白光顺, 张世涛, 刘渊, 杨雪梅, 朱杰勇. 2016: 基于关键层理论的盐岩单井水溶溶腔覆岩垮落带的确定. 工程地质学报, 24(s1): 1152-1155. DOI: 10.13544/j.cnki.jeg.2016.s1.166
    引用本文: 白光顺, 张世涛, 刘渊, 杨雪梅, 朱杰勇. 2016: 基于关键层理论的盐岩单井水溶溶腔覆岩垮落带的确定. 工程地质学报, 24(s1): 1152-1155. DOI: 10.13544/j.cnki.jeg.2016.s1.166
    BAI Guangshun, ZHANG Shitao, LIU Yuan, YANG Xuemei, ZHU Jieyong. 2016: THE DETERMINATION OF SALT SINGLE WELL SOLUTION CAVITY OVERLYING STRATA CAVING ZONE ON KEY STRATUM THEORY. JOURNAL OF ENGINEERING GEOLOGY, 24(s1): 1152-1155. DOI: 10.13544/j.cnki.jeg.2016.s1.166
    Citation: BAI Guangshun, ZHANG Shitao, LIU Yuan, YANG Xuemei, ZHU Jieyong. 2016: THE DETERMINATION OF SALT SINGLE WELL SOLUTION CAVITY OVERLYING STRATA CAVING ZONE ON KEY STRATUM THEORY. JOURNAL OF ENGINEERING GEOLOGY, 24(s1): 1152-1155. DOI: 10.13544/j.cnki.jeg.2016.s1.166

    基于关键层理论的盐岩单井水溶溶腔覆岩垮落带的确定

    THE DETERMINATION OF SALT SINGLE WELL SOLUTION CAVITY OVERLYING STRATA CAVING ZONE ON KEY STRATUM THEORY

    • 摘要: 本文分析提出了溶腔层状覆岩中关键层的破断影响着溶腔覆岩中垮落带的发育高度,基于关键层理论推导出确定盐岩单井水溶溶腔层状覆岩垮落带发育高度的方法和判据。选用弹性圆薄板理论建立了盐岩单井水溶开采溶腔覆岩关键层判别基本模型,推导出了岩溶单井水溶开采溶腔层状覆岩中关键层的确定方法;建立了溶腔层状覆岩中关键层悬露直径是否小于2a1是关键层是否发生破断的判据;根据关键层破断后形成的岩块之间的力学关系,推导了判断关键层发生破断情况下是形成断块铰合而不垮落,还是直接垮落的判据。

       

      Abstract: This paper investigatesandproposes the breaking of cavity layered overlying strata effecting caving zone height, and provides the determination method and criterion of caving zone height of salt single well solution cavity by the key stratum theory. This paper establishes the determination model of key stratum of salt single well solution cavity layered overlying strata by the elastic thin circular plate theory, provides the determination method of key stratum of salt single well solution cavity layered overlying strata, establishes that the hanging dew diameter of ke y stratum of salt single well solution cavity layered overlying strata less than the 2a1 is the criterion of key stratum breaking, and provides the criterion for judging the key stratum producing hinge and does not collapse, or direct collapse when breaking, according to the mechanical relationship between the formation of key stratum fractured rocks.

       

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