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三峡库区消落带湿地土壤有机碳及其组分特征

Characteristics of Soil Organic Carbon and Its Fraction at Riparian Wetland of Three Gorges Reservoir Area

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湿地生态系统土壤有机碳库的组分变化对于全球碳平衡起着极其重要的作用.本研究选取三峡库区消落带湿地3个海拔梯度的土壤,以从未淹没的样地作为对照,研究消落带湿地不同海拔梯度土壤有机碳组分的特征.结果表明:土壤有机碳、易氧化有机碳、水溶性碳水化合物有机碳和和微生物生物量碳均以消落带小于未淹没样地.在消落带,海拔最低、淹没持续时间较长且正处于水位波动期的样地土壤有机碳、易氧化碳和微生物生物量碳显著低于其他样地,而土壤矿化碳显著高于其他样地.相关性分析表明,土壤有机碳与微生物生物量碳(R2=0.94)的正相关性显著高于与易氧化有机碳(R2=0.88)、水溶性有机碳(R2=0.73)及其水溶性碳水化合物(R2=0.70)之间的正相关性,但是与矿化碳之间无显著的相关性.因此,土壤微生物生物量碳是消落带湿地土壤有机碳随不同海拔梯度变化的最敏感的组分.
The change in soil organic carbon fraction in wetland ecosystem plays an important role in global climate change.The objective of this study was to determine the change in organic carbon and its fractions at different elevation gradient in riparian wetland of Three Gorges Reservoir Area.Results showed that soil organic carbon(OC),readily oxidizable carbon(ROC),water-soluble carbohydrates(WSCh),water-soluble organic carbon(DOC) and microbial biomass carbon(MBC) were lower in the riparian wetland than these in the never inundation upland.In riparian zone,the soil OC,ROC and MBC in sites with lower elevation gradient,longer-term inundation and fluctuating were lower than these in other sites,while soil mineralized carbon (MIC) changed oppositely.The positive correlation of MBC with OC (R2=0.94) was significantly higher than that with ROC,DOC and WSCh (R2=0.88,0.73 and 0.70),whereas there was no significant correlation between OC and MIC.These results suggested that MBC was the fraction of soil organic carbon which was the most sensitive to change of elevation gradient in riparian wetland of Three Gorges Reservoir Area.

RiparianOrganic carbonLabile organic carbon fractionSensitive fraction

贾国梅、牛俊涛、席颖

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三峡大学生物与制药学院,湖北宜昌443002

三峡大学三峡库区生态环境教育部工程研究中心,湖北宜昌443002

三峡库区消落带 土壤有机碳 活性有机碳组分 敏感组分

三峡库区生态环境教育部工程研究中心课题三峡大学预研基金

KF2013-09Hy1406

2015

土壤
中国科学院南京土壤研究所

土壤

CSTPCDCSCD北大核心
影响因子:1.052
ISSN:0253-9829
年,卷(期):2015.47(5)
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