Gravitation Comprehensive One-Shot Study Notes

Comparison Between Electrostatics and Gravitation

  • Electrostatic Force (FeF_e):

    • Formula: F=kq1q2r2F = \frac{kq_1q_2}{r^2}

    • Constant: k=14πε09×109Nm2/C2k = \frac{1}{4\pi\varepsilon_0} \approx 9 \times 10^9 \, \text{Nm}^2/\text{C}^2

    • Nature: Can be both attractive and repulsive.

    • Principle: Depends on the product of charges.

  • Gravitational Force (FgF_g):

    • Formula: F=GM1M2r2F = \frac{GM_1M_2}{r^2}

    • Constant (GG): Universal Gravitational Constant, G=6.67×1011Nm2/kg2G = 6.67 \times 10^{-11} \, \text{Nm}^2/\text{kg}^2

    • Nature: Always attractive.

    • Vector Form: F=GM1mr2r^\mathbf{F} = -\frac{GM_1m}{r^2} \hat{r}

    • Field Equation Comparison: kGk \leftrightarrow G, qmq \leftrightarrow m, ε014πG\varepsilon_0 \leftrightarrow \frac{1}{4\pi G}.

Net Force Calculations in Discrete Systems

  • Equilateral Triangle Case:

    • Three masses (mm) placed at the corners of a triangle with side length ll.

    • Force between any two masses: F=Gmml2F = \frac{Gmm}{l^2}

    • Net force on one mass: Fnet=F3=Gm23l2F_{net} = F\sqrt{3} = \frac{Gm^2\sqrt{3}}{l^2}

  • Square Geometry Case:

    • Four masses placed at corners of a square with side length ll.

    • Force from adjacent masses: F1=Gmml2F_1 = \frac{Gmm}{l^2}

    • Force from diagonal mass: F2=Gmm(2l)2=Gm22l2F_2 = \frac{Gmm}{(\sqrt{2}l)^2} = \frac{Gm^2}{2l^2}

    • Resultant of adjacent forces: F2F\sqrt{2}

    • Total net force on one mass: Fnet=F2+F2=Gm2l2(2+12)F_{net} = F\sqrt{2} + \frac{F}{2} = \frac{Gm^2}{l^2} \left( \sqrt{2} + \frac{1}{2} \right)

Mutual Attraction and Circular Motion

  • Four Masses in a Circular Path:

    • For four masses (mm) moving in a circle of radius RR due to mutual attraction, the net gravitational force acts as the centripetal force.

    • Relationship between side length ll and radius RR: l2=2Rl=R2l\sqrt{2} = 2R \rightarrow l = R\sqrt{2}.

    • Centripetal force balance: Fnet=mv2R=mRω2F_{net} = \frac{mv^2}{R} = mR\omega^2

    • Calculation: Gm2l2(2+12)=mv2R\frac{Gm^2}{l^2} \left(\sqrt{2} + \frac{1}{2}\right) = \frac{mv^2}{R}

    • Solving for orbital speed (vv): v=GmR(1+224)v = \sqrt{\frac{Gm}{R} \left( \frac{1 + 2\sqrt{2}}{4} \right)}

  • Two Equal Masses Rotating about COM:

    • Masses mm separated by distance ll, rotating with angular velocity ω\omega.

    • Radius of rotation r=l2r = \frac{l}{2}.

    • Force: F=Gmml2F = \frac{Gmm}{l^2}

    • Equation: Gm2l2=m(l2)ω2\frac{Gm^2}{l^2} = m \left(\frac{l}{2}\right) \omega^2

    • Resulting ω\omega: ω=2Gml3\omega = \sqrt{\frac{2Gm}{l^3}}

Gravitational Field (EgE_g)

  • Definition: Gravitational force per unit mass at a point in space.

    • Eg=FmE_g = \frac{F}{m}

    • For a point mass MM: Eg=GMr2E_g = \frac{GM}{r^2}

  • Field of Specific Geometries:

    • Uniform Ring (at a point on the axis):

    • Eg=GMx(R2+x2)3/2E_g = \frac{GMx}{(R^2 + x^2)^{3/2}}

    • Maximum field occurs at x=±R2x = \pm \frac{R}{\sqrt{2}}.

