Unit 8: Applications of Integration
- Syllabus
- 2020
- Section
- —
- Level
- —

For a continuous function on [a,b], the average value is its total signed accumulation divided by the interval length. It is the constant height whose rectangle of width b−a has the same signed area as the integral of f.
f_{\mathrm{avg}}=\frac{1}{b-a}\int_a^b f(x),dx
For f(x)=x2 on [0,3], favg=3−01∫03x2dx=31[x3/3]03=31(9)=3. The accumulated value is 9 function-units times input-units; dividing by the interval length 3 leaves the units of f.
Average value uses b−a1∫abf(x)dx; average rate of change uses b−af(b)−f(a). They answer different questions. Because the integral is signed, an average value may be zero or negative even when the graph encloses positive geometric area elsewhere.
For motion along a line, v(t)=s′(t) and a(t)=v′(t). Definite integrals reverse these derivative relationships: accumulated acceleration changes velocity, and accumulated velocity changes position.
v(b)=v(a)+\int_a^b a(t),dt,\qquad s(b)=s(a)+\int_a^b v(t),dt
| Quantity on [a,b] | Calculation | Sign meaning |
|---|---|---|
| displacement | ∫abv(t)dt | forward and backward motion cancel |
| final position | s(a)+∫abv(t)dt | initial position plus displacement |
| total distance | ∫ab∣v(t)∣dt | all traveled lengths are positive |
Let v(t)=t−2 meters/second for 0≤t≤4 and s(0)=5 meters. Displacement is ∫04(t−2)dt=0, so s(4)=5 meters. Since velocity changes sign at t=2, total distance is ∫02(2−t)dt+∫24(t−2)dt=2+2=4 meters.
Do not use ∣∫v∣ for total distance: cancellation has already occurred inside that integral. Split at every time when velocity changes sign, or integrate ∣v∣. If velocity is in meters/second and time in seconds, its definite integral is in meters—not meters/second.
If r(t) is the rate of change of a quantity, then A(x)=∫axr(t)dt records the quantity’s net change from input a to input x. The lower bound fixes the starting point; the upper bound makes the accumulated value change with x.
A(x)=\int_a^x r(t),dt,\qquad A(a)=0,\qquad A'(x)=r(x)
| Feature | Interpretation |
|---|---|
| r(t)>0 | positive contributions make A increase |
| r(t)<0 | negative contributions make A decrease |
| ∫abr(t)dt | net change from a to b |
| rate units Q/time | integral units Q |
If the actual quantity is Q and Q(a)=Q0, then Q(x)=Q0+A(x)=Q0+∫axr(t)dt. Thus the integral alone is the change since the start; adding the initial amount gives the current quantity.
Net change is signed. Positive and negative rate contributions can cancel, so it is not automatically the total amount of activity. Also, A(a)=0 does not mean the original quantity was zero; it means no change has accumulated over an interval of zero length.
In an applied accumulation problem, first identify the rate that changes the target quantity. When material enters and leaves, use net rate = incoming rate − outgoing rate. Integrating that net rate gives the signed change, not the final amount by itself.
Q(b)=Q(a)+\int_a^b Q'(t),dt
A tank initially contains 100 liters and has illustrative net inflow r(t)=12−2t liters/minute for 0≤t≤4. Its net change is ∫04(12−2t)dt=[12t−t2]04=32 liters. Therefore the amount after 4 minutes is 100+32=132 liters.
Do not add the initial amount when only net change is requested, and do not omit it when the final amount is requested. Check that rate and integration-variable units match; integrating liters/minute with respect to minutes produces liters.
When curves are written as functions of x, use a vertical slice of width dx. If y=u(x) is above y=ℓ(x) from x=a to x=b, the slice height is u(x)−ℓ(x), so integrating those rectangle areas gives the region’s area.
A=\int_a^b\big(\text{upper}(x)-\text{lower}(x)\big),dx
The curves y=2x and y=x2 intersect where x2=2x, so x=0 and x=2. On (0,2), 2x>x2. Therefore A=∫02(2x−x2)dx=[x2−x3/3]02=4−8/3=4/3 square units.
