The Gravitational Interaction between Moving Mass Particles Explained by the Theory of Informatons

In the article “Newtons Law of Universal Gravitation Explained by the Theory of Informatons” the gravitational interaction between mass particles at rest has been explained by the hypothesis that g-information carried by informatons is the substance of the medium that the interaction in question makes possible. It has been showed that, on the macroscopic level, that medium—the “gravitational field”—manifests itself as the vector field $E_g$ . In this article we will deduce from the postulate of the emission of informatons, that the informatons emitted by a moving mass particle carry not only information about the position (g-information) but also about the velocity (“β-information”) of their emitter. It follows that the gravitational field of a moving mass particle is a dual entity always having a field- and an induction-component ( $E_g$ and $B_g$ ) simultaneously created by their common sources: time-variable masses and mass flows and that the gravitational interaction is the effect of the fact that an object in a gravitational field always tends to become “blind” for that field by accelerating according to a Lorentz-like law.

• Gravity
• Gravitational Field
• Gravitational Interaction
• Informatons

1. Introduction

The theory of informatons [1] - [3] starts from the hypothesis that a material object at rest manifests its presence in space by continuously emitting “informatons”, granular entities carrying “information” about the position of the emitter. The emission of informatons by a material object anchored in an inertial reference frame (IRF) O, is governed by the “postulate of the emission of informatons”:

A. The emission of informatons by a particle at rest is governed by the following rules:

1. The emission is uniform in all directions of space, and the informatons diverge with the speed of light (c = 3 × 10⁸ m/s) along radial trajectories relative to the position of the emitter.

2. $\stackrel{\dot{}}{N}=\frac{\text{d}N}{\text{d}t}$, the rate at which a particle emits informatons¹, is time independent and proportional to the rest mass m₀ of the emitter. So there is a constant K so that:

$\stackrel{\dot{}}{N}=K\cdot m_0$

3. The constant K is equal to the ratio of the square of the speed of light (c) to the Planck constant (h):

$K=\frac{c^2}{h}=1.36\times {10}^{50}{\text{kg}}^{-1}\cdot {\text{s}}^{-1}$

B. We call the essential attribute of an informaton its g-index. The g-index of an informaton refers to information about the position of its emitter and equals the elementary quantity of g-information. It is represented by a vectoral quantity $s_g$:

1. $s_g$ points to the position of the emitter.

2. The elementary quantity of g-information is:

$s_g=\frac{1}{K\cdot {\eta }_0}=\frac{h}{{\eta }_0\cdot c^2}=6.18\times {10}^{-60}{\text{m}}^3\cdot {\text{s}}^{-1}$

where ${\eta }_0=\frac{1}{4\cdot \pi \cdot G}=1.19\times {10}^9\text{kg}\cdot {\text{s}}^2\cdot {\text{m}}^{-3}$, G being the gravitational constant.

In the article “Newtons law of universal gravitation explained by the theory of informatons” [1] it is shown that this postulate leads to the conclusion that the gravitational field—the medium that the gravitational interaction between objects makes possible—is a cloud of “g-information”, i.e. information carried by informatons. At the macroscopic level it is, in the case of an object at rest, completely defined by the vector field $E_g$. E_g, the magnitude of $E_g$ at any point P, is the density of the flow of g-information at that point (the rate per unit area at which g-information at P flows through an elementary surface perpendicular to the direction of $E_g$).

In this article (the follow-up article of [1] ) we will deduce from the postulate of the emission of informatons that the gravitational field of a moving mass particle is a dual entity always having a field- and an induction-component ( $E_g$ and $B_g$) simultaneously created by their common sources: time-variable masses and mass flows. At an arbitrary point P the magnitude of $E_g$ is the density of the flow of g-information at that point and the magnitude of $B_g$ is the density of the cloud of β-information at P. β-information is the information that informatons carry regarding the velocity of their source. This implies that the gravitational field of a moving object besides g-information, i.e. this is information about the position of the emitter, contains also information about its velocity.

We will also show that the gravitational interaction is the effect of the fact that an object in a gravitational field always tends to become “blind” for that field by accelerating according to a Lorentz-like law.

2. Rest Mass and Relativistic Mass

Figure 1

Figure 1. A mass particle m 0 moving with constant velocity relative to an IRF O.

In Figure 1 , we consider a mass point with rest mass m₀ that moves with constant velocity $v=v\cdot e_z$ along the Z-axis of an IRF O. At the moment t = 0, it passes through the origin O and at the moment t = t through the point P₁.

We extend rule A.1 of the postulate of the emission of information to a mass point that is moving relative to an IRF O:

$\stackrel{\dot{}}{N}=\frac{\text{d}N}{\text{d}t}$, the rate at which a particle emits informatons, is independent of the

motion of the emitter and proportional to its rest mass m₀. So there is a constant K so that:

$\stackrel{\dot{}}{N}=K\cdot m_0$

That implies that, if the time is read on a standard clock anchored in O, dN, the number of informatons that during the time interval dt is emitted by a—whether or not moving—point mass, is:

$\text{d}N=K\cdot m_0\cdot \text{d}t$

To emit dN informatons relative to O'—the “proper IRF” of the mass particle (i.e. the IRF anchored to the moving particle)—it takes a time interval dt'. The Lorentz transformation relation between dt and dt' is [4] :

$\text{d}t=\frac{\text{d}{t}^{\prime }}{\sqrt{1-{\beta }^2}}$

where $\beta =\frac{v}{c}$ is the dimensionless speed of the particle.