    • Thin Arc of mass mm and radius RR:

    • Eg=2GλRsin(θ2)E_g = \frac{2G\lambda}{R} \sin\left(\frac{\theta}{2}\right), where λ=MRθ\lambda = \frac{M}{R\theta}.

    • Infinite Line Mass:

    • Eg=2GλrE_g = \frac{2G\lambda}{r}

    • Hollow Sphere:

    • Inside (r < R): Eg=0E_g = 0

    • Outside (r > R): Eg=GMr2E_g = \frac{GM}{r^2}

    • Solid Sphere:

    • Inside (r < R): Eg=GMrR3E_g = \frac{GMr}{R^3}

    • Outside (r > R): Eg=GMr2E_g = \frac{GM}{r^2}

Gravitational Potential (VV) and Potential Energy (UU)

  • Gravitational Potential (VV):

    • Work done per unit mass by an external agent to bring a mass from infinity to a point.

    • For point mass: V=GMrV = -\frac{GM}{r}

    • Relation to Field: Eg=V=(Vxi^+Vyj^+Vzk^)\mathbf{E}_g = -\nabla V = -\left( \frac{\partial V}{\partial x} \hat{i} + \frac{\partial V}{\partial y} \hat{j} + \frac{\partial V}{\partial z} \hat{k} \right)

  • Gravitational Potential Energy (UU):

    • For two masses: U=Gm1m2rU = -\frac{Gm_1m_2}{r}

    • Total energy of a system of particles: U_{total} = \sum_{i

  • Work-Energy Principle:

