中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Carbonate verse silicate Sr isotope in lake sediments and its response to Little Ice Age

文献类型:期刊论文

作者Jin, ZD; Wang, SM; Shen, J; Wang, YX
刊名CHINESE SCIENCE BULLETIN
出版日期2003
卷号48期号:1页码:95-100
关键词chemical weathering Sr isotope inland lake Little Ice Age
ISSN号1001-6538
英文摘要The Sr-87/Sr-86 ratios of silicate (acid-insoluble, AI) and carbonate (acid-soluble, AS) of the lake sediments from the Daihai Lake, Inner Mongolia, since the last 500 years are measured respectively, indicating that chemical weathering of silicate minerals was in an early stage since the Little Ice Age within the Daihai watershed by combination with mineral constitute, Rb/Sr ratio and CaCO3 content in the sediments. During the Little Ice Age maximum, an evident peak in the Sr-87/Sr-86 ratios of both silicate and carbonate in sediments suggests that a cold climate condition is unfavorable to dissolving radiogenic strontium from silicate minerals. Meanwhile, the variation of Sr-87/Sr-86 ratios of silicate and carbonate also reflects a projected warming climate favorable to intensifying chemical weathering after the Little Ice Age. Consequently, the Sr-87/Sr-86 ratio of both silicate and carbonate in inland lake sediments can be used as an effective proxy of the past climate in single watershed.
公开日期2012-03-03
源URL[http://159.226.73.51/handle/332005/2487]  
专题南京地理与湖泊研究所_湖泊室
推荐引用方式
GB/T 7714
Jin, ZD,Wang, SM,Shen, J,et al. Carbonate verse silicate Sr isotope in lake sediments and its response to Little Ice Age[J]. CHINESE SCIENCE BULLETIN,2003,48(1):95-100.
APA Jin, ZD,Wang, SM,Shen, J,&Wang, YX.(2003).Carbonate verse silicate Sr isotope in lake sediments and its response to Little Ice Age.CHINESE SCIENCE BULLETIN,48(1),95-100.
MLA Jin, ZD,et al."Carbonate verse silicate Sr isotope in lake sediments and its response to Little Ice Age".CHINESE SCIENCE BULLETIN 48.1(2003):95-100.

入库方式: OAI收割

来源:南京地理与湖泊研究所

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