← NS-DCRP / DCRP-51 · Curved-Sheet Uncertainty and Fragmentation-Resistant Second-Order Diffusion Activation
Closes the gap in DCRP-50 (the gradient rate can be large while the sheet's enstrophy-carrying mass tends to zero), proves that sheet fragmentation cannot reduce the reciprocal-thickness diffusion ledger, and compiles the multi-sheet filtered gradient sum back into genuinely unfiltered Navier–Stokes second-order diffusion.
Relationship to the rest of the series, stated as closely as possible in the document's own words, not my interpretation.
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