| Literature DB >> 26368131 |
Silvia Fantozzi1, Andrea Giovanardi2, Davide Borra1, Giorgio Gatta3.
Abstract
Walking is one of the fundamental motor tasks executed during aquatic therapy. Previous kinematics analyses conducted using waterproofed video cameras were limited to the sagittal plane and to only one or two consecutive steps. Furthermore, the set-up and post-processing are time-consuming and thus do not allow a prompt assessment of the correct execution of the movements during the aquatic session therapy. The aim of the present study was to estimate the 3D joint kinematics of the lower limbs and thorax-pelvis joints in sagittal and frontal planes during underwater walking using wearable inertial and magnetic sensors. Eleven healthy adults were measured during walking both in shallow water and in dry-land conditions. Eight wearable inertial and magnetic sensors were inserted in waterproofed boxes and fixed to the body segments by means of elastic modular bands. A validated protocol (Outwalk) was used. Gait cycles were automatically segmented and selected if relevant intraclass correlation coefficients values were higher than 0.75. A total of 704 gait cycles for the lower limb joints were normalized in time and averaged to obtain the mean cycle of each joint, among participants. The mean speed in water was 40% lower than that of the dry-land condition. Longer stride duration and shorter stride distance were found in the underwater walking. In the sagittal plane, the knee was more flexed (≈ 23°) and the ankle more dorsiflexed (≈ 9°) at heel strike, and the hip was more flexed at toe-off (≈ 13°) in water than on land. On the frontal plane in the underwater walking, smoother joint angle patterns were observed for thorax-pelvis and hip, and ankle was more inversed at toe-off (≈ 7°) and showed a more inversed mean value (≈ 7°). The results were mainly explained by the effect of the speed in the water as supported by the linear mixed models analysis performed. Thus, it seemed that the combination of speed and environment triggered modifications in the joint angles in underwater gait more than these two factors considered separately. The inertial and magnetic sensors, by means of fast set-up and data analysis, can supply an immediate gait analysis report to the therapist during the aquatic therapy session.Entities:
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Year: 2015 PMID: 26368131 PMCID: PMC4569370 DOI: 10.1371/journal.pone.0138105
Source DB: PubMed Journal: PLoS One ISSN: 1932-6203 Impact factor: 3.240
Fig 1Set-up protocol.
Round plastic boxes for waterproofing the sensors (A). 8 IMMUs fixed to the body segments of the participant by means of elastic bands (B).
Mean and standard deviation values (n = 704 gait cycles in 11 participants) of the parameters that were found different and explained by the different effect of environment and/or of walking speed.
The coefficient of the linear mixed models were reported. * referred to values with p<0.05.
| Mean ± std.dev | Coefficients of Linear mixed models | ||||||||
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| Stride duration [s] | 1.1 ± 0.1 | 2.8 ± 0.7 |
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| Stance percentage [%] | 57.9 ± 2.6 | 59.8 ± 4.6 |
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| Stride distance [cm] | 161.2 ± 13.8 | 150.2 ± 12.1 |
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| Flexion-Extension at toe-off [deg] | -2.1 ± 5.7 | 11.2 ± 9.1 |
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| Flexion-Extension maximum [deg] | 25.0 ± 3.0 | 32.9 ± 7.2 |
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| Flexion-Extension minimum [deg] | -11.1 ± 3.9 | -2.7 ± 6.6 |
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| Flexion-Extension at heel strike [deg] | -3.5 ± 5.7 | 19.4 ± 7.7 |
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| Flexion-Extension maximum [deg] | 56.8 ± 4.4 | 64.9 ± 18.8 |
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| Flexion-Extension Range of Motion [deg] | 64.9 ± 3.8 | 60.0 ± 18.0 |
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| Dorsi-Plantar flexion at heel strike [deg] | -6.6 ± 5.3 | 2.8 ± 7.8 |
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| Dorsi-Plantar flexion Range of Motion [deg] | 29.8 ± 4.3 | 38.4 ± 13.7 |
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| Inversion-Eversion at toe-off [deg] | 11.0 ± 6.2 | 17.5 ± 8.7 |
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| Inversion-Eversion mean [deg] | 3.1 ± 2.7 | 10.3 ± 5.8 |
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Fig 2Angular kinematic patterns of the lower limb joints (hip, knee, and ankle) in the sagittal plane.
Mean values plus and minus one standard deviation for all the participants for Dry-Land (black solid line and grey shaded area) and Under-Water (blue solid line and blue stripes area) conditions.
Fig 3Angular kinematic patterns of the thorax-pelvis, hip, and ankle joints in the frontal plane.
Mean values plus and minus one standard deviation for all the participants for Dry-Land (black solid line and grey shaded area) and Under-Water (blue solid line and blue stripes area) conditions.