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. 2022 Mar 14;119(12):e2200367119. doi: 10.1073/pnas.2200367119

Table 1.

Conductivity and surface impedance in the different regimes and their regions of validity

Regime Valid when Conductivity σ(q,ω) Surface impedance Z(ω)
Low-frequency normal q2v2ΓinterΓmr ωΓinter εωP2[2Γmr+α23Γinterα266151Γmr] eiπ/4μωc2ωP2(2Γmr+α23Γinterα266151Γmr)12
Anomaly-induced nonlocal ΓinterΓmrq2v2Γmr2 ωq2v2/Γmr εωP2[2Γmr+α218Γmrq2v2] See Eq. 56
Hydrodynamic ΓmrΓtotq2v2Γtot2 ωq2v2/Γtot εωP2Γtotq2v2[9.026α2] 12(eiπ/8+ei5π/8)μ(ω3v2c2ωP2Γtot[9.026α2])1/4
Ballistic Γtotqv ωqv εωP21qv[4.5+4.3α2] 439eiπ/3μ(ω2vc2ωP2[4.5+4.3α2])1/3
High-frequency normal qvω Γtotω iεωP21ω[2+85α2] iμωcωP(2+85α2)12

The numerical coefficients in the hydrodynamic and ballistic regimes are rounded up to two significant numbers.