· H2 Mathematics — Ten-Year Series, worked ← All 11 questions

2016 A-Level · Paper 1 · Question 9

2016 H2 Maths Paper 1, Question 9

Differential equations 12 marks motion in a fluid
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Part (i)(a)

1 mark

Since y=dxdty = \frac{dx}{dt}, differentiating with respect to tt gives dydt=d2xdt2\frac{dy}{dt} = \frac{d^{2}x}{dt^{2}}. Substituting into the given differential equation:

dydt+2y=10\frac{dy}{dt} + 2y = 10
dydt=10−2y  (shown)\frac{dy}{dt} = 10 - 2y\ \ \left( \text{shown} \right)

Part (i)(b)

6 marks

Approach

dydt=10−2y\frac{dy}{dt} = 10 - 2y has yy and tt separable, so we integrate directly and use y=0y = 0 at t=0t = 0 (since dxdt=0\frac{dx}{dt} = 0 when t=0t = 0) to fix the constant. Once yy is known in terms of tt, we integrate again — using x=0x = 0 at t=0t = 0 — to get xx.

Since dydt=10−2y\frac{dy}{dt} = 10 - 2y, separating variables,

∫110−2y dy=∫1 dt\int\frac{1}{10 - 2y}\, dy = \int 1\, dt
−12ln⁡∣10−2y∣=t+C- \frac{1}{2}\ln|10 - 2y| = t + C

Using y=0y = 0 when t=0t = 0:

−12ln⁡10=C- \frac{1}{2}\ln 10 = C

Substituting back,

−12ln⁡∣10−2y∣=t−12ln⁡10- \frac{1}{2}\ln|10 - 2y| = t - \frac{1}{2}\ln 10
ln⁡∣10−2y∣=ln⁡10−2t\ln|10 - 2y| = \ln 10 - 2t
∣10−2y∣=10e−2t|10 - 2y| = 10e^{- 2t}

Note: the stone starts at rest and speeds up towards a terminal value, so yy increases from 00 towards 55; 10−2y10 - 2y therefore stays positive throughout, and the modulus can be dropped.

10−2y=10e−2t10 - 2y = 10e^{- 2t}
y=5−5e−2ty = 5 - 5e^{- 2t}

So dxdt=5−5e−2t\frac{dx}{dt} = 5 - 5e^{- 2t}. Integrating with respect to tt:

x=∫(5−5e−2t)dtx = \int\left( 5 - 5e^{- 2t} \right)dt
=5t+52e−2t+D= 5t + \frac{5}{2}e^{- 2t} + D

Using x=0x = 0 when t=0t = 0:

0=52+D0 = \frac{5}{2} + D
D=−52D = - \frac{5}{2}
x=5t+52e−2t−52x = 5t + \frac{5}{2}e^{- 2t} - \frac{5}{2}
To check your answer: at t=0t = 0, x=0+52−52=0x = 0 + \frac{5}{2} - \frac{5}{2} = 0, matching the given initial condition. ✓

∴\therefore y=5−5e−2ty = 5 - 5e^{- 2t} and x=5t+52e−2t−52x = 5t + \frac{5}{2}e^{- 2t} - \frac{5}{2}.

Part (ii)

3 marks

Approach

here d2xdt2\frac{d^{2}x}{dt^{2}} is given directly as a function of tt, so we integrate twice in succession, using dxdt=0\frac{dx}{dt} = 0 at t=0t = 0 to fix the first constant and x=0x = 0 at t=0t = 0 to fix the second.

d2xdt2=10−5sin⁡12t\frac{d^{2}x}{dt^{2}} = 10 - 5\sin\frac{1}{2}t

Integrating with respect to tt:

dxdt=10t+10cos⁡12t+C1\frac{dx}{dt} = 10t + 10\cos\frac{1}{2}t + C_{1}

Using dxdt=0\frac{dx}{dt} = 0 when t=0t = 0:

0=10cos⁡0+C10 = 10\cos 0 + C_{1}
C1=−10C_{1} = - 10
dxdt=10t+10cos⁡12t−10\frac{dx}{dt} = 10t + 10\cos\frac{1}{2}t - 10

Integrating again:

x=5t2+20sin⁡12t−10t+C2x = 5t^{2} + 20\sin\frac{1}{2}t - 10t + C_{2}

Using x=0x = 0 when t=0t = 0:

0=20sin⁡0+C20 = 20\sin 0 + C_{2}
C2=0C_{2} = 0
x=5t2−10t+20sin⁡12tx = 5t^{2} - 10t + 20\sin\frac{1}{2}t

∴\therefore x=5t2−10t+20sin⁡12tx = 5t^{2} - 10t + 20\sin\frac{1}{2}t.

Part (iii)

2 marks

Approach

the pond is 5 m5\ m deep, so for each model we set x=5x = 5 and solve for tt. Neither equation can be solved for tt algebraically, so we treat each as a GC numerical-solution problem.

For Model (i), setting x=5x = 5:

5t+52e−2t−52=55t + \frac{5}{2}e^{- 2t} - \frac{5}{2} = 5

By GC, t=1.47 st = 1.47\ s (2 d.p.).

For Model (ii), setting x=5x = 5:

5t2−10t+20sin⁡12t=55t^{2} - 10t + 20\sin\frac{1}{2}t = 5

By GC, t=1.05 st = 1.05\ s (2 d.p.).

∴\therefore Model (i) predicts the stone reaches the bottom at t=1.47 st = 1.47\ s; Model (ii) predicts t=1.05 st = 1.05\ s.

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