Moon’s
orbital motion.
Values
of analysis:
Moons’ 8th level analyze
inputs and convert them in information following this priority of analysis:
first volumetric value, then time frequency. The dissolving
of the spherical 8th level transferred the analysis department
inside the c/channel: the three spheres next to their 7th level:
each of them analyzed the PRV of the flux of aspheres for each (Moon) motion of
pressure.
Their difference are:
·
volumetric value: gets simultaneously
produced/evaluated. It absorbs volumetric SU in it: do not consider it.
·
time/frequency (t/f): can’t be
simultaneously produced/evaluated out of one value, but after having analyzed
the second asphere, making the field installing a memory on it: it always
avoids it, unless become the only possible reference of analysis. It doesn’t
absorb volumetric SU into the analysis/evaluation generating the
exact extent of the volumetric value unit.
The afields velocity, getting
produced by the constant s/pressure it’s a value not changeable. In ordinary
condition get used only as confirmation of PRV.
In state of constancy, the three spheres adopt
the analysis of the volumetric value also for t/f (direct proportionality SV /
vv as volume/velocity), becoming the main value of analysis.
The aspheres getting
through the c/axis of the spheres of the Planet c/channel generate a m/w
directly proportional to their velocity, which impacting the surrounding
spherical units (areas/levels) generates a level of SV inside their units’ e/c:
(1 sphere c/channel is composed of 480 mfields, they generate/absorb SV inside
their e/c).
·
asphere with
low velocity: high PRV (SV-vv) produces a level of high PRV: SV–v.
Simultaneously absorbed inside their
2th level generates: simultaneous contraction of the levels above it whit lower
PRV / the simultaneous contraction of
the mfields e/c.
·
asphere with
high velocity: low PRV (SV+vv) produces a level of low PRV: SV +v.
Simultaneously absorbed inside their 2th level generates:
simultaneous expansion of the levels above it whit higher PRV / the simultaneous expansion of the mfields
e/c.
This is how the
analysis gets operated. The absorbing of a level of SV is the tool used to
calculate the aspheres PRV. This process operating simultaneously gives
simultaneous value. The volumetric value of the spheres e/c become the data
which shows the aspheres PRV. Their PRV
gets absorbed by the Moon’s 1th level and become the initial value of pressure
from which operate their CW (de)pressure inside the 80 spheres of its 7th
level.
The Moon
analyses the flux of aspheres while orbiting. Being circular produces a flux of
aspheres with constant PRV: SV/vv. It
become the information needed to generate the three planetary value of
pressure: (PRV as pressurizing values)
·
the first sphere (rotational value of
pressure) analyze/convert inputs into information and evaluate it.
it
first analyzes the asphere volumetric value.
The
breaking of the ordinary constancy makes the sphere’s 1th
level switching reference for the analysis of the data adopting t/f
of the process of absorbing SV between the levels of its
two halves.
t/f
obliges the 1th level to absorb the value of the previous asphere
for confirmation of value: the asphere is then
recognized as:
LOW
PRV: decreased distance between two following aspheres: the following asphere
is analyzed by the 7th level of the F/H before the previous crosses
the 7th level of the B/H.
Their
time/distance of frequency is the value converted as information, generating
PRV out of it.
HIGH
PRV: increased distance between two following aspheres: the following asphere
is analyzed by the 7th level of the F/H after the previous crosses
the 7th level of the B/H.
Their
time/distance of frequency is the value converted as information.
The
reference value for the evaluation of data become the previous analysis. It
needs a confirmation input (constancy) before setting again the analysis on
previous value: volumetric value.
The
analysis once evaluated/set as value of pressure can’t be changed: it needs a
change of PRV.
(Structural / mechanical
motion do not get analyzed evaluated: they just occurs / the
mechanical modification of the 2/7 level gets absorbed inside the c/channel / 8th
level.)
·
the second sphere (orbital value of
pressure) during:
Ordinary
orbital path: constant value to get to analyze, do not evaluates information,
just proportionally convert information into value of pressure.
Orbital
loop: block of the orbital path makes it evaluating information into value of
pressure.
It
first analyzes the asphere volumetric value.
The
breaking of the ordinary constancy makes the sphere’s 1th
level switching reference for the analysis of the data adopting t/f
of the following asphere for confirmation of value.
