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CONFIGURATIONS IN A THREE DIMENSIONAL RANDOM FIELD
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CONFIGURATION
GENERATION
DECAY
BEHAVIOR
Spiral Configurations   Field noise
Inside-shelled spiral (ISS) Generated by a single field wave entering a radial array
Generated as a decay product
Annihilation products  
Outside-shelled spiral (OSS) Generated by a single field wave entering a radial array
Generated as a decay product
Annihilation products Persistent motion through the field
Radial configuration, also known as a dual-wave configuration. Generated by simultaneous entry of two waves into a radial array.
Generated by two spiral configurations merging from parallel reversed polarity layers.
Decay
Decay products
The inside-shelled spiral as a decay product
The outside-shelled spiral as a decay product
 
  Spiral configuration and radial configuration stability
Field density enhancement and radial stability
Radial stability
Axial stability
 

SPIRAL CONFIGURATIONS

    After achieving orbit around a spiral array, simple wave winds a spiral configuration so tight, that its spiral surfaces are all nearly touching (approaching zero separation) either along an interior shell:

or an exterior shell:

    For any wave having fallen into orbit around a spiral array, the field surfaces it undergoes interchange with, will be displaced in the direction of its travel, inexorably being drawn into a spiral.   As this wave wraps the field tighter and tighter around the spiral array, it will no longer strike the surfaces ahead at its center, but rather displaced from its wave center towards its orbital center.   As the field tightens, this striking point moves closer and closer to the wave's edge, where the magnitude of the wave's distribution of motion becomes less and less.
    Eventually, as this continues, the wave will encounter surfaces actually moving against it with greater displacement magnitudes;  essentialy field noise.  When this happens, interchange with these surfaces will reverse its direction;  halting the wave in this position.  Field surfaces still moving forward will begin to saturate this region, forming a narrow shell of high surface density;  the simple wave now caught in the embrace of field noise.
    Unable to move forward or backward, the spiral winding becomes locked;  unable to wind tighter or unwind.

    Once such stability is achieved, the orientation of those surfaces caught as spirals remains constant relative to any ray struck from what is believed to be the best center for the spiral configuration and is dependent to their distance from center where they cross this ray.   Conversely, any lateral impulses direct against the spiral at this crossing point between ray and spiral will have a fixed redirection relative to their direction at this crossing point, at the spiral center.
    To the observer, there are two classes of spirals, an inside-shelled spiral and an outside-shelled spiral.
    This first spiral, randomly occurring, as a result of these rather accidental causal conditions of the field, is an inside-shelled spiral.   The outside-shelled spiral achieves standing wave conditions on its outermost edges, and generally occurs as a decay product.
    One thing to note. Other ambient field surfaces which might wander into this region can also be trapped by this mechanism, thereby increasing the array's density to greater than the general field, more or less stealing surfaces from the field and increasing the array's density to greater than that of the field.   As a matter of probability, the rotating wave wave's frequency of interaction with individual surfaces throughout each revolution diminishes as more and more surfaces become part of the array, giving each existing radial a better chance to break free, thus maintaining the array at a saturated maximum.
    If this single wave manages to once get around the newly forming array, it is virtually assured of doing so again and again.
    Each time it undergoes interchange with a radial, it will leave it slightly advanced at the wave center, and as this occurs on average, every other orbit, the radial will become twisted, causing the inner core to rotate, and eventually, after many repeated transits, twist the radials into spirals. All the time this is happening, the wave itself will follow a slowly spiraling outward progression, as its orbital radius increases with each revolution.
    As more surfaces are captured and brought into the array, and spiral curvature increases, at a certain distance from the now spiral center (the radial array having evolved into a spiral array) causing a shell to form. At this shell, all of the spirals exit and enter the radial core, which means that there are twice as many penetrations of the shell, than there are surfaces captured by the spiral. Besides this, the angle of slant is the shallowest than anywhere else on a spiral; the greatest concentration of surfaces found here.
    With each new orbital transit the spiral become tighter and tighter, eventually causing the spiral shell to encroach against the outermost limits of the waves motion, causing the point of non-definity to migrate outward to the outside edges of each wave, where interchange takes place. Because of the extreme density, as the spirals become tighter and tighter, the wave no longer needing to move forward, since any slightest movement in this densely packed zone, from any surface and from any direction will cause interchange. It is at this point, the meager forward motion of the original wave, is overcome by the ambient field motion; its wave motion no longer being a dominant movement of the spiral array. It is at this exact moment, the spiral array is about to become a permanent member of the field:  a spiral field configuration. When this happens, the wave has reached the limit of its rotation; it becomes a standing wave; sometimes moving forward ever so slightly, and then back ever so slightly, stabilizing the spiral configuration into what is called an inside-shelled sprial configuration.

