江西中南部红壤丘陵区主要造林树种碳固定估算  

Carbon fixation estimation for the main plantation forest species in the red soil hilly region of southern-central Jiangxi Province,China

作　　者：吴丹[1,2] 邵全琴[1] 李佳[2,3] 刘纪远[1] 

机构地区：[1]中国科学院地理科学与资源研究所,北京100101 [2]中国科学院研究生院,北京100049 [3]中国科学院新疆生态与地理研究所,乌鲁木齐830011

出　　处：《生态学报》2012年第1期142-150,共9页Acta Ecologica Sinica

基　　金：国家自然科学基金项目(40971281);国家973计划项目(2009CB421100;2010CB950900);国家科技支撑计划项目(2006BAC08B00)

摘　　要：根据江西第6次森林清查小班数据,运用基于实地样方数据拟合的森林植被生物量与蓄积量的关系,并采用空间替代时间的方法,估算了1985—2003年江西中南部红壤丘陵区泰和和兴国县主要造林树种马尾松、湿地松、杉木林的生物量和碳储量,分析了时空动态特征。结果表明:(1)2003年研究区主要造林树种林分面积31.04×104 hm2,总生物量22.20 Tg,植被碳储量13.07T gC,平均碳密度42.36 tC/hm2。(2)1985—2003年研究区主要造林树种碳密度呈逐年上升趋势,增加了8.58 tC/hm2;1985、1994、2003年3个树种植被碳储量分别为4.91、11.41和13.07TgC,年均固碳量0.45 TgC/a。(3)海拔位于700—900 m之间的树种平均碳密度最大,坡度位于25—35°之间的树种平均碳密度最大。森林植被碳密度总体呈现随海拔高度的增加而增加,随坡度的增大而增大的分布。人工造林工程使江西红壤丘陵区森林植被碳储量增加显著,森林生态系统的固碳能力明显增强。Using field survey data from the sixth inventory of forest in Jiangxi Province and calculating the relationship between forest biomass and carbon storage from this,we estimated total forest biomass and carbon storage for the three major plantation forest species,Pinus massoniana,Cunninghamia lanceolata,and Pinus elliottii,in the red soil hilly region of southern-central Jiangxi Province.We also analyzed the relationship between carbon density and age for these forest species,using logistic equations,and described the spatiotemporal dynamics of forest biomass and carbon storage between 1985 and 2003 in the study area. In this study,we used three methods of biomass expansion factor,biomass organ distribution and parameter fitting,to estimate carbon density.Qianyanzhou Experimental Station was chosen to compare these three corresponding results.The result obtained from parameter fitting was found to be the best way of calculating forest biomass and carbon storage on a regional scale.Increasing sample size would increase reliability of results. The following conclusions were obtained from this study.In 2003,total stand area of the three forest species was 31.04×104 hm2;total biomass was 22.20 Tg;vegetation carbon storage was 13.07 Tg C;and average carbon density was 42.36 t C/hm2.Carbon storage by different forest types in descending order was： Pinus massoniana,Pinus elliottii and Cunninghamia lanceolata.Carbon storage by age group in descending order was middle stand forests,young stand forests,near-mature stand forests,mature stand forests.Storage of carbon by plantation forests was 1.89 times higher than by natural forests.Pinus massoniana and Cunninghamia lanceolata forests were the main natural forest carbon sinks,while Pinus elliottii forests were the main plantation carbon sinks.Carbon density of the three species increased each year and increased 8.58 tC / hm2 during the study period;this was 1.66 times higher than in 1985.Forest carbon storage was 4.91,11.41,and 13.07 Tg C in 1985,1994,and 2003,respective

关 键 词：小班数据 碳储量 时空变化 江西省 

分 类 号：S718.5[农业科学—林学]