MAO Zheng-jun,YANG Xiao-hua,WANG Xiao-zhong.Study on Prevention Measures and Development Characteristics of Geological Hazards along the Expressway in the Wushaoling[J].Research of Soil and Water Conservation,2012,19(01):202-205,211.
乌鞘岭地区高速公路沿线地质灾害发育特征及防治措施
- Title:
- Study on Prevention Measures and Development Characteristics of Geological Hazards along the Expressway in the Wushaoling
- 分类号:
- P694
- 摘要:
- 乌鞘岭地区高速公路是国道主干线的重要组成路段。开展高速公路沿线地质灾害研究，将为该区域高速公路沿线地质灾害防灾减灾提供基础依据。通过实地调查和分析，查明了乌鞘岭地区高速公路沿线地质灾害发育特征、时空分布规律及形成条件。结果表明：乌鞘岭地区高速公路沿线地质灾害类型主要为泥石流和不稳定斜坡，其中泥石流灾害具有分布广泛、发生频率高等特点；不稳定斜坡局部或零星分布，且现状危害轻；从时空分布规律上来看，具有条带性和集中性；形成条件包括地形地貌、地层结构、降雨、人类工程活动和地震；泥石流采取合理选线、监测预警、跨越疏导及生态恢复的防治措施；不稳定斜坡采取优化坡面形态、排水措施、工程治理结合植物防护的防治措施。
- Abstract:
- Expressway in the Wushaoling is the important section of national trunk highway. Research for geological hazards along the expressway will provide the basis for disaster prevention and reduction. Based on field investigation and analyses, the development characteristics, temporal and spatial distribution and formation conditions of geological hazards along the expressway in Wushaoling were found. The results indicate that debris flow and unstable slope are the main types of geological hazards along the expressway in Wushaoling. Debris flow disaster distributes widely and occurs frequently. Unstable slope distributes locally or fragmentarily, and its hazards is gentle, which is characterized as zonal and concentrated features in terms of temporal and spatial distribution. Geomorphology, stratum structure, rainfall, human engineering activity and earthquake are considered as the formation conditions of geological hazards. Debris flow is controlled by applying for reasonable selecting lines, monitoring and warning, cross grooming and ecological restoration. Unstable slope is controlled by the means of optimizing slope morphology, drainage measures, engineering treatment combined with plant protection.
参考文献/References:
[1] 中华人民共和国国土资源部.2005年中国国土资源公报[J].国土资源通讯, 2006 (8):26-30.
[2] 中华人民共和国国土资源部.2009年中国国土资源公报[J].国土资源通讯, 2010 (7):4-13.
[3] 陈开圣, 肖涛, 彭小平.贵州省公路地质灾害基本特征及防治对策研究[J].公路, 2007 (11):135-139.
[4] 甘肃省交通规划勘察设计院有限责任公司.连云港至霍尔果斯国道主干线永登 (徐家磨) 至古浪公路工程可行性研究报告[R].兰州:甘肃省交通规划勘察设计院有限责任公司, 2004.
[5] 甘肃省地质环境监测院.连云港—霍尔果斯国道主干线永登 (徐家磨) 至古浪公路地质灾害危险性评估报告[R].兰州:甘肃省地质环境监测院, 2005.
[6] 中国地质调查局.滑坡崩塌泥石流灾害详细调查规范 (DD2008-02)[S].2008:9-11.
[7] 雷祥义, 魏青坷.陕北伤亡性黄土崩塌成因与对策研究[J].岩土工程学报, 1998, 20 (1):64-69.
[8] Nakamura H, Tsuchima S. Analysis of piles works assuming slide movement[J].Journal of the Japan Landslide Society, 1987, 24 (2):17-31.
[9] 曲永新, 张永双, 覃祖淼.三趾马红土与西北黄土高原滑坡[J].工程地质学报, 1999, 7 (3):257-265.
[10] Derbyshire E. Geological hazards in loess terrain, with particular reference to the loess regions of China[J]. Earth-Science Reviews, 2001, 54:231-260.
[11] 李栋梁, 刘德祥.甘肃气候[M].北京:气象出版社, 2000.
[12] 谭炳炎, 段爱英.山区铁路沿线暴雨泥石流预报的研究[J].自然灾害学报, 1995, 4 (2):43-52.
[13] Rosen A M. The impact of environmental change and human land use on alluvial valleys in the Loess Plateau of China during the Middle Holocene[J]. Geomorphology, 2008, 101:298-307.
