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DOI | 10.1002/hyp.6977 |
Preferential exchange rate effect of isotopic fractionation in a melting snowpack | |
Zhou, Shiqiao![]() | |
通讯作者 | Zhou, SQ (通讯作者) |
发表日期 | 2008 |
ISSN | 0885-6087 |
起始页码 | 3734 |
结束页码 | 3740 |
卷号 | 22期号:18 |
英文摘要 | Stable isotope exchange processes between solid and liquid phases of a natural melting snowpack are investigated in detail by separating the liquid water from snow grains at different depths of the snowpack and collecting the bottom discharge using a lysimeter. In the melting-freezing mass exchange process between the two phases, the theoretical slope of the delta D-delta(18)O line for newly refrozen ice is calculated to be nearly that of pore water. However, based on observations of the isotopic evolution and snow grain coarsening of the snowpack, it is demonstrated that the slope of the delta D-delta(18)O line for newly refrozen ice is equal to that of the original ice. This is proved to be due to preferential water flow in the snowpack, which leads to relatively more deuterium and less oxygen-18 in the mobile water than the immobile water because of the kinetic effect. Higher mass exchange rate in the mobile water region results in excess deuterium in the bulk refrozen ice, compared with the fractionation of uniform fractionation factors and exchange rate. This effect, which is termed the 'preferential exchange rate effect of isotopic fractionation'. is shown to be larger in the lower part than the upper part of the snowpack. Copyright (C) 2008 John Wiley & Sons, Ltd. |
关键词 | ONE-DIMENSIONAL MODELSTABLE-ISOTOPESDEUTERIUM EXCESSSOLUTE TRANSPORTOXYGEN-ISOTOPEICEEVOLUTIONWATERPRECIPITATIONSNOWMELT |
英文关键词 | snowpack; isotopic fractionation; preferential water flow; snowmelt |
语种 | 英语 |
WOS研究方向 | Water Resources |
WOS类目 | Water Resources |
WOS记录号 | WOS:000259281300014 |
来源期刊 | HYDROLOGICAL PROCESSES
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来源机构 | 中国科学院青藏高原研究所 |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/257602 |
推荐引用方式 GB/T 7714 | Zhou, Shiqiao,Nakawo, Masayoshi,Hashimoto, Shigemasa,et al. Preferential exchange rate effect of isotopic fractionation in a melting snowpack[J]. 中国科学院青藏高原研究所,2008,22(18). |
APA | Zhou, Shiqiao,Nakawo, Masayoshi,Hashimoto, Shigemasa,&Sakai, Akiko.(2008).Preferential exchange rate effect of isotopic fractionation in a melting snowpack.HYDROLOGICAL PROCESSES,22(18). |
MLA | Zhou, Shiqiao,et al."Preferential exchange rate effect of isotopic fractionation in a melting snowpack".HYDROLOGICAL PROCESSES 22.18(2008). |
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