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| 浅谈山区河流泥石流灾害的成因及其防治措施 | |
| 引用本文： | 宋禹河. 浅谈山区河流泥石流灾害的成因及其防治措施[J]. 中国西部科技, 2009, 8(10): 54-55 |
| 作者姓名： | 宋禹河 |
| 作者单位： | 新疆奎屯农七师奎屯河流域水利工程灌溉管理处,新疆,奎屯,833200 |
| 摘 要： | 奎屯河流域位于新疆天山北坡，发源于高山古冰川，山口以下形成冲积扇，河流在冲积扇中迂回摆动，下切为深槽，形成两岸多级台地地形，冲沟十分发育，植被条件极差，泥石流灾害频繁发生。 |
| 关 键 词： | 山区河流 泥石流灾害 成因 防治措施 |
Elementary Intyoduction the River in the Mountain Area Mud-rock Fiow Calamity Cause of formation and its Prevention and Cure |
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| SONG Yu-he. Elementary Intyoduction the River in the Mountain Area Mud-rock Fiow Calamity Cause of formation and its Prevention and Cure[J]. Science and Technology of West China, 2009, 8(10): 54-55 | |
| Authors: | SONG Yu-he |
| Affiliation: | SONG Yu-he (The kui tun river valley water conservancy project and irrigate area of jurisdiction, The agricultural of the seventh division,kui tun,xin jiang postal service encode,833200) |
| Abstract: | The kui tun river valley lies to the north of slope in Tian shah,it origonates from ancient high mountain glacier,it forms fan-shaped level the ground blow mountain pass,The river flows its way in fan-shaped level the ground,leave off form deep gully,it takes shape more rank step terrain in right shore and left shore,The deep gully grows very quickly,The vegetation ecology very weak,The mud-rock flow calamity happens frequently. |
| Keywords: | Mountain rivers Debris flow Causes Prevention and control measures |
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