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Gravitational Fields -- Diagnostic Tests

Gravity is like an invisible rubber sheet that bends under the weight of massive objects, guiding their motion.

UT-1: Gravitational Field Strength Above and Below the Surface

Section titled “UT-1: Gravitational Field Strength Above and Below the Surface”

Question:

The Earth may be modelled as a uniform sphere of mass ME=5.97×1024kgM_E = 5.97 \times 10^{24}\,\text{kg} and radius RE=6.37×106mR_E = 6.37 \times 10^6\,\text{m}.

(a) Calculate the gravitational field strength at a height h=3REh = 3R_E above the surface.

(b) Calculate the gravitational field strength at a depth d=RE/2d = R_E/2 below the surface (assuming uniform density).

(c) At what height above the surface is the gravitational field strength equal to the field strength at a depth RE/2R_E/2?

Take G=6.67×1011Nm2kg2G = 6.67 \times 10^{-11}\,\text{N}\,\text{m}^2\,\text{kg}^{-2}.

Solution:

(a) Distance from centre: r=RE+3RE=4REr = R_E + 3R_E = 4R_E

g=GMEr2=GME16RE2=g016g = \frac{GM_E}{r^2} = \frac{GM_E}{16R_E^2} = \frac{g_0}{16}

Where g0=GME/RE2=9.81ms2g_0 = GM_E/R_E^2 = 9.81\,\text{m}\,\text{s}^{-2}.

g=9.8116=0.613ms2g = \frac{9.81}{16} = 0.613\,\text{m}\,\text{s}^{-2}

(b) At depth d=RE/2d = R_E/2The distance from the centre is r=RE/2r = R_E/2.

By the shell theorem, only the mass within radius rr contributes:

Menclosed=ME(rRE)3=ME(12)3=ME8M_{\text{enclosed}} = M_E \left(\frac{r}{R_E}\right)^3 = M_E \left(\frac{1}{2}\right)^3 = \frac{M_E}{8}

g=GME/8(RE/2)2=GME8×4RE2=g02=9.812=4.91ms2g = \frac{G M_E/8}{(R_E/2)^2} = \frac{GM_E}{8} \times \frac{4}{R_E^2} = \frac{g_0}{2} = \frac{9.81}{2} = 4.91\,\text{m}\,\text{s}^{-2}

(c) We need gg at height hh to equal g0/2g_0/2:

GME(RE+h)2=g02=GME2RE2\frac{GM_E}{(R_E + h)^2} = \frac{g_0}{2} = \frac{GM_E}{2R_E^2}

(RE+h)2=2RE2(R_E + h)^2 = 2R_E^2 RE+h=2RER_E + h = \sqrt{2}R_E h=(21)RE=0.414×6.37×106=2.64×106mh = (\sqrt{2} - 1)R_E = 0.414 \times 6.37 \times 10^6 = 2.64 \times 10^6\,\text{m}


Question:

Mars has two small moons, Phobos and Deimos. Phobos orbits Mars at a radius of 9.38×106m9.38 \times 10^6\,\text{m} with a period of 7.667.66 hours. Deimos orbits at a radius of 2.35×107m2.35 \times 10^7\,\text{m}.

(a) Use Kepler’s third law to calculate the orbital period of Deimos.

(b) Calculate the mass of Mars.

(c) Calculate the orbital speed of Phobos and explain why Phobos is gradually spiralling inward towards Mars.

Solution:

(a) Kepler’s third law: T2r3T^2 \propto r^3

TD2TP2=rD3rP3\frac{T_D^2}{T_P^2} = \frac{r_D^3}{r_P^3} TD=TP(rDrP)3/2=7.66×(2.35×1079.38×106)3/2T_D = T_P \left(\frac{r_D}{r_P}\right)^{3/2} = 7.66 \times \left(\frac{2.35 \times 10^7}{9.38 \times 10^6}\right)^{3/2} =7.66×(2.505)3/2=7.66×3.965=30.4hours= 7.66 \times (2.505)^{3/2} = 7.66 \times 3.965 = 30.4\,\text{hours}

The accepted value is approximately 30.3hours30.3\,\text{hours}Confirming the calculation.

