Temporal Flow Evolution
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Temporal Flow Evolution: Formulating the Equation of Change
In this post, I'm considering an equation that models how flows evolve over time. This equation is given by:
This equation describes how the flow values change over what we can refer to as temporal progression. It incorporates:
- : the flow values representing the state of the system at any time.
- : the spatial gradient of flow, which describes how the flow varies across space.
- : the rate of change of flow over time.
Now, this equation contains the term on both sides, leading to a potentially recursive structure. To simplify this, we refine it as:
Here, is an operator that governs the dynamics of flow evolution, capturing the essential behavior of the system. The next sections will help us define this operator more clearly.
The Operator
The operator is central to understanding how the system evolves. It should account for several key factors:
- Conservation of Total Flow: The flow in the system must remain conserved, implying no creation or destruction of flow.
- Interaction Rules: The operator governs how different flows interact—whether through diffusion, wave propagation, or other types of interaction.
- Threshold Behaviors: There are conditions where flow behaviors change significantly (e.g., near the speed of light).
- Non-local Correlations: Interactions may involve flows at different spatial locations, requiring a non-local term to respect causality.
Discrete Evolution in Planck Time
To capture the discrete nature of time in the model, we express the evolution in steps corresponding to Planck time . This discretization ensures that changes only occur at sub-Planckian time intervals, as shown in:
Enforcing Key Constraints on the Operator
For the system to be physically meaningful, we impose some constraints on the operator . These constraints ensure the conservation of flow, discrete time evolution, and respect for the speed of light:
- Conservation of Flow: We impose that the total flow at any time remains unchanged, leading to the continuity condition:
Substituting the evolution equation, we get:
This simplifies to:
This condition implies that acts as a divergence operator that redistributes the flow without creating or destroying it. A possible form for is:
where is the flow current.
Discrete Evolution in Planck Time: We have already written the equation in terms of discrete time steps, ensuring changes only occur at intervals of Planck time.
Speed of Light Constraint: We introduce a constraint on the magnitude of the flow to prevent it from exceeding the speed of light :
We modify the operator to respect this constraint by ensuring the flow magnitude does not violate this limit:
This ensures that as the flow approaches the speed limit, the operator reduces its magnitude.
Wave-like Behavior in Certain Regimes
In some regimes, especially for small perturbations, we expect the behavior of the system to resemble wave-like phenomena. In the continuum limit, the equation takes the form of a wave equation:
Thus, the operator must include terms like:
Non-local Interactions
In our system, non-local interactions can arise when the flow at a point is influenced by flows at other points. This is incorporated by defining as an integral over neighboring flows:
where is a kernel function enforcing non-local interactions. To preserve causality, the kernel satisfies the condition:
This ensures that non-local interactions are confined within the light cone, maintaining the principles of causality.
Final Refined Equation
Combining all the constraints, the final form of the equation becomes:
This formulation ensures the system:
- Conserves flow,
- Evolves in discrete time steps,
- Respects the speed of light constraint,
- Exhibits wave-like behavior in certain regimes,
- Incorporates non-local interactions while preserving causality.
Expanding the Correction Factor
To ensure the speed of light constraint is respected, we expand the correction factor . For small values of , this factor approximates:
Alternatively, we can redefine this as a function , where:
Thus, the equation simplifies to:
This form is more concise and maintains all necessary constraints, providing a refined model for temporal flow evolution.
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