So:

$\text{d}N=K\cdot m_0\cdot \text{d}t=K\cdot m_0\cdot \frac{\text{d}{t}^{\prime }}{\sqrt{1-{\beta }^2}}=K\cdot \frac{m_0}{\sqrt{1-{\beta }^2}}\cdot \text{d}{t}^{\prime }=\frac{\stackrel{\dot{}}{N}}{\sqrt{1-{\beta }^2}}\cdot \text{d}{t}^{\prime }$

and:

$\frac{\text{d}N}{\text{d}{t}^{\prime }}=\frac{\stackrel{\dot{}}{N}}{\sqrt{1-{\beta }^2}}=K\cdot \frac{m_0}{\sqrt{1-{\beta }^2}}=K\cdot m$

with

$m=\frac{m_0}{\sqrt{1-{\beta }^2}}$

the “relativistic mass” of the particle.

We conclude:

The rate at which a mass particle moving with constant velocity relative to an IRF O emits informatons is determined by its “rest mass”. Relative to its proper IRF O’ it is determined by its “relativistic mass”. In other words: the rest mass of a particle is representative for the rate at which it emits informatons relative to the IRF of the observer and its relative mass for the emission rate relative to its proper IRF.

3. The g-Field of a Mass Particle Moving with Constant Velocity

In Figure 2(a) , we consider a particle with rest mass m₀ that is moving with constant velocity $v=v\cdot e_z$ along the Z-axis of an IRF O. At the moment t = 0, it passes through the origin O and at the moment t = t through the point P₁. It is evident that:

$O{P}_1=z_{P_1}=v\cdot t$

P is an arbitrary fixed point in O with space coordinates (x, y, z). Its position relative to the moving particle is determined by the time dependent position vector $r=P_{1}P$.

We introduce the IRF O' ( Figure 2(b) ), the proper IRF of the particle, whose origin is anchored to the moving particle and we assume that t = t' = 0 when it passes through O.

Relative to O' ( Figure 1(b) ), the position of P is determined by the time dependent position vector $r^{\prime }=O^{\prime }P$ and in O' the space coordinates of P are (x', y', z').

The particle is at rest in O'. So ${E^{\prime }}_g$, its g-field relative to O', is completely defined by the vectoral quantity [1] :

${E^{\prime }}_g=-\frac{\frac{\text{d}N}{\text{d}{t}^{\prime }}\cdot s_g}{4\cdot \pi \cdot {r^{\prime }}^2}\cdot e_{r^{\prime }}$

Figure 2

Figure 2. The g-field of a mass particle moving with constant velocity relative to an IRF O.

dN is the number of informatons that during the time interval dt' pass through an elementary surface dS' that in O' is perpendicular to $c$, the velocity of these informatons.

Thus ${E^{\prime }}_g$ is—relative to O'—the density of the g-information flow at P and the magnitude of ${E^{\prime }}_g$ is the rate per unit area at which—relative to O'—g-information flows through an elementary surface dS' that at P is perpendicular to the velocity $c$ of the informatons that carry that information.

The components of ${E^{\prime }}_g$ in O', are:

${E^{\prime }}_{g{x}^{\prime }}=-\frac{\frac{\text{d}N}{\text{d}{t}^{\prime }}\cdot s_g}{4\cdot \pi \cdot {r^{\prime }}^3}\cdot x^{\prime }$

${E^{\prime }}_{g{y}^{\prime }}=-\frac{\frac{\text{d}N}{\text{d}{t}^{\prime }}\cdot s_g}{4\cdot \pi \cdot {r^{\prime }}^3}\cdot y^{\prime }$

${E^{\prime }}_{g{z}^{\prime }}=-\frac{\frac{\text{d}N}{\text{d}{t}^{\prime }}\cdot s_g}{4\cdot \pi \cdot {r^{\prime }}^3}\cdot z^{\prime }$

They determine at P the densities of the flows of g-information respectively through a surface element dy'∙dz' perpendicular to the X'-axis, through a surface element dz'∙dx' perpendicular to the Y'-axis and through a surface element dx'∙dy' perpendicular to the Z'-axis.

