西北地质
西北地質
서북지질
NORTHWESTERN GEOLOGY
2014年
3期
192-199
,共8页
泥石流%发育特征%防治工程%效果分析%都江堰
泥石流%髮育特徵%防治工程%效果分析%都江堰
니석류%발육특정%방치공정%효과분석%도강언
debris flow%development characteristics%prevention proj ects%effectiveness analysis%Duj iangyan city
黄央沟位于“5.12”汶川地震的极重灾区四川省都江堰市龙池镇,地震使沟内山体发生大规模的滑坡和崩塌,其为泥石流的形成提供了丰富的松散固体物质。地震后黄央沟泥石流十分活跃,2010年8月13日、8月18日和2013年7月9日均暴发了泥石流,造成了严重的经济损失。笔者通过对黄央沟泥石流灾害现场进行实地调查,详细分析了黄央沟泥石流的形成条件和发育特征,并对已有防治工程效果进行了分析和探讨。针对防治工程存在的问题和黄央沟泥石流的特点,建议在沟道下游和堆积区修建排导沟,使泥石流顺畅排入龙溪河;采取工程和生物措施来稳定沟道内的崩滑堆积体和不稳定斜坡,减少泥石流物源;沟口公路采用高架桥跨越方式通过泥石流堆积扇。该研究结果可为强震区泥石流灾害的防治提供参考。
黃央溝位于“5.12”汶川地震的極重災區四川省都江堰市龍池鎮,地震使溝內山體髮生大規模的滑坡和崩塌,其為泥石流的形成提供瞭豐富的鬆散固體物質。地震後黃央溝泥石流十分活躍,2010年8月13日、8月18日和2013年7月9日均暴髮瞭泥石流,造成瞭嚴重的經濟損失。筆者通過對黃央溝泥石流災害現場進行實地調查,詳細分析瞭黃央溝泥石流的形成條件和髮育特徵,併對已有防治工程效果進行瞭分析和探討。針對防治工程存在的問題和黃央溝泥石流的特點,建議在溝道下遊和堆積區脩建排導溝,使泥石流順暢排入龍溪河;採取工程和生物措施來穩定溝道內的崩滑堆積體和不穩定斜坡,減少泥石流物源;溝口公路採用高架橋跨越方式通過泥石流堆積扇。該研究結果可為彊震區泥石流災害的防治提供參攷。
황앙구위우“5.12”문천지진적겁중재구사천성도강언시룡지진,지진사구내산체발생대규모적활파화붕탑,기위니석류적형성제공료봉부적송산고체물질。지진후황앙구니석류십분활약,2010년8월13일、8월18일화2013년7월9일균폭발료니석류,조성료엄중적경제손실。필자통과대황앙구니석류재해현장진행실지조사,상세분석료황앙구니석류적형성조건화발육특정,병대이유방치공정효과진행료분석화탐토。침대방치공정존재적문제화황앙구니석류적특점,건의재구도하유화퇴적구수건배도구,사니석류순창배입룡계하;채취공정화생물조시래은정구도내적붕활퇴적체화불은정사파,감소니석류물원;구구공로채용고가교과월방식통과니석류퇴적선。해연구결과가위강진구니석류재해적방치제공삼고。
Huangyang gully is located in Longchi town of Dujiangyan city,a severe disaster area of Wenchuan earthquake in Sichuan province.The earthquake induced large scale collapses and landslides which provided plenty of loose solid material for debris flow.The debris flow activity was very active after earthquake.Under the effect of heavy rainfall,debris flow occurred in the Huangyang gully both on August 13 and August 18 of 2010 as well as on July 9 of 2013,which has caused serious economic losses.Based on the field investigation of debris flow disaster,this paper presented a detailed analysis of the formation conditions and development characteristics of the debris flow,and discussed the effectiveness of debris flow prevention projects.For the problems of prevention proj ects and the characteristics of debris flow,following measures has been put forward by the authors:building drainage ditches in the downstream and accumulation region of debris flow to make the debris flow into Longxi river smoothly;and taking engineering and biological measures to stabilize landslides accumulation body and unstable slopes;besides,the road in the exit position of debris flow should adopt viaduct across the debris flow fan.The study results could provide a reference for the prevention and control of debris flow disaster in strong earthquake area.