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Derivation and application of an analytical rock displacement solution on rectangular cavern wall using the inverse mapping method

机译:用逆映射方法推导矩形洞壁解析位移的方法及应用

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摘要

Rectangular caverns are increasingly used in underground engineering projects, the failure mechanism of rectangular cavern wall rock is significantly different as a result of the cross-sectional shape and variations in wall stress distributions. However, the conventional computational method always results in a long-winded computational process and multiple displacement solutions of internal rectangular wall rock. This paper uses a Laurent series complex method to obtain a mapping function expression based on complex variable function theory and conformal transformation. This method is combined with the Schwarz-Christoffel method to calculate the mapping function coefficient and to determine the rectangular cavern wall rock deformation. With regard to the inverse mapping concept, the mapping relation between the polar coordinate system within plane ς and a corresponding unique plane coordinate point inside the cavern wall rock is discussed. The disadvantage of multiple solutions when mapping from the plane to the polar coordinate system is addressed. This theoretical formula is used to calculate wall rock boundary deformation and displacement field nephograms inside the wall rock for a given cavern height and width. A comparison with ANSYS numerical software results suggests that the theoretical solution and numerical solution exhibit identical trends, thereby demonstrating the method’s validity. This method greatly improves the computing accuracy and reduces the difficulty in solving for cavern boundary and internal wall rock displacements. The proposed method provides a theoretical guide for controlling cavern wall rock deformation failure.
机译:矩形洞室越来越多地用于地下工程项目中,矩形洞室围岩的破坏机理由于横截面形状和壁应力分布的变化而显着不同。然而,传统的计算方法总是导致冗长的计算过程和内部矩形壁岩的多重位移解。本文基于复杂变量函数理论和保形变换,采用Laurent级数复杂方法获得了映射函数表达式。该方法与Schwarz-Christoffel方法相结合,以计算映射函数系数并确定矩形洞壁的岩石变形。关于逆映射概念,讨论了平面ς中的极坐标系与洞壁岩石内部相应的唯一平面坐标点之间的映射关系。解决了从平面到极坐标系的映射时多种解决方案的缺点。对于给定的洞穴高度和宽度,该理论公式用于计算围岩边界变形和围岩内部的位移场云图。与ANSYS数值软件结果的比较表明,理论解和数值解具有相同的趋势,从而证明了该方法的有效性。该方法大大提高了计算精度,减少了求解洞室边界和内墙岩体位移的难度。该方法为控制洞室围岩变形破坏提供了理论指导。

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