Gravitational field: Difference between revisions

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[[Category:Done 2015-07-24]]  
[[Category:Done 2016-04-30]]  
[[File:Earth_Western_Hemisphere.jpg|300px|thumb|Figure 1. The Earth, and every other massive object, has a gravitational field that causes other massive objects to interact with it.<ref>Wikimedia Commons [Online], Available: http://upload.wikimedia.org/wikipedia/commons/7/7b/Earth_Western_Hemisphere.jpg</ref>]]
[[File:Earth_Western_Hemisphere.jpg|300px|thumb|Figure 1. The Earth, and every other massive object, has a gravitational field that causes other massive objects to interact with it.<ref>Wikimedia Commons [Online], Available: http://upload.wikimedia.org/wikipedia/commons/7/7b/Earth_Western_Hemisphere.jpg</ref>]]


<onlyinclude>A '''gravitational field''' is a field induced by any object with [[mass]], which will interact with other massive objects by applying a [[force]] on it. Gravitational fields are expressed in [[Newton]]s per [[kilogram]] (N/kg), which is the same units as [[acceleration]].</onlyinclude> This means that any massive object present in another's gravitational field will accelerate towards it, and vice versa. The field of an object is given by the equation:<ref name=Knight>R. D. Knight, "Little g and Big G" in ''Physics for Scientists and Engineers: A Strategic Approach,'' 3nd ed. San Francisco, U.S.A.: Pearson Addison-Wesley, 2008, ch.13, sec.4, pp. 359-360</ref>
<onlyinclude>A '''gravitational field''' is a field induced by any object with [[mass]], which will interact with other massive objects by applying a [[force]] on it. Gravitational fields are expressed in [[Newton]]s per [[kilogram]] (N/kg), which is the same unit as [[acceleration]].</onlyinclude> This means that any massive object present in another's gravitational field will accelerate towards it, and vice versa. The field of an object is given by the equation:<ref name=Knight>R. D. Knight, "Little g and Big G" in ''Physics for Scientists and Engineers: A Strategic Approach,'' 3nd ed. San Francisco, U.S.A.: Pearson Addison-Wesley, 2008, ch.13, sec.4, pp. 359-360</ref>


<center><m>g=-\frac{GM}{\left|R\right|^2}\hat{R}</m></center>
<center><m>g=-\frac{GM}{\left|R\right|^2}\hat{R}</m></center>
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* <m>g</m> is the [[acceleration due to gravity]]
* <m>g</m> is the [[acceleration due to gravity]]


From this equation it is simple to find out the gravitational field strength at the surface of the Earth: by plugging in the mass and radius of the Earth, it is found that <m>g=9.81\frac{m}{s^2}</m> (this value changes the further or closer one gets the the center of the Earth). This value means that all objects will fall at the same rate when present in the Earth's gravitational field (ignoring [[air drag]]).
'''Jason this first sentence is awkward'''
Plugging values into the above equation gives the gravitational field strength. Specifically, using the mass and radius of the Earth, the equation shows that the acceleration due to gravity near the surface of the Earth is: <m>g=9.8\frac{m}{s^2}</m> (this value changes the further or closer one gets the the center of the Earth).  
 
This value means that all objects will fall at the same rate near the surface of the Earth (ignoring [[air drag]] and minor changes due to altitude and [[latitude]]).


Since the gravitational field of the Earth is [[conservative force|conservative]] it must have a [[gravitational potential energy|potential energy]] associated with it. This means that any object at a certain height from the surface of the Earth has a potential energy, which can be translated into [[kinetic energy]] as the object falls. Humans can make use of falling objects such as water to transform this potential energy into something useful, like [[electricity]]. [[Hydroelectric facilities]] make use of the moving water in a river in order to create electricity, which depends on this potential energy in order to operate.  
Since the gravitational field of the Earth is [[conservative force|conservative]] it must have a [[gravitational potential energy|potential energy]] associated with it. This means that any object at a certain height from the surface of the Earth has a potential energy, which can be translated into [[kinetic energy]] as the object falls. Humans can make use of falling objects such as water to transform this potential energy into something useful, like [[electricity]]. [[Hydroelectric facilities]] make use of the moving water in a river in order to create electricity, which depends on this potential energy in order to operate.  

Revision as of 17:18, 22 July 2016

Figure 1. The Earth, and every other massive object, has a gravitational field that causes other massive objects to interact with it.[1]

A gravitational field is a field induced by any object with mass, which will interact with other massive objects by applying a force on it. Gravitational fields are expressed in Newtons per kilogram (N/kg), which is the same unit as acceleration. This means that any massive object present in another's gravitational field will accelerate towards it, and vice versa. The field of an object is given by the equation:[2]

where:

Jason this first sentence is awkward Plugging values into the above equation gives the gravitational field strength. Specifically, using the mass and radius of the Earth, the equation shows that the acceleration due to gravity near the surface of the Earth is: (this value changes the further or closer one gets the the center of the Earth).

This value means that all objects will fall at the same rate near the surface of the Earth (ignoring air drag and minor changes due to altitude and latitude).

Since the gravitational field of the Earth is conservative it must have a potential energy associated with it. This means that any object at a certain height from the surface of the Earth has a potential energy, which can be translated into kinetic energy as the object falls. Humans can make use of falling objects such as water to transform this potential energy into something useful, like electricity. Hydroelectric facilities make use of the moving water in a river in order to create electricity, which depends on this potential energy in order to operate.

References

  1. Wikimedia Commons [Online], Available: http://upload.wikimedia.org/wikipedia/commons/7/7b/Earth_Western_Hemisphere.jpg
  2. R. D. Knight, "Little g and Big G" in Physics for Scientists and Engineers: A Strategic Approach, 3nd ed. San Francisco, U.S.A.: Pearson Addison-Wesley, 2008, ch.13, sec.4, pp. 359-360