| 西昆仑山古里雅冰帽深钻孔冰温的稳定态分析 |
| |
| 引用本文： | 黄茂桓. 西昆仑山古里雅冰帽深钻孔冰温的稳定态分析[J]. 冰川冻土, 1997, 19(3): 202-206 |
| |
| 作者姓名： | 黄茂桓 |
| |
| 作者单位： | 中国科学院兰州冰川冻土研究所 |
| |
| 摘 要： | 在西昆仑山古里雅冰帽海拔６０７０ｍ处钻孔，深３０９ｍ，上部２００ｍ进行了温度测量。对实测资料作稳定态分析后，得出冰内温度梯度大，底部达融点的结果。算出地热通量为１１２ｍＷ／ｍ＾２，与青藏高原为高地热区的观点一致。
|
| 关 键 词： | 冰帽 冰温 地热 稳定态 西昆仑山 冰川 |
A Steady-state Analysis of Ice Temperature in the Guliya Ice Cap, West Kunlun Mountains |
| |
| Huang Maohuan. A Steady-state Analysis of Ice Temperature in the Guliya Ice Cap, West Kunlun Mountains[J]. Journal of Glaciology and Geocryology, 1997, 19(3): 202-206 |
| |
| Authors: | Huang Maohuan |
| |
| Abstract: | A borehole, 309 m in depth, was made at 6 070 m a s l. on the Guliya Ice Cap in the West Kunlun Mountains, of which in the upmost 200 m ice temperature was measured A steady-state analysis of the measured data reveals a great temperature gradient within the ice cap and the melting point appearing at the bottom. The geothermal flux is calculated to be 112 mW/m 2, which is coincident with the idea that the Tibetan Plateau is a high geothemal area. |
| |
| Keywords: | Guliya Ice Cap ice temperature geothermal steady-state |
| 本文献已被 CNKI 维普 等数据库收录！ |
|