THE INSIDE-SHELLED SPIRAL CONFIGURATION

DESCRIPTION
SHAPE:  TOROIDAL 
OCCURRENCE 1:  GENERATED BY A SIMPLE FIELD WAVE 
OCCURRENCE 2:  THROUGH RADIAL DECAY 

FIELD GENERATION OF THE INSIDE-SHELLED SPIRAL

  Anywhere within the field, within any polarized region, a simple field wave will have eventually encountered a radial order of the field and those conditions allowing it to spiral the field into a spiral array, and then into a spiral configuration.
    Here we see a simple wave l depicted as assuming two opposite-handed orbits as it curls in opposite directions along a flat plane (subjective).   The flat plane may have any orientation in the field.  The chance that it will assume one of these two possible directions is is equivalent and most likely slightly less than 0.5 for either.  This probability is based upon a finite overview of these activities where the wave may approach the center of the radial order head on or from one side or the other.
    Head on, there is the possibility that the wave will emerge from the radial order without deflection.  Approaching to the left of center will produce a clockwise orbit and from the right will produce a counterclockwise orbit, each of equivalent possibility.
    By convention, using the left-hand rule with the index finger pointing in the simple wave's pre-orbital direction, the thumb points in the NORTH polar direction.  For either possibility, if this NORTH polar direction points in the positive direction of any axis of a left-hand Cartesian coordinate frame of reference, then the radial order of the field will become a positive normal-spiral configuration.
    If the NORTH polar direction points in the direction of the negative direction of any axis, then the radial order of the field will become a negative anti-spiral configuration.
    Once a spiral configuration is established, it will progressively match the orthonormal orientation of the group of spiral configurations within any finite region of the field, its plane of origination no longer a factor.
    During the initial stages of winding the field, the simple wave in orbit will progressively encounter radial surfaces closer together to the interior of its orbit, than to the outside, causing it to undergo interchange more frequently to the interior.
    As the array evolves into a configuration, these distances diminish not only because of the basic geometry of radial surfaces, which are now becoming spiraled, thus being more appropriately referred to as spiral surfaces, but because more and more surfaces are being captured and held by the configuration, increasing its core density.
    Eventually these distances become so small, the wave edge becomes buffeted by field noise, bringing further advance by the wave to a halt, resulting in a standing wave on its inside edge, resulting in an inside-shelled spiral.
    For these same mechanisms to come into play on the outside edge of the wave, would require great luck to overcome to overcome the more natural development of an inside-shelled spiral configuration, and therefor outside-shelled spirals are not seen to develop strictly from field origination.

GENERATED AS A DECAY PRODUCT

  When a dual-wave radial undergoes polar dissociation, two opposite charged spirals are generated, one being an ISS and the other an OSS. [REFERENCE]

ANNIHILATION PRODUCTS

    If two opposite charged ISSs are drawn together by virtue of their residing on the same plane [REFERENCE], they will unwrap each others respective field, releasing two independent simple waves back into the field which will travel along the same orbital plane they each enjoyed as part of these spirals.

THE OUTSIDE-SHELLED SPIRAL

DESCRIPTION
SHAPE:  TOROIDAL 
LIMITED OCCURRENCE:   THROUGH RADIAL DECAY 

FIELD GENERATION OF THE OUTSIDE-SHELLED SPIRAL

  Unlikely. [REFERENCE]

GENERATED AS A DECAY PRODUCT

    An OSS is a paired decay product with an ISS.  In each pair, the decay products are of opposite charge.  There are two pairs of decay products.  The orientation of each decay product remains the same as prior to decay. [REFERENCE]

ANNIHILATION PRODUCTS

    If two opposite charged OSSs are drawn together by virtue of their residing on the same plane [REFERENCE], they will unwrap each others respective field, releasing two independent simple waves back into the field which will travel along the same orbital plane they each enjoyed as part of these spirals.

