GRAVITATIONAL FIELDS

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  • Created by: CPev3
  • Created on: 06-11-20 18:48

Define gravitational field:

  • A field created around any object with mass

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  • Extends all the way to infinity

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  • Diminishes as the distance from the centre of mass of the object increases
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Define gravitational field strength:

The gravitational force exerted per unit mass at a point within a gravitational field

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Define weight:

  • The gravitational force on an object

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  • An attractive force towards the centre of mass of the object producing the gravitational field
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Equation for gravitational field strength:

g = F / m

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F = ma and F = mg

∴ gravitational field strength at a point = acceleration of free fall of an object at that point

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g on the Earth's surface:

9.81 Nkg-1

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Define gravitational field lines:

  • Lines of force used to map the gravitational field pattern around an object having mass
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Properties of gravitational field lines:

  • Do not cross

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  • The arrows show the direction of the force on an object at that point in the field
    • Gravitational force is always attractive
      •  The direction of the field is always towards the centre of mass of the object producing the field

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  • Closer together = stronger field
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Define radial field:

  • A symmetrical field

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  • Diminishes with distance from the centre of mass of the object producing the field

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  • Shown by the field lines getting further apart
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Define point mass:

A mass with negligible volume

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Define uniform gravitational field:

  • The field lines are parallel

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  • The value for gravitational field strength remains constant

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  • The gravitational field close to the surface of a planet is approximately uniform
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Newton's law of gravitation:

The force between two point masses is:

  • Directly proportional to the product of the masses, F  Mm
  • Inverseley proportional to the square of their separation, F ∝ 1 / r2

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F = - GMm / r2 

G = 6.67e-11 Nm2kg-2

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Equation for g in a radial field:

g = F / m and F = - GMm / r2

g = - GMm / mr2

g = - GM / r2

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The negative sign shows that g at that point is in the opposite direction to r from the centre of mass of the object producing the gravitational field- a gravitational field is an attractive field.

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Kepler's first law of planetary motion:

The orbit of a planet is an ellipse with the Sun at one of the two foci

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Ellipse = an elongated 'circle' with two foci

Eccentricity = a measure of the elongation of an ellipse

Aphelion = the furthest point from the Sun in an orbit

Perihelion = the closest point to the Sun in an orbit

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Kepler's second law of planetary motion:

  • A line segment connecting a planet to the Sun sweeps out equal areas during equal intervals of time

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  • As a planet moves on its elliptical orbit around the Sun, its speed is not constant

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  • When it is closer to the Sun it moves faster
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Kepler's third law of planetary motion:

mv2 / r = GMm / r2

v2 = GM / r

v = 2πr / T so 4π2r2 / T2 = GM / r

T2 = (4π2 / GM) r3

∴ T2 ∝ r3 or T2 / r3 = k

k is a constant for the planets orbiting the Sun approximately equal to 1 y2AU-3

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F for any satellite in orbit:

F =  mv2 / r = centripetal force on the satellite

F = GMm / r2 = gravitational force between the satellite and the Earth

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Only force acting on a satellite is the gravitational attraction between it and the Earth

∴ always falling towards the Earth

↑ speed and ↑ distance

∴ as it falls the Earth curves away beneath it

∴ its height above the Earth's surface remains constant

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v for any satellite in orbit:

  • v =  GM / r

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  • All satellites placed in a given orbit at a given height will be travelling at the same speed, even if their mass varies

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  • Once launched they are normally above the atmosphere

There is no air resistance to slow them down

Their speed remains constant

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Uses of satellites:

  • Communications (e.g. satellite phones)

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  • Military uses (e.g. reconnaissance)

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  • Scientific research (e.g. looking down onto the Earth to monitor pollution)

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  • Weather and climate (e.g. monitoring long-term changes in climate)

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  • Global positioning
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Types of orbit:

Polar orbit

  • Circles the poles
  • Offers a complete view of the Earth over a given time period as the Earth rotates beneath the path of the satellite
  • Useful for reconnaissance

Low Earth orbit

  • In orbit close to the Earth
  • T2 3 so takes less than 2 hours for the satellite to orbit the Earth

Equatorial orbit

  • In orbit above the equator
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Geostationary satellites...

  • Are in a geostationary orbit

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  • Are in orbit above the equator

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  • Rotate in the same direction as the Earth's rotation

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  • Have an orbital period of 24 hours

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  • ∴ Remain above the same point of the Earth whilst the Earth rotates

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  • Are used for satellite television
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Define gravitational potential:

  • The work done per unit mass to bring an object from infinity to a point in the gravitational field

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  • All masses attract each other

External work must be done to move masses apart 

Gravitational potential is a maximum at infinity

= 0 Jkg-1

∴ all values of gravitational potential are negative

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Define infinity:

A distance so far from the object producing the gravitational field that the gravitational field strength is zero

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Equation for Vg in a radial field:

Vg = - (GM / r)

  • All values of Vg within the region of the gravitational field are negative
  • When r = ∞ then Vg = 0
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Changes in gravitational potential:

  • Moving towards a point mass results in a decrease in gravitational potential

∴ the change in gravitational potential would be negative

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  • Moving away from a point mass (towards infinity) results in an increase in gravitational potential

∴ the change in gravitational potential would be positive

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Define gravitational potential energy:

The capacity for doing work as a result of an object's position in a gravitational field

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Equation for gravitational potential energy:

E = mVg

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E in a uniform gravitational field:

↑ r 

↑ Vg

↑ E

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E in a radial field:

E = mVg and Vg = - (GM / r)

∴ E = - (GMm / r)

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Equation for escape velocity:

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