(b) From Phobos:

T=2πrv and v=GMrT = \frac{2\pi r}{v} \text{ and } v = \sqrt{\frac{GM}{r}} T=2πr3GMT = 2\pi\sqrt{\frac{r^3}{GM}} M=4π2r3GT2M = \frac{4\pi^2 r^3}{GT^2}

TP=7.66×3600=27576sT_P = 7.66 \times 3600 = 27576\,\text{s}

M=4π2(9.38×106)36.67×1011×(27576)2M = \frac{4\pi^2 (9.38 \times 10^6)^3}{6.67 \times 10^{-11} \times (27576)^2} =4π2×8.258×10206.67×1011×7.604×108= \frac{4\pi^2 \times 8.258 \times 10^{20}}{6.67 \times 10^{-11} \times 7.604 \times 10^8} =3.263×10225.072×102=6.43×1023kg= \frac{3.263 \times 10^{22}}{5.072 \times 10^{-2}} = 6.43 \times 10^{23}\,\text{kg}

The accepted value is 6.42×1023kg6.42 \times 10^{23}\,\text{kg}.

(c) vP=GM/rP=6.67×1011×6.43×1023/9.38×106v_P = \sqrt{GM/r_P} = \sqrt{6.67 \times 10^{-11} \times 6.43 \times 10^{23}/9.38 \times 10^6}

=4.569×106=2138ms1= \sqrt{4.569 \times 10^6} = 2138\,\text{m}\,\text{s}^{-1}

Phobos orbits Mars faster than Mars rotates. The tidal interaction causes a transfer of angular momentum from Phobos to Mars’s rotation, causing Phobos to lose orbital energy and spiral inward. Phobos completes an orbit in 7.66 hours while Mars rotates once in 24.6 hours, so Phobos is inside the synchronous orbit radius.


UT-3: Gravitational Potential and Escape Velocity

Section titled “UT-3: Gravitational Potential and Escape Velocity”

Question:

(a) Calculate the gravitational potential at the surface of the Moon and at a point 3.0×108m3.0 \times 10^8\,\text{m} from the centre of the Moon, on the line joining the centres of the Earth and the Moon. State which potential is more negative and explain the significance.

(b) Calculate the escape velocity from the surface of the Moon.

(c) A spacecraft is at the point where the gravitational field strengths of the Earth and Moon are equal in magnitude but opposite in direction (the Lagrange point L1). Calculate the distance of this point from the centre of the Earth.

Take: G = 6.67 \times 10^{-11}\,\text{N}\,\text{m}^2\,\text{kg}^{-2}$$M_E = 5.97 \times 10^{24}\,\text{kg}$$M_M = 7.35 \times 10^{22}\,\text{kg}$$R_M = 1.74 \times 10^6\,\text{m}Earth-Moon distance =3.84×108m= 3.84 \times 10^8\,\text{m}.

Solution:

(a) Gravitational potential at the Moon’s surface:

Vsurface=GMMRM=6.67×1011×7.35×10221.74×106=4.902×10121.74×106=2.817×106Jkg1V_{\text{surface}} = -\frac{GM_M}{R_M} = -\frac{6.67 \times 10^{-11} \times 7.35 \times 10^{22}}{1.74 \times 10^6} = -\frac{4.902 \times 10^{12}}{1.74 \times 10^6} = -2.817 \times 10^6\,\text{J}\,\text{kg}^{-1}

At r=3.0×108mr = 3.0 \times 10^8\,\text{m} from Moon’s centre:

VM=GMMr=4.902×10123.0×108=1.634×104Jkg1V_M = -\frac{GM_M}{r} = -\frac{4.902 \times 10^{12}}{3.0 \times 10^8} = -1.634 \times 10^4\,\text{J}\,\text{kg}^{-1}

Distance from Earth: 3.84×1083.0×108=0.84×108m3.84 \times 10^8 - 3.0 \times 10^8 = 0.84 \times 10^8\,\text{m}

VE=GME0.84×108=6.67×1011×5.97×10248.4×107=3.982×10148.4×107=4.740×106Jkg1V_E = -\frac{GM_E}{0.84 \times 10^8} = -\frac{6.67 \times 10^{-11} \times 5.97 \times 10^{24}}{8.4 \times 10^7} = -\frac{3.982 \times 10^{14}}{8.4 \times 10^7} = -4.740 \times 10^6\,\text{J}\,\text{kg}^{-1}

Total potential: Vtotal=VM+VE=1.634×1044.740×106=4.756×106Jkg1V_{\text{total}} = V_M + V_E = -1.634 \times 10^4 - 4.740 \times 10^6 = -4.756 \times 10^6\,\text{J}\,\text{kg}^{-1}

The total potential at the point near the Moon is more negative than the surface potential of the Moon alone. This means more energy is required to escape from this point to infinity than from the Moon’s surface alone, because the Earth’s gravitational well also contributes.