Thus, the amount of information that the particle during the time-interval dt' sends through the different surface elements at P are:

${E^{\prime }}_{g{x}^{\prime }}\cdot \text{d}{y}^{\prime }\cdot \text{d}{z}^{\prime }\cdot \text{d}{t}^{\prime }=-\frac{\frac{\text{d}N}{\text{d}{t}^{\prime }}\cdot s_g\cdot x^{\prime }}{4\cdot \pi \cdot {r^{\prime }}^3}\cdot \text{d}{y}^{\prime }\cdot \text{d}{z}^{\prime }\cdot \text{d}{t}^{\prime }$

${E^{\prime }}_{g{y}^{\prime }}\cdot \text{d}{z}^{\prime }\cdot \text{d}{x}^{\prime }\cdot \text{d}{t}^{\prime }=-\frac{\frac{\text{d}N}{\text{d}{t}^{\prime }}\cdot s_g\cdot y^{\prime }}{4\cdot \pi \cdot {r^{\prime }}^3}\cdot \text{d}{z}^{\prime }\cdot \text{d}{x}^{\prime }\cdot \text{d}{t}^{\prime }$

${E^{\prime }}_{g{z}^{\prime }}\cdot \text{d}{x}^{\prime }\cdot \text{d}{y}^{\prime }\cdot \text{d}{t}^{\prime }=-\frac{\frac{\text{d}N}{\text{d}{t}^{\prime }}\cdot s_g\cdot z^{\prime }}{4\cdot \pi \cdot {r^{\prime }}^3}\cdot \text{d}{x}^{\prime }\cdot \text{d}{y}^{\prime }\cdot \text{d}{t}^{\prime }$

Informatons propagate at the speed of light that—in free space—has the same value in all IRFs. That implies that, by applicating the Lorenz transformation equations, the amount of g-information that during the time interval dt flows through the surface element dS that in O is perpendicular to the velocity of the informatons at P can be derived from the quantity that during the corresponding time interval dt' flows through the corresponding surface element dS' in O'.

$x^{\prime }=x$, $y^{\prime }=y$, $z^{\prime }=\frac{z-v\cdot t}{\sqrt{1-{\beta }^2}}=\frac{z-z_{P_1}}{\sqrt{1-{\beta }^2}}$

The elementary time intervals by: $\text{d}{t}^{\prime }=\text{d}t\cdot \sqrt{1-{\beta }^2}$

$r^{\prime }=r\cdot \frac{\sqrt{1-{\beta }^2\cdot {\sin }^2\theta }}{\sqrt{1-{\beta }^2}}$

So relative to O, the rates at which the moving particle sends g-information in the positive direction through the surface elements dy∙dz, dz∙dx and dx∙dy at P are:

$-\frac{\frac{\text{d}N}{\text{d}t}\cdot s_g}{4\cdot \pi \cdot r^3}\cdot \frac{1-{\beta }^2}{{\left(1-{\beta }^2\cdot {\sin }^2\theta \right)}^{\frac{3}{2}}}\cdot x\cdot \text{d}y\cdot \text{d}z$

$-\frac{\frac{\text{d}N}{\text{d}t}\cdot s_g}{4\cdot \pi \cdot r^3}\cdot \frac{1-{\beta }^2}{{\left(1-{\beta }^2\cdot {\sin }^2\theta \right)}^{\frac{3}{2}}}\cdot y\cdot \text{d}x\cdot \text{d}z$

$-\frac{\frac{\text{d}N}{\text{d}t}\cdot s_g}{4\cdot \pi \cdot r^3}\cdot \frac{1-{\beta }^2}{{\left(1-{\beta }^2\cdot {\sin }^2\theta \right)}^{\frac{3}{2}}}\cdot \left(z-z_{P_1}\right)\cdot \text{d}x\cdot \text{d}z$

By definition, the densities at P of the flows of g-information in the direction of the X-, the Y- and the Z-axis are the components of the g-field caused by the moving particle m₀ at P in O.

Taking into account that

$\frac{\text{d}N}{\text{d}t}=\stackrel{\dot{}}{N}=K\cdot m_0$, $s_g=\frac{1}{K\cdot {\eta }_0}$

We obtain:

$E_{gx}=-\frac{m_0}{4\pi {\eta }_0{r}^3}\cdot \frac{1-{\beta }^2}{{\left(1-{\beta }^2\cdot {\sin }^2\theta \right)}^{\frac{3}{2}}}\cdot x$

$E_{gy}=-\frac{m_0}{4\pi {\eta }_0{r}^3}\cdot \frac{1-{\beta }^2}{{\left(1-{\beta }^2\cdot {\sin }^2\theta \right)}^{\frac{3}{2}}}\cdot y$

$E_{gz}=-\frac{m_0}{4\pi {\eta }_0{r}^3}\cdot \frac{1-{\beta }^2}{{\left(1-{\beta }^2\cdot {\sin }^2\theta \right)}^{\frac{3}{2}}}\cdot \left(z-z_{P_1}\right)$

From which it follows that the g-field caused by the particle at the fixed point P is:

$E_g=-\frac{m_0}{4\pi {\eta }_0{r}^3}\cdot \frac{1-{\beta }^2}{{\left(1-{\beta }^2\cdot {\sin }^2\theta \right)}^{\frac{3}{2}}}\cdot r=-\frac{m_0}{4\pi {\eta }_0{r}^2}\cdot \frac{1-{\beta }^2}{{\left(1-{\beta }^2\cdot {\sin }^2\theta \right)}^{\frac{3}{2}}}\cdot e_r$

