A magnetic field varying over a length has of order . Consequently, the resistive magnetic energy loss contains two inverse powers of , while the resistive magnetic-helicity balance contains only one. Small-scale gradients can therefore dissipate substantial magnetic energy while retaining an approximately conserved large-scale magnetic helicity.
A dimensionally consistent version is the selective decay bound for magnetic helicity. With , the Cauchy-Schwarz inequality givesFor bounded and bounded, possibly nonvanishing as , the resistive change in magnetic helicity tends to zero, even though resistive magnetic energy loss may remain finite. Magnetic energy is preferentially dissipated, while magnetic helicity is approximately conserved in this bounded-energy, bounded-dissipation limit.
This is not a comparison of quantities with different physical units or a universal ordering of fractional decay rates. For a single Beltrami field satisfying , both integrated quantities have fractional decay rate without fluid motion. The boundedness assumptions and distribution of magnetic helicity across spatial scales matter.
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