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Table 1

Compilation of literature values for the effective diameter reproduced from Avdellidou et al. (2021) and completed with recent publications.

# Diameter D (km) Albedo pV Method Ref.
1 72.33 ± 20.18 0.040 ± 0.050 NEATM a
2 76.46 ± 29.36 0.035 ± 0.023 NEATM b
3 79.68 ± 33.85 0.036 ± 0.037 NEATM c
4 79.81 ± 0.31 0.040 ± 0.010 NEATM d
5 80.93 ± 1.46 0.037 ± 0.002 NEATM e
6 83.39 ± 2.97 0.034 ± 0.005 NEATM f
7 86.05 ± 26.43 0.033 ± 0.046 NEATM c
8 87.61 ± 4.40 0.031 ± 0.003 STM g
9 88.50 ± 3.79 0.031 ± 0.003 NEATM h
10 89.37 ± 3.53 0.030 ± 0.002 STM h
11 90.43 ± 20.33 0.030 ± 0.020 NEATM a
12 109.16 ± 0.95 0.020 ± 0.003 NEATM i
13 72.8 ± 6.3 0.034 ± 0.005 CITPM j
14 72.5 ± 4.2 0.035 ± 0.005 CITPM j
15 82.6 ± 8.2 0.032 ± 0.002 c.w. mean
16 83.3 ± 8.1 0.033 ± 0.006 evm mean

Notes. Two different averages are also provided, the classical weighted (c.w.) mean and the EVM value. Entries with asymmetric uncertainties (entries #13 and #14, reference (j)) are therefore symmetrized (Audi et al. 2017, Appendix A, method 2). Methods: STM (standard thermal model), NEATM (near-Earth asteroid thermal model), CITPM (convex inversion thermophysical model).

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