We conclude:

A particle describing a uniform rectilinear movement relative to an inertial reference frame O, creates in the space linked to that frame a time dependent gravitational field. $E_g$, the g-field at an arbitrary point P, points at any time to the position of the mass at that moment² and its magnitude is:

$E_g=\frac{m_0}{4\pi {\eta }_0{r}^2}\cdot \frac{1-{\beta }^2}{{\left(1-{\beta }^2\cdot {\sin }^2\theta \right)}^{\frac{3}{2}}}$ (1)

The magnitude of $E_g$ at an arbitrary point P in the g-field of m₀ is the rate per unit area at which g-information at that point flows—relative to O—through an elementary surface perpendicular to $E_g$.

With N the density of the flow of informatons at P (the number of informatons that per unit time and per unit area crosses an elementary surface perpendicular to the direction of their movement), $E_g$ can be expressed as:

$E_g=N\cdot s_g$

Because the rate at which g-information that escapes from an enclosed space is completely determined by the rate at which g-information is generated inside that space (conservation of g-information):

${\displaystyle ∯E_g\cdot \text{d}S}=-\frac{m_0}{{\eta }_0}$

If the speed of the mass particle is much smaller than the speed of light, the expression (1) reduces to that valid in the case of a mass particle at rest. This non-relativistic result could directly be obtained if one assumes that the displacement of the mass particle during the time interval that the informatons need to move from the emitter to P can be neglected compared to the distance they travel during that period.

4. The Emission of Informatons by a Mass Particle Moving with Constant Velocity

Figure 3

Figure 3. An informaton emitted by a mass particle moving with constant velocity.

In Figure 3 we consider a mass particle with rest mass m₀ that is moving with constant velocity $v$ along the Z-axis of an inertial reference frame O. Its instantaneous position (at the arbitrary moment t) is P₁. The position of P, an arbitrary fixed point in space, is defined by the vector $r=P_{1}P$. This position vector $r$—just like the distance r and the angle θ—is time dependent because the position of P₁ is constantly changing.

The informatons that—with the speed of light—at the moment t are passing near P, are emitted when m₀ was at P₀. Bridging the distance $P_{0}P=r_0$ took the time interval $\Delta t=\frac{r_0}{c}$.

During their rush from P₀ to P their emitter, the particle, moved from P₀ to P₁: $P_0{P}_1=v\cdot \Delta t$.

1. $c$, the velocity of the informatons, points in the direction of their movement, thus along the radius P₀P;

2. $s_g$, their g-index, points to P₁, the position of m₀ at the moment t. This is an implication of rule B.1 of the postulate of the emission of informatons, confirmed by the conclusion of §3.

The lines carrying $s_g$ and $c$ form an angle Δθ. We call this angle—that is characteristic for the speed of the mass particle—the “characteristic angle” or the “characteristic deviation”. The quantity $s_{\beta }=s_g\cdot \sin \left(\Delta \theta \right)$, referring to the speed of its emitter, is called the “characteristic g-information” or the “β-information” of an informaton.

We conclude that an informaton emitted by a moving particle, transports information referring to the velocity of that particle. This information is represented by its “gravitational characteristic vector” or its “β-index” $s_{\beta }$ that is defined as:

$s_{\beta }=\frac{c\times s_g}{c}$

In the case of Figure 3 the β-indices have the orientation of the positive X-axis.

Applying the sine-rule to the triangle P₀P₁P, we obtain:

$\frac{\sin \left(\Delta \theta \right)}{v\cdot \Delta t}=\frac{\sin \theta }{c\cdot \Delta t}$

From which it follows:

$s_{\beta }=s_g\cdot \frac{v}{c}\cdot \sin \theta =s_g\cdot \beta \cdot \sin \theta =s_g\cdot {\beta }_{\perp }$

${\beta }_{\perp }$ is the component of the dimensionless velocity $\beta =\frac{v}{c}$ perpendicular to $s_g$.

Taking into account the orientation of the different vectors, the β-index of an informaton emitted by a point mass moving with constant velocity, can also be expressed as:

$s_{\beta }=\frac{v\times s_g}{c}$

5. The Gravitational Induction (or the g-Induction) of a Mass Particle Moving with Constant Velocity

We consider again the situation of Figure 3 . All informatons in dV—the volume element at P—carry both g-information and β-information. The β-information refers to the velocity of the emitting particle and is represented by the β-indices $s_{\beta }$:

$s_{\beta }=\frac{c\times s_g}{c}=\frac{v\times s_g}{c}$

If n is the density at P of the cloud of informatons (number of informatons per unit volume) at the moment t, the amount of β-information in dV is determined by the magnitude of the vector:

$n\cdot s_{\beta }\cdot \text{d}V=n\cdot \frac{c\times s_g}{c}\cdot \text{d}V=n\cdot \frac{v\times s_g}{c}\cdot \text{d}V$

So the density of the β-information (characteristic information per unit volume) at P is determined by:

$n\cdot s_{\beta }=n\cdot \frac{c\times s_g}{c}=n\cdot \frac{v\times s_g}{c}$

We call this (time dependent) vectoral quantity—that will be represented by $B_g$ (s⁻¹)—the “gravitational induction” or the “g-induction” at P³. Its magnitude $B_g$ determines the density of the β-information at P and its orientation determines the orientation of the β-indices $s_{\beta }$ of the informatons passing near that point.

