CAJ | 학술논문

小石槽沟村位于河南省南阳市淅川县荆紫关镇东南部，豫、鄂、陕三省结合部，是河南省的一块“飞地”，属低山丘陵区，地形起伏较大，沟谷发育，岩层坡度较陡，为山体滑坡的形成提供了有利地形条件。为了有效地防灾减灾，本文以小石槽沟滑坡为典型实例，从滑坡形态特征、形成条件、触发因素等角度入手，阐述了该区滑坡发生的机理，在此基础上对当前滑坡所处的稳定程度进行了分析。并提出了滑坡工程治理的具体方案，对该地区滑坡防治有参考价值。
소석조구촌위우하남성남양시석천현형자관진동남부，예、악、협삼성결합부，시하남성적일괴“비지”，속저산구릉구，지형기복교대，구곡발육，암층파도교두，위산체활파적형성제공료유리지형조건。위료유효지방재감재，본문이소석조구활파위전형실례，종활파형태특정、형성조건、촉발인소등각도입수，천술료해구활파발생적궤리，재차기출상대당전활파소처적은정정도진행료분석。병제출료활파공정치리적구체방안，대해지구활파방치유삼고개치。
The village of Xiaoshicaogou is located in the southeast of Zijingguan Town NanyangCity HenanProvince,which lies just to the east of Shanxi Province and borders Henan and Hebei, is sparsely populated with large areas of desert, low mountains and small villages. This place is a low mountains and hills areas with more stronger topographic relief and developed gully,a steep mountain slope, which is a“enclave”of henan province. For example Xiaoshicaogou landslide in the paper, in order to effectively disaster prevention and mitigation, the author is based on the landslide characteristics,forming conditions and triggers. The mechanism is stated and some relative solutions to the problem are presented.In order to evaluate its stability, detailed geological.