Overview

This book is a theory of a steady-state homogenous, isotropic, adiabatic, elastic solid universal medium, wherein mass convection occurs as an exact differential in the form of transverse-rotary plane wave propagation of Planckian amplitude and elasticity, of transverse velocity, c, dependent upon equipotential stress, pressure, or tension of scalar surfaces, R2, of finite or infinite radius, and invariant near-incompressible density and rigidity, and infinite or near-infinite equivoluminal pressure and instantaneous normal gravitational-pressural action at a distance, and finite tangential electromagnetic pressural variation equal in sum to a constant permanent kinetic energy in the form of a heterogeneous, anisotropic, antisymmetric distribution of anticlastic strain of vanishing total reversible torsional couple.

Full Product Details

9781979729611

Table of Contents

Reviews

Author Information

Tab Content 6

Customer Reviews

Recent Reviews

Countries Available