Characterize silane chemistry and quenching in hydrogen-rich envelopes

Characterize the reaction kinetics and rate-limiting pathways governing silane decomposition and silicon-carbide formation in dense, highly reducing hydrogen-dominated sub-Neptune envelopes, and determine the resulting silane quench pressures and observable abundances.

Background

The predicted visibility of SiH4_4 depends sensitively on whether silane is removed through SiC condensation before atmospheric transport quenches the chemistry. Existing kinetic measurements were obtained in neutral gases or semiconductor-processing environments rather than in the dense, reducing hydrogen atmospheres relevant to sub-Neptunes.

The paper notes that SiC formation may proceed through multiple reactions, so silane decomposition may not be the rate-limiting step. Consequently, current quench-pressure estimates and predictions for silane spectral features remain uncertain.

References

Going beyond equilibrium chemistry for silicon hydrides is difficult, as the kinetics of the relevant reactions, and indeed of SiH$_4$ in sub-Neptune atmospheres, are not well understood.

Magnesium silicate condensation in sub-Neptune envelopes: the fundamental link between chemistry, structure, and observables  (2608.24873 - Misener et al., 25 Aug 2026) in Section 'Which clouds actually form?'