Turnover rate of soil organic matter and origin of soil (CO2)-C-14 in deep soil from a subtropical forest in dinghushan biosphere reserve, South China

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	Ding, P.; Shen, C. D.; Wang, N.; Yi, W. X.; Ding, X. F.; Fu, D. P.; Liu, K. X.; Zhou, L. P.
	Turnover rate of soil organic matter and origin of soil (CO2)-C-14 in deep soil from a subtropical forest in dinghushan biosphere reserve, South China
Source Publication	Radiocarbon
ISSN	0033-8222
	2010
Volume	52 Issue:3 Pages:1422-1434
Language	英语
WOS ID	WOS:000285437900058
Indexed By	sci
Citation statistics	Cited Times:13[WOS] [WOS Record] [Related Records in WOS]
Document Type	期刊论文
Identifier	http://ir.gig.ac.cn/handle/344008/15277
Collection	中国科学院广州地球化学研究所
Recommended Citation GB/T 7714	Ding, P.,Shen, C. D.,Wang, N.,et al. Turnover rate of soil organic matter and origin of soil (CO2)-C-14 in deep soil from a subtropical forest in dinghushan biosphere reserve, South China[J]. Radiocarbon,2010,52(3):1422-1434.
APA	Ding, P..,Shen, C. D..,Wang, N..,Yi, W. X..,Ding, X. F..,...&Zhou, L. P..(2010).Turnover rate of soil organic matter and origin of soil (CO2)-C-14 in deep soil from a subtropical forest in dinghushan biosphere reserve, South China.Radiocarbon,52(3),1422-1434.
MLA	Ding, P.,et al."Turnover rate of soil organic matter and origin of soil (CO2)-C-14 in deep soil from a subtropical forest in dinghushan biosphere reserve, South China".Radiocarbon 52.3(2010):1422-1434.

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