Glacier meltwater runoff process analysis using delta D and delta O-18 isotope and chemistry at the remote Laohugou glacier basin in western Qilian Mountains, China
文献类型：期刊论文
| 作者 | Wang Caixia1; Dong Zhiwen2; Qin Xiang2,3; Zhang Jie1; Du Wentao2,3; Wu Jinkui2 |
| 刊名 | JOURNAL OF GEOGRAPHICAL SCIENCES
 |
| 出版日期 | 2016-06-01 |
| 卷号 | 26期号:6页码:722-734 |
| 关键词 | meltwater runoff stable hydrogen and oxygen isotope chemistry runoff process |
| ISSN号 | 1009-637X |
| DOI | 10.1007/s11442-016-1295-y |
| 通讯作者 | Dong Zhiwen(dongzhiwen@lzb.ac.cn) |
| 英文摘要 | Stable hydrogen and oxygen isotope has important implication on water and moisture transportation tracing research. Based on stable hydrogen (delta D) and oxygen (delta O-18) isotope using a Picarro L1102-i and water chemistry (e.g. major ions, pH, EC and TDS) measurement, this study discussed the temporal variation and characteristics of stable hydrogen and oxygen isotope, chemistry (e.g. TDS, pH, EC, Ca2+, Mg2+, Na+ and Cl-) in various water bodies including glacier meltwater runoff, ice and snow, and precipitation at the Laohugou glacier basin during June 2012 to September 2013. Results showed that dD and delta O-18 in the meltwater runoff varied obviously with the temporal change from June to September, showing firstly increasing trend and then decreasing trend, with the highest values in July with high air temperature and strong glacier melting, which could indicate the temporal change of glacier melting process and extent. Variations of delta D and delta O-18 in the runoff were similar with that of snow and ice on the glacier, and the values were also above the GMWL, which probably implied that the glacier runoff was mainly originated from glacier melting and precipitation supply. The glacier meltwater chemical type at the Laohugou glacier basin were mainly composed by Ca-Na-HCO3-SO4 and Ca-Mg-HCO3-SO4, which also varied evidently with the glacier melting process in summer. By analyzing the temporal change of stable hydrogen and oxygen isotope and chemistry in the melting period, we find it is easy to separate the components of the snow and ice, atmospheric precipitation and melt-runoff in the river, which could reflect the change process of glacier melting during the melting period, and thus this work can contribute to the glacier runoff change study of large-scale region by stable isotope and geochemical method in future. |
| 收录类别 | SCI |
| WOS关键词 | HEIHE RIVER-BASIN ; HYDROGRAPH SEPARATION ; STABLE-ISOTOPES ; NORTHWEST CHINA ; PRECIPITATION ; DEUTERIUM ; ORIGIN ; WATER ; O-18 |
| WOS研究方向 | Physical Geography |
| WOS类目 | Geography, Physical |
| 语种 | 英语 |
| WOS记录号 | WOS:000375111200006 |
| 出版者 | SCIENCE PRESS |
| URI标识 | http://www.irgrid.ac.cn/handle/1471x/2557312 |
| 专题 | 寒区旱区环境与工程研究所 |
| 通讯作者 | Dong Zhiwen |
| 作者单位 | 1.Northwest Normal Univ, Coll Geog & Environm Sci, Lanzhou 730070, Peoples R China 2.Chinese Acad Sci, State Key Lab Cryospher Sci, Lanzhou 730000, Peoples R China 3.Chinese Acad Sci, Cold & Arid Reg Environm & Engn Res Inst, Qilian Mt Glacier & Ecol Environm Res Stn, Lanzhou 730000, Peoples R China |
| 推荐引用方式 GB/T 7714 | Wang Caixia,Dong Zhiwen,Qin Xiang,et al. Glacier meltwater runoff process analysis using delta D and delta O-18 isotope and chemistry at the remote Laohugou glacier basin in western Qilian Mountains, China[J]. JOURNAL OF GEOGRAPHICAL SCIENCES,2016,26(6):722-734. |
| APA | Wang Caixia,Dong Zhiwen,Qin Xiang,Zhang Jie,Du Wentao,&Wu Jinkui.(2016).Glacier meltwater runoff process analysis using delta D and delta O-18 isotope and chemistry at the remote Laohugou glacier basin in western Qilian Mountains, China.JOURNAL OF GEOGRAPHICAL SCIENCES,26(6),722-734. |
| MLA | Wang Caixia,et al."Glacier meltwater runoff process analysis using delta D and delta O-18 isotope and chemistry at the remote Laohugou glacier basin in western Qilian Mountains, China".JOURNAL OF GEOGRAPHICAL SCIENCES 26.6(2016):722-734. |
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来源：寒区旱区环境与工程研究所
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