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The observational detection of a localized reduction in the small planet occurrence rate, sometimes termed a gap, is an exciting discovery because of the implications for planet evolutionary history. This gap appears to define a transition region in which sub-Neptune planets are believed to have lost their H/He envelope, potentially by photoevaporation or core powered mass loss, and have thus been transformed into bare cores terrestrial planets. Here we investigate the transition between sub-Neptunes and super-Earths using a real sample of observed small close-in planets and applying envelope evolution models of the H/He envelope together with the mass-radius diagram and a photoevaporation model. We find that photoevaporation can explain the H/He envelope loss of most super-Earths in 100Myr, although an additional loss mechanism appears necessary in some planets. We explore the possibility that these planets families have different core mass and find a continuum in the primordial population of the strongly irradiated super-Earths and the sub-Neptunes. Our analysis also shows that close-orbiting sub-Neptunes with R < 3.5 R_oplus typically lose ~ 30% of their primordial envelope.
The majority of exoplanets found to date have been discovered via the transit method, and transmission spectroscopy represents the primary method of studying these distant worlds. Currently, in-depth atmospheric characterization of transiting exoplan
UV radiation can induce photochemical processes in exoplanet atmospheres and produce haze particles. Recent observations suggest that haze and/or cloud layers could be present in the upper atmospheres of exoplanets. Haze particles play an important r
The observed radii distribution of {it Kepler} exoplanets reveals two distinct populations: those that are more likely to be terrestrials ($lesssim1.7R_oplus$) and those that are more likely to be gas-enveloped ($gtrsim2R_oplus$). There exists a clea
One of the most significant advances by NASAs ${mathit Kepler}$ Mission was the discovery of an abundant new population of highly irradiated planets with sizes between the Earth and Neptune. Subsequent analysis showed that at ~1.5 Earth radii there i
Extrasolar planets with sizes between that of the Earth and Neptune ($R_{rm p}=1{-}4~{rm R}_oplus$) have a bimodal radius distribution. This planet radius valley separates compact, rocky super-Earths ($R_{rm p}=1.0{-}1.8~{rm R}_oplus$) from larger su