中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Linkage of liquid conductivity of glacier ice with its alkalinity over the north Qinghai-Xizang (Tibet) Plateau - Implication to the past dust recovery

文献类型:期刊论文

作者Xiao, CD; Yao, TD; Qin, DH; Seko, K; Pu, JC; Sheng, WK
刊名SCIENCE IN CHINA SERIES D-EARTH SCIENCES
出版日期2002-04-01
卷号45期号:4页码:300-310
关键词liquid conductivity (EC) Qinghai-Xizang (Tibet) Plateau Asia dust climatic change
ISSN号1006-9313
通讯作者Xiao, CD()
英文摘要Liquid conductivity (EC) measurement was conducted for the samples collected from several snow pits and ice cores over the Qinghai-Xizang (Tibet) Plateau, with their time range covering seasonal, decadal and centennial scales. Unlike the previous attention mostly focused on the acidity (W) responding to the solid conductance (ECM) of glacial ice, we introduce the alkalinity (OH-) of snow and ice to show how it responds to EC. Strong linear relationship was established between EC and OH- for these snow pits and ice cores. Positive correlation is also established between EC and major cations (Ca2+,Mg2+, Na+ and K+). Since the cations are known as the proxies for the intensity of mineral dust influx onto glaciers of the northern Qinghai-Xizang Plateau, we believe that EC could be used as an indicator for the history of dust input in deep ice core study. In fact, records in Guliya ice core since the Little Ice Age (LIA) indicate that dust load in glacier may depend on the combination of temperature and humidity. "Cold-dry" combination favors the dust arising, and results in higher EC and OH- values, while "warm-wet" combination prevents dust form and EC and OH- values are lower. In the past century, with the atmospheric warming and precipitation increasing over the northern plateau, which means an atmospheric condition of dust decreasing, both EC and OH- displayed rapid decline.
收录类别SCI
WOS关键词MELTWATERS ; CORES ; AGE ; CAP
WOS研究方向Geology
WOS类目Geosciences, Multidisciplinary
语种英语
WOS记录号WOS:000175009300002
出版者SCIENCE CHINA PRESS
URI标识http://www.irgrid.ac.cn/handle/1471x/2556740
专题寒区旱区环境与工程研究所
通讯作者Xiao, CD
作者单位1.Chinese Acad Sci, Cold & Arid Reg Environm & Engn Res Inst, Lab Ice Core & Cold Reg Environm, Lanzhou 730000, Peoples R China
2.Nagoya Univ, Inst Hydrospher Atmospher Sci, Nagoya, Aichi 46401, Japan
推荐引用方式
GB/T 7714
Xiao, CD,Yao, TD,Qin, DH,et al. Linkage of liquid conductivity of glacier ice with its alkalinity over the north Qinghai-Xizang (Tibet) Plateau - Implication to the past dust recovery[J]. SCIENCE IN CHINA SERIES D-EARTH SCIENCES,2002,45(4):300-310.
APA Xiao, CD,Yao, TD,Qin, DH,Seko, K,Pu, JC,&Sheng, WK.(2002).Linkage of liquid conductivity of glacier ice with its alkalinity over the north Qinghai-Xizang (Tibet) Plateau - Implication to the past dust recovery.SCIENCE IN CHINA SERIES D-EARTH SCIENCES,45(4),300-310.
MLA Xiao, CD,et al."Linkage of liquid conductivity of glacier ice with its alkalinity over the north Qinghai-Xizang (Tibet) Plateau - Implication to the past dust recovery".SCIENCE IN CHINA SERIES D-EARTH SCIENCES 45.4(2002):300-310.

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来源:寒区旱区环境与工程研究所

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