An Analysis of Thickness-shear Vibrations of an Annular Plate with the Mindlin Plate Equations

TL;DR

This paper derives and validates Mindlin plate equations for analyzing thickness-shear vibrations in annular quartz crystal resonators, aiding optimal design for energy trapping and mode purity.

Contribution

It extends Mindlin plate theory to annular plates with fixed inner and free outer edges, providing detailed frequency analysis for resonator design.

Findings

Validated equations near fundamental thickness-shear frequency

Provided frequency spectra for annular plates

Guided optimal parameter selection for energy trapping

Abstract

The Mindlin plate equations with the consideration of thickness-shear deformation as an independent variable have been used for the analysis of vibrations of quartz crystal resonators of both rectangular and circular types. The Mindlin or Lee plate theories that treat thickness-shear deformation as an independent higher-order vibration mode in a coupled system of two-dimensional variables are the choice of theory for analysis. For circular plates, we derived the Mindlin plate equations in a systematic manner as demonstrated by Mindlin and others and obtained the truncated two-dimensional equations of closely coupled modes in polar coordinates. We simplified the equations for vibration modes in the vicinity of fundamental thickness-shear frequency and validated the equations and method. To explore newer structures of quartz crystal resonators, we utilized the Mindlin plate equations for the analysis of annular plates with fixed inner and free outer edges for frequency spectra. The detailed analysis of vibrations of circular plates for the normalized frequency versus dimensional parameters provide references for optimal selection of parameters based on the principle of strong thickness-shear mode and minimal presence of other modes to enhance energy trapping through maintaining the strong and pure thickness-shear vibrations insensitive to some complication factors such as thermal and initial stresses.