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	TURNOVER RATE OF SOIL ORGANIC MATTER AND ORIGIN OF SOIL (CO2)-C-14 IN DEEP SOIL FROM A SUBTROPICAL FOREST IN DINGHUSHAN BIOSPHERE RESERVE, SO (CPCI-S收录)
	Ding, P.[1]; Shen, C. D.[1,2]; Wang, N.[1]; Yi, W. X.[1]; Ding, X. F.[2]; Fu, D. P.[2]; Liu, K. X.[2]; Zhou, L. P.[3]
会议名称	RADIOCARBON
URL标识	查看原文
内容类型	会议论文
URI标识	http://www.corc.org.cn/handle/1471x/2065613
专题	华南理工大学
作者单位	1.[1]Chinese Acad Sci, Guangzhou Inst Geochem, Key Lab Isotope Geochronol & Geochemistry, Guangzhou 510640, Peoples R China 2.[2]Peking Univ, State Key Lab Nucl Phys & Technol, Beijing 100871, Peoples R China 3.[3]Peking Univ, Dept Geog, Lab Earth Surface Proc, Beijing 100871, Peoples R China
推荐引用方式 GB/T 7714	Ding, P.[1],Shen, C. D.[1,2],Wang, N.[1],等. TURNOVER RATE OF SOIL ORGANIC MATTER AND ORIGIN OF SOIL (CO2)-C-14 IN DEEP SOIL FROM A SUBTROPICAL FOREST IN DINGHUSHAN BIOSPHERE RESERVE, SO (CPCI-S收录)[C]. 见:RADIOCARBON.

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