退耕弃荒洼地土壤有机碳在生态系统转化过程中的动态变化

在贵州喀斯特区域一块典型的退耕弃荒洼地中央和周边坡面采集了4个土壤剖面,研究土壤有机碳（SOC）含量和δ¹³C_org值的变化.结果表明,坡面不同土壤层次SOC的变化范围为6.0～92.3 mg·kg^-1,并沿着土壤层次的加深迅速降低,变化幅度远远大于洼地土壤剖面（6.3～26.7 mg·kg^-1）.坡面土壤δ¹³C_org 介于-25.103‰和-23.666‰之间,但各剖面土层内部δ¹³C_org变化趋势不一致.洼地土壤δ¹³C_org 介于-23.495‰和- 20.809‰之间,并随着土壤层次的加深δ¹³C_org逐渐增加.洼地土壤剖面层次内C₄-C占SOC的比例随土壤层次的加深逐渐增加,与林-农生态系统转变过程中的变化趋势相反;土壤δ¹³C_org与C₃-C之间呈显著相关性（R²=0.7806,n=7）,对δ¹³C_org起到主要影响作用的是退耕弃荒后新加入的C₃-C.

Soil Organic Carbon Variation of De-farming and Wasteland During Alteration of Ecosystem in Billabong

Four soil profile samples were collected in the middle of de-farming and wasteland billabong and around slopes, located at typical karst district of Guizhou province. Soil organic matter (SOC) content and delta Corg, were determined. SOC content ranged from 6.0 mg x kg(-1) to 92.3 mg x kg(-1), and decreased with depth at slope soil profiles. The range of value was bigger than that at billabong soil profile (6.3-26.7 mg x kg(-1)). The value of detla13 Corg, at slope profiles was between - 25.103% per hundred and - 23.666% per hundred, but variation direction of three slope soil profiles was different. The value of delta 13Corg, in billabong soil profile was between - 23.495% per hundred and - 20.809% per hundred, and increased with depth. The correlation between delta13 Csoc and C4-C,C3-C was significant (R = 0.884, n=7), influenced by new C3-C.