中国岩溶
中國巖溶
중국암용
CARSOLOGICA SINICA
2009年
2期
219-224
,共6页
吕勇%李高良%张贵%李继宏%蔡传生%稽仁元%王外全
呂勇%李高良%張貴%李繼宏%蔡傳生%稽仁元%王外全
려용%리고량%장귀%리계굉%채전생%계인원%왕외전
地质灾害%灾害类型%灾害区划%防治建议%云南彝良县
地質災害%災害類型%災害區劃%防治建議%雲南彝良縣
지질재해%재해류형%재해구화%방치건의%운남이량현
geological hazard%hazard type%susceptibility zoning%prevention and control proposals%Yiliang county,Yunnan
彝良县位于云南省东北部,为云南省七个地质灾害重点防治区的一部分.2003年的地质灾害调查显示,县域内有地质灾害236处,其中滑坡181处,不稳定斜坡9处,泥石流34处,地面塌陷12处,以滑坡和泥石流为主.综合研究分析结果表明,地质灾害的主要诱因除地质地理环境(地形地貌、降雨集中、岩溶作用、新构造运动强烈)等自然因素外,人类工程活动中的切坡过陡和采矿活动形成的巨大采空区也是主要诱发因素.在此基础上,根据各种影响因素的作用强度把彝良县划分为洛泽河-小米溪河高易发区、发达-洛旺中等易发区和低易发区(含小草坝亚区和龙街-奎香亚区)三个地质灾害区,并在灾害防治、协调管理、宣传教育等方面提出了一些有益的建议.
彝良縣位于雲南省東北部,為雲南省七箇地質災害重點防治區的一部分.2003年的地質災害調查顯示,縣域內有地質災害236處,其中滑坡181處,不穩定斜坡9處,泥石流34處,地麵塌陷12處,以滑坡和泥石流為主.綜閤研究分析結果錶明,地質災害的主要誘因除地質地理環境(地形地貌、降雨集中、巖溶作用、新構造運動彊烈)等自然因素外,人類工程活動中的切坡過陡和採礦活動形成的巨大採空區也是主要誘髮因素.在此基礎上,根據各種影響因素的作用彊度把彝良縣劃分為洛澤河-小米溪河高易髮區、髮達-洛旺中等易髮區和低易髮區(含小草壩亞區和龍街-奎香亞區)三箇地質災害區,併在災害防治、協調管理、宣傳教育等方麵提齣瞭一些有益的建議.
이량현위우운남성동북부,위운남성칠개지질재해중점방치구적일부분.2003년적지질재해조사현시,현역내유지질재해236처,기중활파181처,불은정사파9처,니석류34처,지면탑함12처,이활파화니석류위주.종합연구분석결과표명,지질재해적주요유인제지질지리배경(지형지모、강우집중、암용작용、신구조운동강렬)등자연인소외,인류공정활동중적절파과두화채광활동형성적거대채공구야시주요유발인소.재차기출상,근거각충영향인소적작용강도파이량현화분위락택하-소미계하고역발구、발체-락왕중등역발구화저역발구(함소초패아구화룡가-규향아구)삼개지질재해구,병재재해방치、협조관리、선전교육등방면제출료일사유익적건의.
Situated in the northeastern of Yunnan province, Yiliang county belongs to geological hazards pivot prevention and control region of Yongshan-Yiliang landslides and debris flows and one of the seven geological hazards pivot prevention and control regions in Yunnan. The geological hazard investigation in 2003 showed that there were 236 geological hazards, including 181 landslides, 9 unstable slopes and 34 debris flows as well as 12 collapses. Moreover, the landslides and debris flows were dominant disasters in this research area.The results from comprehensive analysis indicated the geological hazard mainly resulted from not only geological and geographic environment factors, such as landform and relief, rainstorms and karst as well as neo-tectonic movement, but also slop-cutting and huge goafs in mining areas by human activity. On the basis of the intensity of several influences, three types of geological hazard region are divided, including high susceptible area in Luoze River-Xiaomixi River, middle susceptible area in Fada-Luowang and low susceptible area in Xiaocaoba and Longjie-Kuixiang. Furthermore, the authors put forward some constructive suggestions for the prevention, control and management as well as publicity and education on geological hazard.