9702/43

Physics 9702/43May/June 2010

Cambridge A-Level · A Level Structured Questions · worked solutions for every part, with the mark scheme

12
questions
100
marks
105
minutes

Topics Alternating Currents · Electronics · Gravitational Fields · Oscillations · Temperature · Electric Fields · +5 more

Q1Gravitational FieldsFree sample
(a)

Define gravitational potential at a point.

2M
DifficultyEasy
Worked solution

Answer

Gravitational potential ϕ\phi at a point is the work done per unit mass by an external agent in bringing a small test mass from infinity to that point (with no change in kinetic energy).

Final answer

Work done per unit mass to bring a test mass from infinity to the point (no change in KE).

Detailed explanation

Background Concept

Gravitational potential ϕ\phi at a point is a measure of “how much gravitational potential energy per unit mass” an object would have at that point, taking ϕ=0\phi=0 at infinity.

Because it is per unit mass, its unit is

J kg1.\text{J kg}^{-1}.

For a gravitational field, the change in gravitational potential energy is related to potential by

ΔEp=mΔϕ.\Delta E_p = m\,\Delta \phi.

Understanding the Question

You are asked to define gravitational potential at a point. A good Cambridge definition must include:

  • that it is work done per unit mass, and
  • that the reference position is infinity (where potential is taken as zero), and typically
  • that the mass is brought slowly so there is no change in kinetic energy.

Approach

Write the standard definition: describe moving a small test mass from infinity to the point, then express it as work done per unit mass (or potential energy per unit mass).

Step-by-Step Reasoning

  1. Choose the reference: ϕ=0\phi=0 at infinity.
  2. Bring a small test mass from infinity to the point. If it is moved slowly, its kinetic energy does not change.
  3. The work done by an external agent (against the gravitational attraction) equals the gain in gravitational potential energy.
  4. Divide this work by the mass to get “per unit mass”, which is the gravitational potential ϕ\phi.

Key Takeaways

  • Gravitational potential is work done per unit mass from infinity.
  • Units: J kg1\text{J kg}^{-1}.
  • Infinity is the standard zero of potential for isolated spherical masses.

Common Mistakes

  • Defining it as “force per unit mass” (that is gravitational field strength gg).
  • Missing “per unit mass”.
  • Not stating the reference point (infinity).

Things to Be Careful About

  • Potential ϕ\phi is a scalar.
  • In gravity, potentials near a mass are negative when ϕ()=0\phi(\infty)=0.
Techniques used
state the definition of gravitational potential in terms of work done per unit massreference infinity as the zero of potential
(b)

The Earth may be considered to be an isolated sphere of radius RR with its mass concentrated at its centre.
The variation of the gravitational potential ϕ\phi with distance xx from the centre of the Earth is shown in Fig. 1.1.

The radius RR of the Earth is 6.4×106 m6.4 \times 10^{6}\ \text{m}.

(i)

By considering the gravitational potential at the Earth’s surface, determine a value for the mass of the Earth.

mass = ______ kg\text{kg}

3M
DifficultyMedium-Easy
Worked solution

Working

From Fig. 1.1 at x=Rx = R, take

ϕ(R)6.3×107 J kg1.\phi(R) \approx -6.3 \times 10^{7}\ \text{J kg}^{-1}.

For a spherical mass,

ϕ=GMrM=ϕrG.\phi = -\frac{GM}{r} \Rightarrow M = -\frac{\phi r}{G}. M=(6.3×107)(6.4×106)6.67×10116.0×1024 kg.M = -\frac{\left(-6.3 \times 10^{7}\right)\left(6.4 \times 10^{6}\right)}{6.67 \times 10^{-11}} \approx 6.0 \times 10^{24}\ \text{kg}.

Answer

6.0×1024 kg6.0 \times 10^{24}\ \text{kg}

Final answer

6.0 × 10^24 kg

Detailed explanation

Background Concept

For a spherically symmetric body (mass concentrated at its centre), the gravitational potential at distance rr from the centre is

ϕ(r)=GMr,\phi(r) = -\frac{GM}{r},

taking ϕ=0\phi=0 at infinity. This is why the graph approaches 00 as rr increases.

Understanding the Question

You are given a graph of gravitational potential ϕ\phi against distance xx from Earth’s centre, and the Earth’s radius R=6.4×106 mR = 6.4\times 10^{6}\ \text{m}.

At the Earth’s surface, the distance from the centre is x=Rx=R. Reading ϕ\phi at x=Rx=R lets you solve for Earth’s mass MM using ϕ=GM/R\phi=-GM/R.

Approach

  1. Read the surface potential ϕ(R)\phi(R) from the graph.
  2. Use ϕ(R)=GM/R\phi(R) = -GM/R.
  3. Rearrange to get M=ϕ(R)R/GM = -\phi(R)R/G.
  4. Substitute values carefully (including the negative sign and powers of ten).