PERSISTENT MOTION

    Frontals which encounter an OSS will experience IDDI such that the shell is caused to move forward against the approaching frontal.  Specifically what happens is that IDDI causes both frontal and the first surface it meets belonging to the shell to strike a mean position, essentially moving that surface forward.  Because of the close proximity of many surfaces belonging to the shell and noise, IDDI is occurring everywhere around the shell, thus this specific IDDI which occurs in contact with the frontal, can never make its way around to the backside of the shell, being neutralized by the many other IDDIs which are also occurring, which, if not neutralized, would cause the shell to move backwards.
    A frontal is a termed for independent field surfaces in relative motion towards the OSS.

MOTION OF THE CORE AND SHELL

    In this next illustration we see an approaching field surface or the motion of the array through the field.  The orange surface represents a spiral surface associated with the array.  This surface extends an infinite distance away from the finite array.  It also passes either around the shell or through the central spiral core, where within, lies the standing wave causing all of this to happen.  This orange surface is typical of all surfaces passing through the array from all directions around the orbital plane.

    The shell thickness is finite.  Inside the shell, which is densely packed with surfaces relative to the ambient field, the usual processes of collision, interchange, IDDI and intersection occur.  Here, the separation between surfaces approaches zero, thus all displacements affecting the array from the outside field, such as field noise or lateral displacements due to IDDI between other arrays, is greatly attenuated, approaching zero magnitude.  A finite and instantaneous displacement relative to any surface entering the shell, though now very small, will be shared by many more surfaces already inside the shell.  Wherever a spiral joins the shell, so-to-speak its entry point, its lateral displacement will circle the shell
    Inside the shell, the continuity of surfaces is fragmented.  This is why the orange surface is shown as dashed inside the shell;  it being a composite of the many surfaces there.  The approaching field surface as if conforms to the array's surface, can find itself situated in a difficult condition, as it arrives at location X, and must form a discontinuous cusp in order to continue conforming.  Location X is technically at the edge and inside the shell where a myriad surfaces can connect to either end of the conformed field surface at X, allowing the otherwise potentially discontinuous field surface to remain continuous.  Of course, the free loose end of the other surface will marry another field surface.  This is a random interchange process.
    One might assume that if the shell were caused to move within the field, the core would automatically follow, but this is not the case.  There is no specific mechanism which can make this happen.
    Any action of this finite array must be correlated to the field surfaces all around.  If a field surface causes the displacement of any spiral associated with a shell, the displacement will become attenuated, so that its magnitude cannot exceed the distance between surfaces belonging to the shell.  This displacement will also find itself everywhere at once throughout the shell surfaces, even emerging outside the shell as this same surface rejoins the ambient field.  This displacement, attenuated as such, will also undergo translation to many other surfaces in the shell.  In reference to the following illustration, this original displacement is shown as an orange downward facing vector to the left of the array.  The black dashed line is the distribution of motion associated with this particular vector.  Notice how it automatically undergoes attenuation as it enters the shell at the top.

