工程地质学报
工程地質學報
공정지질학보
Journal of Engineering Geology
2015年
5期
886-895
,共10页
覆盖型岩溶%地面塌陷机理%沙漏型塌陷%土洞型塌陷%泥流型塌陷
覆蓋型巖溶%地麵塌陷機理%沙漏型塌陷%土洞型塌陷%泥流型塌陷
복개형암용%지면탑함궤리%사루형탑함%토동형탑함%니류형탑함
Covered karst%Ground collapse mechanism%Hourglass type collapse%Soil-cave type collapse%Soft soil flow type collapse
为了更好地给覆盖型岩溶地面塌陷的处置和防治提供理论依据,根据可溶岩上覆盖层物质成分、地质结构及其物理力学性能的差异,首次将覆盖型岩溶地面塌陷机制区分为沙漏型、土洞型和泥流型3种类型。砂性土层分布区,由外界因素的触发导致沙颗粒向岩溶通道和溶洞漏失而产生的地面塌陷现象称为沙漏型塌陷。重力和岩溶提供的有效空间是产生沙漏型塌陷的必要条件,地下水作用加速了沙漏型地面塌陷发生,缩短了塌陷发生的过程。发生在黏性土和密实砂性土层中、由于土洞洞顶拱效应失效而产生的地面塌陷现象称为土洞型塌陷;天然土洞通过地表水侵蚀与地下水潜蚀作用、砂土漏失和软土流失等3种方式形成;土洞的形成和发展时期内洞顶上方土体是稳定的,在外部因素触发而导致洞顶拱效应失效时才发生地面塌陷;土洞型塌陷具有隐蔽性和突发性的特点。由软弱土体流失而产生的地面塌陷现象称为泥流型塌陷。泥流型地面塌陷是软弱土体向溶蚀通道和溶洞中流失的结果。岩溶地面塌陷的触发因素包括地下水作用(垂直和水平渗流、土/岩界面处地下水位频繁波动)、外加荷载(动荷载和静荷载)和土洞顶板抗力降低(顶板强度降低、厚度减薄和结构破坏)等方面。这些外因触发了岩溶地面塌陷的发生。
為瞭更好地給覆蓋型巖溶地麵塌陷的處置和防治提供理論依據,根據可溶巖上覆蓋層物質成分、地質結構及其物理力學性能的差異,首次將覆蓋型巖溶地麵塌陷機製區分為沙漏型、土洞型和泥流型3種類型。砂性土層分佈區,由外界因素的觸髮導緻沙顆粒嚮巖溶通道和溶洞漏失而產生的地麵塌陷現象稱為沙漏型塌陷。重力和巖溶提供的有效空間是產生沙漏型塌陷的必要條件,地下水作用加速瞭沙漏型地麵塌陷髮生,縮短瞭塌陷髮生的過程。髮生在黏性土和密實砂性土層中、由于土洞洞頂拱效應失效而產生的地麵塌陷現象稱為土洞型塌陷;天然土洞通過地錶水侵蝕與地下水潛蝕作用、砂土漏失和軟土流失等3種方式形成;土洞的形成和髮展時期內洞頂上方土體是穩定的,在外部因素觸髮而導緻洞頂拱效應失效時纔髮生地麵塌陷;土洞型塌陷具有隱蔽性和突髮性的特點。由軟弱土體流失而產生的地麵塌陷現象稱為泥流型塌陷。泥流型地麵塌陷是軟弱土體嚮溶蝕通道和溶洞中流失的結果。巖溶地麵塌陷的觸髮因素包括地下水作用(垂直和水平滲流、土/巖界麵處地下水位頻繁波動)、外加荷載(動荷載和靜荷載)和土洞頂闆抗力降低(頂闆彊度降低、厚度減薄和結構破壞)等方麵。這些外因觸髮瞭巖溶地麵塌陷的髮生。
위료경호지급복개형암용지면탑함적처치화방치제공이론의거,근거가용암상복개층물질성분、지질결구급기물리역학성능적차이,수차장복개형암용지면탑함궤제구분위사루형、토동형화니류형3충류형。사성토층분포구,유외계인소적촉발도치사과립향암용통도화용동루실이산생적지면탑함현상칭위사루형탑함。중력화암용제공적유효공간시산생사루형탑함적필요조건,지하수작용가속료사루형지면탑함발생,축단료탑함발생적과정。발생재점성토화밀실사성토층중、유우토동동정공효응실효이산생적지면탑함현상칭위토동형탑함;천연토동통과지표수침식여지하수잠식작용、사토루실화연토류실등3충방식형성;토동적형성화발전시기내동정상방토체시은정적,재외부인소촉발이도치동정공효응실효시재발생지면탑함;토동형탑함구유은폐성화돌발성적특점。유연약토체류실이산생적지면탑함현상칭위니류형탑함。니류형지면탑함시연약토체향용식통도화용동중류실적결과。암용지면탑함적촉발인소포괄지하수작용(수직화수평삼류、토/암계면처지하수위빈번파동)、외가하재(동하재화정하재)화토동정판항력강저(정판강도강저、후도감박화결구파배)등방면。저사외인촉발료암용지면탑함적발생。
In order to better provide a theoretical basis for the treatment and prevention of the covered karst collapse (CKGC ),according to the differences of material composition, geological structure, physical and mechanical properties of overburden on karst,for the first time,CKGC is divided into three types of mechanism, which are respectively called by hourglass type collapse,soil-cave type collapse and soft soil flow type collapse.In the distribution area of sandy soil,hourglass type collapse is caused by sand particles loss to the karst channels and karst caves because external factors triggering.Gravity and effective space provided by karst are necessary conditions for the occurrence of hourglass type collapse,and the role of groundwater accelerates the occurrence and shortens the process of hourglass type collapse.The ground subsidence phenomenon caused by soil-cave roof arching failure is called soil-cave type collapse occurring in clay and dense sand soil.The natural soil-cave is formed by three ways of the surface and groundwater erosion action,sand loss and soft soil flow.The roof of soil-cave is stable in the period of the formation and development of soil-cave,and ground subsidence occurs when the cave roof arching failure by triggering of external factors.The soil-cave type collapse has the characteristics of concealment and burst.The ground subsidence phenomenon caused by the soft soil flow is called as soft soil flow type collapse, is the result of the soft soil loss through karst channel and cave.The triggering factors of CKGC include groundwater action(vertical and horizontal seepage and underground water level frequent fluctuation at the soil /rock interface), external load(dynamic load and static load)and soil-cave roof resistance reduction(strength and thickness decrease and structure destruction of the roof).These external factors trigger the occurrence of CKGC.