By the end of this section, you should be able to:
- Determine a new value of a quantity from the old value and the amount of change.
- Calculate the average rate of change and explain how it differs from the instantaneous rate of change.
- Apply rates of change to displacement, velocity, and acceleration of an object moving along a straight line.
- Use derivatives to model rates of change in the physical sciences, including reaction rates and temperature change.
- Predict the future population from the present value and the population growth rate.
In this section we look at some applications of the derivative by focusing on the interpretation of the derivative as the rate of change of a function. Whenever you check how quickly something is increasing or decreasing—whether it’s the speed of a falling object, the concentration of a chemical in a reaction, or the size of a growing population—you are thinking about a rate of change. The derivative gives us a way to make that idea precise.
A key distinction runs through everything that follows: the average rate of change of a function \(f\) over an interval tells us how much \(f\) changed on average between two points, while the instantaneous rate of change \(f'(a)\) tells us how fast \(f\) is changing at the single moment \(t = a\). Whenever we compute a derivative and evaluate it at a point, we are finding an instantaneous rate of change.
We begin with a general estimation technique, then spend most of the section exploring what the derivative tells us in several concrete settings: the motion of objects, the progress of chemical reactions, the cooling of hot objects, and the growth of populations.
3.4.2 Motion Along a Line
Another use for the derivative is to analyze motion along a line. If you have ever watched a speedometer needle climb as you accelerate onto a highway, you have an intuitive sense of what it means for velocity to change over time. In this subsection, we make that intuition precise.
Suppose an object moves along a straight line (imagine a car on a long, straight road, or a ball tossed straight up into the air). We describe the object’s location at time \(t\) by a position function \(s(t)\), which tells us how far the object is from some reference point. The derivative of position with respect to time gives us velocity—the instantaneous rate of change of position. And the derivative of velocity gives us acceleration—the instantaneous rate of change of velocity.
Let \(s(t)\) be a function giving the position of an object at time \(t\).
The velocity of the object at time \(t\) is given by \(v(t) = s'(t)\).
The speed of the object at time \(t\) is given by \(|v(t)|\).
The acceleration of the object at time \(t\) is given by \(a(t) = v'(t) = s''(t)\).
A few things to notice about these definitions. Velocity can be positive or negative: a positive velocity means the object is moving in the positive direction (to the right, or upward, depending on the context), while a negative velocity means it is moving in the negative direction. Speed, on the other hand, is always nonnegative—it tells you how fast the object is moving without regard to direction. And acceleration tells you whether the object is speeding up or slowing down: when velocity and acceleration have the same sign, the object is speeding up; when they have opposite signs, the object is slowing down.
A ball is dropped from a height of 64 feet. Its height above ground (in feet) \(t\) seconds later is given by \(s(t) = -16t^2 + 64\).

Figure 3.4.7: Height of the ball as a function of time.
- What is the instantaneous velocity of the ball when it hits the ground?
- What is the average velocity during its fall?
Solution (click to reveal)
The first thing to do is determine how long it takes the ball to reach the ground. To do this, set \(s(t) = 0\). Solving \(-16t^2 + 64 = 0\), we get \(t = 2\), so it takes 2 seconds for the ball to reach the ground.
The instantaneous velocity of the ball as it strikes the ground is \(v(2)\). Since \(v(t) = s'(t) = -32t\), we obtain \(v(2) = -64\) ft/s. (The negative sign indicates the ball is moving downward.)
The average velocity of the ball during its fall is
\[v_{\text{avg}} = \frac{s(2) - s(0)}{2 - 0} = \frac{0 - 64}{2} = -32 \text{ ft/s}.\]
Notice that the instantaneous velocity at impact (\(-64\) ft/s) is twice the average velocity (\(-32\) ft/s). This makes sense: the ball starts with zero velocity and steadily accelerates, so by the time it hits the ground it is moving much faster than its average. The average velocity tells us the overall rate of descent; the instantaneous velocity tells us the speed at the exact moment of impact.
In the previous example, we compared instantaneous and average velocity for an object with a simple position function. The next example explores a more subtle situation: what happens when velocity and acceleration point in opposite directions?
