Table 4
Median values and 68% confidence intervals for the parameters of TOI-6002 b and TOI-5713 b obtained using EXOFASTv2 for circular and eccentric orbits.
Parameter | Description | TOI-6002 b | TOI-5713 b | ||
---|---|---|---|---|---|
Circular | Eccentric | Circular | Eccentric | ||
Stellar parameters: | |||||
M* | Mass (M⊙) | ![]() |
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0.2653 ± 0.0061 |
R* | Radius (R⊙) | ![]() |
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0.2984 ± 0.0073 | 0 2992+00073 ij. ^--00072 |
L* | Luminosity (10−3 L⊙) | ![]() |
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ρ* | Density (cgs) | ![]() |
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log 𝑔 | Surface gravity (cgs) | 4.998 ± 0.025 | ![]() |
4.912 ± 0.023 | ![]() |
Teff | Effective temperature (K) | ![]() |
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Planetary parameters: | |||||
P | Orbital period (days) | ![]() |
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RP | Planet radius (R⊕) | ![]() |
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TC | Transit time (BJDTDB) | ![]() |
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a | Semi-major axis (AU) | 0.05725 ± 0.00044 | 0.05722 ± 0.00044 | 0.06008 ± 0.00046 | 0.06008 ± 0.00046 |
i | Inclination (Degrees) | ![]() |
89.68 ± 0.21 | ![]() |
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e | Eccentricity | 0 (Fixed) | ![]() |
0 (Fixed) | ![]() |
τcirc | Tidal circularization timescale (Gyr) | ![]() |
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ω* | Argument of periastron (Degrees) | 90 (fixed) | ![]() |
90 (fixed) | ![]() |
Teq | Equilibrium temperature(a) (K) | ![]() |
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RP/R★ | Planet-to-star radius ratio | ![]() |
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a/R★ | Semi-major axis in stellar radii | ![]() |
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δ | (RP/R★)2 (ppt) | ![]() |
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δg′ | Transit depth in ??′ (ppt) | ![]() |
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… | … |
δi′ | Transit depth in i′ (ppt) | ![]() |
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δr′ | Transit depth in r′ (ppt) | ![]() |
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δz′ | Transit depth in z′ (ppt) | ![]() |
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δTESS | Transit depth in TESS (ppt) | ![]() |
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τ | Ingress/egress transit duration (days) | ![]() |
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T14 | Total transit duration (days) | ![]() |
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0.0728 ± 0.0023 |
b | Transit impact parameter | ![]() |
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〈F〉 | Incident flux (S⊕) | ![]() |
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2.4170 ± 0.0881 | ![]() |
d/R* | Separation at mid-transit | ![]() |
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43.3 ± 1.1 | ![]() |
Predicted parameters: | |||||
MP | Planet mass(b) (M⊕) | ![]() |
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K | RV semi-amplitude (m/s) | ![]() |
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TSM | Transmission spectroscopy metric | 60.0 | 50.0 | 38.0 | 40.0 |
MP /M* | Planet-to-star mass ratio (×10−5) | ![]() |
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ρP | Planet mean density (cgs) | ![]() |
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Notes. (a)The equilibrium temperature is estimated supposing a null-albedo and a 100% efficient heat recirculation. (b)The planetary mass is estimated using the Chen & Kipping (2017) mass–radius relation. The radial velocity semi-amplitude (K) is predicted using the estimated mass.
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