Physics Formulae/Gravitation Formulae

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Lead Article: Tables of Physics Formulae


This article is a summary of the laws, principles, defining quantities, and useful formulae in the analysis of Gravitation.

Gravitational Field Definitions

A common misconseption occurs between centre of mass and centre of gravity. They are defined in simalar ways but are not exactly the same quantity. Centre of mass is the mathematical descrition of placing all the mass in the region considered to one position, centre of gravity is a real physical quantity, the point of a body where the gravitational force acts. They are only equal if and only if the external gravitational field is uniform.

Contrary to the strong analogy between (classical) gravitation and electrostatics, there are no "centre of charge" or "centre of electrostatic attraction" analogues.


Quantity Name (Common) Symbol/s Defining Equation SI Units Dimension
Centre of Gravity 𝐫cog

(Symbols can vary

enourmously)

ith moment of mass 𝐦i=𝐫imi


Centre of gravity for a descrete masses

𝐫cog=1M|𝐠(𝐫i)|i𝐦i|𝐠(𝐫i)|


=1M|𝐠(𝐫cog)|i𝐫imi|𝐠(𝐫i)|


Centre of a gravity for a continuum of mass


𝐫cog=1M|𝐠(𝐫cog)||𝐠(𝐫)|d𝐦

=1M|𝐠(𝐫cog)|𝐫|𝐠(𝐫)|dnm


=1M|𝐠(𝐫cog)|𝐫ρn|𝐠(𝐫)|dnx

m [L]
Standard Gravitation

Parameter of a Mass

μ μ=Gm N m2 kg-1 [L]3 [T]-2
Gravitational Field, Field

Strength, Potential Gradient,

Acceleration

𝐠 𝐠=𝐅m N kg-1 = m s-2 [L][T]-2
Gravitational Flux ΦG ΦG=S𝐠d𝐀 m3 s-2 [L]3[T]-2
Absolute Gravitational Potential Φ,ϕ,U,V U=Wrm=1mr𝐅d𝐫=r𝐠d𝐫 J kg-1 [L]2[T]-2
Gravitational Potential Differance ΔΦ,Δϕ,ΔU,ΔV ΔU=Wm=1mr1r2𝐅d𝐫=r1r2𝐠d𝐫 J kg-1 [L]2[T]-2
Gravitational Potential Energy Ep Ep=Wr J [M][L]2[T]-2
Gravitational Torsion Field Ω ×𝐠=Ωt

𝐅=m(𝐯×Ω)

Hz = s-1 [T]-1
Gravitational Torsion Flux ΦΩ ΦΩ=SΩd𝐀 N m s kg-1 = m2 s-1 [M]2 [T]-1
Gravitomagnetic Field ξ Hz = s-1 [T]-1
Gravitomagnetic Flux Φξ Φξ=Sξd𝐀 N m s kg-1 = m2 s-1 [M]2 [T]-1
Gravitomagnetic Vector Potential [1] 𝐑 ξ=×𝐑 m s-1 [M] [T]-1


Gravitational Potential Gradient and Field

𝐠=U

Laws of Gravitation

Modern Laws

Gravitomagnetism (GEM) Equations:

In an relativley flat spacetime due to weak gravitational fields (by General Relativity), the following gravitational analogues of Maxwell's equations can be found, to describe an analogous Gravitomagnetic Field. They are well established by the theory, but have yet to be verified by experiment [2].

Einstein Tensor Field (ETF) Equations Gμν=8πGc4Tμν

where GΞΌΟ… is the Einstien tensor:

Gμν=Rμν12gμνR+gμνΛ

GEM Equations 𝐠=4πGρ

ξ=𝟎

×𝐠=ξt

×ξ=1c2[4πG𝐣m+𝐠t]

Gravitomagnetic Lorentz Force 𝐅=m(𝐠+𝐯×2ξ)

𝐅=m(𝐠+𝐯×Ω)

Classical Laws

It can be found that Kepler's Laws, though originally discovered from planetary observations (also due to Tycho Brahe), are true for any central forces.

