1|Page Newton’s Law Of Universal Gravitation Newton’s Law Of Universal Gravitation states that every particle in the Universe attracts every other particle with a force that is directly proportional to the product of their masses and inversely proportional to the square of the distance between them. đš=đē đ1 đ2 đ2 , where: • • • • • F is magnitude of the gravitational force between the two point masses, G is the gravitational constant, m1 is the mass of the first point mass, m2 is the mass of the second point mass, r is the distance between the two point masses. The gravitational force is inversely proportional to the square of the separation of the particles. F∝ đ12 * Only applicable to point masses Gravitational field strength Gravitational field strength at a point is defined as the gravitational force per unit mass acting on a mass placed at that point. đš đ đ đ=đē 2 đ đ= Units of g is Nkg−1 or ms−2. It is independent of test mass. GRAVITATION NOTES H2 PHYSICS | Created by MS. Zheng, 91640715 2|Page Gravitational Field Lines Gravitational field lines are always pointing towards the center of mass. Magnitude of gravitational field is proportional to the number of field lines per unit area through a surface perpendicular to the lines. Therefore, g is larger when lines are close together and smaller when they are far apart. Gravitational field strength close to the Earth can be considered as uniform as the Earth surface is relatively flat at a point. Variation of gravitational field strength on Earth • • • Earth is not a perfect sphere (ellipsoid, flattened at the poles). Gravitational field strength increases(at sea level) when one moves from equator to poles. Density of Earth is not uniform. Earth is rotating about an axis passing through the poles. Gravitational Pull on a body at equator has to provide for the centripetal acceleration required for rotation. Hence the measured gravitational acceleration is smaller. Weightless Weight of an object is the gravitational force exerted on the object by the Earth’s gravitational field. An object is only truly weightless when there is no gravitational force acting on it. (Only true when object is infinitely far away from other masses where no gravitational field acts on it) An object is considered to be apparently weightless when it exerts no force on its support. GRAVITATION NOTES H2 PHYSICS | Created by MS. Zheng, 91640715 3|Page Gravitational Potential Energy Gravitational potential energy, U of a point mass m, in a gravitational field, is the work done by an external force in bringing that point mass from infinity to that point. đ=đē đđ đ Units of U is Joules (J). Reasons for a negative sign in the equation: • • Zero (reference point) for gravitational potential energy is set to be at infinity. The gravitational pull is an attractive force. Since gravitational potential is defined to be work done per unit mass by an external force to bring a mass from infinity to a point, the external force has to do work against the attractive field. As external force is opposite to the direction of displacement, values of gravitational potential are negative. Gravitational Potential Gravitational potential, Ī, at a point in a gravitational field is the work done per unit mass, by an external force, in bringing the mass from infinity to that point. Ī=–G Units for Ī is JKg−1JKg−1. At infinity, Ī is assumed to be zero. đ đ GRAVITATION NOTES H2 PHYSICS | Created by MS. Zheng, 91640715 4|Page Escape Speed Escape speed is the minimum speed with which a mass should be projected from the Earth’s surface in order to escape Earth’s gravitation field. Vescape=√2gRE , where • • • V is escape speed, g is gravitational field strength, R is radius of the Earth. Derivation of Escape Speed From Earth We know that: Total Energy at infinity=0 Hence, Kinetic energy + Potential energy = 0 (fill in) where v is the velocity of the object m is the mass of the object M is the mass of Earth R is the radius of the Earth G is the universal gravitation constant GRAVITATION NOTES H2 PHYSICS | Created by MS. Zheng, 91640715 5|Page From Gravitational Field Strength, we know that đ đ = đē 2. Substitute this into the equation above, we will have: đ (fill in) In the context of this derivation, we have: Vescape=√2gRE Equations relating to U, g and F U=mĪ Fg= ( ) g=( ) ( ) is known as potential gradient. Gravitational field strength points in direction of decreasing Ī. GRAVITATION NOTES H2 PHYSICS | Created by MS. Zheng, 91640715 6|Page Questions for Gravitation (JC) Set 1 Imagine if the Moon doubles in mass, which of the following is likely to happen? 