    By tracing the direction of this displacement relative to the surface, many other vectors, all of now equal magnitude, may be drawn in relation to this surface as it it wraps around the shell and through the central core.  Notice how this displacement cancels between layers (black vector pairs circled), except on two transition layers;  one entering the core at the top, and the other last layer on the bottom outside.  These two vectors are shown in orange;  representing they residual displacement under these conditions, associated with the original displacement.
    What this means is that all displacement caused to happen against an outside-shelled spiral produces a uniform displacement, greatly attenuated and directed orthogonal to the shell at that surfaces entry point.  This one mechanism, accounts for the interaction between two or more spiral arrays, which produces an impulse equivalency to electrostatic charge, causing like spiral arrays to repel and unlike spiral arrays to attract.
    Regardless of the number of interior shell layers, cancellation of pairs always occurs.
    Another behavior illustrated is the approach of ambient field surfaces, shown as green and descending onto the array from above.   This condition may be viewed in two ways:  either the array is at rest, and field surfaces move through it, or the field is at rest, and the array is moving through them, the latter being more likely.  In any case, interchange between it and spirals associated with the array will most likely occur at location A, as this ambient field line contacts the shell, or at B.  Resultant displacement of the array's spiral will be upward at location A, causing the outermost shell surface to move upward, outward to each side, and downward at the bottom, which to some degree may cancel any overall displacement of the array.  I am uncertain as to whether or not this impact region (A) has any pronounced effect.  However, impact at region B will have a definite effect driving the array upward.
    What this means is, an outside-shelled spiral, once impacted by ambient field surfaces, having undergone conforming or not, will tend to move in the direction against the direction of these ambient field surfaces, thus causing the array to continually move through the field, once set in motion.

THE RADIAL CONFIGURATION OR DUAL-WAVE RADIAL

DESCRIPTION
SHAPE:  OBLATE SPHEROID 
OCCURRENCE 1:   SIMULTANEOUS SIMPLE FIELD WAVES
OCCURRENCE 2:   TWO INSIDE-SHELLED SPIRALS MERGING 

FIELD GENERATION OF THE RADIAL CONFIGURATION

    Another class of configurations, called a radial configuration, evolves from a purely radial array consisting of two waves, rather than one, traveling in opposite directions. Because two waves must enter a radial field virtually simultaneously, the odds of occurrence of this configuration must be substantially less than for a spiral configuration, where only one wave is required for its formation.
        Besides one having one wave, and the other two waves, there are several other significant differences between these two configurations.
    In the case of two waves orbiting around a common radial center, no winding of the field occurs; each wave nicely offsetting the forward displacement of radials caused by the opposing wave. Just as with the spiral configuration, field surfaces are caught and trapped by the same mechanism as before, causing the density of field surfaces within the configuration to rise above the normal ambient field density, until a certain maximum is reached. As mentioned before, this mechanism is called radial restoration.
     Another difference between a spiral configuration and a radial configuration is that a radial configuration is not permanent, eventually decaying, because, unlike the spiral configuration, no standing wave conditions develop. Instead, because of the radial field, both counter rotating waves follow a gradually enlarging spiral path, ultimately causing dissipation of the radial configuration.
    The waves forming a radial configuration do not need to be exactly alike, but may vary in wave size and speed, as well as angle of entryinto the radial field, nor do both need to arrive at exactly the same moment. Once engaged in mutual counter rotation, despite speed variation, the faster moving wave will tend to twist the field, since it gets around more times in the same time.
    By so doing, the faster moving wave will wrap the field in the direction of its passage. The slower and opposite moving wave encountering these slightly spiraled radials, because orthogonal redirection, will take a tack inward. Because it is now traveling along a smaller orbital radius, the slower wave, though not moving any faster than before, is now completing its revolution a little bit more quickly. If its period matches the faster wave, each wave will perfectly offset the forward advancement of radials caused by the other wave, and no further spiraling of radials will occur.
    Besides undergoing change in its orbital radius, the slower wave, as it moves closer to center, will face a predominance of convex radials, and thus become smaller, allowing it to move closer to center than it otherwise would be able if its wave size had not diminished.
    The reverse of this process also occurs. If the outermost wave's period is too long, allowing the innermost wave to wrap radials, the innermost wave will tend to move away from center.
    This process which is not purported to be perfect, probably does not allow perfectly stable orbits, but instead a yo-yoing so-to-speak, or weaving of wave orbits, of the two waves.
    The radial configuration, also called a dual wave configuration, is formed much in the same way as an outside-shelled spiral, except in its case, two waves, rather than only one, are involved; moving in counter rotation. Though both waves do not need to be exactly alike, they should at least be sufficiently similar in order to provide identical, or nearly identical periods of rotation as they orbit around the radial center. If this happens, spiraling cannot occur, because the counter rotational passage of each wave will neutralize the field spiraling caused by the other wave. In other words, though one wave in its passage will start to wrap the field into a spiral, the other wave, coming from the opposite direction will unwrap the field, and vice versa. As is suggested, the field surrounding a radial configuration, by virtue of its mutually restorative counter rotating waves, remains radial.

