Gravitational fields

Gravitational Fields and Motion in a Circle

Learning Objectives

  • Define radian, angular displacement, angular speed (ω), period (T) and frequency (f) for uniform circular motion.
  • Derive and use the three equivalent forms of centripetal acceleration

      \(a_c = \dfrac{v^{2}}{r}= \omega^{2}r = \dfrac{4\pi^{2}r}{T^{2}}\).

  • Identify and calculate the different forces that can provide the required centripetal force (tension, friction, normal reaction, gravity, banking).
  • Define a gravitational field, write its strength \(g\) and potential \(V\), and sketch field‑line diagrams.
  • Apply the equality \(a_c = g\) to satellites, derive orbital speed, period and the condition for a geostationary orbit.
  • Spot common misconceptions and avoid typical exam pitfalls.
  • Solve a range of Cambridge‑style questions involving circular motion and gravitation.

1. Uniform Circular Motion – Kinematics

1.1 Angular quantities

  • Radian: the angle subtended at the centre of a circle by an arc equal in length to the radius. 1 rad = \( \dfrac{\text{arc length}}{r}\). 360° = \(2\pi\) rad.
  • Angular displacement \(\theta\) (rad) – change in direction of the radius vector.
  • Angular speed \(\displaystyle \omega = \frac{\Delta\theta}{\Delta t}\) (rad s⁻¹).
  • Period \(T\) – time for one complete revolution (s). \(\displaystyle T = \frac{2\pi}{\omega}\).
  • Frequency \(f\) – revolutions per second (Hz). \(\displaystyle f = \frac{1}{T} = \frac{\omega}{2\pi}\).

1.2 Relationship between linear and angular quantities

\[

v = \frac{2\pi r}{T}= r\omega ,\qquad

a_t = \frac{dv}{dt}\;( \text{tangential}),\qquad

a_c = \frac{v^{2}}{r}= \omega^{2}r = \frac{4\pi^{2}r}{T^{2}} .

\]

1.3 Derivation of the three forms of centripetal acceleration

  1. Start from the definition of acceleration for a change in direction:

    \[

    a_c = \frac{v^{2}}{r}.

    \]

  2. Substitute \(v = \omega r\):

    \[

    a_c = (\omega r)^{2}/r = \omega^{2}r .

    \]

  3. Replace \(\omega\) by \(2\pi/T\):

    \[

    a_c = \left(\frac{2\pi}{T}\right)^{2}r = \frac{4\pi^{2}r}{T^{2}} .

    \]

All three expressions are mathematically identical; choose the one that contains the quantities given in the question.

1.4 Sources of the required centripetal force

SourceTypical exampleForce expression (inward)
TensionBall on a string\(T = \dfrac{mv^{2}}{r}\)
FrictionCar on a flat curve\(F_f = \mu N = \mu mg = \dfrac{mv^{2}}{r}\)
Normal reaction (banked curve)Road banked at angle θ\(N\sin\theta = \dfrac{mv^{2}}{r}\) with \(N\cos\theta = mg\)
GravitySatellite in orbit\(\dfrac{GMm}{r^{2}} = \dfrac{mv^{2}}{r}\)

1.5 Example – Car on a banked curve (no friction)

\[

\begin{aligned}

N\sin\theta &= \frac{mv^{2}}{r},\\

N\cos\theta &= mg .

\end{aligned}

\]

Eliminate \(N\):

\[

v = \sqrt{rg\tan\theta } .

\]

For \(r=50\;\text{m}\) and \(\theta =30^{\circ}\):

\[

v = \sqrt{50\times9.81\times\tan30^{\circ}} \approx 12.0\;\text{m s}^{-1}.

\]

2. Gravitational Fields

2.1 Definition

The gravitational field \(\mathbf g\) at a point is the force per unit mass that a test mass would experience there:

\[

\mathbf g = \frac{\mathbf F_g}{m}\qquad\text{(units: m s⁻²)} .

\]

2.2 Field strength for a point mass

\[

g = \frac{GM}{r^{2}},\qquad \mathbf g \text{ directed toward the centre of mass}.

\]

2.3 Gravitational potential

Potential \(V\) is the work done per unit mass in bringing a test mass from infinity to a distance \(r\):

\[

V = -\frac{GM}{r}\qquad\text{(units: J kg⁻¹)} .

\]

The field and potential are related by \(\mathbf g = -\nabla V\).

2.4 Field‑line diagrams

  • Lines point radially inward toward the mass.
  • Density of lines ∝ field strength (closer → denser).
  • For a spherical body the field is the same at any point on a sphere of radius \(r\) (symmetry).