A particle moves along a coordinate axis in the positive direction to the right. Its position at time \(t\) is given by \(s(t) = t^3 - 4t + 2\). Find \(v(1)\) and \(a(1)\) and use these values to answer the following questions.
- Is the particle moving from left to right or from right to left at time \(t = 1\)?
- Is the particle speeding up or slowing down at time \(t = 1\)?
Solution (click to reveal)
Begin by finding \(v(t)\) and \(a(t)\):
\[v(t) = s'(t) = 3t^2 - 4 \quad \text{and} \quad a(t) = v'(t) = s''(t) = 6t.\]
Evaluating these functions at \(t = 1\), we obtain \(v(1) = -1\) and \(a(1) = 6\).
Because \(v(1) < 0\), the particle is moving from right to left.
Because \(v(1) < 0\) and \(a(1) > 0\), velocity and acceleration are acting in opposite directions. In other words, the particle is being accelerated in the direction opposite the direction in which it is traveling, causing \(|v(t)|\) to decrease. The particle is slowing down.
This is a subtle but important point. Many students assume that positive acceleration always means “speeding up,” but that is only true when velocity is also positive. What matters is whether velocity and acceleration share the same sign. When they do, the object speeds up. When they don’t, the object slows down.
Now let’s put these ideas together in a more complete analysis. In the next example, we use the velocity function to determine when a particle is at rest, when it is moving left versus right, and how to trace out its entire path.
The position of a particle moving along a coordinate axis is given by \(s(t) = t^3 - 9t^2 + 24t + 4\), \(t \geq 0\).
- Find \(v(t)\).
- At what time(s) is the particle at rest?
- On what time intervals is the particle moving from left to right? From right to left?
- Use the information obtained to sketch the path of the particle along a coordinate axis.
Solution (click to reveal)
The velocity is the derivative of the position function:
\[v(t) = s'(t) = 3t^2 - 18t + 24.\]
The particle is at rest when \(v(t) = 0\), so set \(3t^2 - 18t + 24 = 0\). Factoring the left-hand side of the equation produces \(3(t - 2)(t - 4) = 0\). Solving, we find that the particle is at rest at \(t = 2\) and \(t = 4\).
The particle is moving from left to right when \(v(t) > 0\) and from right to left when \(v(t) < 0\). The figure below gives the analysis of the sign of \(v(t)\) for \(t \geq 0\), but it does not represent the axis along which the particle is moving.

Figure: The sign of \(v(t)\) determines the direction of the particle.
Since \(3t^2 - 18t + 24 > 0\) on \([0, 2) \cup (4, +\infty)\), the particle is moving from left to right on these intervals. Since \(3t^2 - 18t + 24 < 0\) on \((2, 4)\), the particle is moving from right to left on this interval.
Before we can sketch the path of the particle, we need to know its position at the time it starts moving (\(t = 0\)) and at the times that it changes direction (\(t = 2, 4\)). We have \(s(0) = 4\), \(s(2) = 24\), and \(s(4) = 20\). This means that the particle begins on the coordinate axis at 4, moves to the right until it reaches 24 at \(t = 2\), then reverses direction and moves left until it reaches 20 at \(t = 4\), and then reverses direction again and moves to the right indefinitely. The path of the particle is shown on a coordinate axis in the figure below.

Figure: The path of the particle can be determined by analyzing \(v(t)\).
A particle moves along a coordinate axis. Its position at time \(t\) is given by \(s(t) = t^2 - 5t + 1\). Is the particle moving from right to left or from left to right at time \(t = 3\)?
Solution (click to reveal)
Find the velocity: \(v(t) = s'(t) = 2t - 5\). Evaluating at \(t = 3\): \(v(3) = 2(3) - 5 = 1 > 0\). Since \(v(3) > 0\), the particle is moving from left to right.
3.4.3 Reaction Rates in Chemistry
The derivative doesn’t only describe physical motion—it captures the rate of change of any quantity. One of the most striking examples comes from chemistry.
