# 2.2: An Example

- Page ID
- 460

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\(\newcommand{\avec}{\mathbf a}\) \(\newcommand{\bvec}{\mathbf b}\) \(\newcommand{\cvec}{\mathbf c}\) \(\newcommand{\dvec}{\mathbf d}\) \(\newcommand{\dtil}{\widetilde{\mathbf d}}\) \(\newcommand{\evec}{\mathbf e}\) \(\newcommand{\fvec}{\mathbf f}\) \(\newcommand{\nvec}{\mathbf n}\) \(\newcommand{\pvec}{\mathbf p}\) \(\newcommand{\qvec}{\mathbf q}\) \(\newcommand{\svec}{\mathbf s}\) \(\newcommand{\tvec}{\mathbf t}\) \(\newcommand{\uvec}{\mathbf u}\) \(\newcommand{\vvec}{\mathbf v}\) \(\newcommand{\wvec}{\mathbf w}\) \(\newcommand{\xvec}{\mathbf x}\) \(\newcommand{\yvec}{\mathbf y}\) \(\newcommand{\zvec}{\mathbf z}\) \(\newcommand{\rvec}{\mathbf r}\) \(\newcommand{\mvec}{\mathbf m}\) \(\newcommand{\zerovec}{\mathbf 0}\) \(\newcommand{\onevec}{\mathbf 1}\) \(\newcommand{\real}{\mathbb R}\) \(\newcommand{\twovec}[2]{\left[\begin{array}{r}#1 \\ #2 \end{array}\right]}\) \(\newcommand{\ctwovec}[2]{\left[\begin{array}{c}#1 \\ #2 \end{array}\right]}\) \(\newcommand{\threevec}[3]{\left[\begin{array}{r}#1 \\ #2 \\ #3 \end{array}\right]}\) \(\newcommand{\cthreevec}[3]{\left[\begin{array}{c}#1 \\ #2 \\ #3 \end{array}\right]}\) \(\newcommand{\fourvec}[4]{\left[\begin{array}{r}#1 \\ #2 \\ #3 \\ #4 \end{array}\right]}\) \(\newcommand{\cfourvec}[4]{\left[\begin{array}{c}#1 \\ #2 \\ #3 \\ #4 \end{array}\right]}\) \(\newcommand{\fivevec}[5]{\left[\begin{array}{r}#1 \\ #2 \\ #3 \\ #4 \\ #5 \\ \end{array}\right]}\) \(\newcommand{\cfivevec}[5]{\left[\begin{array}{c}#1 \\ #2 \\ #3 \\ #4 \\ #5 \\ \end{array}\right]}\) \(\newcommand{\mattwo}[4]{\left[\begin{array}{rr}#1 \amp #2 \\ #3 \amp #4 \\ \end{array}\right]}\) \(\newcommand{\laspan}[1]{\text{Span}\{#1\}}\) \(\newcommand{\bcal}{\cal B}\) \(\newcommand{\ccal}{\cal C}\) \(\newcommand{\scal}{\cal S}\) \(\newcommand{\wcal}{\cal W}\) \(\newcommand{\ecal}{\cal E}\) \(\newcommand{\coords}[2]{\left\{#1\right\}_{#2}}\) \(\newcommand{\gray}[1]{\color{gray}{#1}}\) \(\newcommand{\lgray}[1]{\color{lightgray}{#1}}\) \(\newcommand{\rank}{\operatorname{rank}}\) \(\newcommand{\row}{\text{Row}}\) \(\newcommand{\col}{\text{Col}}\) \(\renewcommand{\row}{\text{Row}}\) \(\newcommand{\nul}{\text{Nul}}\) \(\newcommand{\var}{\text{Var}}\) \(\newcommand{\corr}{\text{corr}}\) \(\newcommand{\len}[1]{\left|#1\right|}\) \(\newcommand{\bbar}{\overline{\bvec}}\) \(\newcommand{\bhat}{\widehat{\bvec}}\) \(\newcommand{\bperp}{\bvec^\perp}\) \(\newcommand{\xhat}{\widehat{\xvec}}\) \(\newcommand{\vhat}{\widehat{\vvec}}\) \(\newcommand{\uhat}{\widehat{\uvec}}\) \(\newcommand{\what}{\widehat{\wvec}}\) \(\newcommand{\Sighat}{\widehat{\Sigma}}\) \(\newcommand{\lt}{<}\) \(\newcommand{\gt}{>}\) \(\newcommand{\amp}{&}\) \(\definecolor{fillinmathshade}{gray}{0.9}\)We started the last section by saying, "It is often necessary to know how sensitive the value of \(y\) is to small changes in \(x\).'' We have seen one purely mathematical example of this: finding the "steepness'' of a curve at a point is precisely this problem. Here is a more applied example.