1. 2. 3. 4. Each month will be longer than 30 days. Nights will be a lot brighter since the Moon is nearer to the Earth Each day will be longer since the period of the Moon increases. The Moon continues to revolve around the Earth in the same orbit. T2 = kr3 therefore period and orbital radius is independent of mass. Answer: 4 Which quantity is not necessarily the same for satellites that are in geostationary orbits around the Earth? 1. 2. 3. 4. Angular velocity Kinetic energy Centripetal acceleration Orbital period Period of geostationary satellite’s orbit is the same as Earth (24 hours) and hence, its angular velocity is also constant. It can also be found that the radius of the geostationary orbit is fixed using R3∝T2. Hence centripetal acceleration is also constant. The only quantity that varies is the kinetic energy because it depends on the mass of the individual satellites. Answer: 2 Mars is known to possess two satellites, Phobos and Deimos. The former is at a distance of 9,500 km from the centre of Mars and the latter at a distance of 24,500 km. Find the ratio of the period of Phobos to that of Deimos in their revolutions around Mars. Tphobos Tdeimos 3 = √Tđđ 3 phobos deimos =√ 95003 245003 = 0.24 GRAVITATION NOTES H2 PHYSICS | Created by MS. Zheng, 91640715 7|Page Answer: 0.24 Assuming the Earth to be a uniform sphere rotating about an axis through the poles, the apparent weight of a body at the Equator compared with it’s apparent weight at the poles would be 1. greater, because the angular velocity of the Earth is greater at the Equator than at the pole 2. greater, because the weight at the Equator is given by the sum of the gravitational attraction of the Earth and the centripetal force due to the circular motion of the body 3. smaller, because the gravitational attraction of the Earth must provide both the weight and the centripetal force due to the circular motion of the body 4. smaller, because the gravitational attraction at the pole is greater than that at the Equator The Earth spins about the axis through which its poles pass. A person at the Equator undergoes circular motion while a person at the poles does not. Answer: 3 a) The Moon is orbiting at a certain height above the Earth. The Earth exerts a force of 1.99 x 1020 N on the Moon. Given: mass of the Earth = 5.98 x 1024 kg mass of the Moon = 7.35 x 1022 kg radius of the Earth = 6.38 x 106 m i) Find the height above the Earth’s surface where the Moon is orbiting. ii) Using Newton’s Second Law of motion, calculate the linear velocity of the Moon. iii) Calculate the centripetal acceleration of the Moon. GRAVITATION NOTES H2 PHYSICS | Created by MS. Zheng, 91640715 8|Page b) Most artificial satellites are placed in Low Earth Orbits (LEO), at a height typically around 200 km – 1200 km above the Earth’s surface. A 700 kg satellite is in the Low Earth Orbit at a height of 1200 km above the Earth’s surface. i) What is the change in gravitational potential energy of the satellite before it is launched and when it is in orbit? ii) Calculate the period of the satellite. Express your answer in hours. iii) Satellites in LEO are used in telecommunications. State one difference between the LEO and geostationary satellites, and an advantage of using LEO satellites in telecommunications. (a) i) F = G(MEMM/r2) r = 3.8382 x 108 m Height above Earth’s surface = 3.8382 x 108 – 6.38 x 106 = 3.77 x 108 m ii) By Newton’s second law of motion, Fg = Fc v = (GME/r)1/2 v = 1.02 x 103 m/s iii) a = v2/r a = 2.71 x 10-3 m s-2 b) i) Change in GPE = Uo – Us, where o is orbit, s is surface = m(Īo – Īs) = 6.93 x 109 J ii) By Newton’s second law of motion, Fg = mrω2 Fg = mr(2π/T)2 T = 6566s T = 1.82 hrs. GRAVITATION NOTES H2 PHYSICS | Created by MS. Zheng, 91640715 9|Page iii)LEO satellites have a shorter orbital period as compared to geostationary satellites which have a period of 24 hrs. LEO satellites are nearer to the Earth and so the resolution of the images received will be higher. GRAVITATION NOTES H2 PHYSICS | Created by MS. Zheng, 91640715