黔北金佛山方竹林碳储量及其影响因素  

Carbon Storage in Chimonobambusa utilis Forest in North Guizhou Province and Its Influencing Factors

作　　者：张喜 张庭嘉 杨光能 侯贻菊 姜霞 Zhang Xi;Zhang Tingjia;Yang Guangneng;Hou Yiju;Jiang Xia(Guizhou Academy of Forestry,Guiyang 550005,China;Guizhou Institute of Bamboo Industry for New Era,Chishui 564700,Guizhou,China;Research Center of National Forestry and Grassland Administration for Sympodial Bamboo Engineering Technology,Kunming 650224,China;Bamboo Forest Ecosystem National Observation and Research Station,Chishui 564700,Guizhou,China;Key Laboratory of National Forestry and Grassland Administration for Biodiversity Conservation in Southwestern Karst Areas,Guiyang 550005,China)

机构地区：[1]贵州省林业科学研究院,贵阳550005 [2]贵州省新时代竹产业研究院,贵州赤水564700 [3]国家林业和草原局丛生竹工程技术研究中心,昆明650224 [4]贵州赤水竹林生态系统国家定位观测研究站,贵州赤水564700 [5]国家林业和草原局西南喀斯特山地生物多样性保护重点实验室,贵阳550005

出　　处：《世界竹藤通讯》2024年第3期16-25,30,共11页World Bamboo and Rattan

基　　金：贵州省特色林业产业科研项目(特林研2020-02);国家林业部课题(1995-林[中]字-21号)。

摘　　要：竹林碳汇是国际社会关注的热点,其中亚优势层竹林碳汇是观测研究的难点。在黔北大娄山金佛山方竹(以下简称方竹)中心分布区调查了92个样地,其中纯林样地数量占33.70%,分析了纯林及混交林碳储量及组成对方竹林分指标的响应。结果表明:1)纯林及混交林方竹地上部分平均碳储量分别为29.74 t/hm^(2)和30.31 t/hm^(2),地下部分平均碳储量分别为16.07 t/hm^(2)和18.16 t/hm^(2),总碳储量分别为45.81 t/hm^(2)和48.47 t/hm^(2),地下部分碳储量及总碳储量差异显著。不同类型方竹林构件碳储量呈竹秆>鞭根>竹叶>竹枝>竹篼的变化趋势,竹秆碳储量在龄级间比例相近。2)方竹纯林及混交林土壤(土层厚度40 cm)平均碳储量分别为136.36 t/hm^(2)和112.57 t/hm^(2),二者差异极显著,呈土壤B层>A层的变化趋势。土壤碳储量在A层与B层、A层及B层与AB层间相关极显著。3)方竹纯林及混交林灌木地上部分平均碳储量分别为0.01 t/hm^(2)和0.02 t/hm^(2),混交林乔木地上部分及凋落物平均碳储量分别为12.63 t/hm^(2)和2.14 t/hm^(2)。4)在纯林及混交林中,方竹碳储量、灌木地上部分碳储量以及植被层(方竹、乔木和灌木)地上部分碳储量与方竹平均胸径及密度二元线型回归式的相关性极显著,混交林方竹平均胸径及密度与土壤A层、B层及AB层碳储量的二元线型回归模型相关显著。研究为评价方竹林碳储量及影响因素提供了科学依据。Bamboo forest sink is an international concern,among which the sink in subdominant layer is a difficult point in observation and research.In this study,92 plots were investigated in the main distribution area of Chimonobambusa utilis(hereafter referred to as CU)in North Guizhou Province of China,of which pure forest plots accounted for 33.70%.The response of CU stand indexes to the carbon storage in pure CU forest and mixed CU forest as well as to the composition of the storage was analyzed.The results show that:1)The average aboveground carbon storage is 29.74 t/ha and 30.31 t/ha,the underground carbon storage is 16.07 t/ha and 18.16 t/ha,and the total carbon storage is 45.81 t/ha and 48.47 t/ha in the pure CU forests and the mixed CU forests,respectively,and the underground carbon storage and the total carbon storage in the pure CU forests and the mixed CU forest are significantly different.The carbon storage of different components in Ch.utilis forest shows the trend of culms>rhizome>leaves and branches>bamboo basket,and the carbon storage in culms has the similar proportion along different age classes;2)The average soil carbon storage in pure CU forests and mixed CU forests(the total soil thickness at 40 cm)is 136.36 t/ha and 112.57 t/ha,respectively,with significant differences and the change trend of layer B>layer A.Soil carbon storage is significantly associated between layers A and B,A and B and AB;3)The average aboveground carbon storage in pure CU forests and the shrubs in the mixed CU forests is 0.01 t/ha and 0.02 t/ha,respectively,and the average aboveground carbon storage in arbors and litters of the mixed CU forests is 12.63 t/ha and 2.14 t/ha,respectively;and 4)Bamboo carbon storage,shrub aboveground carbon storage,and vegetation aboveground carbon storage(bamboo,trees and shrubs)in the pure CU forests and the CU mixed forests are extremely significantly correlated with the average DBH and the density binary linear regression of the CU forests,and the average DBH and the density of the CU mixed for

关 键 词：金佛山方竹 纯林 混交林 碳储量 贵州北部 

分 类 号：S795[农业科学—林木遗传育种]