So, the g-induction caused by the moving particle with res mass m₀ ( Figure 3 ) at P is:

$B_g=n\cdot \frac{v\times s_g}{c}=\frac{v}{c}\times \left(n\cdot s_g\right)$

N—the density of the flow of informatons at P (the rate per unit area at which the informatons cross an elementary surface perpendicular to the direction of their movement)—and n—the density of the cloud of informatons at P (number of informatons per unit volume)—are connected by the relation:

$n=\frac{N}{c}$

With $E_g=N\cdot s_g$, we can express the gravitational induction at P as:

$B_g=\frac{v}{c^2}\times \left(N\cdot s_g\right)=\frac{v\times E_g}{c^2}$

Taking the result of §3 into account, we find:

$B_g=-\frac{m_0}{4\pi {\eta }_0{c}^2\cdot r^3}\cdot \frac{1-{\beta }^2}{{\left(1-{\beta }^2\cdot {\sin }^2\theta \right)}^{\frac{3}{2}}}\cdot \left(v\times r\right)$

We define the constant ${\nu }_0$ as:

${\nu }_0=\frac{1}{c^2\cdot {\eta }_0}=9.34\times {10}^{-27}\text{m}\cdot {\text{kg}}^{-1}$

And finally, we obtain:

$B_g=\frac{{\nu }_0\cdot m_0}{4\pi r^3}\cdot \frac{1-{\beta }^2}{{\left(1-{\beta }^2\cdot {\sin }^2\theta \right)}^{\frac{3}{2}}}\cdot \left(r\times v\right)$

$B_g$ at P is perpendicular to the plane formed by P and the path of the point mass; its orientation is defined by the rule of the corkscrew; and its magnitude is:

$B_g=\frac{{\nu }_0\cdot m_0}{4\pi r^2}\cdot \frac{1-{\beta }^2}{{\left(1-{\beta }^2\cdot {\sin }^2\theta \right)}^{\frac{3}{2}}}\cdot v\cdot \sin \theta$

If the speed of the mass is much smaller than the speed of light, the expression for the gravitational induction reduces itself to:

$B_g=\frac{{\nu }_0\cdot m_0}{4\pi r^3}\cdot \left(r\times v\right)$

This non-relativistic result could directly be obtained if one assumes that the displacement of the point mass during the time interval that the informatons need to move from the emitter to P can be neglected compared to the distance they travel during that period.

So if $v\ll c$, $B_g$ at P is perpendicular to the plane formed by P and the path of the mass particle; its orientation is defined by the rule of the corkscrew; and its magnitude is:

$B_g=\frac{{\nu }_0\cdot m_0}{4\pi r^2}\cdot v\cdot \sin \theta$

6. The Gravitational Field of a Mass Particle Moving with Constant Velocity

A particle with rest mass m₀, moving with constant velocity $v=v\cdot e_z$ along the Z-axis of an IRF, creates and maintains an expanding cloud of informatons that are carriers of both g- and β-information. That cloud can be identified with a time dependent continuum. It is called the gravitational field⁴ of the particle. It is characterized by two time dependent vectoral quantities: the gravitational field (short: g-field) $E_g$ and the gravitational induction (short: g-induction) $B_g$.

1. With N the density of the flow of informatons at P (the rate per unit area at which the informatons cross an elementary surface perpendicular to their direction of movement), the g-field at that point is:

$E_g=N\cdot s_g=-\frac{m_0}{4\pi {\eta }_0{r}^3}\cdot \frac{1-{\beta }^2}{{\left(1-{\beta }^2\cdot {\sin }^2\theta \right)}^{\frac{3}{2}}}\cdot r$

The magnitude of $E_g$ is the rate per unit area at which g-information is crossing an elementary surface perpendicular to the orientation of the g-indices of the constituent informatons. It’s clear that the direction of the flow of g-information at P is not the same as the direction of the flow of informatons.

2. With n, the density of the cloud of informatons at P (number of informatons per unit volume), the g-induction at that point is:

$B_g=n\cdot s_{\beta }=\frac{{\nu }_0\cdot m_0}{4\pi r^3}\cdot \frac{1-{\beta }^2}{{\left(1-{\beta }^2\cdot {\sin }^2\theta \right)}^{\frac{3}{2}}}\cdot \left(r\times v\right)$

The magnitude of $B_g$ is the density of the cloud of β-information at P (amount of β-information per unit volume). The orientation of $B_g$ is determined by the orientation of the β-indices of the constituent informatons.

