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作 者:齐光[1] 佟伟霜[1] 彭舜磊[1] 陈昌东[1] 杨雨华[1] 梁亚红[1] 赵干卿[1] 杨风岭[1]
机构地区:[1]平顶山学院低山丘陵区生态修复重点实验室,河南平顶山467099
出 处:《平顶山学院学报》2015年第2期90-95,共6页Journal of Pingdingshan University
基 金:河南省科技厅科技计划(142106000090);河南省教育厅科学技术研究重点项目(12B180024);河南省科技厅攻关项目(092102110165);平顶山学院高层次人才科研启动经费(2011009/G)
摘 要:森林是陆地最大的碳库,主要包括植被碳库和土壤碳库两部分.地带性森林植被与土壤碳贮量核算及其分配格局成为全球变化背景下的研究热点.采用样地调查法,对河南省宝天曼不同海拔高度的3种典型栎类林植被与土壤碳贮量及其分配格局进行了对比研究.结果表明3种林型地上和地下植被碳贮量都随海拔升高而降低,但是地上/地下植被碳贮量比率却随海拔升高而增加.0~10 cm、10~20 cm和20~30 cm土壤有机碳(SOC)贮量都随海拔升高表现出先升高后降低的趋势,该波动主要由底层土引起.森林总碳贮量并没有随海拔变化而表现出显著差异(p〉0.05),由此推断植被和土壤碳贮量间存在着补偿效应.Forests incorporating biomass and soil organic carbon(SOC) storage maintain most of the continent carbon(C). Therefore studies on estimation and distribution of both biomass C and SOC in the local forests become hot issues under the background of global change. Based on the data from sampling plots setted up in three typical oak forests located at different altitude levels of Baotianman,we compare the distribution patterns of biomass C and SOC storage of these oak forests. Our results show that both above-and below-ground biomass C storage increase as altitudes increase,whereas the ratios of above-to below-ground C storages decrease simultaneously. SOC storage in 0 ~ 10,10 ~ 20 and 20 ~ 30 cm depth soil layers show an unimodal curve as altitude increases,SOC storage increases initially but decreases as altitude continues to increase. This trend is mainly caused by SOC of the bottom layers. It is interesting that total C storage of three oak forests does not vary significantly(p 0. 05) as altitudes increase,This result implies an offset effect between biomass C and SOC storage.
关 键 词:地上和地下植被碳贮量 土壤有机碳 海拔 碳密度 宝天曼
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