2.5 Example – Gravitational field 400 km above Earth

\[

\begin{aligned}

R_E &= 6.37\times10^{6}\;\text{m},\quad h = 4.0\times10^{5}\;\text{m},\\

r &= R_E + h = 6.77\times10^{6}\;\text{m},\\[4pt]

g &= \frac{GM_E}{r^{2}} = \frac{3.986\times10^{14}}{(6.77\times10^{6})^{2}}

\approx 8.7\;\text{m s}^{-2}.

\end{aligned}

\]

3. Satellite Motion – Using the Gravitational Field

3.1 Equality of centripetal acceleration and field strength

\[

a_c = \frac{v^{2}}{r} = g = \frac{GM}{r^{2}} .

\]

3.2 Orbital speed

\[

v = \sqrt{\frac{GM}{r}} .

\]

3.3 Orbital period

\[

\begin{aligned}

v &= \frac{2\pi r}{T}\;\Longrightarrow\;

T = \frac{2\pi r}{v}

= 2\pi\sqrt{\frac{r^{3}}{GM}} .

\end{aligned}

\]

3.4 Geostationary orbit

A satellite is geostationary when its period equals the Earth’s rotation period (\(T=86400\;\text{s}\)).

Setting \(T\) in the period formula gives the required radius:

\[

r{\text{geo}} = \left(\frac{GME T^{2}}{4\pi^{2}}\right)^{\!1/3}

\approx 4.22\times10^{7}\;\text{m}.

\]

Altitude above the surface:

\[

h{\text{geo}} = r{\text{geo}}-R_E \approx 3.58\times10^{7}\;\text{m}

\;(35\,800\;\text{km}).

\]

Orbital speed at this radius:

\[

v{\text{geo}} = \frac{2\pi r{\text{geo}}}{T}

\approx 3.07\times10^{3}\;\text{m s}^{-1}.

\]

4. Summary Comparison – Circular Motion vs. Gravitational Field

QuantitySymbolExpressionSource / Physical originUnits
Centripetal acceleration\(a_c\)\(\dfrac{v^{2}}{r}= \omega^{2}r = \dfrac{4\pi^{2}r}{T^{2}}\)Resultant inward acceleration of any circular motionm s⁻²
Gravitational field strengthg\(\dfrac{GM}{r^{2}}\)Mass \(M\) (Earth, planet, star)m s⁻²
Centripetal force\(F_c\)\(\dfrac{mv^{2}}{r}=m\omega^{2}r\)Provided by tension, friction, normal reaction, or gravityN
Gravitational force\(F_g\)\(\dfrac{GMm}{r^{2}}\)Interaction between two massesN
Gravitational potentialV\(-\dfrac{GM}{r}\)Work per unit mass from infinity to \(r\)J kg⁻¹

5. Common Misconceptions (Cambridge Checklist)

  • Centripetal force is a new, separate force. It is simply the net inward force supplied by existing interactions (tension, friction, normal reaction, or gravity).
  • ‘Centrifugal force’ is a real force. It only appears in a rotating (non‑inertial) reference frame as a fictitious force.
  • Gravitational field is constant with height. It follows an inverse‑square law; \(g\) decreases as \(1/r^{2}\).
  • Orbital speed depends only on altitude. It also depends on the mass of the central body: \(v=\sqrt{GM/r}\).
  • All satellites have the same period. Period varies with orbital radius; only the specific geostationary radius gives a 24 h period.
  • Banked‑curve formula \(v=\sqrt{rg\tan\theta}\) works on flat roads. It is valid only when friction is negligible.

6. Worked Practice Questions (Cambridge‑style)

  1. Centripetal acceleration of a car

    Speed \(v = 20\;\text{m s}^{-1}\), curve radius \(r = 50\;\text{m}\).

    \[

    a_c = \frac{v^{2}}{r}= \frac{20^{2}}{50}=8.0\;\text{m s}^{-2}.

    \]

    Force required for a 1500 kg car:

    \[

    Fc = mac = 1500\times8.0 = 1.2\times10^{4}\;\text{N}.

    \]

  2. Gravitational field 400 km above Earth (repeat of 2.4)

    \(g \approx 8.7\;\text{m s}^{-2}\).

    Corresponding orbital speed:

    \[

    v = \sqrt{gr}= \sqrt{8.7\times6.77\times10^{6}} \approx 7.68\times10^{3}\;\text{m s}^{-1}.