Step-by-Step Reasoning

  1. From the graph, at x=Rx=R the potential is about 6.3-6.3 on the scale of 107 J kg110^{7}\ \text{J kg}^{-1}, so
ϕ(R)6.3×107 J kg1.\phi(R) \approx -6.3 \times 10^{7}\ \text{J kg}^{-1}.
  1. Use the spherical potential formula:
ϕ(R)=GMR.\phi(R) = -\frac{GM}{R}.
  1. Rearrange:
M=ϕ(R)RG.M = -\frac{\phi(R)\,R}{G}.
  1. Substitute R=6.4×106 mR=6.4\times 10^{6}\ \text{m} and G=6.67×1011 N m2 kg2G=6.67\times 10^{-11}\ \text{N m}^2\ \text{kg}^{-2}:
M(6.3×107)(6.4×106)6.67×10116.0×1024 kg.M \approx -\frac{(-6.3\times 10^{7})(6.4\times 10^{6})}{6.67\times 10^{-11}} \approx 6.0\times 10^{24}\ \text{kg}.

The sign works out because ϕ\phi is negative, but mass must be positive.

Key Takeaways

  • For an isolated sphere, ϕ1/r\phi \propto -1/r.
  • Surface potential gives MM via ϕ(R)=GM/R\phi(R)=-GM/R.
  • Care with signs: ϕ\phi is negative, MM is positive.

Common Mistakes

  • Using r=2Rr=2R or another value instead of r=Rr=R for the surface.
  • Dropping the negative sign and getting a negative mass.
  • Reading the graph value but forgetting the axis scale factor 10710^{7}.

Things to Be Careful About

  • xx is distance from the centre of Earth.
  • Quote MM to a sensible number of significant figures consistent with the graph reading (typically 2 s.f.).
Techniques used
read a value from a graphuse the potential of a spherical mass \(\phi = -GM/r\)rearrange to solve for masssubstitute values with correct powers of ten
(ii)

A meteorite is at rest at infinity. The meteorite travels from infinity towards the Earth.

Calculate the speed of the meteorite when it is at a distance of 2R2R above the Earth’s surface. Explain your working.

speed = ______ m s1\text{m s}^{-1}

4M
DifficultyMedium
Worked solution

Working

At 2R2R above the surface, distance from centre

r=R+2R=3R.r = R + 2R = 3R.

From the 1/r1/r variation,

ϕ(3R)=ϕ(R)36.3×1073=2.1×107 J kg1.\phi(3R) = \frac{\phi(R)}{3} \approx \frac{-6.3\times 10^{7}}{3} = -2.1\times 10^{7}\ \text{J kg}^{-1}.

Meteorite starts from rest at infinity, so using energy per unit mass:

12v2+ϕ=012v2=ϕ.\frac{1}{2}v^2 + \phi = 0 \Rightarrow \frac{1}{2}v^2 = -\phi. v=2ϕ(3R)=4.2×1076.5×103 m s1.v = \sqrt{-2\phi(3R)} = \sqrt{4.2\times 10^{7}} \approx 6.5\times 10^{3}\ \text{m s}^{-1}.

Answer

6.5×103 m s16.5 \times 10^{3}\ \text{m s}^{-1}

Final answer

6.5 × 10^3 m s^-1

Detailed explanation

Background Concept

If gravitational potential is defined with ϕ()=0\phi(\infty)=0, then for a mass mm at radius rr the gravitational potential energy is

Ep=mϕ(r).E_p = m\phi(r).

If an object falls from infinity starting from rest, its total mechanical energy per unit mass stays constant:

12v2+ϕ=constant.\frac{1}{2}v^2 + \phi = \text{constant}.

At infinity, v=0v=0 and ϕ=0\phi=0, so the constant is 00:

12v2+ϕ=012v2=ϕ.\frac{1}{2}v^2 + \phi = 0 \Rightarrow \frac{1}{2}v^2 = -\phi.

This is a very efficient way to find the speed from a known potential.

Understanding the Question

A meteorite starts at rest at infinity and moves towards Earth. You must find its speed when it is a distance 2R2R above Earth’s surface.

2R2R above the surface” is an altitude. The gravitational potential graph is plotted against distance from the centre, so you must convert to radius from the centre:

r=R+2R=3R.r = R + 2R = 3R.

Then you need ϕ\phi at r=3Rr=3R, and use energy conservation to get vv.

Approach

  1. Convert altitude to distance from Earth’s centre (r=3Rr=3R).
  2. Find ϕ(3R)\phi(3R) from the graph (or from the 1/r1/r form).
  3. Apply conservation of energy per unit mass: 12v2=ϕ(3R)\tfrac12 v^2 = -\phi(3R).
  4. Solve for vv.

Step-by-Step Reasoning

  1. Distance from centre:
r=3R.r = 3R.
  1. From the graph, ϕ(R)6.3×107 J kg1\phi(R)\approx -6.3\times 10^{7}\ \text{J kg}^{-1}. For an isolated sphere ϕ1/r\phi\propto -1/r, so tripling rr makes the potential one third as negative:
ϕ(3R)=ϕ(R)32.1×107 J kg1.\phi(3R) = \frac{\phi(R)}{3} \approx -2.1\times 10^{7}\ \text{J kg}^{-1}.
  1. Use energy per unit mass. At infinity, total specific energy is 00. So at 3R3R:
12v2+ϕ(3R)=0.\frac{1}{2}v^2 + \phi(3R)=0.

