| Literature DB >> 25210709 |
Clément Bougard1, Damien Davenne2.
Abstract
The underlying processes responsible for the differences between morning and afternoon measurements of postural control have not yet been clearly identified. This study was conducted to specify the role played by vestibular, visual, and somatosensory inputs in postural balance and their link with the diurnal fluctuations of body temperature and vigilance level. Nineteen healthy male subjects (mean age: 20.5 ± 1.3 years) participated in test sessions at 6:00 a.m. and 6:00 p.m. after a normal night's sleep. Temperature was measured before the subjects completed a sign cancellation test and a postural control evaluation with eyes both open and closed. Our results confirmed that postural control improved throughout the day according to the circadian rhythm of body temperature and sleepiness/vigilance. The path length as a function of surface ratio increased between 6:00 a.m. and 6:00 p.m. This is due to a decrease in the centre-of-pressure surface area, which is associated with an increase in path length. Romberg's index did not change throughout the day; however, the spectral analysis (fast Fourier transform) of the centre-of-pressure excursions (in anteroposterior and mediolateral directions) indicated that diurnal fluctuations in postural control may occur via changes in the different processes responsible for readjustment via muscle contractions.Entities:
Mesh:
Year: 2014 PMID: 25210709 PMCID: PMC4151602 DOI: 10.1155/2014/287436
Source DB: PubMed Journal: Biomed Res Int Impact factor: 3.411
Oral temperature, sign cancellation test, and posturography parameters in subjects under eyes open (EO) and eyes closed (EC) conditions at 6:00 a.m. and 6:00 p.m. (mean ± SD; n = 19).
| 6:00 a.m. | 6:00 p.m. | ||
|---|---|---|---|
| Oral temperature (°C) | 35.99 ± 0.32 | 36.77 ± 0.22* | |
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| Sign cancellation test (s.) | 340.36 ± 62.46 | 287.01 ± 53.41* | |
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| COP surface area (mm2) | EO | 120.73 ± 62.89 | 89.03 ± 40.21* |
| EC | 179.76 ± 86.52 | 128.89 ± 60.43* | |
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| PL (mm) | EO | 375.28 ± 117.34 | 423.49 ± 107.28* |
| EC | 539.86 ± 143.57 | 539.28 ± 149.04 | |
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| Mediolateral PL (mm) | EO | 188.23 ± 63.09 | 208.91 ± 54.59* |
| EC | 251.64 ± 78.33 | 247.95 ± 68.87 | |
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| Anteroposterior PL (mm) | EO | 284.25 ± 90.96 | 316.07 ± 88.32 |
| EC | 424.58 ± 114.18 | 420.51 ± 130.14 | |
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| LFS ratio | EO | 0.86 ± 0.28 | 0.98 ± 0.22* |
| EC | 0.96 ± 0.26 | 0.99 ± 0.24 | |
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| Romberg's index | 168.54 ± 84.14 | 150.67 ± 50.46 | |
COP surface area: centre-of-pressure surface area; PL: path length; anteroposterior PL: anteroposterior path length; lateral PL: lateral path length; LFS ratio: path length as a function of surface; Romberg's index: ratio between the centre-of-pressure surface areas measured under the eyes open (EO) and eyes closed (EC) conditions. ∗Significant difference between 6:00 a.m. and 6:00 p.m.
Figure 1Percentage of total spectral energy in the anteroposterior direction (a) and mediolateral direction (b) measured at 6:00 a.m. and 6:00 p.m. Top: high-frequency band. Middle: medium-frequency band. Bottom: low-frequency band. **indicates a significant difference (P < 0.01); *P < 0.05.
Figure 2Processes involved in changes in postural strategies between morning and evening measurements. COP surface area: center-of-pressure surface area; +: 6:00 a.m. < 6:00 p.m.; −: 6:00 a.m. > 6:00 p.m.