(same procedure as the 1th sphere)
·
the third sphere (latitudinal value of
pressure) always confirm its previous value of pressure:
It’s
set by the Macro field s/pressure: its value of pressure doesn’t ever change.
Latitudinal pressure can’t be blocked or modified.
Using this system, any modification of value of pressure
gets calculated in advance and not made randomly. Each motion of pressure has 8
values, corresponding to each of the field’s areas. Due to it the
analysis/evaluation gets performed 8 times (one areas at time for each value of
pressure), by each of the three spheres before getting absorbed by the Moon’s
1th level as PRV of reference for the value of pressure: the following CW expansion the Moon e/c will expand in proportion to
it, generating the general modification of the PRV of the spheres of its 2/7th
level.
The analysis is
permanent: gets performed every time in each of the aspheres getting through
them, in package of 80 Afields (getting inside the e/c of the 80 spheres of the
Moon’s 7th level).
*Planetary: In dynamic conditions, as
the orbital loop, the value adopted is:
·
Aspheres in
progressive decrease of PRV: getting toward the Sun; the value adopted is the
last one, the largest volumetric value.
·
Aspheres in
progressive increase of PRV: getting away from the Sun; the value adopted is
the first one, the largest volumetric value.
Platform
of analysis:
What you find below is a simplified description of
simultaneously traveling of information through the field’s LR. It will be
taken as analytic platform to describe the Moon’s orbital path and loop. It has
been simplified in three steps using as area of reference H.
·
When the first asphere reaches the
first sphere with a/r H, its volumetric value
gets simultaneously absorbed/analyzed and the information located in the 1th
level.
Its evaluation is simultaneously
converted as value of rotational pressure.
·
When the first asphere reaches the
second sphere, with a/r H, its volumetric value
gets simultaneously absorbed/analyzed and the information located in the 1th
level.
Its evaluation is simultaneously
converted as value of orbital pressure.
·
When the first asphere reaches the
third sphere with a/r H, its volumetric value
gets simultaneously absorbed/analyzed and the information located in the 1th
level.
Its evaluation is simultaneously
converted as value of latitudinal pressure.
Analysis of the orbital revolution around the Planet: first
half. The Moon begins it owing the following condition:
a) Outside
the Sfield/Sunit c/channel.
b) The
Moon doesn’t have own c/channel, it uses the Planet’s. Its dissolving has been
a structural / mechanical process,
(the
4 Mosphere due to over pressure got separated from the 7th level and
the outer flux of mfields merged with the inner to generate the sMoons.)
independently
from analysis: not getting through the memory department, hasn’t been generated
the switching of volumetric value of reference for the analysis/evaluation of
PRV.
Being
generated with ACW pressure, the spheres of its c/channel were supposed to
locate around the e/c of the spheres of the Sfield’s c/channel, below the
Sunit/Planet c/channel carrying 03/10 of SU of mechanical ACW contraction, in
their e/c and c/axis.
Its
1th level: memory department, having this value as reference, generates the
condition which involuntarily set change of constant PRV: SV/ vv, of the
sMoons’ (Organic Fields) aspheres.
Operating
analysis with larger volumetric value: 02/10 of SU of mechanical ACW
contraction, without considering it, makes the afields constant PRV, in form of
volumetric value, resulting smaller, SV-v/v: the m/w generated by their
velocity reaches the mfields located further away, producing inside their e/c a
level of SV with higher PRV: SV/-v.
The Moon’s s/pressure getting inside the c/axis of the
spheres of the Planet c/channel reaching out its 7th level, begins
to suction amfields produced by the sMoons:
When the first asphere reaches the first sphere with a/r H,
its volumetric value gets simultaneously absorbed/analyzed and the information
located in the 1th level.
Evaluation rotational
value. The operated analysis of data: asphere volumetric value, because smaller
than the one set into its memories of motion, gets evaluated as increased
distance between Planet/Moon (SV –vv). Out of it the rotational value of
pressure gets evaluated with proportional increase.
When the first asphere reaches the second sphere, with a/r H,
its volumetric value gets simultaneously absorbed/analyzed and the information
located in the 1th level.
Evaluation orbital
value. The operated analysis of data: asphere volumetric value, because smaller
than the one set into its memories of motion, doesn’t gets the status of previous
value of pressure due to constancy and gets proportionally converted as value
of orbital pressure.
