中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
鼎湖山森林演替序列水文过程中总有机碳(TOC)变化规律及其对土壤碳平衡的贡献(英文)

文献类型:期刊论文

作者乔玉娜3,4; 尹光彩2,4; 罗艳4; 刘艳()4
刊名生态环境学报
出版日期2009
卷号18期号:06页码:2300-2307
关键词Dinghushan forest succession hydrological processes TOC concentrations TOC fluxes
英文摘要The dynamics of total organic carbon (TOC) in hydrological processes are important for understanding carbon cycling in forest ecosystems. TOC was monitored in precipitation, throughfall, stemflow, litter leachate and runoff in subtropical climax forestecosystem-monsoon evergreen broad-leaved forest (MBF), and its two successional forests of natural restoration-mixed Pinus mas-sonniana/broad-leaved forest (PBF), and Pinus massoniana forest (PF) at Dinghushan Nature Reserve (DNR) in southern China for 3 years (from April, 2002 to May, 2005). The major results and conclusions are as follows: TOC concentrations and fluxes of through- fall (DTF), stemflow, and litter leachate in PF were higher than those in MBF and PBF. TOC concentrations in dry season werehigher than that in rainy season, while TOC fluxes were in opposite situation. The contributions of different hydrological processes toforest SOC pools decreased in the order: litter leachate >DTF >stemflow. Forest canopy and litter appeared to be important sourcesfor TOC. Therefore, large TOC fluxes imported to soils with small amount of outputs by runoff may result in SOC accumulation.The net inputs of organic carbon to soil profile from the hydrological processes in MBF, PBF and PF were (27.1 ± 1.65) g·m -2 ·a -1 ,(28.9 ± 2.79) g·m -2 ·a -1 , (30.2 ± 2.65) g·m -2 ·a -1 , respectively. This part of carbon is usually negligible because it is only a small pro-portion of SOC. However, this part of carbon could be imported into the soil through infiltration. Through soil filtration and adsorp-tion, carbon should be distributed in soil evenly, which is helpful to long-term preservation of SOC.
源URL[http://210.77.82.179/handle/2SCSIERX/3698]  
专题研究领域
作者单位1.Guangxi Soil and Water Conservation Monitoring Section,Nanning 530023,China
2.College of Environmental Science and Engineering,Guangdong University of Technology,Guangzhou 510006,China;
3.Graduate School of Chinese Academy of Sciences,Beijing 100049,China;
4.South China Botanical Garden,Chinese Academy of Sciences,Guangzhou 510650,China;
推荐引用方式
GB/T 7714
乔玉娜,尹光彩,罗艳,等. 鼎湖山森林演替序列水文过程中总有机碳(TOC)变化规律及其对土壤碳平衡的贡献(英文)[J]. 生态环境学报,2009,18(06):2300-2307.
APA 乔玉娜,尹光彩,罗艳,&刘艳.(2009).鼎湖山森林演替序列水文过程中总有机碳(TOC)变化规律及其对土壤碳平衡的贡献(英文).生态环境学报,18(06),2300-2307.
MLA 乔玉娜,et al."鼎湖山森林演替序列水文过程中总有机碳(TOC)变化规律及其对土壤碳平衡的贡献(英文)".生态环境学报 18.06(2009):2300-2307.

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来源:华南植物园

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