For Kepler's 1st law, the equation is nothing physically fundamental; simply the polar equation of an ellipse where the pole (origin of polar coordinate system) is positioned at a focus of the ellipse, centred on the central star.


e = elliptic eccentricity

a = elliptic semi-major axes = planet aphelion

b = elliptic semi-minor axes = planet perihelion


e=1(ba)2


Newton's Law of Gravitational Force 𝐅=Gm1m2|𝐫|2𝐫^
Gauss's Law for Gravitation S𝐠d𝐀=4πGMenc
Kepler's 1st Law

Planets move in an ellipse, with the star at a focus

𝐫=a1+ecosθ𝐫^
Kepler's 2nd Law dAdt=|𝐋|2m
Kepler's 3rd Law T2=4π2G(m+M)r3

Gravitational Fields

The general formula for calculating classical gravitational fields, due to any mass distribution, is found by using Newtons Law, definition of g, and application of calculus:

𝐠=GVn𝐫ρndVn|𝐫|3


Uniform Mass Corolaries

For uniform mass distributions the table below summarizes common cases.

For a massive rotating body (i.e. a planet/star etc), the equation is only true for much less massive bodies (i.e. objects at the surface) in physical contact with the rotating body. Since this is a classical equation, it is only approximatley true at any rate.


Superposition Principle for

the Gravitational Field

𝐠=i𝐠i(𝐫)=d𝐠
Gravitational Acceleration 𝐚=𝐠
Gravitational Field for

a Rotating (spinning about axis) body

ϕ = azimuth angle relative to rotation axis

𝐚^ = unit vector perpendicular to rotation

axis, radial from it

𝐠=GM|𝐫|2𝐫^|ω|2|𝐫|sinϕ𝐚^
Uniform Gravitational Field, Parabolic Motion 𝐫0 = Initail Position

𝐯0 = Initail Velocity

t = Time of Flight

Use Constant Acc. Equations to obtain

𝐠=2t2[(𝐫𝐫0)𝐯0t]

Point Mass 𝐠=Gm|𝐫|2𝐫^
At a point in a local

array of Point Masses

𝐠=i𝐠i=Gimi|𝐫i𝐫|2𝐫^i
Line of Mass m=(Δx)λ = Mass

Δx = Length of mass distribution

𝐠=2Gλ|𝐫|𝐫^
Spherical Shell m=4πRσ = Mass

R = Radius

Outside/at Surface |𝐫|R

𝐠=Gm|𝐫|2𝐫^


Inside |𝐫|<R

𝐠=𝟎

Spherical Mass Distribution m=43πR3ρ = Mass

R = Radius

Outside/at Surface |𝐫|R

𝐠=Gm|𝐫|2𝐫^


Inside |𝐫|<R

𝐠=43πρ|𝐫|𝐫^

Gravitational Potential Energy of a

Physical Pendulum in a Uniform Field

L = seperation between pivot and centre of mass

= length from pivot to centre of gravity


m = mass of pendulum

𝐦=mL = mass moment of pendulum

U=𝐦𝐠
Gravitational Torque on a physical

Pendulum in a Uniform Field

τ=𝐦×𝐠


For non-uniform fields and mass-moments, applying differentials of the scalar and vector products then integrating gives the general gravitational torque and potential energy as:


U=(𝐠d𝐦+𝐦d𝐠)


τ=(d𝐦×𝐠+𝐦×d𝐠)

Gravitational Potentials

Potential Energy from gravity U=Gm1m2|𝐫|m|𝐠|y
Escape Speed v=2Gmr
Orbital Energy E=T+V

=GmM|𝐫|+12m|𝐯|2

=m(GM|𝐫|+|ω×𝐫|22)


E=GmM2|r|

See also

References

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  1. ↑ Gravitation and Inertia, I. Ciufolini and J.A. Wheeler, Princeton Physics Series, 1995, Template:ISBN
  2. ↑ Gravitation and Inertia, I. Ciufolini and J.A. Wheeler, Princeton Physics Series, 1995, Template:ISBN