A negative integral signals that the curves were subtracted in the wrong order on part or all of the interval; geometric area is never negative. Do not use one upper-minus-lower expression across an intersection where the curve order switches—split there and write a nonnegative slice height on each piece.
When boundaries are written as x-functions of y, use a horizontal slice of thickness dy. If x=r(y) is the right boundary and x=ℓ(y) is the left boundary from y=c to y=d, the slice width is r(y)−ℓ(y).
A=\int_c^d\big(\text{right}(y)-\text{left}(y)\big),dy
| Integration variable | Slice | Difference | Bounds |
|---|---|---|---|
| dx | vertical | upper − lower | x-values |
| dy | horizontal | right − left | y-values |
For the region bounded by x=y2 and x=2y, intersections satisfy y2=2y, so y=0 and y=2. On 0<y<2, 2y is to the right of y2. Thus A=∫02(2y−y2)dy=[y2−y3/3]02=4/3 square units.
A dy integral must use expressions in y and y-value limits; do not mix them with x-bounds. If a horizontal line meets different right or left curves in different vertical ranges, split the integral at the y-value where that boundary changes.
If two curves intersect several times, their upper–lower order may change at each intersection. Use every relevant intersection as a possible partition point, test the sign of f−g on each subinterval, and make each slice height nonnegative.
A=\sum_i\int_{x_i}^{x_{i+1}}(\text{upper}-\text{lower}),dx=\int_a^b|f(x)-g(x)|,dx
On [0,2π], y=sinx and y=0 intersect at 0, π, and 2π. Since sinx≥0 on [0,π] and sinx≤0 on [π,2π], A=∫0πsinxdx+∫π2π(−sinx)dx=2+2=4. Equivalently, A=∫02π∣sinx∣dx=4.
The unsplit signed integral ∫02πsinxdx=0 is net signed area, not total geometric area. Absolute value must be applied to the height before integration, not to the final signed integral after positive and negative regions have already canceled.
For a solid whose cross sections perpendicular to the x-axis are known, a thin slice of thickness dx has volume approximately A(x)dx. Adding all slices gives the exact volume. The base region supplies a length such as s(x)=top−bottom; the named cross-sectional shape determines how that length becomes area.
V=\int_a^b A(x),dx,\qquad A_{\text{square}}(x)=[s(x)]^2,\qquad A_{\text{rectangle}}(x)=\ell(x)w(x)
Example: the base is between y=x and y=x2 on 0≤x≤1, and perpendicular cross sections are squares. Here s(x)=x−x2, so A(x)=(x−x2)2. Therefore V=∫01(x2−2x3+x4)dx=[3x3−2x4+5x5]01=301 cubic units.
Do not integrate the slice length itself. A distance such as s(x) has linear units; the integrand must be the cross-sectional area A(x), which has square units. Multiplying by slice thickness through integration then produces cubic units.
Let s(x) be the segment cut from the base region by a slice perpendicular to the x-axis. The problem states what that segment represents—such as a triangle base, a triangle leg, or a semicircle diameter. First convert s(x) into cross-sectional area A(x); then accumulate those areas with V=∫abA(x)dx.
| Cross section and meaning of s | Area function |
|---|---|
| Triangle with base s and height h(x) | A(x)=21s(x)h(x) |
| Equilateral triangle with side s | A(x)=43[s(x)]2 |
| Semicircle with diameter s | A(x)=8π[s(x)]2 |
Example: the base lies between y=x and y=0 for 0≤x≤2, and each perpendicular cross section is a semicircle whose diameter is the vertical segment. Thus s(x)=x, so A(x)=8πx2. Therefore V=∫028πx2dx=8π[3x3]02=3π cubic units.
For a semicircle, do not use the given diameter as the radius. If the base segment is the diameter s, then r=s/2 and A=21π(s/2)2=πs2/8. Likewise, a triangle needs both base and height unless its type fixes their relationship.
When a region touches the axis of rotation, a slice perpendicular to that axis sweeps out a solid circular disc. Its radius R is the distance from the axis to the region's outer boundary, so a thin slice has volume approximately π[R]2 times its thickness.
