Gravitational constant
The gravitational
constant is a
fundamental physical constant, a constant of gravitational interaction.
The
gravitational constant G is a key quantity
in Newton's law of universal gravitation.
Contents
Introduction
According to the Newton's law of universal gravitation,
the force of gravitational attraction between two material points with
gravitational masses m1
and m2, which are
located at the distance R, is
equal to:
The proportionality coefficient G in this equation is called the gravitational constant. Numerically it is
equal to the absolute value of gravitational force, acting on a point body with
unit mass from another similar body, which is located at the unit distance.
In SI units the value recommended for the year
2014 is: [1] m3·s−2·kg
−1, or N·м2· kg −2.
The gravitational constant is presented in most
of formulas associated with gravitational interaction. In particular, it is
included in equations of general relativity, gravitoelectromagnetism
and covariant theory of gravitation,
and it is also part of formulas used to determine gravitational torsion
field. The gravitational constant and its coupling
constant have such values that gravitational interaction
between the elementary particles is many orders of magnitude less than the
weak, electromagnetic, and strong interactions.
In the theory of Infinite Hierarchical
Nesting of Matter, based on SPФ symmetry the
existence of strong gravitation is
assumed, which is acting on the level of elementary particles. The strong
gravitational constant is derived from the ordinary
gravitational constant by multiplying it by the similarity coefficients, which
are found on the basis of similarity of matter levels.
The history of measurement
The gravitational constant is used in modern law
of universal gravitation, but it was not used in Newton’s works and in the
works of other scientists until the beginning of the 19 th century.
The gravitational constant apparently was first introduced into the law of
universal gravitation only after transition to the single metric system of
measurements. Possibly it was first done by the French physicist Poisson in
“Treatise on Mechanics” (1809) — at least historians have not found any earlier
works, in which the gravitational constant was mentioned. In 1798 Henry
Cavendish prepared and performed the Cavendish experiment to determine the
average density of the Earth using the torsion balance, invented by John
Michell (Philosophical Transactions 1798). Cavendish compared the pendular
oscillations of test body under action of gravitation of the balls with known
mass and under the action of the Earth's gravitation. The numerical value of gravitational
constant was calculated later based on the average density of the Earth and
resulted in the value m3·s−2·kg −1. [2]
The accuracy of the measured value of G since the time of Cavendish’s experiment
increased insignificantly.
Theoretical definition
In order to calculate the gravitational constant
Maurizio Michelini used the idea of micro-quanta, filling the entire space,
interacting with the bodies’ particles and as a result pushing the bodies to
each other. [3] For the
matter consisting mainly of nucleons he obtains the following:
where J/m3 is the energy density of the fluxes of
micro-quanta;
is the
nucleon mass;
is the
speed of light;
m−2•s−1 is the fluence rate of the fluxes of
micro-quanta in one direction.
Sergey Fedosin expressed the gravitational
constant in the framework of Le Sage’s theory of gravitation in terms of the
parameters describing vacuum field of gravitons. [4] [5] [6] In the model of cubic distribution of
graviton fluxes there
is:
Here is momentum
of gravitons interacting with the nucleon matter; the fluence rate
denotes
the number of gravitons dN, that during the time dt fell to the area dA (perpendicular to the flux) of one face of a
certain cube, which limits the volume under consideration;
m2
is the cross-section of interaction of gravitons and nucleons;
is the
nucleon mass;
J/m3 is the energy density of the
graviton fluxes for cubic distribution.
In the model of spherical distribution of
graviton fluxes there
is:
where the fluence rate denotes
the number of gravitons dN, that during the time dt fell from the unit solid angle
inside
the spherical surface dA;
J/m3 is the energy density of the
graviton fluxes for spherical distribution.
Since the gravitational
constant is expressed in terms of other variables, it is a dynamic variable,
which is constant only on the average.
The interaction
cross-section can be
expressed in terms of the cross-section
m² of
interaction of charged particles of vacuum field (praons) with nucleons: [6]
where is the strong
gravitational constant. The interaction cross-section
is very
close in magnitude to geometrical cross-section of a nucleon and is used to
calculate the electric constant. If we
substitute the expression of
in terms
of
into the
formula for gravitational constant in cubic distribution model, we will obtain
a relationship between the strong gravitational constant, the nucleon’s
parameters and the energy density of graviton fluxes at the nucleon level of
matter:
Similarly, for gravitational
constant at the stellar level of matter, there is a relationship between the
corresponding energy density of graviton fluxes and the parameters of neutron
star, which is an analogue of nucleon:
where J/m³ is the energy density of graviton fluxes
at the stellar level for cubic distribution;
m² is cross-section
of interaction between gravitons and neutron star;
kg is the neutron star’s mass. In the
calculation we used similarity coefficients according to similarity of matter
levels:
is the
coefficient of similarity in mass,
is the
coefficient of similarity in sizes,
is the
coefficient of similarity in speeds of same-type processes.
Thus, it is assumed that at
each level of matter there is its own gravitational constant, besides the
energy density of corresponding graviton fluxes increases with the transition
to the lower levels of matter.
The quantity can be
compared with the energy density of gravitational wave in the GW150914 event.
It is assumed that this event was caused by a merger of two black holes with
masses of 30 and 35 solar masses, rotating near each other under the action of
gravitation, during decrease in the distance between them up to 350 km, while
the maximum power of gravitational radiation reached
W. [7]
If we divide this power by the surface of the sphere with the radius of 175 km,
we will obtain an estimate of density of the energy flux passing through the
surface of the sphere. Then this value can be divided by the speed of light,
and we can estimate the energy density in the wave:
J/m³. The
energy density of the wave is found to be substantially lower than the energy
density of the gravitons’ vacuum field. Thus, the gravitational wave from the
majority of powerful radiation sources only slightly modulates the graviton
fluxes in the cosmic space.
References
See also
External links
Source:
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