Gravitational energy gradients are formed to provide directional balance to 2-D and 3-D bodies of mass-energy – from the smallest electromagnetic particles to the largest bodies of mass.
Let’s assume for purposes of discussion that planets possess approximately the same density throughout. This means that each radius level outward from system center is composed of more and more total mass or energy. The least amount of mass per radius level exists at the system center while the greatest amount of mass-energy exists at the outer radius level. This forms an energy gradient outward from system center. The surrounding energy of space reacts to provide directional balance to this energy gradient by forming an opposing gravitational energy gradient. The gravitational energy gradient is most likely also providing directional balance for the difference in energy density between the body of mass and that of surrounding energy of space.
The energy of space forms the gravitational energy gradient through an increasing ratio of potential energy to kinetic energy of space inward toward system center or the center of gravity. So space possesses a greater ratio of kinetic to potential energy away from the center of gravity, and a greater ratio of potential to kinetic energy nearer and nearer to the center of gravity.
Recall that the potential energy of space is the energy composing the basic 1-D bidirectional units of the energy of space. The kinetic energy of space consists of the rate of motion of the basic 1-D units of the energy of space relative to each other, and possibly the degree of randomness and distribution of the basic 1-D units of energy relative to each other as well. Since there is less kinetic energy of space and more potential energy of space nearer and nearer to the center of gravity, there is less kinetic energy for electromagnetic (e-m) interactions. As a result, the closer to the center of gravity, the slower the rate of e-m interactions. Since time energy is produced with each e-m interaction, the closer to the center of gravity, the slower the rate of time (see Gravitational energy gradient).
The inherent energy of space forms a gravitational energy gradient to provide directional balance to the gradient formed by a body of mass-energy. This means that the inherent energy of space should be able to provide optimal directional balance to the body of mass once the total energy of the gravitational energy gradient is equal to the body of mass for which it is providing directional balance. And this means that the gravitational energy gradient is finite. And this has a lot of implications for the physical world.
For example, the gravitational gradient of the earth only extends outward until it possesses the same total energy as that of the earth. Then it extends no further. Beyond that range, the earth’s gravitational energy gradient can only interact with bodies of mass with gravitational energy gradients that extend into the earth’s gravitational energy gradient.
Of course, the gravitational energy gradient of our sun extends at least outward to the boundaries of our solar system. On the other hand, bodies of mass at the outer edges of our solar system possess gravitational energy gradients that do not extend to the sun. It is the gravitational energy gradient of the sun that holds the entire solar system in place and defines the outer boundaries of our solar system.
In the case of elementary 2-D electromagnetic energy systems, such as electrons, the gravitational energy gradient is also finite. However, the motion of the 2-D electromagnetic energy relative to system center goes through a series of phases similar to a wave. The 2-D electric energy moves from high energy level to low energy level and then back to high energy level (see Electron structure). As it does, the gravitational energy gradient changes its strength. When the 2-D electric energy is at its highest energy level, it is at its greatest energy density. At this point, the gravitational energy gradient is the strongest. When the 2-D electric energy moves outward toward a lower energy level with less and less density, the gravitational energy gradient becomes weaker and weaker. The oscillation of the 2-D gravitational energy gradient strength through the phases of the 2-D electromagnetic interaction produces an outward force or pulsation. This force caused by the changing strength of the 2-D gravitational energy gradient composes the “charge” field.
This means that the “charge” field of an elementary “charged” particle is finite since it is caused by the changing strength of a gravitational energy gradient throughout an electromagnetic interaction.