(b) vesc=2GMMRM=2×4.902×10121.74×106=5.635×106=2374ms1v_{\text{esc}} = \sqrt{\frac{2GM_M}{R_M}} = \sqrt{\frac{2 \times 4.902 \times 10^{12}}{1.74 \times 10^6}} = \sqrt{5.635 \times 10^6} = 2374\,\text{m}\,\text{s}^{-1}

(c) At L1, the fields are equal in magnitude:

GMEr2=GMM(dr)2\frac{GM_E}{r^2} = \frac{GM_M}{(d - r)^2}

Where rr is the distance from Earth and d=3.84×108md = 3.84 \times 10^8\,\text{m}.

r2(dr)2=MEMM=5.97×10247.35×1022=81.22\frac{r^2}{(d-r)^2} = \frac{M_E}{M_M} = \frac{5.97 \times 10^{24}}{7.35 \times 10^{22}} = 81.22

rdr=81.22=9.012\frac{r}{d-r} = \sqrt{81.22} = 9.012

r=9.012(dr)=9.012d9.012rr = 9.012(d - r) = 9.012d - 9.012r 10.012r=9.012×3.84×10810.012r = 9.012 \times 3.84 \times 10^8 r=34.61×10810.012=3.457×108mr = \frac{34.61 \times 10^8}{10.012} = 3.457 \times 10^8\,\text{m}

The L1 point is approximately 3.46×108m3.46 \times 10^8\,\text{m} from the centre of the Earth, or about 3.84×1083.46×108=3.8×107m3.84 \times 10^8 - 3.46 \times 10^8 = 3.8 \times 10^7\,\text{m} from the centre of the Moon.

IT-1: Geostationary Orbit and Energy (with Electric Fields)

Section titled “IT-1: Geostationary Orbit and Energy (with Electric Fields)”

Question:

(a) Calculate the radius of a geostationary orbit around the Earth.

(b) Calculate the total energy of a 1000kg1000\,\text{kg} satellite in geostationary orbit.

(c) A second satellite of mass 500kg500\,\text{kg} is in a circular orbit at half the geostationary radius. Calculate the ratio of their orbital speeds and the ratio of their total energies per unit mass.

Take G = 6.67 \times 10^{-11}\,\text{N}\,\text{m}^2\,\text{kg}^{-2}$$M_E = 5.97 \times 10^{24}\,\text{kg}$$R_E = 6.37 \times 10^6\,\text{m}.

Solution:

(a) For geostationary orbit, the period equals the Earth’s sidereal day: T=86164sT = 86164\,\text{s}.

T=2πr3GMET = 2\pi\sqrt{\frac{r^3}{GM_E}} r3=GMT24π2=6.67×1011×5.97×1024×(86164)24π2r^3 = \frac{GMT^2}{4\pi^2} = \frac{6.67 \times 10^{-11} \times 5.97 \times 10^{24} \times (86164)^2}{4\pi^2} =3.982×1014×7.424×10939.478=2.956×102439.478=7.488×1022= \frac{3.982 \times 10^{14} \times 7.424 \times 10^9}{39.478} = \frac{2.956 \times 10^{24}}{39.478} = 7.488 \times 10^{22} r=7.488×10223=4.216×107mr = \sqrt[3]{7.488 \times 10^{22}} = 4.216 \times 10^7\,\text{m}

(b) Total energy E=GMm2rE = -\frac{GMm}{2r}:

E=6.67×1011×5.97×1024×10002×4.216×107=3.982×10178.432×107=4.723×109JE = -\frac{6.67 \times 10^{-11} \times 5.97 \times 10^{24} \times 1000}{2 \times 4.216 \times 10^7} = -\frac{3.982 \times 10^{17}}{8.432 \times 10^7} = -4.723 \times 10^9\,\text{J}

(c) For circular orbits: v=GM/rv = \sqrt{GM/r}So vr1/2v \propto r^{-1/2}.

Ratio of speeds: vinnervgeo=rgeorinner=rr/2=2\frac{v_{\text{inner}}}{v_{\text{geo}}} = \sqrt{\frac{r_{\text{geo}}}{r_{\text{inner}}}} = \sqrt{\frac{r}{r/2}} = \sqrt{2}

Total energy per unit mass: E/m=GM2rE/m = -\frac{GM}{2r}So E/mr1E/m \propto r^{-1}.

Ratio: Einner/minnerEgeo/mgeo=rgeorinner=rr/2=2\frac{E_{\text{inner}}/m_{\text{inner}}}{E_{\text{geo}}/m_{\text{geo}}} = \frac{r_{\text{geo}}}{r_{\text{inner}}} = \frac{r}{r/2} = 2

The inner satellite has 2\sqrt{2} times the speed and 2 times the energy per unit mass (more negative).