    \]

  3. Satellite around Mars

    \(M_M = 6.42\times10^{23}\;\text{kg}\), orbital radius \(r = 1.0\times10^{7}\;\text{m}\).

    \[

    v = \sqrt{\frac{GM_M}{r}}

    = \sqrt{\frac{6.67\times10^{-11}\times6.42\times10^{23}}{1.0\times10^{7}}}

    \approx 3.28\times10^{3}\;\text{m s}^{-1}.

    \]

    \[

    a_c = \frac{v^{2}}{r}\approx1.08\;\text{m s}^{-2},

    \qquad g = \frac{GM_M}{r^{2}} \approx 1.08\;\text{m s}^{-2}.

    \]

  4. Design speed of a banked curve

    \(r = 80\;\text{m}\), banking angle \(\theta = 20^{\circ}\).

    \[

    v = \sqrt{rg\tan\theta}= \sqrt{80\times9.81\times\tan20^{\circ}}

    \approx 13.2\;\text{m s}^{-1}.

    \]

  5. Geostationary orbit radius and speed (use \(T=86400\;\text{s}\)).

    \[

    r{\text{geo}} = \left(\frac{GME T^{2}}{4\pi^{2}}\right)^{1/3}

    \approx 4.22\times10^{7}\;\text{m},

    \]

    \[

    v{\text{geo}} = \frac{2\pi r{\text{geo}}}{T}

    \approx 3.07\times10^{3}\;\text{m s}^{-1}.

    \]

  6. Energy of a satellite in circular orbit

    Show that the total mechanical energy per unit mass is \(\displaystyle \frac{E}{m}= -\frac{GM}{2r}\).

    Solution:

    Kinetic energy per unit mass \(= \frac{v^{2}}{2}= \frac{GM}{2r}\).

    Potential energy per unit mass \(= -\frac{GM}{r}\).

    Hence \(E/m = \frac{GM}{2r} - \frac{GM}{r}= -\frac{GM}{2r}\).

    (This result is useful for exam questions on orbital energy.)

7. Suggested Diagrams (to be drawn by the student)

  • Top‑down view of uniform circular motion showing radius \(r\), tangential velocity \(\mathbf v\), and inward centripetal acceleration \(\mathbf a_c\).
  • Free‑body diagram of a ball on a string (tension providing \(F_c\)).
  • Banked curve with forces \(N\), \(mg\) and the horizontal component \(N\sin\theta\) supplying \(F_c\).
  • Field‑line diagram for a point mass (lines converging toward the centre, density increasing as \(1/r^{2}\)).
  • Satellite in circular orbit: show \(\mathbf g\) directed toward the planet, \(\mathbf v\) tangent to the orbit, and the equality \(a_c=g\).

8. Quick Reference Sheet

SymbolDefinitionFormula
\(\theta\)Angular displacement (rad)
\(\omega\)Angular speed (rad s⁻¹)\(\omega = \dfrac{2\pi}{T}=2\pi f\)
\(v\)Linear (tangential) speed (m s⁻¹)\(v = r\omega = \dfrac{2\pi r}{T}\)
\(a_c\)Centripetal acceleration (m s⁻²)\(\dfrac{v^{2}}{r}= \omega^{2}r = \dfrac{4\pi^{2}r}{T^{2}}\)
\(Fc\)Centripetal force (N)\(Fc = ma_c = \dfrac{mv^{2}}{r}\)
\(g\)Gravitational field strength (m s⁻²)\(g = \dfrac{GM}{r^{2}}\)
\(V\)Gravitational potential (J kg⁻¹)\(V = -\dfrac{GM}{r}\)
\(T\)Period of revolution (s)\(T = \dfrac{2\pi r}{v}=2\pi\sqrt{\dfrac{r^{3}}{GM}}\)
\(f\)Frequency (Hz)\(f = 1/T\)

9. Checklist for Exam Answers

  • State which form of the centripetal‑acceleration equation you are using and why.
  • Show clearly how the required inward force is supplied (tension, friction, normal, or gravity).
  • When dealing with satellites, start from \(Fc = Fg\) and then substitute \(v = 2\pi r/T\) if the period is required.
  • Include units at every step; convert where necessary.
  • For field‑line diagrams, label the direction of \(\mathbf g\) and indicate that the density of lines ∝ \(1/r^{2}\).
  • Check the final answer against typical magnitude expectations (e.g., \(g\approx9.8\;\text{m s}^{-2}\) at Earth’s surface, orbital speeds of a few km s⁻¹).