Wednesday, March 30, 2016

As To The Poisson Integral

When one is to have two adjacent waves, that are being physically delineated in a common manner of holomorphicity -- then, one is to then be able to integrate the phase exchanges that are to here exist among the two said waves -- in so as to form a Laplacian-based potential overlapping of the topological holonomic substrate of the phenomenology of the two said wave-based patterns, when in terms of the mappable tracing of the entity that may be utilized here, in so as to be an extrapolation of as to how the two said waves are to here then be made in equivalence to each other.  Such a so-stated integral, that I have just here described, in so as to make the two said adjacent waves of a common holomorphicity, equal -- is a manner as to here working to describe what may be called in general, a respective given arbitrary example of what acts here as the Poisson Integral. Next, consider with me an example as to there being the arbitrary existence of two different Njenhuis waves, that are adjacent, yet, are moving in a common manner of holomorphicity, in one manner or another.  Let us say that one were to then utilize an Imaginary-number-based integration of the phase exchange that is to here exist among the two waves, that I have just mentioned in this second so-stated example, in the substringular.  Let us here consider in this given arbitrary case, that the Imaginary-number-based integration of the said phase exchange that I have just mentioned here, is to make the two so-stated waves of this second said example, to then be of the same Laplacian-based topological-based stratum of holonomic substrate of wave-based phenomenology.  One may then call this second so-stated integration of phase exchange, to be a usage of what may be called a Njenhuis-based Poisson Integration.  Such a Njenhuis-based Poisson Integral may be extrapolatable, when in terms of working to determine a mean field oscillation -- that would exist as a common ground between two waves of two respective different universal settings.  The field density of such a common wave-based stratum -- that would here work to strattle between two different universal settings -- would then tend to work to bear a Li-Algebra-based Rarita-Index, that would work to bear a set of complex Gaussian roots -- in so as to form an interdependence of the predominant universal setting of such a given respective case scenario, with the less predominant universal setting of this self-same case scenario.
I will continue with the suspense later!  To Be Continued!  Sincerely, Samuel David Roach.

No comments: