Chemical and Isotopic Characterization of Inland Waters around Desert Area in Xinjiang, NW China

Material type: 文書・図像類

Author: YABUKI, Sadayoほか

Publisher: Chiba University. Center for Environmental Remote Sensing

Publication date: 1997-11-05

Material Format: Digital

Capacity, size, etc.: -

NDC: 450

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Note (General)：: type:text[ABSTRACT] For seeking the origin of water and the hydrologic cycle, we investigated the major ion concentration of inland waters in and arou...

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Digital

Material Type: 文書・図像類
Title: Chemical and Isotopic Characterization of Inland Waters around Desert Area in Xinjiang, NW China
Author/Editor: YABUKI, Sadayo
OKADA, Akihiko
CHANG, Qing
INOUE, Yoshikazu
UEDA, Akira
FAN, Zi-Li
Author Heading: YABUKI, Sadayo
OKADA, Akihiko
CHANG, Qing
INOUE, Yoshikazu
UEDA, Akira
FAN, Zi-Li
Publication, Distribution, etc.: Chiba University. Center for Environmental Remote Sensing
Publication Date: 1997-11-05
Publication Date (W3CDTF): 1997-11-05
Periodical title: Proceedings of the CEReS international symposium = CEReS国際シンポジウム資料集
No. or year of volume/issue: 3
Volume: 3
Pages: 223-230
Text Language Code: eng
NDC: 450
Target Audience: 一般
Note (General): type:text
[ABSTRACT] For seeking the origin of water and the hydrologic cycle, we investigated the major ion concentration of inland waters in and around desert area in Xinjiang, NW China. Concentrations of a short-lived radioactive isotope, tritium, two stable isotope species, oxygen-18 and deuterium (D), and isotopic compositions of strontium are also measured. The chemical and isotopic composition of the waters from these areas have regional characteristics which mean that the geological feature of their water-head and drainage areas control the chemistry of inland waters. Hydrogen and oxygen isotope compositions show that river waters are not directly recharged by rain water, but by glacier and/or frozen ground melt, therefore the seasonal variation of isotopic compositions is not so conspicuous as that of precipitation. The results of tritium concentration of waters also suggest that glacier and/or frozen ground melt are important source of water flow of the basins in Xinjiang.
Format (IMT): application/pdf
Source: https://opac.ll.chiba-u.jp/da/curator/900022269/C-19_38.pdf
https://opac.ll.chiba-u.jp/da/curator/900022269/C-19_38.pdf
Access Restrictions: 限定公開
Related Material (NCID): BA40903676
https://ci.nii.ac.jp/ncid/BA40903676
Data Provider (Database): 国立情報学研究所 : 学術機関リポジトリデータベース（IRDB）（機関リポジトリ）
https://irdb.nii.ac.jp
Original Data Provider (Database): 千葉大学 : 千葉大学学術成果リポジトリ