An edge-on point-mass Hill model gives a 3.79% radius correction for TOI-6255 b at saved catalog inputs
We tested the leading-order shape formula for the five lava planets in JWST program 8864. We used a frozen NASA Planetary Systems extract from 24 October 2026. Four targets have measured masses in that extract. For each, we solved the closed point-mass Hill surface that has the catalog transit area. The model assumes a circular synchronous orbit, zero obliquity, and an edge-on view. For TOI-6255 b, the nonlinear volume-radius increase is 3.79%, compared with 3.09% at leading order. Its quadrature-area increase is 10.63%, compared with 7.94%. For TOI-2431 b, the corresponding nonlinear increases are 2.68% and 7.34%. Corrections are smaller for TOI-1807 b and TOI-431 b. TOI-2260 b has no measured mass in the source extract, so we give an assumed mass grid. Eight marginal error corners per measured-mass target test input sensitivity. They are not confidence intervals. Angular convergence, an independent surface mesh, weak and critical limits, and full circular Roche controls test the numerical method. The finite-mass controls change the central radius and area corrections by less than 0.0003 percentage points. A second-order series gives an additional algebra check. These results are a numerical reference set. They do not measure planetary shapes or include rigidity and deformation of planetary self-gravity. The package preserves source code, frozen data, provenance, figures, numerical checks, and reproduction instructions.
tidal deformation · Hill potential · Roche potential · lava planets · transit radius · projected area · JWST program 8864 · TOI-6255 b · TOI-2431 b · reproducible calculation
References
11- usesdoi:10.26133/NEA12
The frozen NASA Planetary Systems extract supplies the input values and source labels.
- usesdoi:10.48550/arXiv.2609.20155
Version 2 defines the fixed five-target sample for JWST program 8864 and states that the TOI-2260 b mass is a prediction.
- doi:10.1051/0004-6361/201015811
Prior theory gives shape and transit-radius corrections for distorted planets.
- doi:10.48550/arXiv.2310.03553
Prior work includes tidal deformation in planetary phase curves.
- doi:10.21105/joss.06972
The squishyplanet tool models non-spherical transits and phase signals. We do not use its code.
- doi:10.48550/arXiv.2610.22338
Prior work tests the measurement of giant-planet deformation with JWST and Ariel.
- usesdoi:10.3847/1538-4365/ad4484
The saved PS row cites this source for TOI-1807 b planet parameters.
- usesdoi:10.3847/1538-3881/ac4334
The saved PS row cites this source for TOI-2260 b. No measured mass is present.
- usesdoi:10.1093/mnras/stab2313
The saved PS row cites this source for TOI-431 b parameters.
- usesdoi:10.3847/1538-3881/ad5a7d
The saved PS row cites this source for TOI-6255 b. The paper already predicts tidal distortion and an approximate radius correction.
- usesdoi:10.1051/0004-6361/202556365
The saved PS row cites this final source for TOI-2431 b. We preserve its catalog values and report their difference from the first arXiv draft.
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