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Related rates of change
Related rates of change are simply an application of the chain rule. In related-rate problems, you find the rate at which some quantity is changing by relating it to other quantities for which the rate of change is known.
In the following examples, we repeatedly use the result dxdy=1dydx, which is established and discussed in the module Introduction to differential calculus.Example
An upturned cone with semivertical angle 45∘ is being filled with water at a constant rate of 30 cm3 per second.
- h, the depth of the water, is increasing
- r, the radius of the surface of the water, is increasing
- S, the area of the water surface, is increasing.
Solution
The volume V of the water in the cone is given by
V=13πr2h.The cross-section of the cone is a right-angled isosceles triangle, and therefore r=h. Hence,
V=13πr3=13πh3.- We seek dhdt. Now V=13πh3, and therefore dVdh=πh2. Hence,
dhdt=dhdV×dVdt=1πh2×30=30πh2.
When h=60, we have dhdt=1120π cm/s.
- We have seen that r(t)=h(t). Thus, when h=60, we have drdt=1120π cm/s.
- We seek dSdt. The area of the water's surface is
S=πr2.
Therefore
dSdt=dSdr×drdt=2πr×30πr2=60r.
When h=60, we have r=60, and so dSdt=1 cm2/s.
Example
Variables x and y are related by the equation y=2−4x. Given that x and y are functions of t and that dxdt=10, find dydt in terms of x.Solution
If y=2−4x, then dydx=4x2. Therefore dydt=dydx×dxdt=4x2×10=40x2.Related rates questions arise in many situations. The following demanding example involving the flow of liquids relates the rate of change of depth to the rate of change of volume.
Example
A vessel of water is in the form of a frustum of a cone with semivertical angle 45∘. The bottom circle of the vessel is a hole of radius r cm. Water flows from this hole at a velocity of c√2gh cm/s, where c is a constant and h cm is the height of the surface of the water above the hole.
- Find the rate in cm3/s at which water flows from the vessel.
- Find the rate in cm/s at which h is increasing.
Solution
We first find the volume V of water in the frustum. Consider removing a small cone from the 'tip' of a cone. This forms the hole. Let H be the height of the larger cone (up to the water surface) and let h1 be the height of the smaller cone (which is removed). Let R be the radius of the larger cone and let r be the radius of the smaller cone.
The height of the water is h=H−h1. Therefore V=13π(R2H−r2h1)=13π(R2H−r2(H−h)). Because the semivertical angle is 45∘, we have R=H and R−r=h. Hence, R=r+h. Substituting for R and H in the equation for V, we have V=13π(R2H−r2(H−h))=13π(R3−r2(R−h))=13π((r+h)3−r3)=13π(3r2h+3rh2+h3).- Let v cm/s be the velocity of the flow of water from the hole at time t. We are given that v=c√2gh, where h is the height of the water above the hole at time t. Since dVdt=area of the cross-section of the hole × velocity of the flow of water from the hole, we have dVdt=πr2v=πr2c√2gh cm3/s.
- We found that the volume of water V cm3 is given by V=13π(3r2h+3rh2+h3), and so dVdh=π(r+h)2. Using the chain rule, we have dhdt=dhdV×dVdt=cr2√2gh(r+h)2 cm/s.