aims Quantifying forest soil respiration(Rs),its components of heterotrophic respiration(RH) and autotrophic respiration(RA),and their responses to temperature are vital to accurately evaluate response of the terrestrial car-bon balance to future climate change.Our specific objectives were to(1) compare patterns of soil respiration of four types of forests,(2) evaluate relationships among soil respiration and temperature and water content and(3) find the regulation of Q10 value in relation to elevation.Methods Four types of forests along an elevational gradient at Shennongjia were investigated.The trenching plot approach was used to partition soil respiration into autotrophic respiration and heterotrophic respiration.Rates of soil respiration were measured twice a month from July 2009 to June 2010.Soil temperature and soil water content were measured at the same time.Important findings Annual soil respiration of the four types of forests was 1.63,1.79,1.74 and 1.35 μmol CO2·m-2·s-1,and annual heterotrophic respiration was 1.13,1.12,1.12,0.80 μmol CO2·m-2·s-1.Soil respiration and its components displayed obvious seasonal dynamics,with maximum values in summer and minimum values in winter.The soil respiration flux of broad-leaved forest was significantly higher than that of coniferous forests,but there was no obvious differentiation between broad-leaved forests.Soil temperature was the main factor that affected soil respiration and its components,and there were significant exponential relationships between them.There was no significant relationship between soil water content and soil respiration flux,except in broad-leaved forest with a mild inhibition phenomenon.Q10 values of four types of forests were 2.38,2.68,2.99 and 4.24.Soil respiration was more sensitive to temperature along the elevation gradient,while Q10 value increased with eleva-tion increase.
出处 《植物生态学报》 CAS CSCD 北大核心 2011年第7期722-730,共9页 Chinese Journal of Plant Ecology
基金 植被与环境变化国家重点实验室项目"成熟林的重要功能过程对环境变化响应联网研究" 国家自然科学基金(30870416) 中国科学院战略性先导科技专项(XDA050203)共同资助
关键词 自养呼吸 异养呼吸 Q10值 土壤含水量 土壤温度 autotrophic respiration(RA) heterotrophic respiration(RH) Q10 value soil water content soil tem-perature
  • 相关文献

参考文献24

  • 1Bhupinderpat S, Nordgren A, L/Sfvenius MO, H6gberg MN, Mellander PE, H/Sgberg P (2003). Tree root and soil het- erotrophic respiration as revealed by girdling of boreal Scots pine forest: extending observations beyond the first year. Plant, Cell & Environment, 26, 1287-1296. 被引量:1
  • 2Wang CK, Bond-Lamberty B, Gower ST (2002). Soil surface CO2 flux in a boreal black spruce fire chronosequence. Journal of Geophysical Research-Atmospheres, 107, 8224, doi: 10.1029/2001JD000861. 被引量:1
  • 3Gaumont-Guay D, Black TA, McCaughey H, Barr AG, Krish- nan P, Jassal RS, Nesic Z (2009). Soil CO2 efflux in con- trasting boreal deciduous and coniferous stands and its contribution to the ecosystem carbon balance. Global Change Biology, 15, 1302-1319. 被引量:1
  • 4Epron D, Le Dantec V, Dufrence E, Granier A (2001). Sea- sonal dynamics of soil carbon dioxide efflux and simu- lated rhizosphere respiration in a beech forest. Tree Physi- ology, 21,145-152. 被引量:1
  • 5Lee NY, Koo JW, Noh JN, Kim J, Son Y (2010). Autotrophic and heterotrophic respiration in needle fir and Quercus- dominated stands in a cool-temperate forest, central Ko- rea. Journal of Plant Research, 123, 485-495. 被引量:1
  • 6Davidson EA, Janssens IA, Luo Y (2006). On the variability of respiration in terrestrial ecosystems: moving beyond Q10. Global Chang Biology, 12, 154-164. 被引量:1
  • 7Zheng ZM, Yu GR, Fu YL, Wang YS, Sun XM, Wang YH (2009). Temperature sensitivity of soil respiration is af- fected by prevailing climatic conditions and soil organic carbon content: a trans-China based study. Soil Biology & Biochemistry, 41, 1531-1540. 被引量:1
  • 8Campbell JL, Law BE (2005). Forest soil respiration across three climatically distinct chronosequences in Oregon. Biogeochemistry, 73, 109-125. 被引量:1
  • 9Landsberg JJ, Gower ST (1997). Applications of Physiological Ecology to Forest Management. Academic Press, San Diego, USA. 被引量:1
  • 10Schlesinger WH (1990). Evidence from chronosequence stud- ies for a low carbon-storage potential of soil. Nature, 348, 232-234. 被引量:1

共引文献372

同被引文献929

引证文献41

二级引证文献372

相关作者

内容加载中请稍等...

相关机构

内容加载中请稍等...

相关主题

内容加载中请稍等...

浏览历史

内容加载中请稍等...
;
使用帮助 返回顶部