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Worksheet 11.1 Exercises for Parametrization of Plane Curves

If you would like to review this topic before attempting the exercises, click Parametrization of Plane Curves.
The exercises below on the velocity and direction of a projectile after a given time use the figure of a projectile at a general instant.
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Figure 11.1. A particle projected from \(O\) with speed \(v_0\) at elevation \(\theta\text{.}\) At the point \(P\) reached after time \(t\text{,}\) the velocity \(v\) is tangent to the path and makes an angle \(\phi\) with the horizontal; \(h\) is the depth of \(P\) below the directrix.

1.

A particle is projected from \(O\) with speed \(v_0\) at an elevation \(\theta\) to the horizontal, as in FigureΒ 11.1. At time \(t\) it is at the point \(P\text{,}\) moving with speed \(v\) in a direction making an angle \(\phi\) with the horizontal. Show that
\begin{equation*} v = \sqrt{\,v_0^2 - 2\,v_0\,g\,t\sin\theta + g^2 t^2\,} \end{equation*}
and
\begin{equation*} \tan\phi = \frac{v_0\sin\theta - g\,t}{v_0\cos\theta}\text{.} \end{equation*}
Solution.
Take the origin at \(O\) with horizontal and vertical axes. The coordinates of \(P\) at time \(t\) are
\begin{equation*} x = v_0\cos\theta\;t\text{,} \qquad y = v_0\sin\theta\;t - \tfrac{1}{2}g\,t^2\text{.} \end{equation*}
The horizontal and vertical components of the velocity are the time derivatives of these, so
\begin{equation*} v\cos\phi = \frac{dx}{dt} = v_0\cos\theta\text{,} \qquad v\sin\phi = \frac{dy}{dt} = v_0\sin\theta - g\,t\text{.} \end{equation*}
Squaring and adding eliminates \(\phi\text{:}\)
\begin{equation*} v^2 = v_0^2\cos^2\theta + \bigl(v_0\sin\theta - g\,t\bigr)^2 = v_0^2 - 2\,v_0\,g\,t\sin\theta + g^2 t^2\text{,} \end{equation*}
which gives the speed at time \(t\text{.}\) Dividing the vertical component by the horizontal component gives the direction,
\begin{equation*} \tan\phi = \frac{v_0\sin\theta - g\,t}{v_0\cos\theta}\text{,} \end{equation*}
that is, \(\phi = \arctan\!\left(\dfrac{v_0\sin\theta - g\,t}{v_0\cos\theta}\right)\text{.}\)

2.

The directrix of the parabolic path is the horizontal line at height \(\dfrac{v_0^2}{2g}\) above \(O\text{.}\) Using the previous exercise, show that the speed of the particle at \(P\) is equal to the speed it would acquire by falling freely from the level of the directrix down to \(P\text{.}\) That is, if \(h\) denotes the depth of \(P\) below the directrix (see FigureΒ 11.1), then \(v^2 = 2\,g\,h\text{.}\)
Solution.
From the previous exercise,
\begin{equation*} v^2 = v_0^2 - 2\,v_0\,g\,t\sin\theta + g^2 t^2 = v_0^2 - 2g\!\left(v_0\,t\sin\theta - \tfrac{1}{2}g\,t^2\right) = v_0^2 - 2 g y\text{,} \end{equation*}
since \(y = v_0\,t\sin\theta - \tfrac{1}{2}g\,t^2\) is the height of \(P\text{.}\) Writing this as
\begin{equation*} v^2 = 2g\!\left(\frac{v_0^2}{2g} - y\right) \end{equation*}
and recognizing \(\dfrac{v_0^2}{2g}\) as the height of the directrix above \(O\text{,}\) the quantity \(h = \dfrac{v_0^2}{2g} - y\) is exactly the depth of \(P\) below the directrix. Hence \(v^2 = 2\,g\,h\text{,}\) the square of the speed gained by falling freely through the height \(h\text{.}\)
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