REVIEW 2 major objections 4 minor 119 references
Three Hot Jupiters transiting K-dwarfs with a significant heavy element mass
T0 review · 2 major / 4 minor · reviewed 2026-08-07 · deepseek-v4-flash
Pith's one-line read This paper confirms three hot Jupiters transiting mid-K dwarf stars and infers that each contains a large heavy element mass, between 84 and 114 Earth masses.
desk verdict Three well-confirmed hot Jupiters around mid-K dwarfs, but the heavy-element masses rest entirely on one interior-model grid and need a robustness check before the headline is safe. read the letter →
The pith
A machine-rendered reading of the paper's core claim, the machinery that carries it, and where it could break.
The reading
What carries the argument
The central machinery is the joint-fit modeling of transit photometry and radial velocities using the Juliet code with dynesty nested sampling, which produces the mass and radius from which heavy element content is derived. The heavy element masses come from the published grid of interior models used by the authors, which combines an H/He envelope with the SCvH equation of state, models heavy elements as water that is homogeneously mixed, assumes no central core, and uses an internal luminosity prior; the paper also compares these results to non-inflated models from Fortney et al. (2007) and inflated models from Baraffe et al. (2008). The key physical quantity that carries the argument is the degeneracy between heavy element content and heating efficiency: adding heavy elements shrinks the model radius while adding heating inflates it.
What would settle it
Recompute the three planets' heavy element masses using the more recent Chabrier & Debras (2021) hydrogen-helium equation of state while keeping all other assumptions fixed; if the inferred masses fall below roughly 30-40 Earth masses, the claim that these planets carry a 'significant' heavy element content relative to other K-dwarf hot Jupiters would be refuted.
Extended reading notes
Core claim
The paper establishes that TOI-2969 b, TOI-2989 b, and TOI-5300 b are genuine transiting hot Jupiters, not false positives or stellar companions, and that their bulk properties require large internal heavy element reservoirs. Using a joint fit of satellite and ground-based photometry with radial velocities, the authors derive planetary masses of 1.16±0.04, 3.0±0.2, and 0.6±0.1 Jupiter masses and radii of 1.10±0.08, 1.12±0.05, and 0.88±0.08 Jupiter radii. Through the grid of interior models adopted in their analysis, they infer heavy element masses of 88±30, 114±30, and 84±21 Earth masses (the abstract lists the first as 90±30) and conclude that these values are significantly higher than most reported heavy elements for K-dwarf hot Jupiters. They further note that none of the three planets shows radius inflation despite equilibrium temperatures of 1001-1186 K.
Load-bearing premise
The heavy element masses are inferred from interior models that assume a specific hydrogen-helium equation of state (SCvH), model the heavy elements as water mixed homogeneously, and omit a central core; the paper itself notes that newer equations of state generally predict smaller radii and lower heavy element masses.
Editorial extensions
If this is right
- These three systems add precisely characterized data points to the sparse census of hot Jupiters around mid-K dwarfs, sharpening the measured occurrence rate in a regime where population synthesis models predict very few systems.
- Inferred heavy element masses of 84-114 Earth masses imply these planets formed with or accreted a substantial solid component, a constraint that formation models must reproduce.
- The lack of radius inflation under strong insolation, at least for TOI-2989 b and TOI-5300 b, favors models without efficient interior heating beyond stellar irradiation.
- TOI-2969 b, with an emission spectroscopy metric of 149 and a scale height of 205 km, is a promising target for emission spectroscopy that could probe its atmospheric composition.
Reading between the lines
- If the high heavy element masses survive under newer equations of state, they would suggest that disk solids around low-mass stars can be gathered efficiently, possibly through pebble accretion, to form tens-of-Earth-mass cores before gas accretion.
- The host stars' metallicities straddle zero (0.08, -0.04, -0.17 dex), so if the planets are truly enriched, stellar metallicity alone may not set the planetary heavy element budget; expanding the sample could test that.
- Emission spectroscopy of TOI-2969 b, measuring atmospheric metallicity or C/O ratio, would provide an independent, observable check on the interior-model heavy element masses.
Editorial analysis
A structured set of objections, weighed in public.