One can verify that:

1. $div{E}_g=0$

2. $div{B}_g=0$

3. $rot{E}_g=-\frac{\partial B_g}{\partial t}$

4. $rot{B}_g=\frac{1}{c^2}\cdot \frac{\partial E_g}{\partial t}$

These relations are the laws of Maxwell-Heaviside.

If $v\ll c$, the expressions for the g-field and the g-induction reduce to:

$E_g=-\frac{m_0}{4\pi {\eta }_0{r}^3}\cdot r$, $B_g=\frac{{\nu }_0\cdot m_0}{4\pi r^3}\cdot \left(r\times v\right)$

7. The Gravitational Field of a Set of Particles Moving with Constant Velocities

We consider a set of particles $m_1,\cdots ,m_i,\cdots ,m_n$ that move with constant velocities $v_1,\cdots ,v_i,\cdots ,v_n$ relative to an IRF O. It creates and maintains a gravitational field that in O at each point, is characterised by the vector pair ( $E_g$, $B_g$).

1. Each mass m_i continuously emits g-information and contributes with an amount $E_{gi}$ to the g-field at an arbitrary point P. As in [1] we conclude that the effective g-field $E_g$ at P is defined as:

$E_g={\displaystyle \sum E_{gi}}$

2. If it is moving, each mass m_i emits also β-information, contributing to the g-induction at P with an amount $B_{gi}$. It is evident that the β-information in the volume element dV at P at each moment t is expressed by:

${\displaystyle \sum \left(B_{gi}\cdot \text{d}V\right)}=\left({\displaystyle \sum B_{gi}}\right)\cdot \text{d}V$

Thus, the effective g-induction $B_g$ at P is:

$B_g={\displaystyle \sum B_{gi}}$

On the basis of the superposition principle we can conclude that the laws of Maxwell-Heaviside mentioned in the previous section remain valid for the effective g-field and g-induction in the case of the gravitational field of a set of particles describing uniform rectilinear motions.

8. The Gravitational Field of a Stationary Mass Flow

The term “stationary mass flow” refers to the movement of a homogeneous and incompressible fluid that, in an invariable way, flows relative to an IRF. The intensity of the flow at an arbitrary point P is characterized by the flow density $J_G$. The magnitude of this vectoral quantity at P equals the rate per unit area at which the mass flows through a surface element that is perpendicular to the flow at P. The orientation of $J_G$ corresponds to the direction of that flow. So, the rate at which the flow transports—in the positive sense (defined by the orientation of the surface vectors $\text{d}S$)—mass through an arbitrary surface ΔS, is:

$i_G={\displaystyle {\iint }_{\Delta S}{J}_G\cdot \text{d}S}$

$i_G$ is the intensity of the mass flow through ΔS.

Since a stationary mass flow is the macroscopic manifestation of moving mass elements ${\rho }_G\cdot \text{d}V$, it creates and maintains a gravitational field. And since the velocity $v$ of the mass element at a certain point is time independent, the gravitational field of a stationary mass flow will be time independent. It is evident that the rules for a static g-field [1] also apply for this time independent g-field:

1. $div{E}_g=-\frac{{\rho }_G}{{\eta }_0}$

2. $rot{E}_g=0$ what implies: $E_g=-grad{V}_g$

One can prove [2] [3] that the rules for the time independent g-induction are:

1. $div{B}_g=0$ what implies the existence of a vector gravitational potential function $A_g$ for which $B_g=rot{A}_g$

2. $rot{B}_g=-{\nu }_0\cdot J_G$

9. The Gravitational Interaction between Moving Objects

We consider a number of mass particles moving relative to an inertial reference frame O. They create and maintain a gravitational field that at each point of the space linked to O is defined by the vectors $E_g$ and $B_g$. Each mass is “immersed” in a cloud of informatons carrying both g- and β-information. At each point, except at its own position, each particle contributes to the construction of that cloud.

Let us consider the particle with rest mass m₀ that, at the moment t, goes with velocity $v$ through the point P.

1. If the other particles were not there ${E^{\prime }}_g$—the g-field in the immediate vicinity of m₀—would, according to §3, be symmetric relative to the carrier line of the velocity $v$ of m₀. In reality that symmetry is disturbed by the g-information that the other particles send to P. $E_g$, the instantaneous value of the g-field at P, defines the extent to which this occurs.

2. If the other particles were not there ${B^{\prime }}_g$—the g-induction near m₀—would, according to §5, “rotate” around the carrier line of the vector $v$. The pseudo-gravitational-field ${E^{″}}_g=v\times {B^{\prime }}_g$ defined by the vector product of $v$ with the g-induction that characterizes the proper β-field of m₀, would also be symmetric relative to the carrier line of the velocity $v$. In reality this symmetry is disturbed by the β-information send to P by the other particles. The vector product ( $v\times B_g$) of the instantaneous values of the velocity of m₀ and the g-induction at P, characterizes the extent to which this occurs.

So, the characteristic symmetry of the cloud of g-information around a moving particle (the proper gravitational field) is in the immediate vicinity of that particle disturbed by $E_g$ regarding the proper g-field and by ( $v\times B_g$) regarding the proper β-induction.

