Gravity and Space Flashcards
gravity
- An attractive force between 2 objects
- Acceleration due to gravity: 9.81 m/s^2
strength of gravity depends on
- gravitational constant
- size of masses involved (density and volume)
- distance between masses (r)
Changes in gravity: imagine a satellite circling a planet that is a uniform sphere
some gravitational force at the same distance from center of mass
Changes in gravity: imagine a satellite circling a planet that is uniform material, but not perfect sphere
force of gravity is lower over large depressions and higher over high elevations
Changes in gravity: imagine a satellite circling a planet that is a spherical planet, but not uniform material
- higher density materials = stronger force of gravity
- Ex. Mafic igneous rocks have higher density -> higher force of gravity
Changes in gravity: imagine a satellite circling a planet that is a non-uniform body
have to divide it into pieces, calculate gravity from each piece, then add them up
force of gravity at centre of earth
zero!
why are gravity and topography somewhat related?
Elevation that could cause higher gravity is offset by isostasy
isostasy
- Balancing act that prevents huge gravity anomalies on Earth
- Large masses won’t have huge positive gravity anomaly as the dense mantle below will be displaced on either side
- Ex. Causes blocks of same mass but different densities to sink into mantle at same depth
- Ex. Causes blocks of same density but different masses to sink at different depths
isostatic equilibrium
- Mountains come into isostatic equilibrium through erosion -> roots of mountain rise as overlying rock is eroded
- Not all areas are in isostatic equilibrium yet (ie. Himalayas)
isostatic equilibrium: oceanic vs. continental plate
Low density of continental lithosphere compensates for elevation -> same gravitational force on both blocks
isostatic equilibrium: within a continental plate
“root” compensates for elevated continental crust (ie. Mountains)
isostatic rebound
negative anomaly due to removal of ice sheet that once covered the area -> crust is still bouncing back (ie. Hudson’s Bay area)
isostatic compensation (oceanic vs. continental)
Continental crust tends to be more elevated and thicker than oceanic crust in order to account for its smaller density
measuring gravity
- Pendulums
- Weight vs. Spring
- Satellite orbital patterns (Mars, Venus, Earth)
- When reading gravity measurements, remember to check where the black line is -> our measurements can’t go any deeper than that line