Referee Report
Summary. The paper reports the confirmation and characterization of three hot Jupiters transiting mid-K dwarfs: TOI-2969 b (P=1.82 d, M=1.16 M_Jup, R=1.10 R_Jup), TOI-2989 b (P=3.12 d, M=3.0 M_Jup, R=1.12 R_Jup), and TOI-5300 b (P=2.26 d, M=0.6 M_Jup, R=0.88 R_Jup). The analysis combines TESS photometry, ground-based follow-up light curves, speckle interferometry, and CORALIE radial velocities in a joint Juliet/dynesty fit. The authors then use the Sarkis et al. (2021) interior-model grid to infer heavy element masses of 88±30, 114±30, and 84±21 M_Earth, and claim these are significantly higher than most reported heavy element masses for K-dwarf hot Jupiters.
Significance. If confirmed, these three objects add to the sparse sample of gas giants around mid-K dwarfs and provide some of the first heavy-element mass estimates in this regime. The orbital and planetary parameters appear reliable: the transits are confirmed by multiple ground-based light curves, speckle imaging rules out close stellar companions, and the RV semi-amplitudes are detected with high significance. However, the headline claim of 'significant heavy element mass' rests on a single interior-model family, and the comparison to literature is not quantitative. The paper is transparent about these limitations, but the central claim would be much stronger with a systematic error estimate.
major comments (2)
- [Section 6.1] The heavy element masses (88±30, 114±30, 84±21 M⊕) are derived entirely from the Sarkis et al. (2021) model grid, which assumes the SCvH H/He equation of state and no central core. The authors acknowledge in the final paragraph of Section 6.1 that the more recent Chabrier & Debras (2021) EoS 'usually lead to smaller planetary radii and a lower amount of heavy elements', but they do not quantify this shift for their specific targets. The quoted uncertainties therefore reflect only statistical/model-prior scatter, not EoS systematics. Because the title and abstract make the large heavy-element mass the central result, the paper should either (i) recompute the heavy-element masses with the newer EoS or a simple scaling relation (e.g., following Müller et al. 2020), (ii) provide a quantitative estimate of how much the masses would decrease, or (iii) explicitly reframe the claim as conditional on the SCvH EoS. Without one of these, the headline is not robust.
- [Section 6.1] The statement that these heavy element masses are 'significantly higher than most reported heavy elements for K-dwarf Hot Jupiters' is not supported by any quantitative comparison. The references cited (Hartman et al. 2009, 2011; Grunblatt et al. 2017; Torres et al. 2008; Hacker et al. 2024; Delamer et al. 2024; Hellier et al. 2010) are not accompanied by a distribution, a table, or a statistical test. If this claim is a key conclusion, the authors should show where their three planets fall relative to the literature sample, ideally using the same interior-model grid for consistency. Otherwise 'significantly higher' is an unsupported superlative.
minor comments (4)
- [Section 4.4.1] The discussion of TOI-2969's rotation period is confusing: a 26.8-day period is seen in G_BP and G_RP, while a 16-day and a 19-day signal appear in the G band and in all three bands when including the window function; please clarify which period is adopted and why.
- [Section 5] No Gaussian Process model is used, but for TOI-2989 the WASP and Gaia data show a 30-day rotation signal; a brief justification of why activity is negligible for the RV fit would be useful.
- [Section 5.3] For TOI-5300 b, the RV semi-amplitude is 121±22 m/s and the residual RMS is 68 m/s, while the fitted jitter is consistent with zero; the discrepancy between residual RMS and jitter could indicate a slight model mismatch and should be commented on.
- [Table 5] Equilibrium temperatures are listed assuming a Bond albedo of zero; the authors might note that the planets would be cooler for non-zero albedo, although this does not affect the classification.
Circularity Check
No significant circularity: the planet confirmation and orbital characterization are derived from independent photometric and RV data, and the heavy-element masses are explicitly labeled model-dependent inferences from an external grid rather than predictions forced by construction.
full rationale
The paper's central confirmations (orbital periods, radii, masses) follow from joint Juliet fits to TESS, ground-based photometry, and CORALIE RVs, with no parameter fitted to a subset and then renamed as a prediction. The headline heavy-element masses are not observables nor fitted parameters; they are outputs of the externally published Sarkis et al. (2021) interior-model grid, whose assumptions (SCvH EoS, no core, water-like heavy elements) are stated in the text. The paper explicitly flags that the newer Chabrier & Debras (2021) EoS tends to give smaller radii and lower heavy-element masses, which is a model-dependence caveat, not a circular reduction: the masses are not equal to their inputs by construction. The brief Baraffe et al. (2008) radii comparison is presented as a consistency check using fractions derived later in the same section, not as an independent prediction, and it is not the basis of the reported masses. The only self-citations (e.g., Ulmer-Moll et al. 2022 for the M_Z = Z M_p conversion, and the Parc et al. 2024 catalog used in the comparison figure) are methodological or catalog references and are not load-bearing for the main claim. No uniqueness theorem, ansatz, or definitional equivalence is imported from the authors' prior work. Therefore the derivation chain is self-contained, with the usual caveat that interior-composition inferences inherit the assumptions of the chosen model family.
