Planar Drift
Planar Drift is the inherent, chaotic fluctuation of planes in their unbound state. This phenomenon manifests as continuous, non-linear variations in planar tension across all observable regions of both planes.
Physical Characteristics
The drift exhibits turbulent, unpredictable motion patterns that operate across multiple spatial and temporal scales. These fluctuations are not uniform across geographic regions; certain areas demonstrate higher turbulence coefficients (resulting in steeper energy differentials), while others maintain relative stability. The drift persists as a fundamental property of the Ergo and Eidos planes, independent of external influence or Matera plane interaction.
Thermodynamic Properties
Planar drift contains ambient, harvestable energy derived from the kinetic motion of planar tension fluctuations. The energy differential between chaotic (drift) and stabilized (static) states constitutes the foundational fuel source for all Planar Catalysis. This differential is measurable and quantifiable, varying directly with local turbulence intensity.
Energy Harvesting Mechanism
Catalysts function by inducing localized stabilization of chaotic drift. The device captures the energy differential between the chaotic state and the artificially stabilized state, storing that difference as Tenax. The recharge rate is directly proportional to the intensity of local drift turbulence. High-turbulence regions permit rapid energy capture; low-turbulence regions yield negligible recharge rates.
Regional Variation
Drift intensity demonstrates significant geographic variation:
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High-Drift Zones: Areas exhibiting naturally elevated planar turbulence, frequently associated with high-tension regions or locations of recent planar disturbance.
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Low-Drift Zones: Regions of inherent planar stability, typically distant from major Aperture activity or ancient planar scars.
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Depleted Zones: Areas where drift has been flattened through excessive stabilization. See Planar Drift Depletion.