Seasonal dynamics of suprapermafrost groundwater and its response to the freeing-thawing processes of soil in the permafrost region of Qinghai-Tibet Plateau
文献类型：期刊论文
| 作者 | Chang Juan1; Wang GenXu2 ; Li ChunJie2; Mao TianXu2
|
| 刊名 | SCIENCE CHINA-EARTH SCIENCES
 |
| 出版日期 | 2015-05-01 |
| 卷号 | 58期号:5页码:727-738 |
| 关键词 | suprapermafrost groundwater seasonal dynamics soil hydrothermal characteristics freezing-thawing process |
| ISSN号 | 1674-7313 |
| 通讯作者 | Chang Juan |
| 英文摘要 | The suprapermafrost groundwater in permafrost region not only is an important component of the water cycle and land surface process, but also is closely associated with the charges of ecological environment in cold region. However, the seasonal dynamics, driving factors, and mechanism of suprapermafrost groundwater are not well understood. Based on observation at slope scale on suprapermafrost groundwater dynamics of typical alpine meadows in the Qinghai-Tibet Plateau, the seasonal dynamics, spatial distribution and driving factors of suprapermafrost groundwater were analyzed. The results showed that there were close relationships between the seasonal dynamics of suprapermafrost groundwater and the freezing-thawing processes of active soil in permafrost region. The seasonal dynamics of suprapermafrost groundwater and its slope distribution pattern were controlled by soil temperature of active layers. The phase and range of the suprapermafrost groundwater dynamics are determined by deep soil (below 60 cm depth) moisture and groundwater recharging sources. The relationship between active soil temperatures and dynamics of suprapermafrost groundwater levels was better described by Boltzmann functions. However, the influencing thresholds of soil temperature on groundwater dynamics varied at different depths of active layers and in different slope positions, which resulted in the significant spatial heterogeneity of suprapermafrost groundwater dynamics in slope scale. Land cover change and global warming certainly altered the dynamics of suprapermafrost groundwater and the hydraulic interaction between groundwater and rivers, and consequently altered the overall hydrologic cycle of watershed scale. |
| WOS标题词 | Science & Technology ; Physical Sciences |
| 类目[WOS] | Geosciences, Multidisciplinary |
| 研究领域[WOS] | Geology |
| 关键词[WOS] | VEGETATION ; RUNOFF ; LAYER |
| 收录类别 | SCI |
| 语种 | 英语 |
| WOS记录号 | WOS:000353882500007 |
| 源URL | [http://ir.imde.ac.cn/handle/131551/9600]  |
| 专题 | 成都山地灾害与环境研究所_山地表生过程与生态调控重点实验室 |
| 作者单位 | 1.Lanzhou Univ, Coll Earth & Environm Sci, Lanzhou 730000, Peoples R China 2.Chinese Acad Sci, Inst Mt Hazards & Environm, Chengdu 610041, Peoples R China |
| 推荐引用方式 GB/T 7714 | Chang Juan,Wang GenXu,Li ChunJie,et al. Seasonal dynamics of suprapermafrost groundwater and its response to the freeing-thawing processes of soil in the permafrost region of Qinghai-Tibet Plateau[J]. SCIENCE CHINA-EARTH SCIENCES,2015,58(5):727-738. |
| APA | Chang Juan,Wang GenXu,Li ChunJie,&Mao TianXu.(2015).Seasonal dynamics of suprapermafrost groundwater and its response to the freeing-thawing processes of soil in the permafrost region of Qinghai-Tibet Plateau.SCIENCE CHINA-EARTH SCIENCES,58(5),727-738. |
| MLA | Chang Juan,et al."Seasonal dynamics of suprapermafrost groundwater and its response to the freeing-thawing processes of soil in the permafrost region of Qinghai-Tibet Plateau".SCIENCE CHINA-EARTH SCIENCES 58.5(2015):727-738. |
入库方式： OAI收割
来源：成都山地灾害与环境研究所
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