Slow deformation of intervertebral discs.
Intervertebral discs exhibit pronounced time-dependent deformations when subjected to load variations. These deformations are caused by fluid flow to and from the disc and by viscoelastic deformation of annulus fibres. The fluid flow is caused by differences between mechanical and osmotic pressure. A mechanical model of lumbar disc functions allows one to calculate both the extent of fluid flow and its implications for disc height as well as the role played by viscoelastic deformation of annulus fibres. From such calculations changes in body height are estimated. Experimental results already documented in the literature offer bases for the determination of the parameters involved. Body height variations are studied, both those related to normal diurnal rhythmicity and those related to somewhat exceptional circumstances. The normal diurnal fluid flow is found to be about +/- 40% of the disc fluid content late in the evening. Viscoelastic deformation of annulus fibres contributes approximately one quarter of the height change obtained after several hours normal activity, but dominates during the first hour.
Broberg
K B
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D000328:Adult; D001834:Body Water / Q000502:physiology; D002940:Circadian Rhythm; D004548:Elasticity; D006801:Humans; D007403:Intervertebral Disc / Q000033:anatomy & histology / Q000502:physiology*; D008124:Locomotion / Q000502:physiology; D008159:Lumbar Vertebrae; D008297:Male; D008954:Models, Biological; D011187:Posture / Q000502:physiology; D011312:Pressure; D012212:Rheology; D012420:Running / Q000502:physiology; D013314:Stress, Mechanical; D013997:Time Factors; D014783:Viscosity; D016474:Weight-Bearing / Q000502:physiology; D014893:Weightlessness