| 大兴安岭北部霍拉河盆地多年冻土与地下水的相互作用 |
| |
| 引用本文： | 王保来,周幼吾,郭东信.大兴安岭北部霍拉河盆地多年冻土与地下水的相互作用[J].冰川冻土,1988(2). |
| |
| 作者姓名： | 王保来 周幼吾 郭东信 |
| |
| 作者单位： | 中国科学院兰州冰川冻土研究所
(王保来，周幼吾)，中国科学院兰州冰川冻土研究所(郭东信) |
| |
| 摘 要： | 多年冻土作为冷生隔水层,影响到地下水的补给、径流及排泄。融区的分布可增加地下水的交替强度和降低地下水的矿化度。在断层破碎带及其他富水性好的地段,多年冻土厚度变化较大。
|
| 关 键 词： | 多年冻土 地下水 融区 |
Effects of permafrost on Ground water in Huola Basin, Northern Daxinganling Ridge |
| |
| Wang Baolai,Zhou Youwu and Guo Dongxin.Effects of permafrost on Ground water in Huola Basin, Northern Daxinganling Ridge[J].Journal of Glaciology and Geocryology,1988(2). |
| |
| Authors: | Wang Baolai Zhou Youwu and Guo Dongxin |
| |
| Abstract: | Permafrost, as, an impermeable frost-seam, increases the artesian pressure and depth of groundwa-ter. The seam lies below the permafros layer. The recharge and discharge of groundwater are conducted mainly through taliks and shattered fault zones. Existence of taliks with a large area can increase the exchange intensity of groundwater and lower mineralization of groundwater. |
| |
| Keywords: | permafrost ground water talik |
| 本文献已被 CNKI 等数据库收录！ |
