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Last words past and present, plus questions, at www.last-word.com THE LAST WORD On a high A number of athletics and cycling world records have been s...

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Last words past and present, plus questions, at www.last-word.com

THE LAST WORD On a high A number of athletics and cycling world records have been set at high-altitude venues, for example during the 1968 Olympic games in Mexico City. Presumably the air is thinner so there is less resistance, enabling them to run or cycle faster. But surely oxygen uptake at altitude is more difficult, so there must be a point at which altitude no longer favours athletes. What is this point and why? And which tracks or velodromes come nearest to it?

■ Mexico City is about 2250 metres

In the short term, athletes will breathe harder, leading to respiratory alkalaemia (increased blood pH), and heart output will increase to circulate the blood faster in an attempt to compensate. After several weeks acclimatisation, the density of blood vessels in muscle and the number of red blood cells both increase, carrying more oxygen to the working muscle. In addition, the kidneys excrete extra bicarbonate to compensate for the alkalaemia caused by rapid respiration and consequent reduction in carbon dioxide levels. These effects will not confer any advantages to the exerciser while they remain at

above sea level so as the questioner correctly points out, air is less dense here because of the “Above about 2500 metres reduced atmospheric pressure – heart rate and oxygen 580 millimetres of mercury delivery are stretched (mmHg) compared with to the utmost” 760 mmHg at sea level – so you can’t make a decent cup of tea because the water boils at 92 °C altitude, though they would as opposed to 100 °C. briefly be of benefit if the athlete This reduced density of the air were to return to sea level. undoubtedly reduces the work At yet higher altitudes, above that needs to be done by a cyclist, about 2500 metres, heart rate and who must cut a path through it, oxygen delivery are stretched to but it poses problems in terms of the utmost, beyond the ability of oxygen availability. Although the body to compensate for them, oxygen always makes up 21 per and work output and athletic cent of the atmosphere, the performance decrease. fractional pressure it exerts in It would appear that reduced Mexico City is only 120 mmHg, air density is the only explanation compared with 160 mmHg at for the performances at the 1968 sea level. This means there is Olympics, though doubtless a noticeable reduction in oxygen athletes undertook extensive pressure at the interface between altitude training. air and blood in the lungs’ alveoli, Ian Jeffcoate leading to mild hypoxia and a Department of Veterinary Cell reduction in the amount of Sciences oxygen delivered to body tissue. University of Glasgow, UK

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■ Altitude affects both running and cycling in two opposing ways. The power needed to overcome air resistance varies approximately with the velocity cubed and in direct proportion to the density of the air. The important consequences of this are that air resistance is far more significant at high speeds, and that it can be reduced by going to altitude, where the air is less dense. The other effect of thin air is that the athlete receives less oxygen. In a race lasting less than 20 seconds, most of the energy comes from oxygen-independent glycolysis, in which the muscles break down carbohydrates without requiring large amounts of oxygen. This, combined with the sprinters’ high speed, means that sprint race times will be quicker at high altitude. Competitors in longer events depend more on aerobic respiration, so for any running race taking more than about a minute the benefits of altitude are lost. In cycling, the equation differs, because the higher velocity means that up to 90 per cent of the energy expended by a cyclist is used to counter air resistance, so almost all world record times would be faster at altitude. The 400 metres athletics event sits somewhere between a flat-out sprint and an aerobic distance race. A 1991 study in the Journal of Applied Physiology (vol 70, p 399) suggests that the ideal altitude for this event would be between 2400 and 2500 metres, close to that of Mexico City.

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Indeed, one of the more enduring records set at the 1968 Olympics was achieved by Lee Evans in the 400 metres. Sam Baylis Malvern, Worcestershire, UK

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