When the first asphere reaches the third sphere with a/r H,
its volumetric value gets simultaneously absorbed/analyzed and the information
located in the 1th level.
Evaluation latitudinal
value. The value is already set, gets always previous value.
The breaking of the constancy of the PRV, makes their 1th
level switching the reference of analysis to time of frequency to generating
accurate value of pressure, condition needed to set the analysis back on
volumetric value. Constancy gets then evaluated as previous value.
Communicating in continuum within the field (Moon) t/u of
pressure, makes the 1th level switching areas for the values of analysis.
When the second asphere reaches the first sphere with a/r H, its t/f gets
simultaneously absorbed/analyzed and the information located in the 1th
level.
Evaluation rotational
value. Generating analysis of t/f over
constant velocity, originated by the constant s/pressure, produces ordinary
PRV. The t/f of the analyzed asphere produces PRV which doesn’t match the
previous analysis: it’s faster (SV +v/v). Out of it, the rotational value of
pressure gets evaluated with proportional decrease. Due to the impossibility of changing the value of
pressure because the first asphere is still inside the following spheres
getting analyzed, it simultaneously blocks the rotational motion of pressure not
its increased value (first evaluation).
When the second asphere reaches the second sphere, with a/r H, its t/f gets
simultaneously absorbed/analyzed and the information located in the 1th
level.
Evaluation orbital
value. The time/frequency of the
analyzed asphere do matches the previous analysis, its constancy gets the
status of previous value and set the analysis back on volumetric value.
When the second asphere reaches the third sphere with a/r H, its t/f gets
simultaneously absorbed/analyzed and the information located in the 1th
level.
Evaluation latitudinal
value. The value is already set, gets always previous value.
That create the following condition:
a) Because
to change the state of pressure it’s needed a variation of PRV and the first
sphere has made operative the block of the rotational motion out of constant
value: aspheres’ PRV, analyzed through their volumetric value and t/f, it will
keep confirming the previous value of pressure: its block, until the next
change of PRV.
b) The
Moon’s general PRV increased: rotational value, generates a mechanical decrease
of the space among the Moon spheres (80 each level): they get smaller, so the
space among them and their mfields. Decreasing their space decreases their
storing capacity: the new generated DF (Moon’s 7th level) locate
among them.
For the following 13.5 days of orbital path around the
Earth, the Moon’s field keeps the rotational value of pressure increased, until
the beginning of the orbital loop.
*DF: mfield generated with PRV higher than afields. The
absence of value of pressure inside the 7th level makes the Moon not
visible.
Orbital
loop:
The monthly orbital loop begins with the Planet c/channel
aligned with the Sunit c/channel.
The Moon, being located in the middle of it gets the inner
flux of aspheres suctioned by the Sun e/c, getting through its c/axis,
generating its temporarily mechanical decrease of PRV (gets simultaneously
absorbed by its 8th level: sMoons).
(size
are out of proportion. They just fit in as visual description)
Analysis of the orbital loop. The Moon begins it owing the
following condition:
a) Mechanical
decreased own PRV.
b) Aligned
with the Sunit c/channel.
The
Planet c/channel getting over the Sunit c/channel, set above on top of the e/c
of its spheres, simultaneously mechanically decreasing its PRV (equalizes
the Moon field mechanical decrease): increases the
distance among its mfields, SV+v. Getting operative structurally / mechanically
and not as direction given by the analysis/evaluation of its 1th level, do not
get considered into its analysis, generating the condition which involuntarily
set change of constant PRV of an asphere:
Operating
analysis with larger volumetric value, makes the afields constant PRV, in form
of volumetric value, resulting smaller, SV-v/v: the m/w generated by their
velocity reaches the mfields located further away, producing inside their e/c a
level of SV with higher PRV: SV/-v.
c) The
rotational motion of pressure blocked.
When the first asphere reaches the first sphere with a/r H,
its volumetric value gets simultaneously absorbed/analyzed and the information
is sent to the 1th level.
Evaluation rotational
value. The operated analysis of data: asphere volumetric value, because smaller
than the one set into its memories of motion, gets evaluated as increased
distance between Planet/Moon (SV –vv). Out of it the rotational value of
pressure gets evaluated with proportional increase.
