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Wave Theory of Seismic Resistance of Underground Pipelines

机译:地下管道地震抗震波理论

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摘要

The object of the research is an underground straight horizontal pipeline subjected to seismic impact. The research method was analytical. The results were compared with the experimental results of other authors and computer calculations. It was shown that the main disadvantage of the dynamic theory of seismic resistance of underground pipelines is the neglect of the dynamic stress state in soil under seismic wave propagation. The next drawback of the dynamic theory is an inaccurate, approximate accounting for the displacement of the soil medium to which the underground pipeline is embedded. The complete interaction process includes the stages of nonlinear changes in the interaction force (the friction force) by manifesting its peak value and the Coulomb friction. The contact layer of soil undergoes shear deformations until complete structural destruction of the soil contact layer. The interaction force is the friction force, and its peak value does not appear. The seismic resistance of underground pipelines should be considered based on the theory of propagating seismic waves in a soil medium and the interaction of seismic waves with underground pipelines, i.e., based on the wave theory of seismic resistance of underground pipelines. A one-dimensional coupled problem of seismic resistance of underground pipelines under seismic impacts was posed based on the wave theory. An algorithm and a program for the numerical solution of the stated wave problems were developed using the method of characteristics and the method of finite differences. An analysis of the laws of interaction of underground pipelines with soil under seismic influences shows that it is necessary to use in the calculations the laws of interaction that account for the complete interaction processes observed in experiments. The analysis of the obtained numerical solutions and the posed coupled problems of the wave theory of seismic resistance of underground pipelines show the occurrence mechanisms of longitudinal stresses in underground pipelines under seismic influences. The results of calculations stated that an account for the dynamic stress normal to the underground pipeline’s outer surface leads to multiple increases in longitudinal stress in the underground pipeline. This multiple increase is due to the transformation of the interaction force into an active frictional force, resulting from a greater strain in soil than the one in the underground pipeline. Based on the analysis results, a theory of the seismic wave propagation process in an underground pipeline and surrounding soil was proposed.
机译:该研究的目的是一种遭受地震影响的地下横向水平管道。研究方法是分析的。将结果与其他作者和计算机计算的实验结果进行了比较。结果表明,地下管道的地震抗震性能的动态理论的主要缺点是忽视地震波传播下土壤中的动态应力状态。动态理论的下一个缺点是一种不准确的,对地下管线嵌入的土壤介质的移位的近似核算。完整的相互作用过程包括通过体现其峰值和库仑摩擦来包括相互作用力(摩擦力)的非线性变化的阶段。土壤接触层经历剪切变形,直到土壤接触层的完全结构破坏。相互作用力是摩擦力,并且不会出现其峰值。基于土壤介质中的地震波的理论以及地震波与地下管道的相互作用,基于地下管道波理论,基于地下管道的地震波的相互作用,基于地下管道的相互作用的地震管道的地震抗性。基于波理论,摆动地震撞击下地下管道抗震性抗震性的一维耦合问题。使用特性方法和有限差异方法开发了算法和规定波问题的数值解的程序。地震影响下土壤与土壤相互作用规律的分析表明,在计算实验中观察到的完全相互作用过程的互动规律是必要的。地下管道地震抗震波理论的测量数值求解的分析显示地震影响下地下管道纵向应力的发生机制。计算结果表明,用于地下管道的外表面的动态应力的账户导致地下管道纵向应力的多次增加。这种多个增加是由于相互作用力的变化为活性摩擦力,由土壤中的较大菌株比地下管道中的一个更大。基于分析结果,提出了地下管线和周围土壤中地震波传播过程的理论。

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