Specific Examples of Negative Mass


by

Edmond S. Miksch

ed_miksch@yahoo.com

(412)373-4919

First Copyright: June 1, 2005

Latest Copyright: November 11, 2008





Abstract


         A simple thought experiment shows that the gravitational field has negative mass. Negative mass is also found in the acceleration field of Einstein's elevator. The negative mass density of a gravitational or acceleration field is proportional to the square of the field strength.

         A simple thought experiment indicates that the Coriolis field has negative mass. A factor of 2 discrepancy in the calculation remains to challenge the reader.

         A simple thought experiment indicates that gravitational radiation has negative mass. A gravitational radiator is believed to gain mass as it radiates negative mass.




Contents





Prerequisites


         An understanding of basic physics including electromagnetism, and an understanding of the basic principles of special and general relativity, will be helpful for understanding the following.




Terminology and Conventions


         We use the term "mass" to refer to the conserved quantity, and never use it for the rest mass of a particle, since rest mass is not conserved. Mass has gravitational properties and inertial properties. We see no reason for questioning the equivalence of gravitational and inertial mass. Energy is viewed as comprising mass in any volatile form.

         Vector quantities, which have both direction and magnitude, are denoted by bold face characters. When the symbol for a vector quantity is not in boldface, it denotes the magnitude of the vector quantity. Asterisks are sometimes used to denote multiplication. Weight is considered to be a real force, as is centrifugal force and the Coriolis force. In this, we rely on the relativistic principle that we may view the universe from any coordinate frame we choose.

         We do not, however, disparage purists who prefer to consider geodesics in Minkowsky space, rather than considering gravitational forces as contributing to the acceleration of a mass. Our attempt is to stay as close as possible to everyday experience. SI units are employed. These include the meter, second, kilogram, Joule, Newton, Volt, Ampere, Coulomb, etc.

         A local observer formulation is always employed. Distance between nearby points in space is measured by a local meter stick. The time interval between two nearby events is measured by a local clock. Mass at a point in space is measured by local instruments. Quantities extending over large regions are measured by a sum or integral of incremental values made by local observers, in the limit as the size of the increments approaches zero. This is consistent with the use of a metric tensor to define the properties of the space-time continuum since the incremental distances and times related by a metric tensor are measured by local instruments.




Introduction


         Negative mass is not antimatter. When matter and antimatter contact each other, they release energy, and hence mass. For example, an electron contacting a positron causes emission of gamma rays, which have positive energy and, therefore, positive relativistic mass. (Gamma rays, like other photons, do not have rest mass, but, since they have energy, they do have relativistic mass.)

         Negative mass is not a shield against gravity. A region of space having negative mass acts as a source of the gravitational field vector which, at any point, is added to all the other gravitational fields at that point.

         A chunk of material having negative mass in a laboratory on Earth would have negative weight. However, if we released it, it would not fall toward the ceiling. Since its mass is negative, it would accelerate in the direction opposite to the direction of the force on it. Since the force on it is upward, it accelerates downward. All masses, whether positive or negative, tend to accelerate toward a positive mass such as Earth. All masses, whether positive or negative, tend to accelerate away from a negative mass.

         If I had a chunk of matter in my hand, which had negative mass, it would feel pretty strange. If I exert a northward force on it, it accelerates toward the south. If I exert an eastward force on it, it accelerates toward the west. However, lets not be put off by strange feelings. After all, a gyroscope also feels strange. If I have a spinning gyroscope with a vertical axis and try to tilt it toward the north, it tilts toward the east or west, depending on the direction of its rotation.

         A chunk of matter having negative mass would be quite difficult to control. It would have to be held in position by a restraint having a positive dF/dx. (Most springs have a negative dF/dx, that is, they push back against any displacement. A magnet near an iron wall experiences a positive dF/dx. A spring with a bent knee, like a chevron, can also have a positive dF/dx.) Also, the angular position of the chunk of matter would have to be controlled by springs with a positive derivative of torque with respect to angular displacement, just the opposite of the balance spring in a clock.