When the first asphere reaches the second sphere, with a/r H,
its volumetric value gets simultaneously absorbed/analyzed and the information
located in the 1th level.
Evaluation orbital
value. The operated analysis of data: asphere volumetric value, because smaller
than the one set into its memories of motion, gets evaluated as increased
distance between Planet/Moon (SV –vv). Out of it the orbital value of pressure
gets evaluated with proportional increase.
When the first asphere reaches the third sphere with a/r H,
gets simultaneously absorbed/analyzed: The information is sent to the 1th
level.
Evaluation latitudinal
value The latitudinal value is already set, gets always previous value.
The breaking of the constancy of the PRV, makes their 1th
level switching the reference of analysis to time of frequency to generating
accurate value of pressure and setting the analysis back on volumetric value.
Constancy gets then evaluated as previous value.
When the second asphere reaches the first sphere with a/r H, gets absorbed/analyzed on its t/f. The
information is sent to the 1th level.
Evaluation rotational
value: the t/f of the following asphere do not matches the previous analysis:
it’s faster (SV +v/v, resulting closer). Out of it, the rotational value of
pressure gets evaluated with proportional decrease. Due to the impossibility of changing the value of
pressure because the first asphere is still inside the following spheres
getting analyzed, it simultaneously blocks the rotational motion of pressure
not its increased value (first evaluation).
When the second asphere reaches the second sphere with a/r H, gets absorbed/analyzed on its time of
frequency. The information is sent to the 1th level.
Evaluation orbital
value: the t/f of the following asphere do not matches the previous analysis:
it’s faster (SV +v/v, resulting closer). Out of it, the orbital value of
pressure gets evaluated with proportional decrease. Due to the impossibility of changing the value of
pressure because the first asphere is still inside the following spheres
getting analyzed, it simultaneously blocks the orbital motion of pressure not
its increased value (first evaluation).
When the second asphere reaches the third sphere with a/r H, gets absorbed/analyzed on its time of
frequency. The information is sent to the 1th level.
Evaluation latitudinal
value: The latitudinal value is already set, gets always previous value.
At this point the block of the rotational/orbital motion of
pressure can’t be changed anymore: to change the state of pressure it’s needed
a variation of the aspheres’ PRV (SV v/v) and the Moon’s first two spheres have
made operative the block of the rotational/orbital motion out of constant PRV
as: aspheres’ velocity, analyzed through their volumetric value and
time/frequency. Because of it, they will keep confirming the PRV as:
·
the block of rotorbital motion,
·
their increased value of pressure,
until the next change of it (PRV).
The Moon 1th level is now facing this conditions: during the
orbital loop gets performed the switching the field’s halves. Operating it with
modified PRV would change their timing of execution, setting incommunicability
of direction of motion.
Due to it, the 1th level simultaneously withdraws volumetric
value as main reference to convert information into PRV, and adopt t/f of two
following aspheres (which makes it keeping a memory on it at each analysis,
rarely used). Consequently, t/f becoming main reference begins to reanalyze
data. That gives the capability of realigning the rotorbital PRV to ordinary
value, not the block of the two motions of pressure.
Time of frequency with pressurizing restriction: constancy
of aspheres’ PRV, forbid/prevent it (Moon’s 1th level: memories of motion) to
change the block of its rotational and orbital motions of pressure, keeping
them during the orbital loop, all time long.
When the third asphere reaches the first sphere with a/r L, gets absorbed/analyzed on its time of frequency.
The information is sent to the 1th level.
Evaluation rotational
value: the switching of reference guide to operate analysis of data require the
absorbing of the last analysis as reference: from it result same value and both
of them match the ordinary value. Out of it, the block of the rotational motion
gets confirmed, its value of pressure get proportionally evaluated.
When the third asphere reaches the second sphere with a/r L, gets absorbed/analyzed on its time of frequency.
The information is sent to the 1th level.
Evaluation orbital
value: the switching of reference guide to operate analysis of data require the
absorbing of the last analysis as reference: from it result same value and both
of them match the ordinary value. Out of it, the block of the orbital motion
gets confirmed, its value of pressure get proportionally evaluated.
When the third asphere reaches the third sphere with a/r L, gets absorbed/analyzed. The information is sent to
the 1th level.
Evaluation latitudinal
value: the latitudinal value is already set, gets always previous value.
