| EFFECT
OF 30°C HEAT ON THE ANAEROBIC CAPACITY OF HEAT ACCLIMATISED ATHLETES
|
James P. Finn1,2 ,
Rob J. Wood1 and John F. Marsden11 |
1National Heat Training and Acclimatisation Centre, Northern
Territory Institute of Sport, Marrara, Australia.
2School of Health Sciences, Northern Territory University, Darwin,
Australia.
| Received |
|
28 August 2003 |
| Accepted |
|
31
October 2003
|
| Published |
|
01 December 2003 |
©
Journal of Sports Science and Medicine (2003) 2, 158-162
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The main finding of
this study was that for heat acclimatised athletes, there was no significant
difference (p=0.58) in anaerobic capacity for temperate (21.8 ± 0.5 °C;
52 ± 5 % relative humidity) compared with warm conditions (29.6 ± 0.5 °C;
51 ± 9 % relative humidity). Anaerobic capacity was estimated using the
maximal accumulated oxygen deficit (MAOD) during constant intensity cycling
at 120% peak rate of O2 consumption until exhaustion. This yielded mean
MAOD values of 3.3 ± 0.9 and 3.5 ± 1.1 L for temperate and warm conditions,
respectively. Peak post-exercise lactate values of 14.7 ± 3.8 and 14.4 ±
4.5 mmol·L-1 for temperate and warm conditions respectively, were also not
significantly different (p=0.72). Time to exhaustion (TTE) was similarly
unchanged (p=0.56), being 175 ± 19 and 170 ± 18 s for temperate and warm
conditions, respectively. These results suggest that the MAOD remains a
valid test throughout environmental temperatures for the range of 20-30
°C when used with heat acclimatised athletes.
KEY WORDS: Maximal accumulated oxygen deficit, anaerobic metabolism,
environmental temperature, maximal exercise
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