         Furthermore, to prevent vibratory motion of the negative mass, all possible vibratory velocities would have to be energized, rather than being damped as occurs naturally for positive masses. If, at an instant, it was moving north, then the system holding it would have to push north on it to reduce that velocity. If it was moving east, then the system would have to push east on it to reduce that velocity. This would also be true for angular vibrations. If it started to rotate to the right, as seen by an observer, then it would have to be torqued toward the right, as seen by that observer, to decrease the velocity of that rotation. Furthermore, if it could vibrate in a bending mode like a tuning fork, or vibrate in any other deformation mode, that mode would have to be energized to decrease the mode.

         Let us speculate on a particle having a negative mass interacting with an atom of ordinary matter. Could they annihilate, leaving nothing? We see many problems. Mass, momentum and angular momentum would have to be conserved, as seen by all observers. Electrical charge would have to be conserved. What about entropy? The entropy of both the negative mass particle and the ordinary atom would have to be destroyed. Hence, some mechanism would be needed which would increase entropy elsewhere as it annihilated the two particles, to avoid a decrease in entropy.

         If a particle having negative mass entered Earth's atmosphere and had any interaction with atoms of the atmosphere, it would energize those atoms. Hence, the energy of the negative mass particle would have to become more negative to have an energy balance. If the negative mass particle was traveling at less than the speed of light, its speed would increase as its energy went more negative. One can imagine it passing through the earth like a neutrino, increasing its velocity as it went, and emerging from the Earth with more than sufficient velocity to escape. Hence, we do not expect any fortunate prospector to chance upon a nugget of matter having negative mass.

         However, what about force fields? We take the view that the electric field, the magnetic field, the gravitational field, and the Coriolis field all are observable realities each having, at any point in space, as seen by a particular observer, a mass density, a momentum density, a stress tensor and other physical properties. Do any of these fields have a negative mass density?

         Clearly, the electric field does not. A charged capacitor stores positive energy and hence positive mass. Likewise, the magnetic field does not have a negative mass density. An inductor carrying a current stores positive energy and hence positive mass. But what about the gravitational field.... ?





Calculation of the Mass Density of the Gravitational Field


         Our method of calculation is as follows: We set up a thought experiment involving a system comprising masses that can be positioned in two configurations. In an initial configuration of the system, there is no gravitational field in a particular region of space. In a final configuration of the system, there is a gravitational field in that region. We avoid making changes to gravitational fields in any other region. We then do an energy balance, considering the energy we obtained or expended when we moved the masses from the initial configuration to the final configuration.

         Of course, it is taken as understood that energy is a type of mass. A charged battery has more mass than the same battery when it is discharged. Likewise, a charged capacitor has more mass than the same capacitor uncharged. We may consider energy to be a volatile form of mass. By contrast, matter contains mass in a stable form. If, in our thought experiment, we find that positive energy is necessary to create a gravitational field in the particular region we selected, then we will conclude that the gravitational field has a positive mass density. However, if we find that energy is produced when the gravitational field is created, then we will conclude that the gravitational field has a negative mass density.


Electrical Example

         As background for the gravitational calculation, we set up a thought experiment to calculate the mass density of the electric field. Rather than considering a capacitor which has, on its plates, both positive and negative charges, we prefer an electric field generated by positive charges alone, because for the gravitational case, we don't want to invoke negative masses at this point in the logical process.

         We consider a spherical shell of positive charges having a lesser radius, RL, which we permit to expand to a greater radius, RG. We assume that the distribution of charges on the spherical shell is uniform, and we denote the total charge as Q.

         Figure G1 shows the configuration when the charges are at the lesser radius, RL. Figure G2 shows the configuration when the charges are at the greater radius, RG. In Figure G1, the heavy circle shows the charges at the lesser radius, RL and the greater radius is shown in phantom. In Figure G2, the heavy circle shows the charges at the greater radius, RG, and the lesser radius is shown in phantom. In both figures, the vector denoted R is the vector to any point in space, either inside the spheres, or outside.

