Table C.1
Retrieved parameters and their uncertainties.
| Parameter | Description | Prior} | Luhman 16A | Luhman 16B | ||
|---|---|---|---|---|---|---|
| Free chem. | Dis-eq. | Free chem. | Dis-eq. | |||
| Retrieved | Derived(a) | Retrieved | Derived(a) | |||
| log H2O | H2O abundance | ![]() |
![]() |
![]() |
![]() |
![]() |
| log H218O | H218O abundance | ![]() |
![]() |
![]() |
![]() |
![]() |
| log H217O | H217O abundance | ![]() |
<-7.53 | <-7.01 | <-7.00 | <-6.80 |
| log 12CO | 12CO abundance | ![]() |
![]() |
![]() |
![]() |
![]() |
| log 13CO} | 13CO abundance | ![]() |
![]() |
![]() |
![]() |
![]() |
| log C18O | C18O abundance | ![]() |
<-6.04 | ![]() |
<-6.22 | ![]() |
| log C17O | C17O abundance | ![]() |
<-6.42 | <-6.31 | <-6.46 | <-6.36 |
| log CH4 | CH4 abundance | ![]() |
![]() |
![]() |
![]() |
![]() |
| log NH3 | NH3 abundance | ![]() |
![]() |
![]() |
![]() |
![]() |
| log H2S | H2S abundance | ![]() |
![]() |
![]() |
![]() |
![]() |
| log HF | HF abundance | ![]() |
![]() |
![]() |
![]() |
![]() |
| log CO2 | CO2 abundance | ![]() |
<-5.37 | ![]() |
![]() |
![]() |
| log HCN | HCN abundance | ![]() |
<-6.28 | ![]() |
<-6.52 | ![]() |
| Derived(b) | Retrieved | Derived(b) | Retrieved | |||
| Projected(c) | Projected(c) | Projected(c) | Projected(c) | |||
| [C/H] | Carbon abundance | ![]() |
![]() |
![]() |
![]() |
![]() |
![]() |
![]() |
![]() |
![]() |
|||
| [O/H] | Oxygen abundance | ![]() |
![]() |
![]() |
![]() |
![]() |
![]() |
![]() |
![]() |
![]() |
|||
| [N/H] | Nitrogen abundance | ![]() |
![]() |
![]() |
![]() |
![]() |
![]() |
![]() |
![]() |
![]() |
|||
| [S/H] | Sulphur abundance | ![]() |
![]() |
![]() |
![]() |
![]() |
![]() |
![]() |
![]() |
![]() |
|||
| [F/H] | Fluorine abundance | ![]() |
![]() |
![]() |
![]() |
![]() |
![]() |
![]() |
![]() |
![]() |
|||
| log 12CO/13CO | 12CO/13CO ratio | ![]() |
![]() |
![]() |
![]() |
![]() |
| log C16O/C18O | C16O/C18O ratio | ![]() |
>3.04 | ![]() |
>3.08 | ![]() |
| log C16O/C17O | C16O/C17O ratio | ![]() |
>3.86 | >3.35 | >3.56 | >3.26 |
| log H216O/H218O | H216O/H218O ratio | ![]() |
![]() |
![]() |
![]() |
![]() |
| log H216O/H217O | H216O/H217O ratio | ![]() |
>5.37 | >3.97 | >4.58 | >3.63 |
| log Kzz [cm2 s−1] | Eddy diffusion coefficient | ![]() |
− | ![]() |
− | ![]() |
| Derived(d) | Derived(d) | Derived(d) | Derived(d) | |||
| C/O | C/O ratio | − | ![]() |
![]() |
![]() |
![]() |
| log g [cm s−2] | Surface gravity | ![]() |
![]() |
![]() |
![]() |
![]() |
![]() |
||||||
| v sin i [km s−1] | Projected rotation velocity | ![]() |
![]() |
![]() |
![]() |
![]() |
| vrad [km s−1] | Radial velocity | ![]() |
![]() |
![]() |
![]() |
![]() |
| ∇1 | Temperature gradient at P1 | ![]() |
![]() |
![]() |
![]() |
![]() |
| ∇2 | Temperature gradient at P2 | ![]() |
![]() |
![]() |
![]() |
![]() |
| ∇3 | Temperature gradient at P3 | ![]() |
![]() |
![]() |
![]() |
![]() |
| ∇4 | Temperature gradient at P4 | ![]() |
![]() |
![]() |
![]() |
![]() |
| ∇5 | Temperature gradient at P5 | ![]() |
![]() |
![]() |
![]() |
![]() |
| log P3 [bar] | Pressure of central knot | ![]() |
![]() |
![]() |
![]() |
![]() |
| T3 [K] | Temperature at central knot | ![]() |
![]() |
![]() |
![]() |
![]() |
| Δlog P23 [bar] | Separation of P2 and P3 | ![]() |
![]() |
![]() |
![]() |
![]() |
| Δlog P34 [bar] | Separation of P3 and P4 | ![]() |
![]() |
![]() |
![]() |
![]() |
| log κcl,0 [cm2 g−1] | Cloud-base opacity | ![]() |
![]() |
![]() |
![]() |
![]() |
| log Pcl,0 [bar] | Cloud-base pressure | ![]() |
![]() |
![]() |
![]() |
![]() |
| fsed | Cloud-opacity decay | ![]() |
![]() |
![]() |
![]() |
![]() |
| log a | GP amplitude | ![]() |
![]() |
![]() |
![]() |
![]() |
| log ℓ [km s−1] | GP length-scale | ![]() |
![]() |
![]() |
![]() |
![]() |
| Δ BIC | 0 | −20.31 | 0 | −305.67 | ||
Notes. (a) The disequilibrium mixing ratios are not directly retrieved but instead derived near the photosphere, at 2 bar. (b) The free-chemistry elemental abundances and isotopologue ratios are derived from the retrieved VMRs above. (c) The elemental abundances are projected onto the expected surface gravities, as described in Sect. 3.2 and shown in brackets. (d) The C/O ratios derived from the free-chemistry model trace only the gaseous carbon and oxygen, while the disequilibrium model accounts for oxygen condensation.
Current usage metrics show cumulative count of Article Views (full-text article views including HTML views, PDF and ePub downloads, according to the available data) and Abstracts Views on Vision4Press platform.
Data correspond to usage on the plateform after 2015. The current usage metrics is available 48-96 hours after online publication and is updated daily on week days.
Initial download of the metrics may take a while.












































































































































































