If you have taken a chemistry course, you may already be familiar with the ideas in this subsection. If you haven’t, here’s all you need to know: in a chemical reaction, one or more starting substances (called reactants) transform into new substances (called products). Think of baking soda and vinegar fizzing in a science-fair volcano—the baking soda and vinegar are reactants, and the carbon dioxide gas bubbling out is a product. As the reaction proceeds, the amount of reactant decreases while the amount of product increases. Chemists track this by measuring concentration—the amount of a substance dissolved in a given volume of solution, typically measured in moles per liter (mol/L). You can think of concentration as a measure of “how much stuff is packed into the liquid.”
The natural question from a calculus perspective is: how fast is that concentration changing at a given instant? This is called the reaction rate. If \(C(t)\) denotes the concentration of a reactant at time \(t\), then the instantaneous rate of change of concentration is \(C'(t)\). Because the concentration of a reactant decreases as it gets used up, \(C'(t)\) is typically negative during a reaction. By convention, chemists define the rate of the reaction as \(-C'(t)\) so that the rate is reported as a positive number.
In practice, chemists often model reactions using exponential functions, but those require differentiation rules we develop later in the course (the chain rule in Section 3.6 and derivatives of exponential functions in Section 3.9). For now, rational functions capture the same essential behavior—rapid change early, tapering off later—using only the differentiation rules we already have.
The concentration (in mol/L) of a reactant in a chemical reaction is modeled by
\[C(t) = \frac{1}{2t + 1}\]
where \(t\) is measured in minutes after the reaction begins.
- Find the instantaneous rate of change of concentration at \(t = 0\) and \(t = 3\) minutes.
- Is the concentration decreasing faster at the start of the reaction or after 3 minutes? Why does this make physical sense?
Solution (click to reveal)
We differentiate using the quotient rule with numerator \(1\) and denominator \(2t + 1\):
\[C'(t) = \frac{(0)(2t + 1) - (1)(2)}{(2t + 1)^2} = \frac{-2}{(2t + 1)^2}.\]
At \(t = 0\):
\[C'(0) = \frac{-2}{(2(0) + 1)^2} = \frac{-2}{1} = -2 \text{ mol/L per minute}.\]
At \(t = 3\):
\[C'(3) = \frac{-2}{(2(3) + 1)^2} = \frac{-2}{49} \approx -0.041 \text{ mol/L per minute}.\]
The magnitude of the instantaneous rate of change at \(t = 0\) is \(|C'(0)| = 2\), while at \(t = 3\) it is \(|C'(3)| \approx 0.041\). The concentration is decreasing much faster at the start of the reaction.
This makes physical sense: early in the reaction, there are many reactant molecules present, so collisions between them are frequent and the reaction proceeds quickly. As the reactant is consumed, fewer molecules remain, collisions become less frequent, and the reaction slows down. You can see this visually in the figure below—the tangent line at \(t = 0\) is steep, while the tangent line at \(t = 3\) is nearly flat.

Figure: The concentration \(C(t) = \frac{1}{2t+1}\) with tangent lines at \(t = 0\) and \(t = 3\). The steep tangent at \(t = 0\) reflects a fast reaction rate; the nearly flat tangent at \(t = 3\) reflects a slow one.
The concentration (in mol/L) of a reactant is given by \(C(t) = \dfrac{10}{t + 5}\), where \(t\) is measured in seconds.
- Find \(C'(t)\).
- Find the instantaneous reaction rate (that is, \(-C'(t)\)) at \(t = 0\) and \(t = 15\) seconds.
Solution (click to reveal)
Using the quotient rule:
\[C'(t) = \frac{(0)(t + 5) - (10)(1)}{(t + 5)^2} = \frac{-10}{(t + 5)^2}.\]
The instantaneous reaction rate is \(-C'(t) = \frac{10}{(t+5)^2}\).
At \(t = 0\): \(-C'(0) = \frac{10}{25} = 0.4\) mol/L per second.
At \(t = 15\): \(-C'(15) = \frac{10}{400} = 0.025\) mol/L per second.
The reaction is 16 times faster at the start than after 15 seconds.
