New Zealand Scholarship Earth and Space Science study materials
New Zealand Scholarship Earth and Space Science study resources

A low-density planet in the habitable zone?

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A low-density planet in the habitable zone?

An M-dwarf star of 0.80 M☉ and 0.75 R☉ (Teff 4800 K) shows a periodic 1.20% dimming every 12.30 days. The transit lasts 3.1 hours and has a flat bottom. Radial-velocity measurements give a semi-amplitude K = 8.0 ± 0.6 m/s. No secondary eclipse is detected to a limit of 30 ppm; odd–even transit differences are <5 ppm; the transit centroid shift is <0.1 pixel. The star rotates every 18 days with 1.5% photometric variability. Assuming the signal is a planet, its radius is 8.9 R⊕ and its mass is 25 M⊕. The calculated equilibrium temperature is about 590 K for an albedo of 0.3. A colleague claims this is a rocky planet in the habitable zone.

1. Assess whether the transit signal is most likely a planet, an eclipsing binary, or a blended background eclipsing binary. Use the RV, odd–even, centroid and secondary-eclipse evidence.

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Most likely a planet. The RV signal at the transit period with K = 8 m/s is direct evidence of a companion mass; an eclipsing binary would normally produce a much larger RV amplitude and a deep secondary eclipse. The flat-bottomed transit, the absence of odd–even differences (<5 ppm), and the tiny centroid shift (<0.1 pixel) argue against a blended background eclipsing binary. The 30 ppm secondary-eclipse limit is consistent with a planet that is not self-luminous; a stellar companion would produce a much larger secondary. Stellar rotation is 18 days, far from 12.3 days, and the 1.5% variability is not phased with the transit, so starspots are unlikely to be the cause. A planet is the best explanation, though a diluted binary cannot be fully excluded without high-resolution imaging.

2. Calculate the planet's mean density and evaluate whether a rocky composition is possible. What does the density imply about its envelope?

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Density scales as mass divided by radius cubed. Relative to Earth: ρ/ρ⊕ = (M/M⊕)/(R/R⊕)^3 = 25 / 8.9^3 = 25/705 ≈ 0.0355. With ρ⊕ = 5.51 g/cm3, the mean density is about 0.20 g/cm3. That is far below rock (~3–5 g/cm3) and even below water (1 g/cm3); it is comparable to a very low-density gas envelope. A 25 M⊕ body with radius 8.9 R⊕ cannot be rocky: a rocky planet of that mass would be roughly 1.8 R⊕. The radius requires a thick H/He envelope or a very volatile-rich interior, so this is a mini-Neptune or sub-Saturn, not a rocky planet. Radius uncertainty matters, but even a 20% smaller radius would leave the density below about 0.4 g/cm3.

3. The colleague calls it 'a rocky planet in the habitable zone'. Critically evaluate that claim, including the equilibrium temperature and the prospects for life.

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The claim is wrong on two counts. First, the density shows no solid surface; it is a gas-enveloped planet. Second, an equilibrium temperature of about 590 K is too hot for liquid water at the surface even before greenhouse warming, and the planet orbits well inside the conservative habitable zone for a 4800 K star. A hydrogen-rich atmosphere could have a deep hot interior and no habitable surface. The planet may be useful for atmospheric studies because its large scale height gives a strong transmission signal, but it is not a rocky habitable-zone planet. Any claim of habitability would require a measured mass, radius, atmospheric composition, and evidence of a solid surface or moons; none is established.