When the last
latitudinal value of pressure (L second half)
reaches the 1th level, adds up to the previous 23 an become value of pressure,
becoming simultaneously operative with the new CW motion of pressure.
During the Planetary orbital loop, the Moon move only
latitudinally: keeps not rotates its N/S axis and stops to orbit the Planet,
remaining blocked with the Planet c/channel on top of the Sunit c/channel, all
time long.
The mechanical decrease of PRV allows to store DF among its
spheres/mfields, filling the empty space up without generating value of
pressure. The absence of value of pressure inside
the 7th level makes the Moon not visible.
Analysis of the orbital revolution around the Planet: second
half. The Moon begins it owing the following condition:
a) The
orbital loop, produces a structural retrograde motion of 3 minutes (circa), due
to the Earth’s final acceleration which produces an enlarging of its last
straight segment, locating the Planet/Moon not in the point left to begin the
orbital path, but 3 minutes before.
b) Aligned
with its c/channel on top of the Sunit c/channel, all time long.
d) The
rotational and orbital motion of pressure blocked.
The Planet, getting on the ordinary orbital path with 3
minutes of backward position, generated the last increase of PVR: its increased
distance from the Sun generate flux of aspheres with higher PRV (SV –vv). It
simultaneously produces an increase of PRV: SV –v in the spheres of the Sunit
c/channel.
Getting simultaneously absorbed by the spheres of the Planet
c/channel with proportional increase of their PRV, generates the condition in
which the aspheres constant PRV, gets recognized by their memories of motion as
the value which generated the switching of value of reference to generate
analysis of data, producing:
·
makes the Moon’s 1th level
simultaneously swishing the value of reference for the analysis, from t/f back
to volumetric value.
·
the Moon to reanalyze data (flux of
aspheres) coming from the Planet c/channel.
·
The increase of PRV of the spheres of
(Sunit)/Pfield c/channel, being mechanical do not get considered into the
analysis setting decrease of PRV: the analyzed aspheres’ volumetric value get
larger in it: SV +v/v: the m/w generated by their velocity reaches the mfields
located closer, producing inside their e/c a level of SV with lower PRV:
SV/+v.
When the first asphere reaches the first sphere with a/r H,
its volumetric value gets simultaneously absorbed/analyzed: The information is
sent to the 1th level.
Evaluation rotational
value: the switching of reference guide to operate analysis of data require the
absorbing of the asphere PRV from last analysis. From it result motion: the
increase of the aspheres volumetric value gets evaluated as decreased distance
between Planet/Moon. Out of it the rotational value of pressure gets evaluated
with proportional decrease.
When the first asphere reaches the second sphere with a/r H,
its volumetric value gets simultaneously absorbed/analyzed: The information is
sent to the 1th level.
Evaluation orbital
value: the operated analysis of data: asphere volumetric value, because larger
than past analysis, doesn’t gets previous value of pressure: constancy and gets
proportionally converted as value of orbital pressure.
When the first asphere reaches the third sphere with a/r H,
gets simultaneously absorbed/analyzed: The information is sent to the 1th
level.
Evaluation latitudinal
value: the value is already set, gets always previous value.
The breaking of the constancy of the PRV, makes their 1th
level switching the reference of analysis to time of frequency to generating
accurate value of pressure and setting the analysis back on volumetric value.
Constancy gets then evaluated as previous value.
When the second asphere reaches the first sphere with a/r H, gets absorbed/analyzed on its time of
frequency. The information is sent to the 1th level.
Evaluation rotational
value: The t/f of the following asphere do not matches the previous analysis:
it’s slower (SV -v/v, further away). Out of it, the rotational value of
pressure gets evaluated with proportional increase. Due to the impossibility of changing the value of
pressure because the first asphere is still inside the following spheres
getting analyzed, it simultaneously blocks the rotational motion of pressure
not its decreased value of pressure (first evaluation).
When the second asphere reaches the second sphere with a/r H, gets absorbed/analyzed on its time of
frequency. The information is sent to the 1th level.
Evaluation orbital
value: the t/f of the analyzed asphere do matches the previous analysis, its
constancy gets the status of previous value and set the analysis back on
volumetric value.
When the second asphere reaches the third sphere with a/r H, gets simultaneously absorbed/analyzed. The
information is sent to the 1th level.
