Foundational Axioms: Time in Extended Classical Mechanics (ECM)

DOI: 10.13140/RG.2.2.12275.18721

Abstract

This section presents the foundational axioms of time in Extended Classical Mechanics (ECM). Time is defined reciprocally in terms of oscillatory frequency and temporal interval, with the fundamental period T representing a complete oscillation. Observable temporal intervals may correspond to a fraction of a cycle, expressed through the phase fraction x°/360, which can vary under external influences such as motion, gravitation, or thermochemical processes. Standard clock time is defined as a stable reference where the frequency is fixed and the phase increment approaches zero, while cosmic time reflects the effective temporal progression of physical processes, incorporating deviations due to environmental and entropic influences. In ECM, time emerges from oscillatory phase evolution, providing a unified framework for understanding both reference and cosmic temporal intervals.

Axiom T1 – Reciprocal Definition of Time:
Time is defined through the reciprocal relation between frequency and temporal interval:

f = 1 / Δt,     Δt = 1 / f = T

where f is the oscillatory frequency, Δt the fundamental temporal interval, and T the full oscillatory period of the process.

Axiom T2 – Phase-Dependent Temporal Intervals:
Observable time intervals may correspond to only a fraction of a complete oscillatory cycle:

Δt = T (x° / 360)

where x°/360 represents the phase fraction of the cycle. This fraction may vary due to external influences such as motion, gravitational interaction, thermal processes, or chemical reactions.

Axiom T3 – Standard Clock Time:
Standard clock time is defined as the reference condition in which f>0 remains fixed and stable. In this state, the phase increment approaches zero (x → 0), ensuring that temporal intervals are constant and independent of external factors.

Axiom T4 – Cosmic Time and Phase Deviation:
Cosmic time corresponds to the effective temporal progression of physical processes. Deviations from clock time arise when the phase fraction varies under entropic or environmental influences:

Δt = tcos − tcl = T (x° / 360)

where tcos is cosmic time, tcl is the clock-time reference, and the right-hand side represents phase-evolved temporal increments.

Interpretation: Time in ECM emerges from oscillatory phase progression, with clock time providing a stable reference, while cosmic time reflects the influence of environmental and entropic factors.