         We now look for regions of space in which the electric field has been created or eliminated as a result of moving the charges from RL to RG. It is well understood that inside a uniformly charged sphere, the electric field due to the charged sphere is zero. Hence, for both the configuration shown in Figure G1 and the configuration shown in Figure G2, the electric field inside the smaller sphere having radius RL is zero. Therefore, there is no change in the electric field inside of RL

         It is also well understood that, anywhere outside of a uniformly charged sphere, at a radius R from the center of the sphere, the electric field is given by:

E = Q/(4πε0R2)         Equation G1


         The quantity ε0 is the permittivity of free space, which equals 8.85 * 10-12 in SI units. Hence, for both the configuration shown in Figure G1 and the configuration shown in Figure G2, the electric field outside the larger sphere having radius RG has the value given by Equation G1. Therefore, there is no change in the electric field outside of RG.

         There is, however, a change in the electric field in the region for which R is greater than RL but less than RG. In both Figure G1 and Figure G2, the three inequalities define the three regions, and the corresponding three equations give the electric field in the corresponding region. We see that expanding the charged sphere from RL to RG only affects the electric field in the region between the two spheres, where RL < R < RG.

Two figures are shown which illustrate two concentric spheres of charged 
particles.  Each figure shows two concentric spheres, one having having a lesser 
radius R<sub>L</sub> and another having a greater radius 
R<SUB>G</SUB>.


         From this point, we will calculate the pressure on the charged sphere as it is expanded from RL to RG, and we will calculate the energy we obtain as we expand the sphere from RL to RG. To simplify the problem, we consider a case in which RL and RG are very nearly equal. We now denote the radius of the shell as RS.

         The pressure equals the surface charge multiplied by the electric field just outside the shell divided by 2. (The factor of 2 is because the electric field seen by the charge is averaged through the thickness of the charged spherical shell, and it is zero inside the shell.)

         Just outside the shell, the electric field, E is:

E = Q/(4πε0RS2)


         The surface charge is:

QS = Q/(4πRS2) = ε0 E


         The pressure on the spherical shell, which is outward, is, therefore:

PE = ε0 E2/2


         From simple mechanical considerations, we find that the energy density of the electric field equals the pressure of the field on the spherical shell and division by c2 yields the mass density. (The speed of light is denoted c.) The mass density of the electric field, therefore, is:

MV = ε0 E2/(2c2)


         As the spherical shell expanded from RL to RG, we consumed electric field and obtained positive mass. Hence, as surprises no one, the electric field has positive mass.


Gravitational Case

         In a similar calculation for the gravitational field, we start with a spherical shell of mass particles (positive mass particles) having a greater radius, RG and contract the shell of mass particles to form a spherical shell having a lesser radius, RL . The total mass of the spherical shell is denoted M, and the mass is assumed to have a uniform surface density on the spherical shell. The mass particles could be gold dust, buckshot, sand, etc.

         Figure 3 shows the configuration when the mass particles are disposed at the greater radius, RG, and Figure G4 shows the configuration when the mass particles are disposed at the lesser radius, RL. In Figure G3, the heavy circle shows the mass particles at the greater radius, RG and the lesser radius is shown in phantom. In Figure G4, the heavy circle shows the mass particles at the lesser radius, RL, and the greater radius is shown in phantom. In both figures, the vector denoted R is the vector to any point in space, either inside the spheres, or outside.

         We now look for regions of space in which the gravitational field has been created or eliminated as a result of moving the mass particles from RG to RL. It is well understood that inside a massive spherical shell having a uniform surface density, the gravitational field due to the spherical shell is zero. Hence, for both the configuration shown in Figure G1 and the configuration shown in Figure G2, the gravitational field inside the smaller sphere having radius RL is zero. Therefore, there is no change in the gravitational field inside of RL.

         It is also well understood that, anywhere outside of a spherical shell having a uniform surface mass density, and a total mass M, at a radius R from the center of the sphere, the gravitational field is given by:

g = GM/R2         (Equation G2)


         (Equation G2 resembles Newton's law of gravity, where G is the gravitational constant. In SI units, G = 6.672*10-11. Equation G2 may be obtained from the law of gravity by integrating that law over all the mass particles in the spherical shell. It is noted that Equation G2 is an approximation because it ignores the mass density of the gravitational field itself. It is extremely accurate, however, for a system having much less mass or density than a black hole.) We will discuss this approximation later.

         Hence, for both the configuration shown in Figure G3 and the configuration shown in Figure G4, the gravitational field outside the larger sphere having radius RG has the value given by Equation G2. Therefore, there is no change in the gravitational field outside of RG.