相似文献/References:
[1]盛海洋,翟秋敏,郭志永.环境地质灾害及其防御研究[J].水土保持研究,2002,9(04):67.
SHENG Hai-yang,ZHAI Qiu-min,GUO Zhi-yong.Environgeological Hazards and Study of Protection and Control of the Disasters[J].Research of Soil and Water Conservation,2002,9(01):67.
[2]雷宇,刘大安,莫多闻.川藏公路地质分区三维可视化信息管理初探—八宿至林芝路段工程分析[J].水土保持研究,2003,10(03):66.
LEI Yu,LIU Da-an,MO Duo-wen.Primary Discussion on Engineering Geology Partition and 3D-visualizing Information Management of Chuan-Zang Road--Basu-Linzhi Setion[J].Research of Soil and Water Conservation,2003,10(01):66.
[3]张会刚,姜志玲,王维早.西南山区水电站库区地质灾害模糊综合评价[J].水土保持研究,2006,13(04):30.
ZHANG Hui-gang,JIANG Zhi-ling,WANG Wei-zao.Geological Hazard Fuzzy Comprehensive Evaluationestimation of Power Station in Southwest Mountainous Area[J].Research of Soil and Water Conservation,2006,13(01):30.
[4]李细生,刘红年,张华,等.湖南“5·31”特大暴雨山洪成因及对策[J].水土保持研究,2006,13(04):68.
LI Xi-sheng,LIU Hong-nian,ZHANG Hua,et al.Cause and Countermeasure of the Heavy Rain Flush Flood in Hunan Province on 31 May[J].Research of Soil and Water Conservation,2006,13(01):68.
[5]张兵,傅荣华,夏克勤.四川省屏山县县城新址地质灾害分布、形成条件与防治[J].水土保持研究,2006,13(05):47.
ZHANG Bing,FU Rong-hua,XIA Ke-qin.The Geology Hazards’Distribution, Formation Condition and Prevention Measures in Pingshan County, Sichuan Province[J].Research of Soil and Water Conservation,2006,13(01):47.
[6]彭社琴,赵其华,陈明东,等.浙江省某公路边坡地质灾害特点及其成因[J].水土保持研究,2006,13(05):124.
PENG She-qin,ZHAO Qi-hua,CHEN Ming-dong,et al.Mechanism of Geological Hazard of a Highway Slope in Zhejiang Province[J].Research of Soil and Water Conservation,2006,13(01):124.
[7]尚志海,王兴水,袁丽芬.广东省紫金县地质灾害风险评价[J].水土保持研究,2013,20(06):102.
SHANG Zhi-hai,WANG Xing-shui,YUAN Li-fen.Assessment on Geo-hazard Risk of Zijin County, Guangdong Province[J].Research of Soil and Water Conservation,2013,20(01):102.
[8]王高峰,王爱军,田运涛,等.基于图幅调查的六盘山镇孕灾地质条件分析[J].水土保持研究,2016,23(05):364.
WANG Gaofeng,WANG Aijun,TIAN Yuntao,et al.Analysis on Disaster-Pregnant Geological Environment of Liupanshan Town Based on Map Sheet Survey[J].Research of Soil and Water Conservation,2016,23(01):364.
[9]魏成武,巫锡勇.喇嘛溪沟泥石流运动特征及其对工程影响分析[J].水土保持研究,2008,15(06):170.
WEI Cheng-wu,WU Xi-yong.The Debris Flow Movement Characteristics and Their Influences on Engineering Projects in the Lamaxi Channel[J].Research of Soil and Water Conservation,2008,15(01):170.
[10]陈维治,付保红.基于地质灾害危险性区划的盈江县农村居民点空间布局优化[J].水土保持研究,2017,24(03):320.
CHEN Weizhi,FU Baohong.Spatial Distribution and Optimization of the Rural Residential Area in Yingjiang County Based on Geological Hazard Zoning[J].Research of Soil and Water Conservation,2017,24(01):320.
备注/Memo
收稿日期:2011-7-7;改回日期:2011-8-11。
基金项目:西部交通建设科技项目（200731800038）；西部交通建设科技项目（200131800053）
作者简介:毛正君（1983- ），男，宁夏固原人，博士研究生，从事地质灾害、地质工程与岩土工程方面的研究工作。E-mail：zhengjun_mao@163.com
通讯作者:杨晓华（1961- ），男，河北唐山人，教授，博士生导师，博士，从事公路岩土与隧道工程的研究。E-mail：xiaohuay@126.com