3.4.4 Temperature Change and Cooling
Here is a situation everyone has experienced: you pour a cup of hot coffee and set it on the counter. At first it cools rapidly, but as its temperature gets closer to room temperature, the cooling slows down. You may have also noticed the reverse: a cold drink taken out of the refrigerator warms up quickly at first, then more and more slowly as it approaches room temperature.
Physicists describe this pattern with Newton’s Law of Cooling, which states that the instantaneous rate at which an object’s temperature changes is proportional to the difference between the object’s temperature and the surrounding temperature. In other words, a large temperature gap produces rapid temperature change, while a small gap produces slow change. The precise formulation and derivation of Newton’s Law of Cooling involves exponential functions, the chain rule (Section 3.6), and derivatives of exponential functions (Section 3.9); the full treatment appears in Section 6.8. For now, we can capture the same qualitative behavior—rapid change early, slower change later, approaching the surrounding temperature—with a simpler model that requires only the quotient rule.
A function of the form
\[T(t) = T_{\text{env}} + \frac{k}{t + b}\]
exhibits exactly this behavior: it starts at \(T_{\text{env}} + \frac{k}{b}\) when \(t = 0\), decreases over time, and approaches the environmental temperature \(T_{\text{env}}\) as \(t \to \infty\).
A metal rod heated to \(200°\text{C}\) is placed in a room where the temperature is \(25°\text{C}\). Suppose the temperature of the rod at time \(t\) (in minutes) is modeled by
\[T(t) = 25 + \frac{700}{t + 4}.\]
- Verify that \(T(0) = 200°\text{C}\) and describe the long-term behavior of \(T(t)\).
- Find the instantaneous rate of change of temperature at \(t = 0\) and \(t = 20\) minutes.
- Interpret the results.
Solution (click to reveal)
At \(t = 0\): \(T(0) = 25 + \frac{700}{4} = 25 + 175 = 200°\text{C}\). ✓
As \(t \to \infty\), the fraction \(\frac{700}{t + 4} \to 0\), so \(T(t) \to 25°\text{C}\)—the rod’s temperature approaches room temperature, which is exactly what we expect.
Differentiate using the quotient rule (with numerator \(700\) and denominator \(t + 4\)):
\[T'(t) = \frac{(0)(t + 4) - (700)(1)}{(t + 4)^2} = \frac{-700}{(t + 4)^2}.\]
At \(t = 0\):
\[T'(0) = \frac{-700}{(4)^2} = \frac{-700}{16} = -43.75°\text{C per minute}.\]
At \(t = 20\):
\[T'(20) = \frac{-700}{(24)^2} = \frac{-700}{576} \approx -1.22°\text{C per minute}.\]
At the instant the rod is placed in the room, it is cooling at an instantaneous rate of \(43.75°\text{C}\) per minute—extremely rapid. After 20 minutes, the instantaneous cooling rate has slowed dramatically to about \(1.22°\text{C}\) per minute.
This makes sense: at \(t = 0\), the temperature difference between the rod and the room is \(200° - 25° = 175°\text{C}\), which is enormous, so the rod sheds heat quickly. By \(t = 20\) minutes, \(T(20) = 25 + \frac{700}{24} \approx 54.2°\text{C}\), so the temperature difference has shrunk to about \(29°\text{C}\)—and the cooling rate has shrunk accordingly. You can see this in the figure below: the tangent line at \(t = 0\) is steep, while the tangent line at \(t = 20\) is much more gentle.
Compare these instantaneous rates with the average rate of change over the entire 20-minute interval:
\[\frac{T(20) - T(0)}{20 - 0} = \frac{54.2 - 200}{20} = \frac{-145.8}{20} \approx -7.29°\text{C per minute}.\]
The average rate (\(-7.29°\text{C/min}\)) falls between the fast instantaneous rate at the start (\(-43.75°\text{C/min}\)) and the slow one at \(t = 20\) (\(-1.22°\text{C/min}\)), just as we would expect.

Figure: The temperature \(T(t) = 25 + \frac{700}{t+4}\) with tangent lines at \(t = 0\) and \(t = 20\). The rod cools rapidly at first, then more slowly as it approaches room temperature (\(25°\text{C}\), dotted line).