If it is free to move, the particle m₀ could restore the characteristic symmetry in its immediate vicinity by accelerating—relative to its proper IRF O'—with an amount $a^{\prime }=E_g+\left(v\times B_g\right)$. In that manner it would become “blind” for the disturbance of symmetry of the gravitational field in its immediate vicinity. These insights form the basis of the following postulate.

A particle with rest mass m₀, moving with velocity $v$ in a gravitational field ( $E_g,B_g$), tends to become blind for the influence of that field on the symmetry of its proper gravitational field. If it is free to move, it will accelerate relative to its proper inertial reference frame with an amount $a^{\prime }$:

$a^{\prime }=E_g+\left(v\times B_g\right)$

10. The Gravitational Force Law

The action of the gravitational field ( $E_g,B_g$) on a particle with rest mass m₀ that is moving with velocity $v$ relative to the IRF O, is called the gravitational force $F_G$ on that particle. In extension of [1] we define $F_G$ as:

$F_G=m_0\cdot \left[E_g+\left(v\times B_g\right)\right]$

If it is free to move, the effect of ${\bar{F}}_G$ on a particle with rest mass m₀ is that this will be accelerated relative to the its proper IRF O' with an amount $a^{\prime }$:

$a^{\prime }=E_g+\left(v\times B_g\right)$

This acceleration can be decomposed in a tangential ( ${a^{\prime }}_T$) and a normal component ( ${a^{\prime }}_N$):

${a^{\prime }}_T={a^{\prime }}_T\cdot e_T$ and ${a^{\prime }}_N={a^{\prime }}_N\cdot e_N$

where $e_T$ and $e_N$ are the unit vectors, respectively along the tangent and along the normal to the path of the point mass in O' (and in O).

We express ${a^{\prime }}_T$ and ${a^{\prime }}_N$ in function of the characteristics of the motion relative to the IRF O [4] :

${a^{\prime }}_T=\frac{1}{{\left(1-{\beta }^2\right)}^{\frac{3}{2}}}\cdot \frac{\text{d}v}{\text{d}t}$ and ${a^{\prime }}_N=\frac{v^2}{R\cdot \sqrt{1-{\beta }^2}}$

(R is the radius of curvature of the path in O, and that radius in O' is $R\sqrt{1-{\beta }^2}$.)

The gravitational force is:

$\begin{array}{c}{F}_G=m_0\cdot a^{\prime }=m_0\cdot \left({a^{\prime }}_T\cdot e_T+{a^{\prime }}_N\cdot e_N\right)\\ =m_0\cdot \left[\frac{1}{{\left(1-{\beta }^2\right)}^{\frac{3}{2}}}\cdot \frac{\text{d}v}{\text{d}t}\cdot e_T+\frac{1}{{\left(1-{\beta }^2\right)}^{\frac{1}{2}}}\cdot \frac{v^2}{R}\cdot e_N\right]=\frac{\text{d}}{\text{d}t}\left[\frac{m_0}{\sqrt{1-{\beta }^2}}\cdot v\right]\end{array}$

With:

$\frac{m_0}{\sqrt{1-{\beta }^2}}\cdot v=p$

We finally obtain:

$F_G=\frac{\text{d}p}{\text{d}t}$

$p$ is the linear momentum of the particle relative to the IRF O. It depends on the relativistic mass m op the particle:

$m=\frac{m_0}{\sqrt{1-{\beta }^2}}$

In §2 it has been showed that m is the parameter of the mass particle that determines the rate at which it emits informatons relative to its proper IRF. Thus it is representative for the density of the cloud of informatons generated in that IRF and thus for the ability to persist in its dynamic state. It is a measure for its inertia.

11. The Interaction between Two Moving Particles

Two particles with rest masses m₁ and m₂ ( Figure 4 ) are anchored in the IRF O' that is moving relative to the inertial reference frame O with constant velocity $\stackrel{\to }{v}=v\cdot {\stackrel{\to }{e}}_z$. The distance between the masses is R.

Figure 4

Figure 4. The gravitational interaction between moving particles.

According to §6, the components of the gravitational field created and maintained by m₁ at the position of m₂ are—in magnitude—determined by:

$E_{g2}=\frac{m_1}{4\pi {\eta }_0{R}^2}\cdot \frac{1}{\sqrt{1-{\beta }^2}}$

$B_{g2}=\frac{m_1}{4\pi {\eta }_0{R}^2}\cdot \frac{1}{\sqrt{1-{\beta }^2}}\cdot \frac{v}{c^2}$

$E_{g2}$ points to the position of m₁ and $B_{g2}$ points in the direction of the X-axis.