         There is, however, a change in the gravitational field in the region for which R is greater than RL but less than RG. In both Figure G3 and Figure G4, the three inequalities define the three regions, and the corresponding three equations give the gravitational field in the corresponding region. We see that contracting the shell of mass particles from RG to RL only affects the gravitational field in the region between the two spheres, where RL < R < RG.

Two figures are shown which illustrate two concentric spheres of mass 
particles.  Each figure shows two concentric spheres, one having having a lesser 
radius R<sub>L</sub> and another having a greater radius 
R<SUB>G</SUB>.

         From this point, we will calculate the pressure on the spherical shell as it is contracted from RG to RL, and we will calculate the energy we obtain as we contract the spherical shell from RG to RL. To simplify the problem, we consider a case in which RG and RL are very nearly equal. (Our calculation would exactly apply in the limit in which the thickness becomes vanishingly small compared to the radius of the shell.) We now denote the radius of the shell as RS.

         The pressure equals the mass per unit area of the shell multiplied by the gravitational field just outside the shell divided by 2. (The factor of 2 is because the gravitational field seen by the mass particles is averaged through the thickness of the spherical shell of mass particles, and it is zero inside the shell.)

Just outside the shell, the gravitational field, g is:

g = MG/(RS2)


         M is the total mass of the shell and G is the gravitational constant. The mass per unit area on the shell is:

MS = M/(4πRS2) = g/(4πG)


         The pressure on the spherical shell due to the gravitational field, is, therefore:

PG = MSg/2 = g2/(8πG)


         The pressure is inward, and the spherical shell moved inwardly from RG to RL. Hence, we obtained positive energy as we lowered the mass particles from RG to RL.

         Thus, we obtained energy as we created a gravitational field in the region for which RL < R < RG. Therefore, conservation of energy requires that the gravitational field have a negative energy density. The magnitude of the energy density equals the magnitude of the pressure on the spherical shell. Hence, the energy density of the gravitational field is:

-g2/(8πG)


         Thus, the mass density of the gravitational field is:

MV = -g2/(8πGc2)         Equation G3


         QED.

         At this point, it is of interest to calculate the divergence of the gravitational field vector due to its own mass density. To do this, we rewrite Newton's law of gravity in differential form as follows, where MV is the mass density of space, g is the gravitational field vector and div is the divergence operator:

MV = - div g/(4πG)         Equation G4

         Combining Equations G3 and G4, we obtain for the divergence of the gravitational field vector due to the mass density of the gravitational field itself the following:

div g = g2/(2c2)          Equation G5


         We note that the divergence of the gravitational field vector due to its own mass density is positive because its mass density is negative. (The Earth has a positive mass density and causes a negative divergence of the gravitational field vector.)

         At this point, we can look at the approximation we made previously in Equation G2, in which we ignored the mass density of the gravitational field itself. First of all, the mass density of the gravitational field itself is small compared to the mass that causes it, for masses which do not approximate black hole conditions. Second, only the mass of the gravitational field within the thickness of the shell of mass particles affects the gravitational field immediately outside the shell. Since our calculation is for the limit in which the thickness of the shell becomes vanishingly small compared to the radius of the shell, the mass of the gravitational field itself does not cause an error in our calculation of its mass density. Thus, our calculation of the mass density of the gravitational field should be valid, even in the vicinity of a black hole.

         Since in the vicinity of a black hole, the gravitational field becomes very great, we anticipate that there is a very high negative mass density surrounding a black hole.

         We do not intend here to disparage Schwarzshield and others who have performed analyses of the geometry of the space-time continuum near black holes. However, those analyses may produce results so esoteric that the negative mass density of the gravitational field is not obvious. In the present analysis, we wish to stay as close as possible to ordinary experience, using credible thought experiments, but to point out that we find the mass density of the gravitational field to be negative.

         Extrapolating the present analysis, we wonder: Do other attractive agents, for example, the fields or particles which mediate the strong nuclear force that binds the protons together in an atomic nucleus also have negative mass? Also, would repulsive agents such as that which causes the outward acceleration of distant galaxies, be better understood as comprising negative mass, rather than "dark energy"?




