Gravitation, or gravity, is one of the four fundamental interactions of nature, along with strong interaction, electromagnetic force and weak interaction. It is the means by which objects with mass attract one another.^{[1]} In everyday life, gravitation is most familiar as the agent that lends weight to objects with mass and causes them to fall to the ground when dropped. Gravitation causes dispersed matter to coalesce, thus accounting for the existence of the Earth, the Sun, and most of the macroscopic objects in the universe. It is responsible for keeping the Earth and the other planets in their orbits around the Sun; for keeping the Moon in its orbit around the Earth; for the formation of tides; for convection, by which fluid flow occurs under the influence of a density gradient and gravity; for heating the interiors of forming stars and planets to very high temperatures; and for various other phenomena observed on Earth.
Modern physics describes gravitation using the general theory of relativity, in which gravitation is a consequence of the curvature of spacetime which governs the motion of inertial objects. The simpler Newton's law of universal gravitation provides an accurate approximation for most calculations.
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Modern work on gravitational theory began with the work of Galileo Galilei in the late 16th and early 17th centuries. In his famous (though possibly apocryphal)^{[2]} experiment dropping balls from the Tower of Pisa, and later with careful measurements of balls rolling down inclines, Galileo showed that gravitation accelerates all objects at the same rate. This was a major departure from Aristotle's belief that heavier objects are accelerated faster.^{[3]} Galileo correctly postulated air resistance as the reason that lighter objects may fall more slowly in an atmosphere. Galileo's work set the stage for the formulation of Newton's theory of gravity.
In 1687, English mathematician Sir Isaac Newton published Principia, which hypothesizes the inversesquare law of universal gravitation. In his own words, “I deduced that the forces which keep the planets in their orbs must [be] reciprocally as the squares of their distances from the centers about which they revolve: and thereby compared the force requisite to keep the Moon in her Orb with the force of gravity at the surface of the Earth; and found them answer pretty nearly.”^{[4]}
Newton's theory enjoyed its greatest success when it was used to predict the existence of Neptune based on motions of Uranus that could not be accounted by the actions of the other planets. Calculations by John Couch Adams and Urbain Le Verrier both predicted the general position of the planet, and Le Verrier's calculations are what led Johann Gottfried Galle to the discovery of Neptune.
Ironically, it was another discrepancy in a planet's orbit that helped to point out flaws in Newton's theory. By the end of the 19th century, it was known that the orbit of Mercury showed slight perturbations that could not be accounted for entirely under Newton's theory, but all searches for another perturbing body (such as a planet orbiting the Sun even closer than Mercury) had been fruitless. The issue was resolved in 1915 by Albert Einstein's new General Theory of Relativity, which accounted for the small discrepancy in Mercury's orbit.
Although Newton's theory has been superseded, most modern nonrelativistic gravitational calculations are still made using Newton's theory because it is a much simpler theory to work with than General relativity, and gives sufficiently accurate results for most applications.
The equivalence principle, explored by a succession of researchers including Galileo, Loránd Eötvös, and Einstein, expresses the idea that all objects fall in the same way. The simplest way to test the weak equivalence principle is to drop two objects of different masses or compositions in a vacuum, and see if they hit the ground at the same time. These experiments demonstrate that all objects fall at the same rate with negligible friction (including air resistance). More sophisticated tests use a torsion balance of a type invented by Loránd Eötvös. Satellite experiments are planned for more accurate experiments in space.^{[5]}
Formulations of the equivalence principle include:
The equivalence principle can be used to make physical deductions about the gravitational constant, the geometrical nature of gravity, the possibility of a fifth force, and the validity of concepts such as general relativity and BransDicke theory.
General relativity  
Einstein field equations  
Introduction Mathematical formulation Resources


In general relativity, the effects of gravitation are ascribed to spacetime curvature instead of a force. The starting point for general relativity is the equivalence principle, which equates free fall with inertial motion, and describes freefalling inertial objects as being accelerated relative to noninertial observers on the ground.^{[8]}^{[9]} In Newtonian physics, however, no such acceleration can occur unless at least one of the objects is being operated on by a force.
Einstein proposed that spacetime is curved by matter, and that freefalling objects are moving along locally straight paths in curved spacetime. These straight lines are called geodesics. Like Newton's First Law, Einstein's theory stated that if there is a force applied to an object, it would deviate from the geodesics in spacetime.^{[10]} For example, we are no longer following the geodesics while standing because the mechanical resistance of the Earth exerts an upward force on us. Thus, we are noninertial on the ground. This explains why moving along the geodesics in spacetime is considered inertial.