And according to the force law F₁₂, the magnitude of the force exerted by the gravitational field ( $E_{g2},B_{g2}$) on m₂—this is the attraction force of m₁ on m₂—is:

$F_{12}=m_2\cdot \left(E_{g2}-v\cdot B_{g2}\right)$

After substitution:

$F_{12}=\frac{1}{4\pi {\eta }_0}\cdot \frac{m_1{m}_2}{R^2}\cdot \sqrt{1-{\beta }^2}={F^{\prime }}_{12}\cdot \sqrt{1-{\beta }^2}$

with:

${F^{\prime }}_{12}=\frac{1}{4\pi {\eta }_0}\cdot \frac{m_1{m}_2}{R^2}$

the magnitude of the force that m₁, according Newtons universal law of gravitation, in the IRF O'—where both particles are at rest—exerts on m₂.

In the same way we find:

$F_{21}=\frac{1}{4\pi {\eta }_0}\cdot \frac{m_1{m}_2}{R^2}\cdot \sqrt{1-{\beta }^2}={F^{\prime }}_{12}\cdot \sqrt{1-{\beta }^2}$

We conclude that the moving masses attract each other with a force:

$F=F_{12}=F_{21}=F^{\prime }\cdot \sqrt{1-{\beta }^2}$

This result perfectly agrees with that based on S.R.T. Indeed, relative to O' the particles are at rest. According to Newton’s law of universal gravitation, they exert on each other equal but opposite forces:

$F^{\prime }={F^{\prime }}_{12}={F^{\prime }}_{21}=G\cdot \frac{m_1\cdot m_2}{R^2}=\frac{1}{4\cdot \pi \cdot {\eta }_0}\cdot \frac{m_1\cdot m_2}{R^2}$

Relative to O both masses are moving with constant speed v in the direction of the Z-axis. From the transformation equations between an inertial frame O and another inertial frame O', in which a point mass experiencing a force F' is instantaneously at rest, we can immediately deduce the force F that the point masses exert on each other in O [4] :

$F=F_{12}=F_{21}=F^{\prime }\cdot \sqrt{1-{\left(\frac{v}{c}\right)}^2}=F^{\prime }\cdot \sqrt{1-{\beta }^2}$

From the above we can also conclude that the component of the gravitational force due to the g-induction is β-times smaller than that due to the g-field. This implies that, for speeds much smaller than the speed of light, the effects of the β-information are masked.

It can be shown that the β-information emitted by moving gravitating objects is responsible for deviations (as the advance of Mercury Perihelion) of the real orbits of planets with respect to these predicted by the classical theory of gravitation [5] .

12. Conclusions

A mass particle moving relative to an inertial IRF O is the emitter of informatons that are carriers of information regarding the positon (g-information) and regarding the velocity (β-information) of their source. As a result, the gravitational field, of a moving mass particle (and by extension of a set of moving particles, a moving material object and a mass flow) manifests itself at the macroscopic level in O as a dual entity, always having a field- and an induction component ( $E_g$ and $B_g$) simultaneously created by their common sources.

The interaction between material objects in that field is made possible by the intermediation of the gravitational field. An object in a gravitational field tends to become blind for that field. It experiences a force described by a Lorentz like law.

Thus, it is clear that the kinematics of the gravitating objects play a role in the gravitational phenomena. This is taken into account in the framework of the gravitoelectromagnetic description of gravitation [6] [7] (GEM) where the idea is developed that the gravitational field must be isomorphic with the electromagnetic field in a vacuum.

Because the role of the kinematics of the gravitating objects is not relevant when the speed of the object is small relative to the speed of light, this phenomenon is not taken into account in the “classical” description of the gravitational phenomena and laws.

13. Epilogue

In the follow-up article “The Maxwell-Heaviside Equations Explained by the Theory of Informatons” we mathematically deduce the Maxwell-Heaviside equations from the kinematics of the informatons. That deduction indicates that there is no causal link between $E_g$ and $B_g$.

NOTES

¹We neglect the possible stochastic nature of the emission, that is responsible for noise on the quantities that characterize the gravitational field. So, $\stackrel{\dot{}}{N}$ is the average emission rate.

²The orientation of the g-field implies that the g-indices of the informatons that at a certain moment pass near P, point at that moment to the position of the emitting mass and not to its light delayed position.

³also called “gravitomagnetic induction”.

⁴Also called: “gravito-electromagnetic” (GEM field) or “gravito-magnetic” field (GM field).

References

1. Acke, A. (2024) Newton’s Law of Universal Gravitation Explained by the Theory of Informatons. Journal of High Energy Physics, Gravitation and Cosmology, 10, 918-929. >https://doi.org/10.4236/jhepgc.2024.103056

2. Acke, A. (1990) Beginselen van de informatonentheorie. Uitgeverij Nevelland.

3. Acke, A. (2008) Gravitatie en elektromagnetisme. Uitgeverij Nevelland.

4. Resnick, R. (1968) Introduction to Special Relativity. John Wiley&Sons, Inc.

5. Tajmar, M. and de Matos, C.J. (2003) Advance of Mercury Perihelion Explained by Cogravity. arXiv: gr-qc/0304104.

6. Heaviside, O. (1893) A Gravitational and Electromagnetic Analogy, Part I. sl : The Electrician 1893.

7. Jefimenko, O. (1992) Causality, Electromagnetic Induction, and Gravitation. sl : Electret Scientific 1992, Vol. 1992.