Arid
DOI10.1017/S0016756820000242
Origin of aeolian dust emitted from the Tarim Basin based on the ESR signal intensity and crystallinity index of quartz: the recycling system of fine detrital material within the basin
Isozaki, Yuko1; Tada, Ryuji1,2,3; Sun, Youbin4; Zheng, Hongbo2; Toyoda, Shin5; Sugiura, Naomi1; Karasuda, Akinori1; Hasegawa, Hitoshi1,6
通讯作者Tada, Ryuji
来源期刊GEOLOGICAL MAGAZINE
ISSN0016-7568
EISSN1469-5081
出版年2020
卷号157期号:5页码:707-718
英文摘要The Tarim Basin is the major source of aeolian dust in the northern hemisphere. Glacial activity in the mountains, transportation by rivers and homogenization by wind are believed to be responsible for dust production within the basin. However, the major source(s) and homogenization process(es) are not clear. Moreover, provenance studies on fine fractions have never been conducted. Here, we measured electron spin resonance (ESR) signal intensity and the crystallinity index of quartz in fine (< 16 mu m) and coarse (> 64 mu m) fractions of river sediments, dry lake sediments and mountain loess to examine the process(es) that produce aeolian dust. The result suggests that the coarse fraction of the river sediment was derived from the bedrock in the drainage area. The ESR signal intensity and crystallinity index of the fine fraction of river sediments from the Tian Shan Mountains and mountainous rivers in the westernmost Kunlun and Pamir mountains are also similar to the coarse fraction, suggesting the same sources. However, the ESR signal intensity and crystallinity index of the fine fraction of river sediments from the Kunlun Mountains are different from the coarse fraction and converge towards values close to the average for the fine fraction of river sediments and mountain loess. Convergence of the ESR and crystallinity index values for the fine fraction of river sediments from the Kunlun Mountains can be explained by contamination of the river sediments by aeolian dust. The convergent values resulted from the homogenization of fine detrital material by repeated recycling within the basin.
英文关键词Tarim Basin Taklimakan Desert aeolian dust provenance ESR signal intensity crystallinity index quartz
类型Article
语种英语
国家Japan ; Peoples R China
收录类别SCI-E
WOS记录号WOS:000534526500002
WOS关键词TAKLIMAKAN DESERT ; WESTERLY JET ; UPLIFT ; MOUNTAINS ; SEDIMENTS ; LOESS ; CHINA ; ASIA
WOS类目Geosciences, Multidisciplinary
WOS研究方向Geology
来源机构中国科学院地球环境研究所
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/319011
作者单位1.Univ Tokyo, Dept Earth & Planetary Sci, Bunkyo Ku, 7-3-1 Hongo, Tokyo 1130033, Japan;
2.Yunnan Univ, Res Ctr Earth Syst Sci, Kunming 650500, Yunnan, Peoples R China;
3.Chiba Inst Technol, Inst Geocosmol, 2-17-1 Tsudanuma, Narashino, Chiba 2750016, Japan;
4.Chinese Acad Sci, Inst Earth Environm, 97 Yanxiang Rd, Xian 710061, Shaanxi, Peoples R China;
5.Okayama Univ Sci, Dept Appl Phys, Kita Ku, 1-1 Ridaicho, Okayama 7000005, Japan;
6.Kochi Univ, Dept Global Environm & Disaster Prevent, 200 Otsu, Nankoku, Kochi 7838502, Japan
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Isozaki, Yuko,Tada, Ryuji,Sun, Youbin,et al. Origin of aeolian dust emitted from the Tarim Basin based on the ESR signal intensity and crystallinity index of quartz: the recycling system of fine detrital material within the basin[J]. 中国科学院地球环境研究所,2020,157(5):707-718.
APA Isozaki, Yuko.,Tada, Ryuji.,Sun, Youbin.,Zheng, Hongbo.,Toyoda, Shin.,...&Hasegawa, Hitoshi.(2020).Origin of aeolian dust emitted from the Tarim Basin based on the ESR signal intensity and crystallinity index of quartz: the recycling system of fine detrital material within the basin.GEOLOGICAL MAGAZINE,157(5),707-718.
MLA Isozaki, Yuko,et al."Origin of aeolian dust emitted from the Tarim Basin based on the ESR signal intensity and crystallinity index of quartz: the recycling system of fine detrital material within the basin".GEOLOGICAL MAGAZINE 157.5(2020):707-718.
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