Einstein discovered the field equations of general relativity, which relate the presence of matter and the curvature of spacetime and are named after him. The Einstein field equations are a set of 10 simultaneous, nonlinear, differential equations. The solutions of the field equations are the components of the metric tensor of spacetime. A metric tensor describes a geometry of spacetime. The geodesic paths for a spacetime are calculated from the metric tensor.
Notable solutions of the Einstein field equations include:
The tests of general relativity included:^{[11]}
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Several decades after the discovery of general relativity it was realized that general relativity is incompatible with quantum mechanics.^{[17]} It is possible to describe gravity in the framework of quantum field theory like the other fundamental forces, such that the attractive force of gravity arises due to exchange of virtual gravitons, in the same way as the electromagnetic force arises from exchange of virtual photons.^{[18]}^{[19]} This reproduces general relativity in the classical limit. However, this approach fails at short distances of the order of the Planck length,^{[17]} where a more complete theory of quantum gravity (or a new approach to quantum mechanics) is required. Many believe the complete theory to be string theory,^{[20]} or more currently Mtheory, and, on the other hand, it may be a background independent theory such as loop quantum gravity or causal dynamical triangulation.
Every planetary body (including the Earth) is surrounded by its own gravitational field, which exerts an attractive force on all objects. Assuming a spherically symmetrical planet (a reasonable approximation), the strength of this field at any given point is proportional to the planetary body's mass and inversely proportional to the square of the distance from the center of the body.
The strength of the gravitational field is numerically equal to the acceleration of objects under its influence, and its value at the Earth's surface, denoted g, is approximately expressed below as the standard average.
g = 9.81 m/s^{2} = 32.2 ft/s^{2}
This means that, ignoring air resistance, an object falling freely near the Earth's surface increases its velocity with 9.81 m/s (32.2 ft/s or 22 mph) for each second of its descent. Thus, an object starting from rest will attain a velocity of 9.81 m/s (32.2 ft/s) after one second, 19.6 m/s (64.4 ft/s) after two seconds, and so on, adding 9.81 m/s (32.2 ft/s) to each resulting velocity. Also, again ignoring air resistance, any and all objects, when dropped from the same height, will hit the ground at the same time.
According to Newton's 3rd Law, the Earth itself experiences an equal [in force] and opposite [in direction] force to that acting on the falling object, meaning that the Earth also accelerates towards the object (until the object hits the earth, then the Law of Conservation of Energy states that it will move back with the same acceleration with which it initially moved forward, canceling out the two forces of gravity.). However, because the mass of the Earth is huge, the acceleration of the Earth by this same force is negligible, when measured relative to the system's center of mass.
Under an assumption of constant gravity, Newton's law of universal gravitation simplifies to F = mg, where m is the mass of the body and g is a constant vector with an average magnitude of 9.81 m/s². The acceleration due to gravity is equal to this g. An initiallystationary object which is allowed to fall freely under gravity drops a distance which is proportional to the square of the elapsed time. The image on the right, spanning half a second, was captured with a stroboscopic flash at 20 flashes per second. During the first 1/20th of a second the ball drops one unit of distance (here, a unit is about 12 mm); by 2/20ths it has dropped at total of 4 units; by 3/20ths, 9 units and so on.
Under the same constant gravity assumptions, the potential energy, E_{p}, of a body at height h is given by E_{p} = mgh (or E_{p} = Wh, with W meaning weight). This expression is valid only over small distances h from the surface of the Earth. Similarly, the expression for the maximum height reached by a vertically projected body with velocity v is useful for small heights and small initial velocities only.
The discovery and application of Newton's law of gravity accounts for the detailed information we have about the planets in our solar system, the mass of the Sun, the distance to stars, quasars and even the theory of dark matter. Although we have not traveled to all the planets nor to the Sun, we know their masses. These masses are obtained by applying the laws of gravity to the measured characteristics of the orbit. In space an object maintains its orbit because of the force of gravity acting upon it. Planets orbit stars, stars orbit Galactic Centers, galaxies orbit a center of mass in clusters, and clusters orbit in superclusters. The force of gravity is proportional to the mass of an object and inversely proportional to the square of the distance between the objects.
