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Skeletal muscle transverse strain during isometric contraction at different lengths
C C van Donkelaar1, P J Willems, A M Muijtjens
1Department of Movement Sciences, Cardiovascular Research Institute Maastricht (Carim), The Netherlands.
Journal of Biomechanics
|August 5, 1999
Summary
Plane strain models inadequately capture skeletal muscle contraction's 3D deformation. Muscle length significantly impacts transverse strains, limiting the applicability of 2D models for studying length-dependent effects.
Area of Science:
- Biomechanics
- Skeletal Muscle Physiology
- Computational Modeling
Background:
- Two-dimensional (2D) numerical models of skeletal muscle contraction often assume plane strain conditions.
- These models may overlook crucial three-dimensional (3D) deformations occurring in the muscle section.
Purpose of the Study:
- To investigate the validity of the plane strain assumption in 2D skeletal muscle models.
- To quantify 3D muscle surface deformation during isometric contractions at varying muscle lengths.
Main Methods:
- 3D muscle surface deformation was measured using marker displacements.
- Measurements were taken during isometric contractions across a range of initial muscle lengths.
- Longitudinal and transverse strains of superficial muscle fibers and aponeurosis were analyzed.
Main Results:
- Longitudinal and transverse strains in muscle fibers and aponeurosis varied with initial muscle length.
- Transverse strains were comparable at intermediate lengths but diverged at short and long lengths.
- Muscle fiber surface area change was approximately -11% and independent of muscle length, suggesting a 3D strain of 11% perpendicular to the surface.
Conclusions:
- The plane strain assumption is insufficient for studying the effect of muscle length on skeletal muscle deformation.
- 2D models may be suitable for contractions with ~ -9% longitudinal strain where transverse strains are minimal.
- Superficial muscle fibers likely flatten during isometric contractions, a phenomenon not fully captured by 2D models.