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1 Laboratory for Applied Human Physiology, Faculty of Human Development, Kobe University, Kobe 657-8501; and 2 Institute of Health and Sports Sciences, University of Tsukuba, Tsukuba 305-8574, Japan
To investigate how the sweating response
to a sustained handgrip exercise depends on changes in the exercise
intensity, the sweating response to exercise was measured in eight
healthy male subjects. Each subject lay in the supine position in a
climatic chamber (35°C and 50% relative humidity) for ~60 min.
This exposure caused sudomotor activation by increasing skin
temperature without a marked change in internal temperature. After this
period, each subject performed isometric handgrip exercise [15,
30, 45, and 60% maximal voluntary contraction (MVC)] for 60 s.
Although esophageal and mean skin temperatures did not change with a
rise in exercise intensity and were similar at all exercise
intensities, the sweating rate (SR) on the forearm increased
significantly (P < 0.05) from baseline (0.094 ± 0.021 mg · cm
2 · min
1
at 30% MVC, 0.102 ± 0.022 mg · cm
2 · min
1
at 45% MVC, 0.059 ± 0.009 mg · cm
2 · min
1
at 60% MVC) in parallel with exercise intensity above exercise intensity at 30% MVC (0.121 ± 0.023 mg · cm
2 · min
1
at 30% MVC, 0.242 ± 0.051 mg · cm
2 · min
1
at 45% MVC, 0.290 ± 0.056 mg · cm
2 · min
1
at 60% MVC). Above 45% MVC, SR on the palm increased significantly from baseline (P < 0.05). Although SR on the forearm and palm tended to increase with a rise in exercise intensity, there was a
difference in the time courses of SR between sites. SR on the palm
showed a plateau after abrupt increase, whereas SR on the forearm
increased progressively during exercise. These results suggest that the
increase in SR with the increase in sustained handgrip exercise
intensity is due to nonthermal factors and that the magnitude of these
factors during the exercise may be responsible for the magnitude of SR.
sweating rate; skin blood flow; thermal factors; nonthermal factors; regional differences in sweating response
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