\text{about the }x\text{-axis: }V=\pi\int_a^b[R(x)]^2,dx,\qquad \text{about the }y\text{-axis: }V=\pi\int_c^d[R(y)]^2,dy
Example: rotate the region under y=x from x=0 to x=4 around the x-axis. Each vertical slice forms a disc with R(x)=x. Therefore V=π∫04(x)2dx=π∫04xdx=π[2x2]04=8π cubic units.
Square the radius, not the original function automatically: the radius must first be identified as a distance to the chosen axis. The disc formula also assumes no central hole; if the region does not reach the axis of rotation, subtracting an inner circular area is required instead.
For rotation around a line other than a coordinate axis, the disc radius is not usually the function value. It is the perpendicular distance from the axis of rotation to the outer boundary. The region must reach the axis so each perpendicular slice forms a solid disc.
y=k:\ R(x)=|f(x)-k|,\quad V=\pi\int_a^b[R(x)]^2,dx;\qquad x=h:\ R(y)=|g(y)-h|,\quad V=\pi\int_c^d[R(y)]^2,dy
Example: rotate the region between y=−1 and y=x2 for 0≤x≤1 about y=−1. Each vertical slice forms a disc with R(x)=x2−(−1)=x2+1. Thus V=π∫01(x2+1)2dx=π[5x5+32x3+x]01=1528π cubic units.
Do not use R=f(x) merely because the boundary is y=f(x); that is valid only when the axis is y=0. For a shifted axis, compute the distance first. If the rotated region leaves a central gap, the cross section is not a disc and this single-radius formula does not apply.
If a region does not reach the axis of rotation, a perpendicular slice produces a washer rather than a solid disc. Let R be the farther distance from the axis and r the nearer distance, with R≥r≥0. The washer area is the area of the outer circle minus the inner circular hole.
A=\pi(R^2-r^2);\qquad \text{about the }x\text{-axis: }V=\pi\int_a^b\big(R(x)^2-r(x)^2\big),dx;\qquad \text{about the }y\text{-axis: }V=\pi\int_c^d\big(R(y)^2-r(y)^2\big),dy
Example: rotate the region between y=x and y=x2 on 0≤x≤1 around the x-axis. Since x≥x2, R(x)=x and r(x)=x2. Thus V=π∫01[(x)2−(x2)2]dx=π∫01(x−x4)dx=π[2x2−5x5]01=103π cubic units.
A washer is a difference of two circular areas: πR2−πr2=π(R2−r2). It is not π(R−r)2. If the farther and nearer boundaries exchange, split the integral where their roles change so the cross-sectional area stays nonnegative.
A region rotated around a horizontal line y=k or vertical line x=h forms washers when neither boundary reaches the axis. Measure both radii perpendicular to the axis. The outer radius R is the farther distance and the inner radius r is the nearer distance, regardless of which function is named first.
V=\pi\int\big(R^2-r^2\big),d(\text{perpendicular variable}),\qquad R=\text{farther distance to the axis},\quad r=\text{nearer distance}
Example: rotate the region between y=x2 and y=x on 0≤x≤1 around y=2. The axis lies above both curves. The lower curve y=x2 is farther away, so R(x)=2−x2; the upper curve is nearer, so r(x)=2−x. Thus V=π∫01[(2−x2)2−(2−x)2]dx=π∫01(4x−5x2+x4)dx=158π cubic units.
“Upper” does not always mean “outer.” With an axis above the region, the lower boundary is farther from the axis; with an axis below, the upper boundary may be farther. Determine distance first, then square, and keep the area as π(R2−r2) rather than π(R−r)2.
A short piece of a smooth graph has horizontal change dx and vertical change dy, so its length behaves like the hypotenuse ds=dx2+dy2. Dividing by the chosen differential produces a nonnegative length rate that can be accumulated across the interval.
y=f(x):\ L=\int_a^b\sqrt{1+[f'(x)]^2},dx;\qquad x=g(y):\ L=\int_c^d\sqrt{1+[g'(y)]^2},dy
Example: for y=32x3/2 on 0≤x≤1, f′(x)=x. Therefore L=∫011+xdx=[32(1+x)3/2]01=32(22−1) units.
The integrand contains the square of the derivative, not the square of the original function. Use this single-function formula only where the chosen orientation represents the curve smoothly across the full interval; otherwise a different orientation or a split into smooth pieces is needed.