    As a direct consequence of this, no shell is formed, and standing waves will not develop. Instead, both waves will continue to orbit around the radial center with progressively larger and larger orbits. This is true by virtue of the nature of orthogonal wave propagation from surface to surface; each wave describing a segmented path from one radial to the next, until eventually the waves begin to encroach upon the ambient, random field which surrounds the configuration. Once reaching this portion of the field containing fewer and fewer radials belonging to the configuration itself, the waves dissociate from the radial configuration, causing its decay.

THE RADIAL CONFIGURATION GENERATED BY THE MERGING OF TWO UNLIKE SPIRALS

    Two unlike spirals normally reside on opposite layers and will at moments be in near polar colinearity with each other.  Under these conditions they will axially repel. [REFERENCE] They will also under these conditions be in close radial proximity and radial attract.  [REFERENCE]
    If they succeed in radial attraction, they will undergo annihilation by virtue that their respective opposite wound spiral surfaces will quickly unwind, generating a radial array, releasing two simple waves back into the field, each directed coplanar to their originating layer.  Accordingly, it is unlikely that a dual wave radial configuration might result.
    If despite axial repulsion, if both spirals move exceedingly close to each other, nearly common to the same plane and axially aligned, both axial and radial restorative impulses could come into play, keeping both waves in opposite rotation about a nearly common axis and plane of rotation.  If these conditions were met, with their passage in orbit, each will displace the others winding, eventually unwinding the field altogether, generating a dual-wave radial configuration.
    After some the radial configuration will undergo decay. [REFERENCE]

RADIAL DECAY

    After having made about 1.85 x 1026 orbital revolutions, both waves begin to encroach upon the surrounding field and undergo interchange with ambient field surfaces not belonging to the radial order, causing their paths to become erratic and zig-zagged, increasing their orbital periods. This can happen very quickly to the outermost wave, causing it to take languishing orbits in respect to the innermost wave, which begins to spiral the field.
    If the spiraling is moderate and the differential in periods not too great, the outermost wave will compensate by striking a closer orbit to center, in turn shortening its orbital radius and period to less than that of the other wave, which then follows a outward spiraling orbit, achieving an orbital radius now greater than the other wave. This is of course all a matter of geometry where both waves merely follow the orthogonal re-direction as they undergo interchange with subsequent radials and field surfaces. In so doing, the field becomes wrapped in the opposite direction. Of course, nothing is perfect, the outermost wave overcompensating and achieving a smaller orbit than the other wave, thus reversing conditions with the other wave now following the greater orbit.
    Since there is nothing governing orbital parity between both waves, presumably this trade-off between waves occurs throughout their orbital passage, causing an oscillation of sorts: first one wave taking the closest orbit and wrapping the field, thus driving the other wave closer to center, and then the other wave taking the closer orbit and wrapping the radial field in the other direction.
    Once however, one of the waves seriously intrudes into the ambient field, recovery to equilibrium once enjoyed becomes more difficult, to the extent, that expedient re-entry into the configuration's array is denied.
    During this yo-yoing of counter rotating waves, each wave experiences a change in its wave size depending upon whether it is passing through a series of concave or convex surfaces, a condition set up by the opposite wave as it wraps the radials. A cursory examination indicates that the wave which is moving outward from center, in contrast to the outer wave which is moving in, as they trade positions, encounters a series of predominantly concave radials which causes its wave size to increase. The other wave, conversely, encounters more convex radials, causing its wave size to become smaller. This is good, since it allows a closer approach to the radial core of the incoming wave, which, by virtue of it becoming smaller, is less likely to overlap the interior core.
    Presumably as this whole process continues, and more and more ambient surfaces become involved, the two orbiting waves comprising and holding the radial configuration together, make one last gasp excursion as a pair; the outermost wave virtual dissociating itself from the central core and from the other wave. This allows the innermost wave to begin to severely wrap the radials, ultimately stabilizing the configuration, now minus one of its waves, into a permanent outside-shelled spiral configuration.
    During their last oscillatory swing, both waves undergo drastic changes in size, with the wave heading towards center always becoming smaller, and the wave ending up on the outside, larger. This phase is called pre dissociation.
    Final dissociation between waves occurs as an axial shift to either side of the innermost and smaller wave's orbital plane. This is an imaginary plane which remains coincident to the configuration's center and the center of the orbiting wave. Since the waves rotate in opposite directions around a common axis, a repulsive polar force comes into play, driving both waves farther and farther away from each other. This phase marks polar dissociation, shortly following on the heels of pre dissociation.
    After polar dissociation, both waves wrap their respective radials into left-hand and right-hand spirals, as the case may be. The smaller, and remaining innermost wave of the radial configuration, now having the shortest orbital period, is the first to create a shell and evolve into a stable standing wave. The outermost wave, having moved some distance away, begins to exert its own influence on the field by wrapping field surfaces it captures, into a reverse spiral.
     Generally, in the formation of the shell, there is a greater likelihood that an outside-shell will be formed, rather than an inside-shell. Consequently, the smaller wave will form an outside-shell. This is also true for spiral configurations which are not radial configuration byproduct, but otherwise randomly occur throughout the field.
    During actual decay of this configuration, when one or the other of its two waves eventually spirals too far away from the configuration's orbital center, causing it to slow down in period even more as it begins to encounter ambient field surfaces, the instability of orbital period becomes very severe. Just before decay, which is technically the dissociation of these two waves from each other, thus dissipating the radial configuration, they are thought to widely gyrate; first one becoming the innermost wave and rapidly winding the field, and then the other, until eventually one or the other, which ever happens to be the furthest out, leaves the whole assemblage, leaving the innermost wave behind in an already greatly spiraled field.
    Thus as each wave passes the other, it strikes out on a path more closely following the other.  This restores each wave to a common orbital distance from the radial center.  This process goes on indefinitely with each passage, producing a momentarily stable radial configuration, whose waves progressively and together move outward from the radial center.

