A particle dropped from a vertical height and falls freely for a time interval t. Sketch and explain a graph to show how h varies with (a) t (b) t\(^{2}\).
A particle dropped from a vertical height and falls freely for a time interval t. Sketch and explain a graph to show how h varies with (a) t (b) t\(^{2}\).
Take h as the height of the particle above the ground and let it be released from rest from a height H. Since the fall is free (only gravity acts), the distance fallen after time t is \(\tfrac{1}{2}gt^{2}\), so the height still remaining above the ground is
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\[ h = H - \tfrac{1}{2}\,g\,t^{2}. \]
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Using \(H = 45\ \text{m}\) and \(g = 10\ \text{m s}^{-2}\) as a worked illustration, \(h = 45 - 5t^{2}\). The values are:
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\n
t /s
0
0.5
1.0
1.5
2.0
2.5
3.0
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t\(^{2}\) /s\(^{2}\)
0
0.25
1.0
2.25
4.0
6.25
9.0
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h /m
45
43.75
40
33.75
25
13.75
0
\n
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(a) How h varies with t
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h against t: starts at the release height H and curves downward (concave-down parabola), falling faster as time increases.
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Because \(h = H - \tfrac{1}{2}gt^{2}\), the term subtracted grows as the square of the time. The graph therefore starts at \(h = H\) on the vertical axis and curves downward (a parabola, concave down). Its slope, which is the negative of the speed \(\left(\dfrac{dh}{dt} = -gt\right)\), is zero at the instant of release and becomes steadily steeper as the particle accelerates, reaching the ground (\(h = 0\)) after \(t = 3\ \text{s}\). So h falls slowly at first and ever faster afterwards, giving a curved (non-linear) graph.
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(b) How h varies with t\(^{2}\)
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h against t^2: a straight line of intercept H = 45 m and negative slope -1/2 g = -5 m/s^2, giving g = 10 m/s^2.
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Writing \(x = t^{2}\), the relation becomes \(h = H - \tfrac{1}{2}g\,x\), which is of the linear form \(y = c + mx\). The graph of h against \(t^{2}\) is therefore a straight line with
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intercept on the h-axis equal to the release height, \(c = H = 45\ \text{m}\);
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a negative slope equal to \(-\tfrac{1}{2}g\).
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Reading the slope from the line, \[ \text{slope} = \frac{0 - 45}{9 - 0} = -5\ \text{m s}^{-2} = -\tfrac{1}{2}g, \] which gives \(g = 10\ \text{m s}^{-2}\). Thus plotting h against \(t^{2}\) straightens the curve of part (a) into a line whose gradient conveniently yields the acceleration due to gravity.
Take h as the height of the particle above the ground and let it be released from rest from a height H. Since the fall is free (only gravity acts), the distance fallen after time t is \(\tfrac{1}{2}gt^{2}\), so the height still remaining above the ground is
\n
\[ h = H - \tfrac{1}{2}\,g\,t^{2}. \]
\n
Using \(H = 45\ \text{m}\) and \(g = 10\ \text{m s}^{-2}\) as a worked illustration, \(h = 45 - 5t^{2}\). The values are:
\n
\n
t /s
0
0.5
1.0
1.5
2.0
2.5
3.0
\n
t\(^{2}\) /s\(^{2}\)
0
0.25
1.0
2.25
4.0
6.25
9.0
\n
h /m
45
43.75
40
33.75
25
13.75
0
\n
\n
(a) How h varies with t
\n
h against t: starts at the release height H and curves downward (concave-down parabola), falling faster as time increases.
\n
Because \(h = H - \tfrac{1}{2}gt^{2}\), the term subtracted grows as the square of the time. The graph therefore starts at \(h = H\) on the vertical axis and curves downward (a parabola, concave down). Its slope, which is the negative of the speed \(\left(\dfrac{dh}{dt} = -gt\right)\), is zero at the instant of release and becomes steadily steeper as the particle accelerates, reaching the ground (\(h = 0\)) after \(t = 3\ \text{s}\). So h falls slowly at first and ever faster afterwards, giving a curved (non-linear) graph.
\n
(b) How h varies with t\(^{2}\)
\n
h against t^2: a straight line of intercept H = 45 m and negative slope -1/2 g = -5 m/s^2, giving g = 10 m/s^2.
\n
Writing \(x = t^{2}\), the relation becomes \(h = H - \tfrac{1}{2}g\,x\), which is of the linear form \(y = c + mx\). The graph of h against \(t^{2}\) is therefore a straight line with
\n
\n
intercept on the h-axis equal to the release height, \(c = H = 45\ \text{m}\);
\n
a negative slope equal to \(-\tfrac{1}{2}g\).
\n
\n
Reading the slope from the line, \[ \text{slope} = \frac{0 - 45}{9 - 0} = -5\ \text{m s}^{-2} = -\tfrac{1}{2}g, \] which gives \(g = 10\ \text{m s}^{-2}\). Thus plotting h against \(t^{2}\) straightens the curve of part (a) into a line whose gradient conveniently yields the acceleration due to gravity.