The temperature (in \(°\text{F}\)) of a cup of coffee \(t\) minutes after it is poured is given by
\[T(t) = 70 + \frac{600}{t + 4}.\]
- What is the initial temperature of the coffee? What temperature does it approach over time?
- Find the instantaneous rate of change \(T'(10)\) and explain what it means in practical terms.
Solution (click to reveal)
\(T(0) = 70 + \frac{600}{4} = 70 + 150 = 220°\text{F}\). As \(t \to \infty\), \(T(t) \to 70°\text{F}\) (room temperature).
Differentiate: \(T'(t) = \frac{-600}{(t + 4)^2}\).
At \(t = 10\):
\[T'(10) = \frac{-600}{(14)^2} = \frac{-600}{196} \approx -3.06°\text{F per minute}.\]
After 10 minutes, the coffee is cooling at an instantaneous rate of approximately \(3.06°\text{F}\) per minute. At that moment the coffee’s temperature is \(T(10) = 70 + \frac{600}{14} \approx 112.9°\text{F}\), which is still well above room temperature (\(70°\text{F}\)), so it is still cooling at a noticeable rate.
3.4.5 Further Applications in the Physical Sciences
The examples above—reaction rates and temperature change—illustrate how the derivative captures rates of change in chemistry and physics. But these are far from the only settings where the idea applies. Any time a physical quantity changes with respect to time, distance, pressure, or any other variable, the derivative tells us how fast that change is happening. Here are two more examples from different corners of the physical sciences.
A cylindrical water tank initially holds 100 gallons. A drain valve is opened, and the volume of water remaining in the tank (in gallons) after \(t\) minutes is modeled by
\[V(t) = 100 - 20t + t^2, \quad 0 \leq t \leq 10.\]
- At what rate is water draining from the tank at the instant the valve is opened? After 5 minutes?
- At what time does the tank empty, and what is the instantaneous rate of change at that moment?
- Compute the average rate of change over the entire draining period and compare it to the instantaneous rates.
Solution (click to reveal)
Differentiate using the power rule:
\[V'(t) = -20 + 2t.\]
At \(t = 0\): \(V'(0) = -20 + 0 = -20\) gallons per minute. The tank is losing water at a rate of 20 gallons per minute the instant the valve opens.
At \(t = 5\): \(V'(5) = -20 + 10 = -10\) gallons per minute. After 5 minutes, the draining has slowed to 10 gallons per minute.
Setting \(V(t) = 0\): \(100 - 20t + t^2 = (t - 10)^2 = 0\), so \(t = 10\) minutes. The tank empties at \(t = 10\).
At that moment: \(V'(10) = -20 + 20 = 0\) gallons per minute. The instantaneous rate of change is zero—the flow has stopped completely because there is no water left to drain.
The average rate of change over \([0, 10]\) is
\[\frac{V(10) - V(0)}{10 - 0} = \frac{0 - 100}{10} = -10 \text{ gallons per minute}.\]
The instantaneous rate starts at \(-20\) gal/min (fast), passes through \(-10\) gal/min at \(t = 5\) (matching the average), and ends at \(0\) gal/min (stopped). The average rate of \(-10\) gal/min falls right in the middle, as we would expect for a process that slows down steadily.
Atmospheric pressure decreases as you go higher above sea level—this is why your ears pop on an airplane and why climbers on Mount Everest need supplemental oxygen. A simplified model for atmospheric pressure \(P\) (in millimeters of mercury, mmHg) as a function of altitude \(h\) (in kilometers above sea level) is
\[P(h) = \frac{15{,}200}{h + 20}.\]
- Verify that \(P(0) = 760\) mmHg (the standard sea-level pressure) and find \(P(10)\).
- Find the instantaneous rate of change of pressure with respect to altitude at sea level and at \(h = 10\) km.
- Interpret the results.
Solution (click to reveal)
At sea level (\(h = 0\)): \(P(0) = \frac{15{,}200}{20} = 760\) mmHg. ✓
At \(h = 10\) km: \(P(10) = \frac{15{,}200}{30} \approx 506.7\) mmHg—about two-thirds of sea-level pressure.
