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9.31 - Oscillatory Motion creating Waveforms

Particles of a medium subjected to periodic impulses will behave in similar manner as the orbiting planet just mentioned. With the inducting forces impacting upon them they will change from a quiescent state which is to say a harmonic state of circular orbit to an elliptical orbit. During this elliptical orbit periodic increase and decrease of volume of the media in which it is a part will occur as the elliptical orbits synchronize, phase in together adding themselves to peaks and subtracting themselves into troughs. Hence tons of ocean water can be elevated in peaks and troughs with seeming little effort. Should these directions of motion be considered orthogonally (xyz coordinates and vectors over Time) we could easily develop a mathematics and geometry describing these motions, expansions and contractions. (Care must be introduced here to not get detoured by Cartesian geometries or trigonometry which are inherently inaccurate and therefore misleading.)

The more attractive phases synchronize into tighter accumulations while the less attractive phases synchronize into "looser" or more dispersed concerted actions. Hence we then have the compression and rarefaction phases of a standard sound wave.

Power is accumulated in the slowing of the spin of rotation, simultaneous decrease of orbital radius and increase of orbital speed. Power is released in the accelerating of spin of rotation, simultaneous increase of orbital radius and decrease of orbital speed.

See Also


3.8 - There are no Waves
3.9 - Nodes Travel Faster Than Waves or Light
8.3 - Conventional View of Wave Motion
8.4 - Wave types and metaphors
8.5 - Wave Motion Observables
8.6 - Wave Form Components
8.8 - Water Wave Model
9.2 - Wave Velocity Propagation Questions
9.30 - Eighteen Attributes of a Wave
9.31 - Oscillatory Motion creating Waveforms
9.34 - Wave Propagation
9.35 - Wave Flow
12.05 - Three Main Parts of a Wave
16.06 - Electric Waves are Sound Waves
Compression Wave
Compression Wave Velocity
Curved Wave Universe of Motion
Dissociating Water with Microwave
Figure 6.9 - Russell depicts his waves in two ways
Figure 6.10 - Wave Dynamics between Cube Corners
Figure 7.1 - Step 1 - Wave Vortex Crests at Maximum Polarization
Figure 8.1 - Russells Painting of Wave Form Dynamics
Figure 8.10 - Each Phase of a Wave as Discrete Steps
Figure 8.11 - Four Fundamental Phases of a Wave
Figure 8.14 - Some Basic Waveforms and their constituent Aliquot Parts
Figure 8.2 - Compression Wave Phase Illustration
Figure 8.3 - Coiled Spring showing Longitudinal Wave
Figure 8.4 - Transverse Wave
Figure 9.10 - Phases of a Wave as series of Expansions and Contractions
Figure 9.11 - Compression Wave with expanded and contracted Orbits
Figure 9.13 - Wave Flow as function of Periodic Attraction and Dispersion
Figure 9.14 - Wave Flow and Phase as function of Particle Rotation
Figure 9.15 - Wave Flow and Wave Length as function of Particle Oscillatory Rotation
Figure 9.5 - Phases of a Wave as series of Expansions and Contractions
Figure 9.9 - Wave Disturbance from 0 Center to 0 Center
Figure 12.10 - Russells Locked Potential Wave
Figure 12.12 - Russells Multiple Octave Waves as Fibonacci Spirals
Figure 13.13 - Gravity Syntropic and Radiative Entropic Waves
Figure 14.07 - Love Principle: Two sympathetic waves expanding from two points have one coincident centering locus
In the Wave lies the Secret of Creation
Laws of Vibration
Longitudinal Wave
Longitudinal Waves in Vacuum
Matter Waves and Electricity
Nodal Waves
One More Step Toward Building The Cube-Sphere Wave-Field
Quantum Entanglement
Raleigh Wave
Shock Wave
Sympathetic Oscillation
Sympathetic Vibration
Table 12.02.01 - Wavelengths and Frequencies
Three Main Parts of a Wave
Transverse Wave
wave
Wave Field
Wave Fields - Summarize and Simplify
wave number
WaveLength

Created by Trene. Last Modification: Thursday December 15, 2011 23:47:09 MST by Trene.