Evaluation latitudinal
value. The value is already set, gets always previous value.
That create the following condition:
a) Because
to change the state of pressure it’s needed a variation of PRV and the first sphere
has made operative the block of the rotational motion out of constant value:
aspheres’ PRV, analyzed through their volumetric value and t/f, it will keep
confirming the previous value of pressure: its block, until the next change of
PRV.
b) The
Moon’s general PRV decreased: rotational value, generates a mechanical increase
of the space among the Moon spheres (80 each level): they get larger, so the
space among them and their mfields. Increasing their space increases their
storing capacity: the new generated DF (Moon’s 7th level) locate
among them.
For the first 13.5 days the Moon
undergone increase of PRV: decreasing the empty space among the Moon spheres /
their mfields, decreased their storing capacity. The new generated DF gets
stored among them.
During the orbital loop, the new
generated DF absorbed the m/w generated by the switching of the halves: being
operative with 180° rotational motion and equal time/value in both of them,
equally distributed the DF inside the Moon’s areas, next to the ones previously
stored (because of its mechanical decrease of PRV, filled up the
empty space without generating value of pressure).
Now, the increased space among
spheres makes the Moon field keeping storing the new generated DF nest to the
magnitude produced in the previous 16 days: their absorbing any motion wave as
direction of motion, makes them being driven by the one generated with the
value of pressure needed to block the rotational motion, compacting always in
the same area of the field, with the same magnitude of DF.
Moving out of the Sunit c/channel
generated mechanical increase of pressure,
as soon as the Sunit c/channel
moves from the Moon’s c/axis ceases the global decrease of PRV and become
local: the area in which the inner flux of afield suctioned by the Sunit e/c,,
gets through.
decreasing the space among the
Moon’s spheres/mfields, completely annulling the generated decrease of PRV.
Because of it the magnitude of new generated DF, adding to the magnitude of DF
produced the previous 16 days: orbital loop / first 13.5 days,
overcome their storing capacity: empty space among the
Moon spheres’/mfields.
The m/w which makes the DF
moving/flowing through the Moon field,
(very general/very
brief description) the DF keep generating a level of SV
inside their e/c..
Not
getting absorbed gets expelled: by the new generated level: getting generated
inside the e/c expels the one located in it, through the back half’s axis.
Getting pushed away with high pressure through the back axis, with diameter
smaller than e/c, generates value of pressure which transform in m/w, pushing
them away with velocity inversely proportional to PRV, generating flowing flux
of it.
makes them forcing their way in,
among the existing DF generating mechanical ACW contraction: 0.675/10 SU, in
the Moon’s spheres/mfields of the area in which they get stored.
The value of pressure on them gets
shown by the regular increase of the light in the 7th level: daily
phase of the crescent Moon.
For the following 13.5 days of orbital path around the
Earth, the Moon field keeps the rotational value of pressure decreased, until
full Moon.
Analysis of the orbital revolution around the Planet: first
half. The Moon begins it owing the following condition:
1)
The volumetric magnitude of DF stored
inside the 7th level of the Moon field, as soon as fills its whole
volume create the condition in which the 0.675/10 of SU of value of pressure
gets global, generating decrease of PRV: the 7th level become
larger: SV+v and consequently mechanically absorbed in the other level: 2/6th
and 8th level (sMoons). The information of PRV getting through the
Pfield c/channel produces proportional decrease of PRV in it. The SU generated
inside the Moon’s 7th level: outside its mfields become twice larger
traveling inside the mfield of the Pfield
c/channel, generating 1.35 unit of decrease of PRV in them..
The
simultaneous absorbing of lower PRV (SV +v), being mechanical do not gets
considered into the analysis: do not gets through the 1th level, generating the
condition which involuntarily set increase of PRV (SV -v/v) of the analyzed
asphere:
2)
the rotational motion blocked.
When the first asphere reaches the first sphere with a/r H, its volumetric value gets simultaneously
absorbed/analyzed: The information is sent to the 1th level.
Evaluation rotational
value. The operated analysis of data: asphere volumetric value, results smaller
than previous value. Getting evaluated as increased distance between
Planet/Moon, the rotational value of pressure gets proportional increase.
When the first asphere reaches the second sphere with a/r H, its volumetric value gets simultaneously
absorbed/analyzed: The information is sent to the 1th level.
