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Table 4

Equipartition analysis.

γmin = 10, k = 0 γmin = 100, k = 1 γmin = 100, k = 10
Reg. D B eq p min t B eq p min t B eq p min t p th
[kpc]  [μG]  [Myr]  [μG]  [Myr]  [μG]  [Myr]

C 5 55.1 83.9 36.0 35.7 56.0 86.5 640
W1 20 21.9 13.2 14.3 5.6 22.2 13.6 104
W1 40 18.3 9.2 11.9 3.9 18.6 9.5 ′′
W2 20 20.0 11.0 13.0 4.7 20.3 11.4 53
W2 40 16.7 7.7 10.9 3.3 17.0 7.9 ′′
W3 20 20.9 12.1 13.7 5.2 21.3 12.5 49
W3 40 17.5 8.4 11.4 3.6 17.8 8.7 ′′
W4 20 19.0 10.0 12.4 4.2 19.3 10.3 58
W4 40 15.9 7.0 10.4 3.0 16.1 7.2 ′′
E1 20 23.9 15.7 15.6 6.7 24.2 16.2 81
E1 40 19.9 11.0 13.0 4.7 20.2 11.3 ′′
E2 20 20.2 11.2 13.2 4.8 20.5 11.6 68
E2 40 16.9 7.8 11.0 3.3 17.1 8.1 ′′
H1 20 16.0 7.1 10.5 3.0 16.3 7.3 59
H1 40 13.4 5.0 8.7 2.1 13.6 5.1 ′′
H2 20 20.0 11.1 13.1 4.7 20.3 11.4 65
H2 40 16.7 7.7 10.9 3.3 17.0 8.0 ′′
H3 20 17.0 7.9 11.1 3.4 17.2 8.2 46
H3 40 14.2 5.5 9.2 2.4 14.4 5.7 ′′

Notes. D is the depth of the region assuming a cylindrical configuration. Beq and pmin are the magnetic field and the pressure from the equipartition analysis. t is the estimated zone age. Errors on t are derived from errors on νb in Table 3.

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