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Table 4

Integrated Te, ne, ionic and elemental abundances from this study in comparison with previous ones.

Our study MH16 (†††) MG13 PB08 KC06 TS03

Te (K)/ne (cm−3)
Te ([S III]) 12 700 ± 800
Te ([O III]) 11 700 ± 300 12 900 ± 720 10 800 12 140 ± 31 11 700
Te ([N II]) 11 500 ± 600 11 670 ± 1000 11 000 13 400
ne ([Cl III]) 1600 ± 900 2380 ± 1300 3000 2531 ± 1227 1200
ne ([S II]) 2300 ± 700 3120 ± 1400 1900 1016 ± 436 1970
ne (C II]) 4500 ± 300

Ionic and elemental abundances

He+/H+ (×10−2) 7.35 ± 0.42 6.25 ± 0.45 8.0 7.07 7.12 ± 0.13 7.89
He2+/H+(×10−2) 2.24 ± 0.11 4.40 ± 0.07 0.945 2.12 3.47 ± 0.01 2.08
He/H(×10−2) 9.60 ± 0.47 10 ± 5 9 9.2 10.0 ± 1.3 10
O°/H+(×10−7) 1.22 ± 0.30 0.211
O+/H+(×10−6) (6.7 ± 1.6)(†) (2.23 ± 0.90)(††) -− (5.1) (††) (1.4 ± 0.1)(††) 3.33
O2+/H+(×10−4) 2.11 ± 0.41 2.59 ± 0.21 2.34 3.78 2.36 ± 0.06 2.8
O3+/H+(×10−5) 4.3 35.1
O/H(×10−4) (2.53 ± 0.48)(†) 4.44 ± 0.36 2.55 3.80 3.09 ± 0.09 3.3

ICF(O) 1.2 ± 0.3 1.70 ± 0.05 1.07 1 1.30 ± 0.01 1.17

S+/H+(×10−8) 1.55 ± 0.25 0.602 1.80 0.93 ± 0.02 0.337
S2+/H+(×10−7) 6.00 ± 0.95 7.43 8.3 6.1 ± 0.2 6.62
S3+/H+(×10−6) 1.94
S/H(×10−6) (1.40 ± 0.25)(†) 2.24 2.80 2.60 ± 0.11 2.4

ICF(S) (2.3 ± 0.2)(†) 3.00 1 4.20 ± 0.11 3.52

N°/H+(×10−8) 2.32 ± 0.95
N+/H+(×10−7) (3.00 ± 0.60)(†) 2.63 4.1 1.9 ± 0.1 3.2
N2+/H+(×10−5) 5.7 2.2
N3+/H+(×10−6) 43.9 6.77
N4+/H+(×10−5) 3.6 2.35
N/H(×10−5) (1.50 ± 0.41)(†) 2.05 13.5 4.19 ± 0.39 3.4

ICF(N) 49 ± 14 80 1 220 ± 17.0 1.53

Notes. The pseudo-slit employed for our estimations is centered at the center of the PN with dimensions 36.8″ × 42.6″. For the ionic abundances from previous studies, in the case where many emission lines were employed, and the adopted value was not available, the mean value of the individual ionic abundances was accounted in the table. (†)The resulted values after the correction for recombination contribution. (††)Only [O II] λλ3726,3729 (blended) were available for the estimation of O+/H+. (†††)In the case of MH16, the values in the table are those that came from the pseudo-slit that covers the full region. Miller et al. (2016):MH16, Monteiro et al. (2013):MG13, Pottasch & Bernard-Salas (2008):PB08, Krabbe & Copetti (2006):KC06, Tsamis et al. (2003):TS03.

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