Evaluation orbital
value. The operated analysis of data: asphere volumetric value, because smaller
than previous value, doesn’t get confirmed with previous value and gets
proportionally converted as value of orbital pressure.
When the first asphere reaches the third sphere with a/r H, its volumetric value gets simultaneously
absorbed/analyzed: The information is sent to the 1th level.
Evaluation latitudinal
value. The value is already set, gets always previous value.
The breaking of the constancy of the PRV, makes their 1th
level switching the reference of analysis to t/f to generating accurate value
of pressure and setting the analysis back on volumetric value. Constancy gets
then evaluated as previous value.
When the second asphere reaches the first sphere with a/r H, gets absorbed/analyzed on its time of
frequency. The information is sent to the 1th level.
Evaluation rotational
value. The t/f of the analyzed asphere do not matches the previous analysis:
it’s faster (SV +v/v). Out of it, the rotational value of pressure gets
evaluated with proportional decrease. Due to
the impossibility of changing the value of pressure because the first
asphere is still inside the following spheres getting analyzed, it simultaneously
blocks the rotational motion of pressure not its increased value of pressure
(first evaluation).
When the second asphere reaches the second sphere with a/r H, gets absorbed/analyzed on its time of
frequency. The information is sent to the 1th level.
Evaluation orbital
value. The time/frequency of the analyzed asphere do matches the previous
analysis, its constancy gets the status of previous value and set the analysis
back on volumetric value.
When the second asphere reaches the third sphere with a/r H, gets absorbed/analyzed. The information is sent
to the 1th level.
Evaluation latitudinal
value. The value is already set, gets always previous value.
That create the following condition:
a) Because
to change the state of pressure it’s needed a variation of PRV and the first
sphere has made operative the block of the rotational motion out of constant
value: aspheres’ PRV, analyzed through their volumetric value and t/f, it will
keep confirming the previous value of pressure: its block, until the next
change of PRV.
b) The
Moon’s general PRV increased: rotational value, generates a mechanical decrease
of the space among the Moon spheres (80 each level): they get smaller, so the
empty space among them and their mfields.
Decreasing their space decreases
their storing capacity: the new generated DF (Moon’s 7th level)
locate among them.
The new generated DF absorbing the
m/w generated by the block of the rotational motion, flow with it following the
existent flux.
Forcing their way in, among the
existing DF, generate mechanical ACW contraction: 0.675/10 SU, of the Moon’s
spheres/mfields. This value of pressure adding to the one generated the past
13.5 days, reaches 1.35 unit of mechanical ACW contraction, crossing the SU,
directly interfering with the Moon own value of pressure of the afiels located inside
the mfields of its spheres.
It
gets simultaneously balanced with proportional sharp CW expansion. Acting only
over the specific 1.35 unit of value of pressure, makes the Mspheres /mfields,
reestablishing ordinary volumetric value: their CW expansion contract the DF
pushing them with proportional value down inside the 6th level.
The
flow of new generated DF being constant and from the same direction, keep
forcing their way in, among the existing DF, generating 1.35 unit of value of
pressure, all time long.
Getting
simultaneously balanced with sharp CW expansion makes the mass of stored DF,
keeping constantly and gradually disappearing with reversed motion (related
to the gradual progression of DF which produced light in the Moon 7th
level, the past 13.5 days): produces the regular decrease of
the light in the Moon’s 7th level: daily phase of the decrescent
Moon.
For the following 13.5 days of orbital path around the
Planet, the Moon’s field keeps the rotational value of pressure increased,
until the end of the orbital revolution around the Planet / beginning of its
orbital loop.
The Moon’s LP, do not ever rotate.
Its latitudinal motion up and down the equatorial plane of
the LR moves it, with a rate of 0.025° per day reaching the extension of 2.25°
above and below it, of 4.5°. Combined with the Earth’s field latitudinal motion
generates the inconstant monthly progression of the Eclipses. Its volumetric
PRV (as weight) slows the orbital motion. The Macro field
s/pressure generates all the fields orbital values: Planets / Moons. As force
acts globally and not singularly: the Moon is a secondarily field: it’s part of
the Sfields 8th level, consequently its location among its components
has also to be considered as value which determines its orbital velocity.
Operating latitudinal motion with the block of the
rotational motion causes the librations.