With careful measurement it might be possible to discover that a dropped ball has height \( h(t)=h_0-kt^2\), \(t\) seconds after it is released. (Here \(h_0\) is the initial height of the ball, when \(t=0\), and \(k\) is some number determined by the experiment.) A natural question is then, "How fast is the ball going at time \(t\)?'' We can certainly get a pretty good idea with a little simple arithmetic. To make the calculation more concrete, let's say \( h_0=100\) meters and \(k=4.9\) and suppose we're interested in the speed at \(t=2\). We know that when \(t=2\) the height is \(100-4\cdot 4.9=80.4\). A second later, at \(t=3\), the height is \(100-9\cdot 4.9=55.9\), so in that second the ball has traveled \(80.4-55.9=24.5\) meters. This means that the *average* speed during that time was 24.5 meters per second. So we might guess that 24.5 meters per second is not a terrible estimate of the speed at \(t=2\). But certainly we can do better. At \(t=2.5\) the height is \( 100-4.9(2.5)^2=69.375\). During the half second from \(t=2\) to \(t=2.5\) the ball dropped \(80.4-69.375=11.025\) meters, at an average speed of \(11.025/(1/2)=22.05\) meters per second; this should be a better estimate of the speed at \(t=2\). So it's clear now how to get better and better approximations: compute average speeds over shorter and shorter time intervals. Between \(t=2\) and \(t=2.01\), for example, the ball drops 0.19649 meters in one hundredth of a second, at an average speed of 19.649 meters per second.

We cannot do this forever, and we still might reasonably ask what the actual speed precisely at \(t=2\) is. If \(\Delta t\) is some tiny amount of time, what we want to know is what happens to the average speed \((h(2)-h(2+\Delta t))/\Delta t\) as \(\Delta t\) gets smaller and smaller. Doing a bit of algebra:

\[\eqalign{{h(2)-h(2+\Delta t)\over \Delta t}&={80.4-(100-4.9(2+\Delta t)^2)\over \Delta t}\cr& ={80.4 - 100 + 19.6+19.6\Delta t+4.9\Delta t^2\over \Delta t}\cr& ={19.6\Delta t+4.9\Delta t^2\over \Delta t}\cr& =19.6 + 4.9\Delta t\cr} \]

When \(\Delta t\) is very small, this is very close to 19.6, and indeed it seems clear that as \(\Delta t\) goes to zero, the average speed goes to 19.6, so the exact speed at \(t=2\) is 19.6 meters per second. This calculation should look very familiar. In the language of the previous section, we might have started with \( f(x)=100-4.9x^2\) and asked for the slope of the tangent line at \(x=2\). We would have answered that question by computing

\[ {f(2+\Delta x) - f(2)\over \Delta x} ={-19.6\Delta x-4.9\Delta x^2\over \Delta x} =-19.6-4.9\Delta x \]

The algebra is the same, except that following the pattern of the previous section the subtraction would be reversed, and we would say that the slope of the tangent line is \(-19.6\). Indeed, in hindsight, perhaps we should have subtracted the other way even for the dropping ball. At \(t=2\) the height is 80.4; one second later the height is 55.9. The usual way to compute a "distance traveled'' is to subtract the earlier position from the later one, or \(55.9-80.4=-24.5\). This tells us that the distance traveled is 24.5 meters, and the negative sign tells us that the height went down during the second. If we continue the original calculation we then get \(-19.6\) meters per second as the exact speed at \(t=2\). If we interpret the negative sign as meaning that the motion is downward, which seems reasonable, then in fact this is the same answer as before, but with even more information, since the numerical answer contains the direction of motion as well as the speed. Thus, the speed of the ball is the value of the derivative of a certain function, namely, of the function that gives the position of the ball. (More properly, this is the *velocity* of the ball; velocity is signed speed, that is, speed with a direction indicated by the sign.)

The upshot is that this problem, finding the speed of the ball, is *exactly* the same problem mathematically as finding the slope of a curve. This may already be enough evidence to convince you that whenever some quantity is changing (the height of a curve or the height of a ball or the size of the economy or the distance of a space probe from earth or the population of the world) the rate at which the quantity is changing can, in principle, be computed in exactly the same way, by finding a derivative.

## Contributors

Integrated by Justin Marshall.