层状介质的等效性质

A.H. Hadjian, Byrwec Ellison
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引用次数: 2

摘要

对于一类重要的土-结构相互作用问题,土介质具有非均匀性。这包括层状场地和具有深度相关刚度特征的连续土。提出了一种近似的方法来描述这些地点,以帮助初步分析。虽然存在非均匀介质分析的数值求解技术,但也有基于均匀介质的近似方法。为了便于将后一种方法应用于非均匀介质,用等效均匀介质的性质来近似其性质。在垂直运动中,非均匀介质由一系列受应力水平随深度影响的弹簧来模拟。弹簧系统然后被一个弹簧取代,因此,一个单一的均匀半空间。这种分析的结果外推到除垂直运动以外的自由度。该方法同时适用于刚度和阻尼,在刚度或阻尼的每个自由度上给出一组不同的等效均匀特性。算例表明,该方法对阻抗值的求解结果可靠。这种近似在岩土工程精度范围内是可以接受的。唯一的不保守性出现在平动阻尼值上,因为该方法没有考虑分层对辐射阻尼的影响。建议采用一个整体阻尼减少系数来考虑这些影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Equivalent properties for layered media

For a significant class of soil-structure interaction problems, soil media have nonuniform properties. This includes both layered sites and soil continua with depth-dependent stiffness characteristics. An approximate method to characterize such sites is proposed as an aid to preliminary analysis.

Although numerical solution techniques exist for nonuniform media analysis, there are also appoximate methods based on uniform media. To aid in applying the latter method to a nonuniform medium, its properties are approximated by those of an equivalent uniform medium. In vertical motion, the nonuniform medium is modeled by a series of springs as influenced by stress level with depth. The spring system is then replaced by a single spring and hence, a single uniform half-space. The results of this type of analysis are extrapolated to degrees of freedom other than vertical motion. The method is applied to both stiffness and damping, giving a different set of equivalent uniform properties for each degree of freedom in either stiffness or damping.

An example problem indicates that the proposed method yields reliable results for impedance values. The approximation is acceptable within the limits of geotechnical accuracy. The only unconservatism occurs for values of translational damping because the method does not consider layering effects on radiation damping. A blanket damping reduction factor is recommended to account for those effects.

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