Planar Drift Depletion is the phenomenon wherein multiple Catalysts operating within a shared geographic area collectively over-stabilize local Planar Drift, reducing the energy differential to zero and preventing further energy harvesting.
Mechanism
A single Catalyst stabilizes a finite volume of drift, permitting the surrounding chaotic movement to replenish the harvested area at a rate exceeding consumption. When multiple Catalysts operate in spatial proximity, their stabilization fields overlap and reinforce one another.
As chaotic movement flattens into a static, ordered state, the energy differential between chaotic and stabilized states asymptotically approaches zero. Recharge rates decline progressively until cessation. The local planar environment becomes thermodynamically flat—devoid of the turbulence required for energy harvesting.
Recovery Dynamics
Following depletion, the affected area requires an undisturbed period to allow natural drift to restore chaotic movement. Recovery time is determined by:
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Depletion Magnitude: Larger Catalyst concentrations create deeper depletion states, requiring extended recovery periods.
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Regional Drift Coefficient: High-drift zones demonstrate faster recovery than low-drift zones.
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Temporal Duration: Prolonged catalysis in a single location creates more severe depletion than brief, intermittent use.
Observed recovery periods range from hours (minor, localized depletion) to decades or centuries (catastrophic, continental-scale depletion events).
Observable Characteristics
Depleted zones exhibit the following measurable properties:
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Zero energy differential between chaotic and stabilized states
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Complete cessation of Catalyst recharge capability
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Absence of detectable planar turbulence
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Gradual restoration of turbulence following cessation of catalytic activity