IEECAS OpenIR  > 加速器质谱中心
逐级温度热解法在黄土古土壤样品14 C测年中的应用
程鹏; 吴书刚; 杜花; 陈清敏; 卢雪峰
2012-12-30
Source Publication干旱区资源与环境
Volume26Issue:12Pages:81-85
Subtype期刊论文
Abstract利用已知可靠年代的黄土古土壤样品,采用逐级热解的方法,获取不同温度下的热解组分,运用加速器(14)~C测年技术,测试各个组分的(14)~C年龄,探讨获得可靠测年组分所需的逐步解热的实验条件。研究表明,逐级热解过程中,100℃~ 600℃温度段的热解挥发组分为年轻碳,而600~800℃温度段热解残余物(Py -R)则为老碳,600℃-800℃热解挥发组分(Py-V)是黄土-古土壤“C测年的可靠组分。
Indexed ByCSCD
Language中文
CSCD IDCSCD:4699700
Citation statistics
Cited Times:1[CSCD]   [CSCD Record]
Document Type期刊论文
Identifierhttp://ir.ieecas.cn/handle/361006/10747
Collection加速器质谱中心
Recommended Citation
GB/T 7714
程鹏,吴书刚,杜花,等. 逐级温度热解法在黄土古土壤样品14 C测年中的应用[J]. 干旱区资源与环境,2012,26(12):81-85.
APA 程鹏,吴书刚,杜花,陈清敏,&卢雪峰.(2012).逐级温度热解法在黄土古土壤样品14 C测年中的应用.干旱区资源与环境,26(12),81-85.
MLA 程鹏,et al."逐级温度热解法在黄土古土壤样品14 C测年中的应用".干旱区资源与环境 26.12(2012):81-85.
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