Oxygen uptake and blood metabolic responses to a 400-m run

Springer Science and Business Media LLC - Tập 109 - Trang 233-240 - 2010
Christine Hanon1, Pierre-Marie Lepretre1,2, David Bishop3, Claire Thomas1,4
1Laboratory of Biomechanics and Physiology, French National Institute of Sports (INSEP), Paris, France
2University of Picardie Jules Verne, Amiens Cedex, France
3Institute of Sport, Exercise and Active Living (ISEAL), Victoria University, Melbourne, Australia
4STAPS Department, EA 3872, University of Evry Val d’Essonne, Evry, France

Tóm tắt

This study aimed to investigate the oxygen uptake and metabolic responses during a 400-m run reproducing the pacing strategy used in competition. A portable gas analyser was used to measure the oxygen uptake $$ \left( {\dot{V}{{{\text{O}}_{ 2} }} } \right) $$ of ten specifically trained runners racing on an outdoor track. The tests included (1) an incremental test to determine maximal $$ \dot{V}{{{\text{O}}_{ 2} }} \,\left( {\dot{V}{{{\text{O}}_{{ 2 {\text{max}}}} }} } \right) $$ and the velocity associated with $$ \dot{V}{{{\text{O}}_{{ 2 {\text{max}}}} }} \left( {{\text{v}}-\dot{V}{{{\text{O}}_{{ 2 {\text{max}}}} }} } \right), $$ (2) a maximal 400-m (400T) and 3) a 300-m running test (300T) reproducing the exact pacing pattern of the 400T. Blood lactate, bicarbonate concentrations $$ \left[ {{\text{HCO}}_{ 3}^{ - } } \right], $$ pH and arterial oxygen saturation were analysed at rest and 1, 4, 7, 10 min after the end of the 400 and 300T. The peak $$ \dot{V}{{{\text{O}}_{ 2} }} $$ recorded during the 400T corresponded to 93.9 ± 3.9% of $$ \dot{V}{{{\text{O}}_{2\max } }} $$ and was reached at 24.4 ± 3.2 s (192 ± 22 m). A significant decrease in $$ \dot{V}{{{\text{O}}_{ 2} }} $$ (P < 0.05) was observed in all subjects during the last 100 m, although the velocity did not decrease below $$ {\text{v}}-\dot{V}_{{{\text{O}}_{{ 2 {\text{max}}}} }} . $$ The $$ \dot{V}{{{\text{O}}_{ 2} }} $$ in the last 5 s was correlated with the pH (r = 0.86, P < 0.0005) and $$ \left[ {{\text{HCO}}_{ 3}^{ - } } \right] $$ (r = 0.70, P < 0.05) measured at the end of 300T. Additionally, the velocity decrease observed in the last 100 m was inversely correlated with $$ \left[ {{\text{HCO}}_{ 3}^{ - } } \right] $$ and pH at 300T (r = −0.83, P < 0.001, r = −0.69, P < 0.05, respectively). These track running data demonstrate that acidosis at 300 m was related to both the $$ \dot{V}{{{\text{O}}_{ 2} }} $$ response and the velocity decrease during the final 100 m of a 400-m run.

Tài liệu tham khảo

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