Differentiate using the quotient rule:
\[P'(h) = \frac{(0)(h + 20) - (15{,}200)(1)}{(h + 20)^2} = \frac{-15{,}200}{(h + 20)^2}.\]
At \(h = 0\):
\[P'(0) = \frac{-15{,}200}{(20)^2} = \frac{-15{,}200}{400} = -38 \text{ mmHg/km}.\]
At \(h = 10\):
\[P'(10) = \frac{-15{,}200}{(30)^2} = \frac{-15{,}200}{900} \approx -16.9 \text{ mmHg/km}.\]
Pressure drops faster at lower altitudes: at sea level, each additional kilometer of altitude costs about 38 mmHg of pressure, while at 10 km the rate of pressure drop has slowed to about 16.9 mmHg per km. This makes physical sense—near sea level, the atmosphere is dense and heavy, so rising through it produces a large pressure change. Higher up, the air is already thin, so the same change in altitude produces a smaller change in pressure.
Boyle’s Law states that for a fixed amount of gas at constant temperature, the volume of the gas is inversely proportional to its pressure. Suppose the volume \(V\) (in liters) of a gas sample is given by
\[V(p) = \frac{120}{p}\]
where \(p\) is measured in atmospheres.
- Find \(V'(p)\).
- Find the instantaneous rate of change of volume with respect to pressure at \(p = 2\) atm and \(p = 6\) atm.
Solution (click to reveal)
Using the quotient rule:
\[V'(p) = \frac{(0)(p) - (120)(1)}{p^2} = \frac{-120}{p^2}.\]
At \(p = 2\): \(V'(2) = \frac{-120}{4} = -30\) liters per atmosphere.
At \(p = 6\): \(V'(6) = \frac{-120}{36} \approx -3.33\) liters per atmosphere.
The volume is much more sensitive to pressure changes at low pressures. Increasing pressure from 2 to 3 atm compresses the gas by about 30 liters per atm, while increasing from 6 to 7 atm compresses it by only about 3.3 liters per atm.
3.4.6 Population Change
We have now seen the derivative at work in physics and chemistry. Our final application in this section comes from biology: how fast is a population growing?
If you’ve ever watched a nature documentary that tracks a species recovering from near-extinction, or read a news article about a booming city, you’ve encountered the idea of a growth rate. In mathematical terms, if \(P(t)\) is the number of entities present in a population at time \(t\), then the instantaneous population growth rate is simply the derivative \(P'(t)\). A large positive value of \(P'(t)\) means the population is growing rapidly; a value near zero means it is relatively stable; and a negative value means the population is declining. We can use a current population, together with a growth rate, to estimate the size of a population in the future.
If \(P(t)\) is the number of entities present in a population, then the population growth rate of \(P(t)\) is defined to be \(P'(t)\).
Combined with the amount of change formula from Section 3.4.1, this definition gives us a practical way to estimate future population sizes.
The population of a city is tripling every 5 years. If its current population is 10,000, what will be its approximate population 2 years from now?
Solution (click to reveal)
Let \(P(t)\) be the population (in thousands) \(t\) years from now. Thus, we know that \(P(0) = 10\) and based on the information, we anticipate \(P(5) = 30\). Now estimate \(P'(0)\), the current growth rate, using the average rate of change over the 5-year interval as an approximation:
\[P'(0) \approx \frac{P(5) - P(0)}{5 - 0} = \frac{30 - 10}{5} = 4.\]
By applying Equation (3.4.1) to \(P(t)\), we can estimate the population 2 years from now by writing
\[P(2) \approx P(0) + (2)P'(0) \approx 10 + 2(4) = 18;\]
thus, in 2 years the population will be approximately 18,000.
The current population of a mosquito colony is known to be 3,000; that is, \(P(0) = 3{,}000\). If \(P'(0) = 100\), estimate the size of the population in 3 days, where \(t\) is measured in days.
Solution (click to reveal)
Using the amount of change formula (Equation 3.4.1):
\[P(3) \approx P(0) + (3)P'(0) = 3{,}000 + 3(100) = 3{,}300.\]
The mosquito colony will have approximately 3,300 mosquitoes after 3 days.