IT-2: Binary Star System (with Circular Motion)

Section titled “IT-2: Binary Star System (with Circular Motion)”

Question:

Two stars of mass M1=3.0×1030kgM_1 = 3.0 \times 10^{30}\,\text{kg} and M2=1.0×1030kgM_2 = 1.0 \times 10^{30}\,\text{kg} orbit their common centre of mass in circular orbits. Their separation is d=2.0×1011md = 2.0 \times 10^{11}\,\text{m}.

(a) Calculate the position of the centre of mass relative to M1M_1.

(b) Calculate the orbital period of the system.

(c) Calculate the speeds of each star.

Take G=6.67×1011Nm2kg2G = 6.67 \times 10^{-11}\,\text{N}\,\text{m}^2\,\text{kg}^{-2}.

Solution:

(a) Centre of mass from M1M_1:

r1=M2dM1+M2=1.0×1030×2.0×10114.0×1030=5.0×1010mr_1 = \frac{M_2 d}{M_1 + M_2} = \frac{1.0 \times 10^{30} \times 2.0 \times 10^{11}}{4.0 \times 10^{30}} = 5.0 \times 10^{10}\,\text{m}

So M1M_1 orbits at radius r1=5.0×1010mr_1 = 5.0 \times 10^{10}\,\text{m} and M2M_2 at r2=1.5×1011mr_2 = 1.5 \times 10^{11}\,\text{m}.

(b) The gravitational force provides the centripetal force for each star:

GM1M2d2=M1ω2r1=M2ω2r2\frac{GM_1 M_2}{d^2} = M_1 \omega^2 r_1 = M_2 \omega^2 r_2

Using M1ω2r1M_1 \omega^2 r_1:

GM2d2=ω2r1\frac{G M_2}{d^2} = \omega^2 r_1 ω2=GM2d2r1=6.67×1011×1.0×1030(2.0×1011)2×5.0×1010\omega^2 = \frac{GM_2}{d^2 r_1} = \frac{6.67 \times 10^{-11} \times 1.0 \times 10^{30}}{(2.0 \times 10^{11})^2 \times 5.0 \times 10^{10}} =6.67×10192.0×1033=3.335×1014= \frac{6.67 \times 10^{19}}{2.0 \times 10^{33}} = 3.335 \times 10^{-14} ω=1.826×107rads1\omega = 1.826 \times 10^{-7}\,\text{rad}\,\text{s}^{-1} T=2πω=2π1.826×107=3.441×107s=398daysT = \frac{2\pi}{\omega} = \frac{2\pi}{1.826 \times 10^{-7}} = 3.441 \times 10^7\,\text{s} = 398\,\text{days}

Alternatively, using the general formula: T2=4π2d3G(M1+M2)T^2 = \frac{4\pi^2 d^3}{G(M_1 + M_2)}

Numerator: 4π2×(2×1011)3=4π2×8×1033=3.158×10354\pi^2 \times (2 \times 10^{11})^3 = 4\pi^2 \times 8 \times 10^{33} = 3.158 \times 10^{35}

Denominator: 6.67×1011×4×1030=2.668×10206.67 \times 10^{-11} \times 4 \times 10^{30} = 2.668 \times 10^{20}

T2=3.158×10352.668×1020=1.184×1015T^2 = \frac{3.158 \times 10^{35}}{2.668 \times 10^{20}} = 1.184 \times 10^{15}

T=1.184×1015=3.441×107s=398daysT = \sqrt{1.184 \times 10^{15}} = 3.441 \times 10^7\,\text{s} = 398\,\text{days}

(c) v1=ωr1=1.826×107×5.0×1010=9130ms1v_1 = \omega r_1 = 1.826 \times 10^{-7} \times 5.0 \times 10^{10} = 9130\,\text{m}\,\text{s}^{-1}

v2=ωr2=1.826×107×1.5×1011=27390ms1v_2 = \omega r_2 = 1.826 \times 10^{-7} \times 1.5 \times 10^{11} = 27390\,\text{m}\,\text{s}^{-1}

Check: M1v1=M2v2M_1 v_1 = M_2 v_2 (centre of mass frame): 3×1030×9130=2.739×10343 \times 10^{30} \times 9130 = 2.739 \times 10^{34} and 1×1030×27390=2.739×10341 \times 10^{30} \times 27390 = 2.739 \times 10^{34}. Consistent.