Two waves in stable orbit slowly spiraling outward
from center, forming a radial configuration.
    In time, one wave or the other will encroach upon the ambient field causing an indirect passage around the radial.
   When this happens, the innermost wave is able to orbit faster, causing the field to twist in its direction.  This produces a yo-yoing effect, where both waves alternately assume the greater orbit and then the smaller orbit;  the wave closest to center spiraling the field in its direction.

    As these waves move from an inner to an outer position and visa versa, their wave diameters also change.

      Eventually one wave or the other will end up in the smallest orbit, and permanently begin to wrap the field in its direction.

 Then the other wave will drive towards it in a counterclockwise direction.  Both waves will now be following different orbital distances around a common center, forming a shell of surfaces so tightly wrapped, they are virtually parallel and touching.  Under these new conditions, the wave in smaller orbit will momentarily stabilize as a standing wave, shortly thereafter, followed by the outermost wave.

     This new intermediate array above, designated as A1, principally generated by wave l1, also inclusive of wave l2, is not a stable configuration, but a momentary and intermediate array.  At this phase, only wave l2 produces a spiral field.  Using the left-hand rule, the spiral field produced by wave l2 is a positive electrostatic field.
    Both waves enjoy a common center inside a common shell.  This relationship though is subject to random influences which might drive apart these common centers, and no particular mechanism keeping them together.

DECAY PRODUCTS

    Just as elementary particles in the real world demonstrate a sundry decay schemes, these geometric arrays also undergo a variety of phases, some of which might be fleeting, if there was time, some of which are momentary, and some of which are stable, again, the notion of time having not been introduced at this level.
    The first of these arrays arises spontaneously from the field in the presence of two simple waves (the photon equivalent) which begin to orbit around an imaginary, common axis in opposite directions.  As these two waves continue to counter rotate, more and more field surfaces are attracted to their central core, greatly increasing its density to over three times the normal field density, so it is estimated.
    This array, initially referred to as a dual wave radial configuration is a single axis array demonstrating a sedentary behavior and a long range attractive mechanism between other arrays.  There are two types (I and II).