    • \Delta U = U_f - U_i = W_{ext}</p></li><li><p>IfaparticleismovedfromthesurfaceofEarth(</p></li><li><p>If a particle is moved from the surface of Earth (R)toheight) to heighth=2R:</p></li><li><p>:</p></li><li><p>U_i = -\frac{GMm}{R}</p></li><li><p></p></li><li><p>U_f = -\frac{GMm}{3R}</p></li><li><p></p></li><li><p>\Delta U = \frac{2}{3} \frac{GMm}{R} = \frac{2}{3} mgR_e</p></li></ul></li></ul><h3id="832cde0b438a4e68b53b1047413fb723"datatocid="832cde0b438a4e68b53b1047413fb723"collapsed="false"seolevelmigrated="true">EscapeVelocity(</p></li></ul></li></ul><h3 id="832cde0b-438a-4e68-b53b-1047413fb723" data-toc-id="832cde0b-438a-4e68-b53b-1047413fb723" collapsed="false" seolevelmigrated="true">Escape Velocity (v_e)andOrbitalVelocity() and Orbital Velocity (v_o)</h3><ul><li><p><strong>EscapeVelocity()</h3><ul><li><p><strong>Escape Velocity (v_e):</strong></p><ul><li><p>Minimumspeedtoleavethegravitationalpullofaplanet.</p></li><li><p>Formula:):</strong></p><ul><li><p>Minimum speed to leave the gravitational pull of a planet.</p></li><li><p>Formula:v_e = \sqrt{\frac{2GM}{R}} = \sqrt{2gR}</p></li><li><p>ForEarth:</p></li><li><p>For Earth:v_e \approx 11.2 \, \text{km/s}.</p></li><li><p>Valuesindifferentforms:.</p></li><li><p>Values in different forms:v_e = R \sqrt{\frac{8\pi G \rho}{3}}.</p></li></ul></li><li><p><strong>OrbitalVelocity(.</p></li></ul></li><li><p><strong>Orbital Velocity (v_o):</strong></p><ul><li><p>Speedrequiredtomaintainacircularorbitatradius):</strong></p><ul><li><p>Speed required to maintain a circular orbit at radiusr.</p></li><li><p>Formula:.</p></li><li><p>Formula:v_o = \sqrt{\frac{GM}{r}}</p></li><li><p>FororbitsclosetoEarth(</p></li><li><p>For orbits close to Earth (r \approx R):):v_o = \sqrt{gR} \approx 8 \, \text{km/s}.</p></li><li><p>Relationship:.</p></li><li><p>Relationship:v_e = \sqrt{2} v_o.</p></li></ul></li></ul><h3id="89b9ce50789b4863b2dfdd3fa33bde27"datatocid="89b9ce50789b4863b2dfdd3fa33bde27"collapsed="false"seolevelmigrated="true">EarthsAccelerationduetoGravity(.</p></li></ul></li></ul><h3 id="89b9ce50-789b-4863-b2df-dd3fa33bde27" data-toc-id="89b9ce50-789b-4863-b2df-dd3fa33bde27" collapsed="false" seolevelmigrated="true">Earth's Acceleration due to Gravity (g)</h3><ul><li><p><strong>ValueatSurface:</strong>)</h3><ul><li><p><strong>Value at Surface:</strong>g_0 = \frac{GM}{R^2} \approx 9.8 \, \text{m/s}^2</p></li><li><p><strong>VariationwithAltitude(</p></li><li><p><strong>Variation with Altitude (h):</strong></p><ul><li><p>Exact:):</strong></p><ul><li><p>Exact:g_h = g_0 \left( \frac{R}{R+h} \right)^2</p></li><li><p>For</p></li><li><p>Forh \ll R::g_h \approx g_0 \left( 1 - \frac{2h}{R} \right)</p></li></ul></li><li><p><strong>VariationwithDepth(</p></li></ul></li><li><p><strong>Variation with Depth (d):</strong></p><ul><li><p>):</strong></p><ul><li><p>g_d = g_0 \left( 1 - \frac{d}{R} \right)</p></li></ul></li><li><p><strong>VariationwithRotation:</strong></p><ul><li><p></p></li></ul></li><li><p><strong>Variation with Rotation:</strong></p><ul><li><p>g' = g_0 - R\omega^2 \cos^2(\phi),where, where\phiisthelatitude.</p></li><li><p>AtPoles(is the latitude.</p></li><li><p>At Poles (\phi = 90^\circ):):g' = g_0</p></li><li><p>AtEquator(</p></li><li><p>At Equator (\phi = 0^\circ):):g' = g_0 - R\omega^2</p></li></ul></li></ul><h3id="4e8b2235fa684d3d88f7b1d563af3151"datatocid="4e8b2235fa684d3d88f7b1d563af3151"collapsed="false"seolevelmigrated="true">KeplersLawsofPlanetaryMotion</h3><ul><li><p><strong>FirstLaw(LawofOrbits):</strong>PlanetsmoveinellipticalorbitswiththeSunatonefocus.</p></li><li><p><strong>SecondLaw(LawofAreas):</strong>AlinesegmentjoiningaplanetandtheSunsweepsoutequalareasduringequalintervalsoftime.</p><ul><li><p>Impliesconstantarealvelocity:</p></li></ul></li></ul><h3 id="4e8b2235-fa68-4d3d-88f7-b1d563af3151" data-toc-id="4e8b2235-fa68-4d3d-88f7-b1d563af3151" collapsed="false" seolevelmigrated="true">Kepler's Laws of Planetary Motion</h3><ul><li><p><strong>First Law (Law of Orbits):</strong> Planets move in elliptical orbits with the Sun at one focus.</p></li><li><p><strong>Second Law (Law of Areas):</strong> A line segment joining a planet and the Sun sweeps out equal areas during equal intervals of time.</p><ul><li><p>Implies constant areal velocity:\frac{dA}{dt} = \frac{L}{2m} = \text{constant}.</p></li><li><p>Conservationofangularmomentum(.</p></li><li><p>Conservation of angular momentum (L).</p></li></ul></li><li><p><strong>ThirdLaw(LawofPeriods):</strong>Thesquareoftheorbitalperiod().</p></li></ul></li><li><p><strong>Third Law (Law of Periods):</strong> The square of the orbital period (T)isproportionaltothecubeofthesemimajoraxis() is proportional to the cube of the semi-major axis (a).</p><ul><li><p>).</p><ul><li><p>T^2 \propto a^3</p></li><li><p>Calculation:</p></li><li><p>Calculation:T = 2\pi \sqrt{\frac{a^3}{G(M + m)}}</p></li></ul></li></ul><h3id="ac8e8f614d9442129cc43d2a1c1482e3"datatocid="ac8e8f614d9442129cc43d2a1c1482e3"collapsed="false"seolevelmigrated="true">GeostationarySatellites</h3><ul><li><p><strong>Characteristics:</strong></p><ul><li><p>TimePeriod:</p></li></ul></li></ul><h3 id="ac8e8f61-4d94-4212-9cc4-3d2a1c1482e3" data-toc-id="ac8e8f61-4d94-4212-9cc4-3d2a1c1482e3" collapsed="false" seolevelmigrated="true">Geostationary Satellites</h3><ul><li><p><strong>Characteristics:</strong></p><ul><li><p>Time Period:T = 24 \, \text{hours}.</p></li><li><p>OrbitalRadius:.</p></li><li><p>Orbital Radius:r \approx 42,000 \, \text{km}(fromcenter)oraltitude(from center) or altitudeh \approx 36,000 \, \text{km}.</p></li><li><p>Direction:RotateWesttoEast(sameasEarth).</p></li><li><p>Plane:Mustbeintheequatorialplane.</p></li><li><p>RelativeMotion:Appearsstationaryrelativetoapointonthesurface.</p></li></ul></li></ul><h3id="ad6ee2a1a1354bd2b933441ea79dda5b"datatocid="ad6ee2a1a1354bd2b933441ea79dda5b"collapsed="false"seolevelmigrated="true">BinaryStarSystems</h3><ul><li><p><strong>Configuration:</strong>Twostarsofmasses.</p></li><li><p>Direction: Rotate West to East (same as Earth).</p></li><li><p>Plane: Must be in the equatorial plane.</p></li><li><p>Relative Motion: Appears stationary relative to a point on the surface.</p></li></ul></li></ul><h3 id="ad6ee2a1-a135-4bd2-b933-441ea79dda5b" data-toc-id="ad6ee2a1-a135-4bd2-b933-441ea79dda5b" collapsed="false" seolevelmigrated="true">Binary Star Systems</h3><ul><li><p><strong>Configuration:</strong> Two stars of massesm_1andandm_2rotatingaroundtheircommonCenterofMass(COM).</p></li><li><p><strong>DistancesfromCOM:</strong>rotating around their common Center of Mass (COM).</p></li><li><p><strong>Distances from COM:</strong>r_1 = \frac{m_2 L}{m_1 + m_2}andandr_2 = \frac{m_1 L}{m_1 + m_2},where, whereListheseparation.</p></li><li><p><strong>AngularVelocity:</strong>is the separation.</p></li><li><p><strong>Angular Velocity:</strong>\omega = \sqrt{\frac{G(m_1 + m_2)}{L^3}}</p></li><li><p><strong>TimePeriod:</strong></p></li><li><p><strong>Time Period:</strong>T = 2\pi \sqrt{\frac{L^3}{G(m_1 + m_2)}}