IT-3: Gravitational Slingshot (with Kinematics)

Section titled “IT-3: Gravitational Slingshot (with Kinematics)”

Question:

A spacecraft approaches Jupiter (mass 1.90×1027kg1.90 \times 10^{27}\,\text{kg}Radius 6.99×107m6.99 \times 10^7\,\text{m}) with speed 8.0×103ms18.0 \times 10^3\,\text{m}\,\text{s}^{-1} relative to Jupiter. The closest approach distance is 3.0×108m3.0 \times 10^8\,\text{m} from Jupiter’s centre. Jupiter orbits the Sun at speed 1.31×104ms11.31 \times 10^4\,\text{m}\,\text{s}^{-1}.

(a) Calculate the speed of the spacecraft at closest approach to Jupiter, relative to Jupiter.

(b) Assuming an elastic gravitational interaction (the spacecraft’s speed relative to Jupiter is unchanged but its direction reverses), calculate the maximum speed the spacecraft can gain relative to the Sun.

(c) Explain why the spacecraft can gain kinetic energy without violating conservation of energy.

Take G=6.67×1011Nm2kg2G = 6.67 \times 10^{-11}\,\text{N}\,\text{m}^2\,\text{kg}^{-2}.

Solution:

(a) Using conservation of energy relative to Jupiter:

12v2=12vmin2GMJrmin\frac{1}{2}v_{\infty}^2 = \frac{1}{2}v_{\min}^2 - \frac{GM_J}{r_{\min}}

Where v=8.0×103ms1v_{\infty} = 8.0 \times 10^3\,\text{m}\,\text{s}^{-1} is the speed far from Jupiter.

12(8.0×103)2=12vmin26.67×1011×1.90×10273.0×108\frac{1}{2}(8.0 \times 10^3)^2 = \frac{1}{2}v_{\min}^2 - \frac{6.67 \times 10^{-11} \times 1.90 \times 10^{27}}{3.0 \times 10^8} 3.2×107=12vmin24.223×1083.2 \times 10^7 = \frac{1}{2}v_{\min}^2 - 4.223 \times 10^8 12vmin2=4.543×108\frac{1}{2}v_{\min}^2 = 4.543 \times 10^8 vmin=9.086×108=3.014×104ms1v_{\min} = \sqrt{9.086 \times 10^8} = 3.014 \times 10^4\,\text{m}\,\text{s}^{-1}

(b) In the best-case slingshot, the spacecraft’s velocity relative to Jupiter is reversed. If the spacecraft approaches Jupiter from behind (in the direction of Jupiter’s orbital motion), the velocity vectors add:

Maximum speed relative to Sun =vJupiter+v=1.31×104+8.0×103=2.11×104ms1= v_{\text{Jupiter}} + v_{\infty} = 1.31 \times 10^4 + 8.0 \times 10^3 = 2.11 \times 10^4\,\text{m}\,\text{s}^{-1}

The spacecraft gains Δv=2v=1.6×104ms1\Delta v = 2v_{\infty} = 1.6 \times 10^4\,\text{m}\,\text{s}^{-1} in the Sun’s frame.

(c) The spacecraft gains kinetic energy in the Sun’s frame because it transfers kinetic energy from Jupiter’s orbital motion. Jupiter’s orbit slows imperceptibly (by an amount proportional to the ratio of the spacecraft’s mass to Jupiter’s mass). The total energy of the spacecraft-Jupiter system is conserved. The slingshot works because the gravitational interaction is elastic (no energy dissipation), and the reference frame transformation (from Jupiter’s to the Sun’s frame) allows the spacecraft to extract energy from Jupiter’s orbital motion.

Confusing current and voltage: Current (A) is the flow of charge; voltage (V) is the energy per unit charge. Resistance opposes current, not voltage. Students often say “the resistor uses up the voltage” when they should say “the voltage drops across the resistor.”

Forgetting Ohm’s law applies only to ohmic conductors: = IRisvalidonlywhenresistanceisconstant(ohmicconductorsatconstanttemperature).Fornonohmicdevices(diodes,thermistors,filamentlamps),resistancechangeswithvoltageortemperature,so=IRis valid only when resistance is constant (ohmic conductors at constant temperature). For non-ohmic devices (diodes, thermistors, filament lamps), resistance changes with voltage or temperature, so = IR gives the resistance at that point, not a constant.

Confusing the conventions for electron flow and conventional current: Conventional current flows from positive to negative (the direction a positive charge would move). Electron flow is from negative to positive (the actual movement of electrons). Most circuit analysis uses conventional current. Using electron flow when conventional current is expected gives reversed directions.

  • Mechanics: Mechanics covers motion, forces, and energy
  • Waves: Waves transfer energy through oscillations
  • Electricity: Electricity covers circuits and fields