Hence

12v2=ϕ(3R)=2.1×107.\frac{1}{2}v^2 = -\phi(3R) = 2.1\times 10^{7}.
  1. Solve for speed:
v=2(2.1×107)=4.2×1076.5×103 m s1.v = \sqrt{2(2.1\times 10^{7})} = \sqrt{4.2\times 10^{7}} \approx 6.5\times 10^{3}\ \text{m s}^{-1}.

Key Takeaways

  • Convert “above the surface” to radius from the centre before using ϕ(r)\phi(r).
  • Falling from rest at infinity gives the very useful relation 12v2=ϕ\tfrac12 v^2 = -\phi.
  • Gravitational potential is negative; the minus sign is essential.

Common Mistakes

  • Taking the distance as 2R2R instead of 3R3R.
  • Using Δϕ\Delta \phi with the wrong sign (getting negative kinetic energy).
  • Treating ϕ\phi as if it were gravitational field strength gg.

Things to Be Careful About

  • Use distance from the centre consistently.
  • Keep units as J kg1\text{J kg}^{-1} for potential; then vv comes out in m s1\text{m s}^{-1} because 1 J kg1=1 m2 s21\ \text{J kg}^{-1} = 1\ \text{m}^2\ \text{s}^{-2}.
Techniques used
interpret distance above the surface as distance from the centreuse conservation of energy per unit massuse \(\frac{1}{2}v^2 = -\phi\) for a drop from infinityextract potential at a given radius using the \(1/r\) dependence
(iii)

In practice, the Earth is not an isolated sphere because it is orbited by the Moon, as illustrated in Fig. 1.2.

The initial path of the meteorite is also shown.
Suggest two changes to the motion of the meteorite caused by the Moon.

  1. ______

  2. ______

2M
DifficultyMedium-Easy
Worked solution

Answer

  1. The meteorite’s path is deflected (trajectory curves) towards the Moon, so it is not along the isolated-Earth path.
  2. The meteorite’s speed at a given position changes because the Moon’s gravity changes the gravitational potential/energy (it may be accelerated towards the Moon and could even strike or be captured by it).
Final answer

Trajectory deflected towards Moon; speed at a given point altered (may be accelerated towards Moon / possibly collide or be captured).

Detailed explanation

Background Concept

Gravitational effects from more than one body combine by superposition:

  • The net gravitational field at a point is the vector sum of the individual fields.
  • The net gravitational potential at a point is the scalar sum of the individual potentials.

So with Earth and Moon present, the meteorite experiences an additional gravitational pull towards the Moon as well as towards Earth.

Understanding the Question

In the earlier parts, Earth was treated as an isolated sphere so the meteorite would accelerate directly towards Earth’s centre (a symmetric situation).

Now the Moon is present. The question asks for two changes to the motion (so typically one about direction/trajectory and one about speed/energy, or two distinct trajectory outcomes).

Approach

Think in terms of:

  1. Direction of acceleration: the Moon adds a sideways component of gravitational force, so the meteorite’s velocity direction changes.
  2. Speed/energy: the Moon changes the potential energy landscape, so the speed at a given location relative to Earth alone will not be the same.

Step-by-Step Reasoning

  • Without the Moon, forces point towards Earth’s centre only, giving a path aimed at Earth.
  • With the Moon, there is an additional force towards the Moon. Unless the meteorite is exactly on the Earth–Moon line in a symmetric position, this extra force is not collinear with the Earth’s force.
  • Therefore the resultant acceleration is not directly towards Earth’s centre, so the path bends (deflects) towards the Moon.
  • Because potential is a scalar that adds, the total gravitational potential at a point is more negative than with Earth alone (especially near the Moon). As the meteorite moves into a region of lower (more negative) potential, it loses more potential energy and gains kinetic energy differently, so its speed profile changes.
  • Depending on the geometry, the meteorite could pass closer to the Moon, be pulled into collision with the Moon, or be gravitationally deflected so it misses Earth.

Key Takeaways

  • Superposition: fields add as vectors, potentials add as scalars.
  • An extra massive body generally causes (i) a change in direction (trajectory) and (ii) a change in speed/energy compared with the isolated-body case.

Common Mistakes

  • Saying only “it goes faster” twice (need two distinct changes).
  • Claiming the potential graph of Earth alone still applies exactly (it does not when another mass is nearby).
  • Ignoring that force is a vector: the key effect is often a sideways deflection.

Things to Be Careful About

  • Keep statements qualitative but physically specific (e.g. “deflected towards the Moon” is better than “path changes”).
  • If you mention collision/capture, tie it to the Moon’s gravitational attraction (not random chance).
Techniques used
apply the idea of superposition of gravitational fieldspredict qualitative changes in trajectory from an additional gravitational attractionrelate changes in potential energy to changes in speed

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