In general relativity, gravitational radiation is generated in situations where the curvature of spacetime is oscillating, such as is the case with coorbiting objects. The gravitational radiation emitted by the Solar System is far too small to measure. However, gravitational radiation has been indirectly observed as an energy loss over time in binary pulsar systems such as PSR B1913+16. It is believed that neutron star mergers and black hole formation may create detectable amounts of gravitational radiation. Gravitational radiation observatories such as LIGO have been created to study the problem. No confirmed detections have been made of this hypothetical radiation, but as the science behind LIGO is refined and as the instruments themselves are endowed with greater sensitivity over the next decade, this may change.
There are some observations that are not adequately accounted for, which may point to the need for better theories of gravity or perhaps be explained in other ways.


Newton devised a formula to determine the gravitational force between any two given bodies.
"Any two bodies in the universe attract each other with a force that is directly porportional product of the masses of the two bodies and inversely proportional to the square of the distance between them."
Where
=
gravitational force (N)
=
gravitational constant
=
mass of the 1st body
=
mass of the 2nd body
=
distance between the center of object 1 and center of object
2
To understand what is going on, one should be clear about the concept of mass. So what is mass? Nothing but one of the properties of any particle. Then what are the other properties? There are many other properties that have been discovered by scientists. Some of these are Mass, Electric charge, Strangeness, Spin, etc.
Everything in the universe is a collection of particles. And some particles couldn't exist without others. Whatever we see (or can't see) is just a collection of particles. Earth is also a collection of particles, as is a stone. By Newton's Law, both of these should attract each other with a force of magnitude proportional to the product of their masses and inversely proportional to the distance between their centers.
Take that stone. It's attracted toward earth's center with a constant force as neither mass nor distance changes. You can now see what happens if you throw a stone away from the center of earth. The stone is attracted toward the center with variable force as the distance changes. The distance between centers is ( radius of earth + distance of stone from ground + radius of stone ). Radius of the earth is constant and can be found by guessing.
If we compare the radius of the earth to the height and radius of the stone, we'll find those to be negligible. But only if we've guessed a suitably large value. Calculate the force between the earth and the stone by substituting into the above equation.
We know that force applied is the product of mass and acceleration (F=M*a). Force between the earth and the stone is the equivalence of the equations (F = m*a = G*M*m/r^2 ). Now we will find the acceleration of the stone toward center as G*M/r^2 which we denote as 'g', the acceleration due to gravity. It can be considered constant at the height to which one can toss a stone.
Gravitational potential energy can be expressed as
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Gravity is the force that draws an object or living thing downwards. The word comes from the Latin gravis, meaning "heavy".
Objects that have mass pull on each other. We call this 'pull' gravity. The strength of the pull between two objects depends on two things. The first is the mass of both of the objects. The larger the masses the stronger the pull of gravity. The second is the distance between the objects. The larger the distance the weaker the pull of gravity. Both of the objects will feel this pull equally. The formula for the strength of this pull is:
You and the Earth have mass, so the Earth pulls on you and you pull on the Earth. This pull is what we call weight. The Moon has 1/6 the mass of the Earth. So if you were on the moon the pull between you and the moon would be six times smaller. This means your weight on the Moon would be six times smaller. Your mass is always the same. It does not matter if you are on the Earth, or the Moon, or anywhere else, your mass does not change.
Things that are falling still have mass, but we cannot measure their weight, so we say that they are "weightless". Astronauts and spacecraft in outer space can be weightless. They look like they are floating. Really they are falling in an orbit around the Earth. So as you can see that weight is the illusion created by gravity.
They still have mass, so we still have to push them or pull them to make them go or stop. Astronauts inside spacecraft use their arms and legs to jump or to stop. Spacecraft use rockets to move.
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Sir Isaac Newton is said to have discovered gravity when he saw an apple fall from a tree. He wondered what made this happen, and worked out the laws the force of gravity seems to follow. These rules are simple but surprisingly accurate; they have been used to work out how to get space probes to planets across billions of miles
In 1915, Albert Einstein showed that gravity could be explained as the bending of space (and time) by mass. A planet makes a dent in space that makes things fall towards it or curve around it. The moving object is passing through more space, in the same amount of time, at the same speed. In fact there is also an effect on time: Einstein predicted that time slows down near a large mass, and this has been verified using very accurate clocks on satellites. Some scientists have looked at Einstein's theories and found ideas in them that gravity could not actually be a force. However, they have not yet come up with a more precise definition.
Recent studies suggest that framedragging may be responsible for gravity. Frame dragging is a theory which states that particles interact with space, and are constantly changing energy levels. They are performing tests such as Gravity Probe B to see if this theory is correct.
