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Introduction to Sports Biomechanics: Analysing Human Movement ...

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INTRODUCTION TO SPORTS BIOMECHANICS<br />

plane of the plate – the frictional <strong>to</strong>rque, sometimes called the free moment (Figure<br />

5.25(d)) – can be easily calculated. With appropriate knowledge of the position of the<br />

performer’s centre of mass, in principle at one instant only, the component <strong>to</strong>rques<br />

(moments) of the ground contact force (Figure 5.25(d)) can also be calculated about the<br />

two horizontal and mutually perpendicular axes passing through the performer’s centre<br />

of mass and parallel <strong>to</strong> the plate.<br />

From the force–time and <strong>to</strong>rque–time data, integration can be performed <strong>to</strong> find<br />

overall or instant-by-instant changes in centre of mass velocity and whole-body angular<br />

momentum. Absolute magnitudes of these variables at all instants (Figures 5.25(e) and<br />

(f)) can be calculated only if their values are known at least at one instant. These values<br />

could be obtained from videography or another motion analysis system. They are easily<br />

obtained if the performer is at rest on the plate at some instant, when both linear<br />

and angular momentums are zero. If absolute velocities are known, then the changes<br />

in position – displacement – can be found by integration. In this case, absolute values<br />

of the position of the centre of mass with respect <strong>to</strong> the plate coordinate system<br />

(Figure 5.25(g)) can be obtained if that position is known for at least one instant. Again,<br />

that value could be obtained from videography or another motion analysis system.<br />

Alternatively, the horizontal coordinates can be obtained from the centre of pressure<br />

position with the person stationary on the plate, and the vertical coordinate as a fraction<br />

of the person’s height.<br />

Figure 5.26 (a) Side view of force vec<strong>to</strong>rs for a standing broad jump; (b) centre of pressure path from above. (S shows the start<br />

of the movement and T take-off.) Note: (a) and (b) are not <strong>to</strong> the same scale.<br />

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