Class 12 Maths, Worked in Full Past papersGet updates
Chapter 6 · Application of Derivatives

Example 31: Conical tank with α=tan⁡−1(0.5)\alpha=\tan^{-1}(0.5)⁠: how fast the water level rises at depth 4 m

ExamplesRate of change of quantities · Section 6.2 · Miscellaneous Examples
The question

A water tank has the shape of an inverted right circular cone with its axis vertical and vertex lowermost. Its semi-vertical angle is tan⁡−1(0.5)\tan^{-1}(0.5)⁠. Water is poured into it at a constant rate of 5 cubic metre per hour. Find the rate at which the level of the water is rising at the instant when the depth of water in the tank is 4 m.

Exam answer

Let rr m, hh m and VV m³ be the radius, depth and volume of the water at time tt h. Given dVdt=5\frac{dV}{dt} = 5 m³/h.

If α\alpha is the semi-vertical angle, tan⁡α=rh\tan\alpha = \frac{r}{h} and tan⁡α=0.5\tan\alpha = 0.5⁠, so r=h2r = \frac{h}{2}⁠.

V=13πr2h=13π(h2)2h=πh312\begin{aligned} V &= \frac13\pi r^2h \\ &= \frac13\pi\left(\frac{h}{2}\right)^2h = \frac{\pi h^3}{12} \end{aligned}

Differentiating w.r.t. tt⁠,

dVdt=πh24⋅dhdt\frac{dV}{dt} = \frac{\pi h^2}{4}\cdot\frac{dh}{dt}

At h=4h = 4⁠, with dVdt=5\frac{dV}{dt} = 5⁠:

5=π(4)24⋅dhdt=4π dhdt⇒ dhdt=54π\begin{aligned} 5 &= \frac{\pi(4)^2}{4}\cdot\frac{dh}{dt} = 4\pi\,\frac{dh}{dt} \\ \Rightarrow\ \frac{dh}{dt} &= \frac{5}{4\pi} \end{aligned}

∴\therefore the water level is rising at 54π\dfrac{5}{4\pi} m/h, that is 3588\dfrac{35}{88} m/h taking π=227\pi = \dfrac{22}{7}⁠.

Want the reason behind every step, the basics and the checks?

The one idea this problem is built on

The water inside a conical tank is itself a cone, with the same semi-vertical angle as the tank. That fixes the ratio of its radius to its depth, r=htan⁡αr = h \tan\alpha⁠, so the volume can be written using the depth alone. Then one differentiation with respect to time (chain rule) links the known rate dVdt\frac{dV}{dt} to the wanted rate dhdt\frac{dh}{dt}⁠. The particular depth 4 m is put in only after differentiating.

Given, to find, and the plan
Given
Inverted cone, vertex down, semi-vertical angle α=tan⁡−1(0.5)\alpha = \tan^{-1}(0.5)⁠. Water flows in at dVdt=5\frac{dV}{dt} = 5 m³/h. At the instant considered, the depth is h=4h = 4 m.
To find
dhdt\frac{dh}{dt} at that instant: how fast the water level rises, in m/h.
Plan
Name hh⁠, rr⁠, VV at time tt⁠. Use tan⁡α=rh\tan\alpha = \frac{r}{h} to get r=h2r = \frac{h}{2}⁠. Write VV in terms of hh only. Differentiate with respect to tt by the chain rule. Then substitute h=4h = 4 and dVdt=5\frac{dV}{dt} = 5 and solve for dhdt\frac{dh}{dt}⁠.

Basics you need

1Volume of a cone

A right circular cone of base radius rr and height hh has volume V=13πr2hV = \frac{1}{3}\pi r^2 h⁠. Basics: area and volume formulas

2Semi-vertical angle and tan

The semi-vertical angle α\alpha is the angle between the axis and the slant side. In the right triangle formed by the axis (length hh⁠), a radius of the top circle (length rr⁠) and the slant side, the side opposite α\alpha is rr and the adjacent side is hh⁠, so tan⁡α=rh\tan\alpha = \frac{r}{h}⁠.

3tan⁡(tan⁡−1y)=y\tan(\tan^{-1} y) = y

For every real yy⁠, tan⁡−1y\tan^{-1} y is the angle in (−π2,π2)\left(-\frac{\pi}{2}, \frac{\pi}{2}\right) whose tangent is yy (Chapter 2). So α=tan⁡−1(0.5)\alpha = \tan^{-1}(0.5) means exactly tan⁡α=0.5\tan\alpha = 0.5⁠, with α\alpha between 0 and π2\frac{\pi}{2} (about 26.57°).