How can this be True?


         In the preceding section, we arrived at the scary conclusion that the gravitational field has a negative mass density. This was calculated in Equation G4. Let us consider carefully how we reached that conclusion. In the thought experiment illustrated in Figures G3 and G4, we assumed that the mass of each particle is independent of its gravitational potential. This is consistent with our local observer formulation.

         A person uncomfortable with the idea of negative mass might say that since each mass particle has a potential energy, and since energy has mass, a portion of its mass must be attributed to its potential energy. Such a person would say that each mass particle in Figure G2, after the contraction, would have less mass than it had in Figure G1, before the contraction. That reduction of mass of the particles would be the source of the energy we obtained when we lowered the particles. That person would then say that the energy density and mass density of the gravitational field are both zero.

         From such a view, we would conclude that the mass of objects in a laboratory on Earth would decrease if massy bodies from the Oort cloud were brought closer to the sun and placed in the asteroid belt. This is because such an inward movement of massy bodies would lower the potential energy of every mass in the solar system, including the objects in the laboratory. Now, suppose I operate three clocks in my laboratory, specifically:

         If such an inward movement of massy bodies to the asteroid belt occurred, that person's view would cause us to believe that my three clocks would be affected in the following ways:

         A formulation of physics which would have such complicated results should be rejected by the principle of Occam's razor. Our physics is much simpler if we define the mass of an object by local measurements based on local meter sticks and local clocks. We do not need to define the mass of an object by reference to any standard such as the standard kilogram in Paris. We can instead use Equation G4, which is repeated here:

MV = - div g/(4πG)         (Equation G4)


         The quantities on the right side of Equation G4 depend only on space and time, and thus, the mass density of space can be defined without reference to any standard of mass. Furthermore, because we assume that the velocity of light in vacuo, as seen by a local observer, is a universal constant, we can use a clock to determine length as well as time. A nucleus or atom which emits electromagnetic radiation can thus be used to provide a standard second, standard meter, and standard kilogram.

         If a region of space has a positive divergence of the gravitational field, then, so be it - we have found negative mass. Let's not be too upset. After all, in the Minkowski formulation of space-time, a time interval works out as an imaginary distance. If we can work with imaginary numbers, surely we can work with negative numbers.


Experimental Measurement of the Mass Density of the Gravitational Field


         We propose the following experiment to measure the mass density of Earth's gravitational field, as a verification of Equation G3. We would employ a pair of counter-orbiting satellites in a low orbit, the orbit having just enough altitude to avoid friction due to Earth's atmosphere. This would yield us the mass of the Earth, its atmosphere, and its gravitational field up to the orbit of the satellites. The value so obtained would be compared with the mass obtained by another pair of counter-orbiting satellites at a much higher elevation. Subtracting the two mass values would yield the mass of the gravitational field in the space between a sphere havintg its center at Earth's center and having a radius equal to that of the low satellites and a similar sphere having the radius of the orbits of the higher satellites.

         Both pairs of satellites would be in polar orbits. The low pair would be at an altitude of about 7,500,000 meters. This altitude is selected to be high enough for the satellites to be substantially unaffected by Earth's atmosphere. The radius of the Earth at the equator is taken to be 6,480,000 meters, leaving an altitude of 1,020,000 meters (about 633.8 miles) above the surface at the equator.

         The two satellites in either pair, preferably, would pass as close as possible to each other, and they would obtain a reading of the time between passings, and the relative velocity with which they approach each other. Two passings would occur for each orbit. For example, they could pass each other above Earth's North pole, and again above Earth's South pole. The time between passings would be determined by on board clocks, and the velocity of approach would be obtained from the frequency shift of electromagnetic radiation sent from one to the other. Since the Earth rotates within the circle defined by the orbits, the satellites scan the entire Earth as it rotates, thus detecting the effects due to the local mass concentrations due to continents and mountains.