    Eventually either of these two types of this array will decay into an intermediate and unstable array, of which there are two types:  A and B.

    Once in this phase, in either case, the two counter rotating waves have both twisted the field in opposite directions between them, generating a shell of closely packed surfaces, which is continually wound by the innermost wave until it reaches standing wave conditions.  If both of these arrays were displaced from each other along their common axis, because of their spiral structures, they would repel each other along their polar axis, leading them to a phase of planar dissociation.
Shortly thereafter, the dynamic outside-shelled spiral (OSS) will move laterally away from its old axis shared with the inside-shelled spiral (ISS) and find its way near the orbital plane of the the other array by virtue of the attractive (also repulsive) radial mechanism associated with spiral configurations.   When this happens, both arrays have become much more independent from each other;  essential becoming two axial independent spiral configurations held in association by long range field mechanisms.
   Up to this point, we have been dealing with the decay and subsequent phases of a single dual wave radial configuration, rather than three such configurations combined as a single configuration comprising three orthogonal dual wave radials.
    If all three radial configurations belonging to one orthogonal configuration decay at the same moment, or nearly so, the three sedentary ISSs, consisting of l1s may remain in conjunction with each other, forming a sedentary ISS configuration consisting of three standing waves in orthogonal orbits.  This three orthogonal wave ISS is called an TRION.  The three OSSs consisting of l2s initially remain in separate orbits, traveling around the ISS TRION.

    Eventually it is expected, these should migrate together into one orbit because of the attraction of radial arrays explained earlier, forming a TRION.
    Though the notion of a spherical orbit has not been introduced, it may now be anticipated, its radius is in part governed by close range geometric repulsion relative to each orthogonal orbital plane, keeping these two TRIONS associated.

    Given three TRIONS as illustrated, it is possible for two opposite spiraled TRIONS to draw close together, since they can move in any direction, especially in the case of two OSS TRIONS.
    Here, two TRIONS move closer together because of IDDI and because of their radial attraction.

    The following illustration shows this relationship in more detail.  Only certain spirals emanating from the negative TRION may interact with spirals coming from the positive TRION, which collectively drive the negative TRION in the direction shown;  the many short blue vectors showing the magnitude and direction of the many discrete impulses generated by the IDDIs occurring in greater frequency in certain areas, and the lighter blue vector showing the resultant motion of the TRION, driving it towards the positive TRION.
    The green dot represents the direction an object will travel, such as a simple wave, in the presence of a spiral field, which if to the right drives closer to the spiral center, and to the left, drives away from center.


 

ADVANCED NOTES

ANNIHILATION COUPLES

    If two unlike spirals collide and merge, in this case as show, two OSSs, the shell will unwind and breakdown between the two, allowing both opposite directed waves to unwind the remaining two shells, thus leading to the annihilation of both spirals.

    Because of this end result, these two spirals represent an annihilation couple.
    Annihilation couples must have reversed spirals and include both ISS and OSS.  Of these, single wave spirals are the most likely to experience this, because they are stable arrays, and intermediate two wave spirals having a lesser chance because they are not stable arrays.  Given four possible spirals to chose, both ISS and OSSs may interact and undergo annihilation.

DECAY PRODUCTS

     If the larger and outer wave were unaffected by the presence of the smaller and innermost wave, it too would most likely form an outside-shell. If however, during the rapid development of the inner waves outside-shell, and the still relative close proximity of both waves to each other, the shell formed will be grazed by the edges of both waves, which not only sets up conditions for a standing wave of the innermost wave, but as well a standing wave for the outermost wave, in which case, the innermost fringes of the outer wave just touch this shell already formed by the innermost wave. Simultaneous to this, polar repulsion is taking effect, causing both newly form spiral configurations to slide away from each other along their polar axis. This is the final dissociative step called polar or axial dissociation.