4Chain rule for related rates

If VV depends on hh and hh depends on tt⁠, then dVdt=dVdh⋅dhdt\frac{dV}{dt} = \frac{dV}{dh}\cdot\frac{dh}{dt}⁠. This is how a rate we know is linked to a rate we want. Basics: related rates

Solution

  1. Name the changing quantities

    At time tt hours after some moment, let

    • hh = depth of the water (m), measured up the axis from the vertex,
    • rr = radius of the water surface (m),
    • VV = volume of water in the tank (m³).

    We know dVdt=5\frac{dV}{dt} = 5 m³/h at every instant, and we want dhdt\frac{dh}{dt} at the instant when h=4h = 4 m.

    r h = 4 m now α water in: dV/dt = 5 m³/h tan α = r/h = 0.5 so r = h/2 vertex (lowest point)
    The water forms a smaller cone inside the tank, with the same angle α\alpha at the vertex. Its depth is hh and its surface radius is rr⁠.
    All three quantities change as water is poured in, so they are functions of tt⁠. Writing their units now tells us what unit the answer must have: dhdt\frac{dh}{dt} will be in metres per hour.
    "Level rising" means the depth hh increasing, so the rate asked for is dhdt\frac{dh}{dt}⁠. Basics: rate of change as a derivative
  2. Link rr and hh using the angle

    The water is a cone with the tank's vertex and axis, so its semi-vertical angle is also α\alpha⁠. In its right triangle (Basic 2),

    tan⁡α=rh.\tan\alpha = \frac{r}{h}.

    Since α=tan⁡−1(0.5)\alpha = \tan^{-1}(0.5)⁠, we have tan⁡α=0.5\tan\alpha = 0.5⁠, so

    rh=0.5,r=h2.\frac{r}{h} = 0.5, \qquad r = \frac{h}{2}.

    This holds at every instant, whatever the depth.

    The volume formula contains two changing lengths, rr and hh⁠, but we are told about dV/dtdV/dt and asked about dh/dtdh/dt only. The fixed shape of the tank lets us remove rr⁠. Note the order of the ratio: rr is opposite α\alpha⁠, hh is adjacent.
    tan⁡(tan⁡−1y)=y\tan(\tan^{-1}y) = y for every real yy (Chapter 2, principal value branch of tan⁡−1\tan^{-1}⁠).
  3. Volume in terms of the depth alone

    V=13πr2h=13π(h2)2h=13π⋅h24⋅h=πh312.\begin{aligned} V &= \frac{1}{3}\pi r^2 h = \frac{1}{3}\pi\left(\frac{h}{2}\right)^2 h \\ &= \frac{1}{3}\pi\cdot\frac{h^2}{4}\cdot h = \frac{\pi h^3}{12}. \end{aligned}
    Now VV is a function of the single variable hh⁠, which in turn is a function of tt⁠. That is exactly the set-up the chain rule needs.
    Cone volume 13πr2h\frac{1}{3}\pi r^2 h⁠; (h2)2=h24\left(\frac{h}{2}\right)^2 = \frac{h^2}{4}⁠. Basics: area and volume formulas
  4. Differentiate with respect to time (chain rule)

    dVdt=ddh(πh312)⋅dhdt=3πh212⋅dhdt=πh24⋅dhdt.\begin{aligned} \frac{dV}{dt} &= \frac{d}{dh}\left(\frac{\pi h^3}{12}\right)\cdot\frac{dh}{dt} \\ &= \frac{3\pi h^2}{12}\cdot\frac{dh}{dt} = \frac{\pi h^2}{4}\cdot\frac{dh}{dt}. \end{aligned}

    Here the outer function is h↦πh312h \mapsto \frac{\pi h^3}{12} and the inner function is t↦h(t)t \mapsto h(t)⁠.

    This equation holds at every instant. It is the bridge between the rate we know (dV/dtdV/dt⁠) and the rate we want (dh/dtdh/dt⁠). We differentiate before substituting h=4h = 4⁠: if we put h=4h = 4 first, VV would become the constant 16π3\frac{16\pi}{3}⁠, whose derivative is 0, and all information about the change would be lost.
    Chain rule: dVdt=dVdh⋅dhdt\frac{dV}{dt} = \frac{dV}{dh}\cdot\frac{dh}{dt}⁠; power rule ddhh3=3h2\frac{d}{dh}h^3 = 3h^2⁠. Basics: related rates
  5. Substitute the instant and solve

    At the instant, dVdt=5\frac{dV}{dt} = 5 and h=4h = 4⁠:

    5=π(4)24⋅dhdt=4π dhdt,5 = \frac{\pi (4)^2}{4}\cdot\frac{dh}{dt} = 4\pi\,\frac{dh}{dt}, dhdt=54π m/h.\frac{dh}{dt} = \frac{5}{4\pi}\ \text{m/h}.
    Only now, with the derivative relation in hand, do we use the particular depth. The equation is linear in dhdt\frac{dh}{dt}⁠, so we just divide by 4π4\pi⁠.
    π⋅164=4π\frac{\pi\cdot 16}{4} = 4\pi⁠.
  6. Put a number on it

    Exactly, dhdt=54π≈0.3979\frac{dh}{dt} = \frac{5}{4\pi} \approx 0.3979 m/h. The textbook uses π=227\pi = \frac{22}{7}⁠:

    54⋅227=5⋅788=3588≈0.3977 m/h.\frac{5}{4\cdot\frac{22}{7}} = \frac{5\cdot 7}{88} = \frac{35}{88} \approx 0.3977\ \text{m/h}.

