Table 3
The observational quantities, D, pobs, and fgrad, are listed for each line of Table 2.
HARPS-N observations | Hydrodynamical model | ||||
Line | D a | pobs ± σfluor−stat ± σd−stat ± σd−syst b | fgrad c | phydro d | p0 e |
|
|||||
Line 1 | 0.281 ±0.001 | 1.287 ±0.031±0.014±0.023 | 0.983 ±0.007 | 1.307 | 1.360 |
Line 2 | 0.147 ±0.001 | 1.323 ±0.031±0.014±0.023 | 0.991 ±0.004 | 1.328 | 1.365 |
Line 3 | 0.348 ±0.001 | 1.280 ±0.031±0.014±0.023 | 0.979 ±0.009 | 1.304 | 1.369 |
Line 4 | 0.573 ±0.001 | 1.282 ±0.031±0.014±0.023 | 0.967 ±0.014 | 1.292 | 1.375 |
Line 5 | 0.297 ±0.001 | 1.297 ±0.031±0.014±0.023 | 0.982 ±0.008 | 1.309 | 1.375 |
Line 6 | 0.612 ±0.001 | 1.282 ±0.031±0.014±0.023 | 0.964 ±0.015 | 1.288 | 1.375 |
Line 7 | 0.562 ±0.001 | 1.273 ±0.031±0.014±0.023 | 0.967 ±0.014 | 1.272 | 1.376 |
Line 8 | 0.500 ±0.001 | 1.285 ±0.031±0.014±0.023 | 0.971 ±0.012 | 1.297 | 1.378 |
Line 9 | 0.364 ±0.001 | 1.307 ±0.031±0.014±0.023 | 0.979 ±0.009 | 1.302 | 1.383 |
Line 10 | 0.326 ±0.001 | 1.329 ±0.031±0.014±0.023 | 0.981 ±0.008 | 1.301 | 1.387 |
Line 11 | 0.429 ±0.001 | 1.295 ±0.031±0.014±0.023 | 0.975 ±0.011 | 1.304 | 1.385 |
Line 12 | 0.283 ±0.001 | 1.300 ±0.031±0.014±0.023 | 0.983 ±0.007 | 1.312 | 1.385 |
Line 13 | 0.290 ±0.002 | 1.294 ±0.031±0.014±0.023 | 0.983 ±0.008 | 1.304 | 1.386 |
Line 14 | 0.317 ±0.002 | 1.292 ±0.031±0.014±0.023 | 0.981 ±0.008 | 1.310 | 1.387 |
Line 15 | 0.497 ±0.001 | 1.280 ±0.031±0.014±0.023 | 0.971 ±0.012 | 1.290 | 1.389 |
Line 16 | 0.348 ±0.001 | 1.301 ±0.031±0.014±0.023 | 0.979 ±0.009 | 1.301 | 1.389 |
Line 17 | 0.366 ±0.001 | 1.323 ±0.031±0.014±0.023 | 0.978 ±0.009 | 1.297 | 1.390 |
Notes. The quantities phydro, p0 and fo−g are derived from hydrodynamical model.
The observational projection factors pobs is derived from HARPS-N and FLUOR/CHARA interferometric data using the inverse BW approach (Sect. 3.2).
The fgrad coefficient involved in the projection factor decomposition (p = p0fgradfo−g, Nardetto et al. 2007) is derived from Eqs. 5 and 6 (Sect. 4.2).
The inverse projection factors phydro is calculated with the hydrodynamical model (Sect. 4.1).
The modeled geometric projection factor p0 is derived in the continuum next to each spectral line. The fo−g quantity, which is obtained using the projection factor decomposition (), is derived in Sect. 5.
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