Assumptions & free parameters
free parameters (3)
- Dilution factor for TOI-2969 =
0.79 to 0.91 per light curve
- Planet interior heavy element fraction Z =
0.24 +/- 0.08, 0.12 +/- 0.03, 0.44 +/- 0.08
- Internal luminosity (heating efficiency) =
Not explicitly quoted
assumptions (3)
- domain assumption The Sarkis et al. (2021) interior models, using the SCvH equation of state for H/He, no central core, and heavy elements modeled as water, are accurate enough to infer heavy element masses.
- domain assumption The CORALIE RV variations are caused by the transiting planet and not by stellar activity or an unseen companion.
- domain assumption The transiting objects are confirmed planets and not brown dwarfs or blended eclipsing binaries.
Cite this review
Pith. "Pith review of Three Hot Jupiters transiting K-dwarfs with a significant heavy element mass." pith.science (2026). https://pith.science/paper/VBN25T5N
@misc{pith2026250604923,
author = {Pith},
title = {Pith review of: Three Hot Jupiters transiting K-dwarfs with a significant heavy element mass},
year = {2026},
howpublished = {\url{https://pith.science/paper/VBN25T5N}},
note = {Machine review of arXiv:2506.04923}
}
abstract
Albeit at a lower frequency than around hotter stars, short-period gas giants around low-mass stars ($T_\mathrm{eff} < 4965$ K) do exist, despite predictions from planetary population synthesis models that such systems should be exceedingly rare. By combining data from TESS and ground-based follow-up observations, we seek to confirm and characterize giant planets transiting K dwarfs, particularly mid/late K dwarfs. Photometric data were obtained from the TESS mission, supplemented by ground-based imaging- and photometric observations, as well as high-resolution spectroscopic data from the CORALIE spectrograph. Radial velocity (RV) measurements were analyzed to confirm the presence of companions. We report the confirmation and characterization of three giants transiting mid-K dwarfs. Within the TOI-2969 system, a giant planet of $1.16\pm 0.04\,M_\mathrm{Jup}$ and a radius of $1.10 \pm 0.08\,R_\mathrm{Jup}$ revolves around its K3V host in 1.82 days. The system of TOI-2989 contains a $3.0 \pm 0.2\,M_\mathrm{Jup}$ giant with a radius of $1.12 \pm 0.05\,R_\mathrm{Jup}$, which orbits its K4V host in 3.12 days. The K4V TOI-5300 hosts a giant of $0.6 \pm 0.1\,M_\mathrm{Jup}$ with a radius of $0.88 \pm 0.08\,R_\mathrm{Jup}$ and an orbital period of 2.3 days. The equilibrium temperatures of the companions range from 1001 to 1186 K, classifying them as Hot Jupiters. However, they do not present radius inflation. The estimated heavy element masses in their interior, inferred from the mass, radius, and evolutionary models, are $90 \pm 30\,M_\oplus$, $114 \pm 30\,M_\oplus$, and $84 \pm 21\,M_\oplus$, respectively. The heavy element masses are significantly higher than most reported heavy elements for K-dwarf Hot Jupiters. These mass characterizations contribute to the poorly explored population of massive companions around low-mass stars.
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, " * write output.state after.block = add.period write newline
ENTRY address archiveprefix author booktitle chapter edition editor howpublished institution eprint journal key month note number organization pages publisher school series title type volume year label extra.label sort.label short.list INTEGERS output.state before.all mid.sent...
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write newline
" write newline "" before.all 'output.state := FUNCTION n.dashify 't := "" t empty not t #1 #1 substring "-" = t #1 #2 substring "--" = not "--" * t #2 global.max substring 't := t #1 #1 substring "-" = "-" * t #2 global.max substring 't := while if t #1 #1 substring * t #2 gl...
Reviewed August 7, 2026 · model on record in the stance chip above.
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