In fundamental physics, we are taught, that "force" equals, "mass times acceleration."
Now; Imagine a level of "force," that is here to work to involve a Ward-Cauchy-Related case scenario, as in the superstring-related realm, that is tantamount, to being potentially below the mass-bearing level. Consider the analogous replacement for mass here, to be the phenomenology of "metric-gauge." Next; Consider the analogous acceleration to be utilized, to be the initial spontaneous altering rate of dispersion, of a distinct set of metric-gauge-related eigenstates of homotopy.Thereby; The "thrust" of such a mentioned set, of a respective given arbitrary group of metric-gauge-related eigenstates, may be considered here, to be the product that is to be present here, between the correlative net metric-gauge eigenstate, WITH, the directly associated accelerative dispersion of homotopy. "Strain" may be thought of, as a form of "pressure." Reductional pressure, is "force per area." The analogous regional "area,"at which such a dispersion of homotopy is to be enacted upon, may be physically represented, as the product that is to exist, between the inferred Lagrangian-Based-Trace -- which would here be parametrically localized, at the covariant trivially isometric positioning, of which is to literally be delineated in a Laplacian-Related manner, at the projected covariant co-differentiable co-determinable "spot," upon which such a stated "thrust" of metric-gauge-related homotopy, is to be tugged away from, as taken at its initial region of formative iteration -- AS MULTIPLIED BY THE STOKE'S-BASED PARAMETERIZATION, (to where the just stated/inferred product of such, may be perceived of, as being the Hamiltonian Operand, upon which such a dispersion-related thrust of homotopy is to "directly" come into contact with, in so as to facilitate the initially needed gauged-action to be able to occur), so that, WHEN THIS IS HERE TO BE INVERSELY COUPLED WITH the physical delineation-related world-sheet-based region-bearing eigenstate of "force," at which such an ensuing "thrust"of homotopy-related dispersion is to be formed, the resultant physical phenomenology, may therefore potentially work to help facilitate the effectual physical attributes, of that general physically consequentially formed "strain" that is needed, in so as to help to allow, for the subsequently permissible formation of those cohomology-related generation/de-generation modes, that are here to be related to those needed characteristics of electromotive charge, that are here to perpetually be existent at this level. TO BE CONTINUED! SINCERELY, SAMUEL DAVID ROACH. (1989).
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