| 汶川地震后四川省绵竹市清平乡文家沟泥石流灾害调查研究 |
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| 引用本文： | 余斌, 马煜, 吴雨夫. 2010: 汶川地震后四川省绵竹市清平乡文家沟泥石流灾害调查研究. 工程地质学报, 18(6): 827-836. |
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| 作者姓名： | 余斌 马煜 吴雨夫 |
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| 作者单位： | 成都理工大学地质灾害防治与地质环境保护国家重点实验室,成都,610059;成都理工大学地质灾害防治与地质环境保护国家重点实验室,成都,610059;成都理工大学地质灾害防治与地质环境保护国家重点实验室,成都,610059 |
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| 基金项目： | 国家自然科学基金(40871054,40772206); 地质灾害防治地国家重点实验室自主研究基金(DZKJ-0810) |
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| 摘 要： | 在2008年5月12日汶川地震后的地震灾区暴发了许多泥石流灾害,其中以四川省绵竹市清平乡文家沟泥石流最为显著。文家沟原来不是泥石流沟,在汶川地震时由于滑坡形成的巨大的滑坡-碎屑流堆积体改变了文家沟的泥石流形成条件,在此后的3个雨季内,文家沟先后暴发了5次大规模和特大规模的泥石流灾害,其中以8 13文家沟泥石流规模和危害最大。8 13文家沟泥石流暴发时的总降雨量为227mm,泥石流持续时间约2.5h,泥石流总量约310104m3; 泥石流造成7人死亡, 5人失踪, 39人受伤, 479户农房被掩埋,直接经济损失4.3亿元。5次大规模和特大规模的泥石流以及洪水仅带走了16%的可以很容易形成泥石流的滑坡-碎屑流堆积物,文家沟如再遭遇较大降雨还会暴发泥石流。即使在今后的雨季中暴发几次规模如8 13泥石流一样大的特大规模泥石流,文家沟在较大降雨下仍然可能暴发泥石流灾害,因此对文家沟泥石流的防治工作将是一个长期的工作。
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| 关 键 词： | 文家沟 泥石流 滑坡-碎屑流 地震 降雨 |
| 收稿时间： | 2010-11-20 |
| 修稿时间： | 2010-11-29 |
INVESTIGATION OF SEVERE DEBRIS FLOW HAZARDS IN WENJIA GULLY OF SICHUAN PROVINCE AFTER THE WENCHUAN EARTHQUAKE |
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| YU Bin, MA Yu, WU Yufu. 2010: INVESTIGATION OF SEVERE DEBRIS FLOW HAZARDS IN WENJIA GULLY OF SICHUAN PROVINCE AFTER THE WENCHUAN EARTHQUAKE. JOURNAL OF ENGINEERING GEOLOGY, 18(6): 827-836. |
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| Authors: | YU Bin MA Yu WU Yufu |
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| Affiliation: | 1.State Key Laboratory of Geohazard Prevention and Geoenvironment Protection,Chengdu University of Technology,Chengdu 610059 |
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| Abstract: | Many debris flow hazards were triggered recently in the epicenter area of the 2008 Wenchuan Earthquake. The severest debris flow is the debris flow in Wenjia Gully on Aug.13, 2010.Wenjia Gully was a simply and ordinary gully and had no debris flow at all before the Wenchuan Earthquake.The formation conditions of debris flows were totally changed by a giant landslide caused by the earthquake.The giant landslide formed a landslidedebris deposition in the gully.The debris deposition had a volume of more than 30million cubic meters.The sediments were easily eroded by flash flood and formed debris flows.In the three raining seasons after the earthquake, a total of five large scale and giant scale debris flow were triggered.The largest and most harmful debris flow occurred on Aug.13, 2010.The total rainfall during the debris flow was 227mm,and the duration of debris flow was 2.5 hours.The volume of debris flow was 3.1 million cubic meters.The debris flow resulted in 7 fatalities, 5 persons listed as missing, 39 persons injured, 479 houses buried,and a direct economic loss of RMB 430 million. About 16%sediments of the landslide-debris deposition flew down out of the gully during the five large scale debris flows.New debris flows will be triggered by rainfall in the gully in the future.It will be a long-term effort for prevention and mitigation of the debris flow hazards in the gully. |
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| Keywords: | Wenjia Gully Debris flow Landslide-debris Hazards Wenchuan Earthquake Rainfall |
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