    The rate is positive, so the level is rising at 54π\frac{5}{4\pi} m/h, that is 3588\frac{35}{88} m/h with π=227\pi = \frac{22}{7}, roughly 40 cm per hour.

    The two decimals differ only in the fourth place because 227\frac{22}{7} is a close approximation to π\pi (227≈3.1429\frac{22}{7} \approx 3.1429⁠, π≈3.1416\pi \approx 3.1416⁠). The book's answer 3588\frac{35}{88} uses this approximation; 54π\frac{5}{4\pi} is the exact value.
    A positive rate of change means the quantity is increasing at that instant. Basics: rate of change as a derivative
Result

At the instant the water is 4 m deep, the level is rising at dhdt=54π≈0.398\frac{dh}{dt} = \frac{5}{4\pi} \approx 0.398 m/h, which is 3588\frac{35}{88} m/h when π\pi is taken as 227\frac{22}{7}⁠. (Textbook's own solution: 3588\frac{35}{88} m/h.)

Check it with numbers

Thin-layer picture. At depth 4 m the surface radius is r=2r = 2 m, so the surface area is πr2=4π≈12.5664\pi r^2 = 4\pi \approx 12.5664 m². In a short time the new water spreads as a thin layer over this surface: volume ≈\approx area ×\times rise, so the rise rate is 54π\frac{5}{4\pi}⁠, the same as Step 5.

A small time step. At depth 4 m, V=π⋅6412≈16.755161V = \frac{\pi\cdot 64}{12} \approx 16.755161 m³. After 0.001 h a further 0.005 m³ has entered, and solving πh312=16.760161\frac{\pi h^3}{12} = 16.760161 gives h≈4.000398h \approx 4.000398 m. The depth rose by about 0.000398 m in 0.001 h, a rate of about 0.398 m/h.

Common mistakes
  1. Substituting h=4h = 4 before differentiating. This turns VV into a constant and gives a rate of 0.
  2. Treating rr as a constant. Writing dVdt=13πr2dhdt\frac{dV}{dt} = \frac{1}{3}\pi r^2 \frac{dh}{dt} ignores that the surface widens as the water rises. Remove rr first with r=h2r = \frac{h}{2}⁠.
  3. Inverting the ratio. tan⁡α\tan\alpha is opposite over adjacent, rh\frac{r}{h}⁠, not hr\frac{h}{r}⁠. Using h=r2h = \frac{r}{2}⁠, that is r=2hr = 2h⁠, would describe a much wider tank (one with tan⁡α=2\tan\alpha = 2⁠) and give dhdt=564π\frac{dh}{dt} = \frac{5}{64\pi} m/h, 16 times too small.
  4. Forgetting units. The answer is a rate of length per time: metres per hour.
What to take away
  1. Related rates: name the quantities, find a relation true at every instant, differentiate with respect to time, and only then substitute the instant.
  2. Use the geometry (similar shapes, a fixed angle) to reduce the relation to one variable before differentiating.
  3. In general dhdt=4πh2⋅dVdt\frac{dh}{dt} = \frac{4}{\pi h^2}\cdot\frac{dV}{dt}⁠: at a steady inflow the level rises more slowly as the water gets deeper, because the cone gets wider.

Every fact used, and where it comes from

FactUsed inSource
Rate of change of a quantity is its derivativeSteps 1, 6Section 6.2 (Lesson: rate of change)
tan⁡α=rh\tan\alpha = \frac{r}{h} for the semi-vertical angleStep 2Right-triangle trigonometry; Fig 6.20 of the textbook
tan⁡(tan⁡−1y)=y\tan(\tan^{-1}y) = yStep 2Chapter 2, Inverse Trigonometric Functions
Cone volume V=13πr2hV = \frac{1}{3}\pi r^2 hStep 3Mensuration
Chain rule dVdt=dVdh⋅dhdt\frac{dV}{dt} = \frac{dV}{dh}\cdot\frac{dh}{dt}Step 4Chapter 5 (chain rule); used for rates in Section 6.2
π≈227\pi \approx \frac{22}{7} in the book's final figureStep 6Example 31, Miscellaneous Examples, Chapter 6
Found an error, or want more?

Tell us if something on this page is wrong or unclear, or if you would like a fuller explanation, another method or a new feature. Send feedback on this problem →