    Questions & Discussion

    • Q: What is the ratio of escape velocities of two planets if Planet B has 4 times the density and half the radius of Planet A?

      • v_e \propto R\sqrt{\rho}</p></li><li><p>Ratio:</p></li><li><p>Ratio:1:1.Calculation:. Calculation:\frac{v_B}{v_A} = \frac{1/2 \sqrt{4}}{1 \sqrt{1}} = 1.</p></li></ul></li><li><p><strong>Q:Abodyweighs300Nonthesurface.Findweightatdepth.</p></li></ul></li><li><p><strong>Q: A body weighs 300 N on the surface. Find weight at depthR/4.</strong></p><ul><li><p>.</strong></p><ul><li><p>g_d = g(1 - 1/4) = 3g/4.</p></li><li><p>Weight=.</p></li><li><p>Weight =300 \times 3/4 = 225 \, \text{N}.</p></li></ul></li><li><p><strong>Q:Ifasatellitelosesenergyatrate.</p></li></ul></li><li><p><strong>Q: If a satellite loses energy at rateC \, \text{J/s},howlongdoesittaketoreachEarth?</strong></p><ul><li><p>Energychange, how long does it take to reach Earth?</strong></p><ul><li><p>Energy change\Delta E = E_{final} - E_{initial}.</p></li><li><p>TotalEnergy.</p></li><li><p>Total EnergyE = -\frac{GMm}{2r}.</p></li><li><p>Time.</p></li><li><p>Timet = \frac{\Delta E}{C} = \frac{GMm}{2C} \left( \frac{1}{R_e} - \frac{1}{r} \right)$$.