THE INSIDE-SHELLED SPIRAL AS A DECAY PRODUCT

    One might say, that in a quick snap, though now dissociated, both waves continue on to form two independent spiral configurations.
    In the case of the innermost wave at the time of dissociation, it is thought to evolve into an outside-shelled spiral configuration; similar to an outside-shelled configuration accidentally occurring spontaneously from the field.
    The outermost wave is seen to favor evolution into an inside-shelled spiral, which achieves standing wave conditions at the innermost edges of the wave, thus allowing it to achieve stability and permanence.
    These two new spiral configurations, as byproducts of radial configurations, of course have opposite spiraling; based upon the direction of travel of their respective waves before dissociation. As convention relative to the observer, spiral configurations comprising a clockwise orbiting wave are called right-hand spirals and spiral configurations comprising a counterclockwise rotating wave are called a left-hand spirals.
    Given these possible combinations, a radial configuration can decay into either a pair of spiral configurations consisting of a right-hand outside-shelled spiral and a left-hand inside-shelled spiral or a left-hand outside-shelled spiral and a right-hand inside-shelled spiral; the outcome of either being random.

THE OUTSIDE-SHELLED SPIRAL AS A DECAY PRODUCT

FIELD NOISE

Field noise is merely a term for the activity within a field caused by the presence of simple waves.  It varies in both wavelength and displacement magnitude.
  In the broadest sense, noise is the presence of the smallest and least energetic system waves permeating their local system region, and it is this noise which governs the degree of spiraling, which, if their was no noise at all, spirals would wind up indefinitely, and if the noise level was not constant, neither would be the electrostatic charge.
     In general, Coulomb's law is dependent upon and governed by spurious and ambient waves in the vicinity of a spiral array, as a direct consequence of their frequency, size and amplitude.

SPIRAL CONFIGURATION AND RADIAL CONFIGURATION STABILITY

INITIAL FIELD ENHANCEMENT AND RADIAL STABILITY

    Since all surfaces associated to this radial order are moving and not glued to it, each and all will eventually dissociate themselves from it. Each time though this wave circulates around the radial center, it will displace surfaces slightly forwards relative to its forward motion and their original positions. But depending upon the orientation of field surfaces in proximity to the radial order, some will escape interchange simply because the wave is cutting through them at too steep an angle such that it can never bulge into them at a point of non-definity, but rather otherwise intersect them well outside the wave diameter, thus disallowing the possibility of touching without intersecting. This is illustrated showing the wave at position b unable to make contact by simply touching without intersecting; which is essential if a point of non-definity is to occur. In this same illustration, both waves at position a and c can undergo interchange with other field waves

associated with the radial. In the case of the wave at position a, all field surfaces parallel to the line x (shown horizontal) and lying between line a and line x will be driven back towards line x because of IDDI, whereas none lying above line a will undergo interchange. This remains true as the wave continues to move clockwise passing through position b and on to position c. As the wave moves between positions a and c, interchange cannot occur. On the same token, at position b, as the wave drops down towards line x, interchange can occur, driving surfaces upwards. This of course is not conducive in maintaining radial cohesion, but rather defeating it. Fortunately though, on the other side, the wave operates in a much large zone, causing the surfaces to be driven back towards center, the net result, more times the waves will be driven towards center than away. This is true for all reference orientations of line x, as well as for waves traveling counterclockwise. Cosmic glue in this sense, is all a matter of geometry!
 

AXIAL STABILITY

    In the case of two waves, one might ask, what keeps these waves rotating near each other? What keeps them from wandering off? Certainly radial restorative mechanism has little to do with this, since it provides only axial cohesiveness.
    In order to visualize this mechanism, maintaining both counter rotating waves orbiting near or on the same plane, we must view the radial configuration from the side.

    In this illustration, the radial configuration seen from the side, let's assume both waves to be slightly displaced from each other. In other words, their orbital planes are not coplanar. As each wave moves forward, it moves through the field set up by the other wave in its passage; a field where each surface is angled, such that its orthogonal redirection deflects its passage towards the plane of the other wave, thus both waves are driven towards the common ground lying between their orbital planes. It does not matter which side which wave is on, in either case both waves are deflected inward towards the middle.  This is called axial restoration of counter rotating waves, and directly relates to magnetic properties.

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