         From the relative velocity and the time between passings, the length of the orbits would be obtained, and from that, an area for a sphere having a center coincident with Earth's center and a radius equal to the altitude of their orbits would be obtained. Also, from the time and velocity, the radial gravitational field of the Earth along the paths of the satellites would be obtained. In this manner, the flux of the gravitational field would be obtained and from that, the total mass enclosed by the sphere. The measurement of flux would be made by local observers (the satellites) and thus the mass enclosed could be obtained by integrating Equation G4. Data obtained by the satellites would, preferably, be transformed to a stationary coordinate system that does not rotate relative to the distant stars. The left side of Equation G4 would be integrated over the volume of the sphere to obtain the combined mass of the Earth, its atmosphere, and the portion of its gravitational field inside the sphere. The right side would be integrated over the surface of the sphere to obtain the flux of the gravitational field vector which enters the sphere. The mass so obtained would be compared with the mass measured by another pair of counter-orbiting satellites in orbits having a much greater altitude to obtain the mass of the gravitational field between the sphere enclosed by the orbits of the low satellites and a sphere enclosed by the orbits of the satellites at the greater altitude. From Equation G3, we expect that the mass will be negative.

         To determine the accuracy that would be required to verify Equation G3, Table G1, which follows, provides a calculation of the total mass of the gravitational field outside of the smaller sphere, according to Equation G3. From Equation G3, we expect that the magnitude of the mass is about 2.95660 * 10-10 times the mass of the Earth. Thus, the times between passings and the relative velocities need to be measured with an error less than 10-10. The required time measurement is well within the capability of state of the art atomic clocks, and the accuracy of the Doppler measurement of velocity measurement is much less than that required in the Harvard Tower experiment by Pound and Rebka, which employed gamma rays to measure a frequency shift of about 4.9 * 10-15.

         Some very complex mathematics would be required to interpret the data obtained from the satellites. For one thing, the counter-orbiting satellites do not approach each other exactly, they must miss each other. Also, perturbations due to gravity gradient effects of the sun and moon would need to be included, and the uneven mass concentrations of the Earth would need to be considered. Such mathematics is believed to be within the state of the art of global positioning satellites.

Table G1
Calculation of the Mass of the Gravitational Field outside the Orbits of the Low Satellites
 
  Description or label of the quantityValue of the quantity
 
 1 
 
Mass of Earth:
5.97200 * 1024  kg
 
 2 
 
   Gravitational Constant:  
6.674280 * 10-11   m3 kg-1s-2
 
 3 
 
 Radius from geocenter: 
 7,500,000   m  
 
 4 
 
g at altitude of orbit:
7.08601   m sec-2
 
 5 
 
  Mass density of field g from Equation G3:  
-3.30576 * 10 -7  kg m-3
 
 6 
 
Area of sphere enclosed by the orbit:
7.068578 * 1014   m2
 
 7 
 
  Mass of g field in spherical shell 1 meter thick:  
-2.3542 * 108   kg
 
 8 
 
Mass of g field outside radius of orbit:
-1.76568 * 1015   Kg
 
 9 
 
  Ratio of mass of field outside orbit to mass of the Earth:  
-2.95660 * 10-10


         Row 1 of the table presents the mass of the Earth, and row 2 presents the gravitational constant. The product of these values is known to a high degree of accuracy, although the value of neither is precisely known. Row 3 presents the radius of the satellites' orbits from the center of the Earth. The gravitational field at the radius of the orbits, presented in row 4, is then obtained from the law of gravity, based on the mass of the Earth, the gravitational constant and the radius of the orbits. Equation G3 is then employed to calculate the mass density of the gravitational field at the radius of the orbits. The mass density, of course, is negative.

         Our purpose is to calculate the expected (negative) mass of the gravitational field outside the orbits of the satellites to determine the accuracy needed to verify that value based on the mass within the orbits of the satellites and the mass of the Earth (and its gravitational field) as observed from a great distance.

         To that end, Row 7 presents the mass of the gravitational field in a spherical shell one meter thick and a radius equal to the radius of the orbits. Corresponding values for successive shells (which decrease with radius according to an inverse square law) is integrated to infinity and the result presented in row 8, and that value is compared with the mass of the Earth in row 9. To obtain meaningful results, orbital parameters would need to be accurate to better than one part in 1010. This is far less accuracy than has been required in some other experiments, such as the Harvard tower experiment, that measured the relativistic time rate gradient effect over an elevation of 22.6 meters.


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