Secular Excitation of Polar Neptune Orbits in Pure Disk-Planet Systems
Luke B. Handley, Konstantin Batygin
TL;DR
The paper addresses why Neptune-mass planets around Sun-like stars show a bimodal distribution of spin–orbit angles, particularly polar orbits at short periods. It proposes a self-contained mechanism operating during disk dispersal: photoevaporation opens a gap near $1$ au, the inner disk precesses rapidly under the outer disk while the outer disk erodes, and as the inner edge shrinks its precession slows until crossing a secular resonance with the planet’s $J_2$-driven precession, leading to adiabatic capture into a polar configuration. Using a decoupled disk–planet framework with softened Laplace–Lagrange coefficients, an extended Hamiltonian reduction to Henrard’s second fundamental model of resonance shows that Neptune-mass planets can be driven to $i_N\sim90^{\circ}$ for plausible disk parameters without requiring giant perturbers. The model aligns with observations of Neptune obliquities, offers falsifiable predictions for young systems, and highlights the imprints of disk dispersal on planetary architectures, suggesting that primordial disk processes play a significant role in shaping spin–orbit distributions.
Abstract
The stellar spin-orbit angles of Neptune-sized planets present a primordial yet puzzling view of the planetary formation epoch. The striking dichotomy of aligned and perpendicular orbital configurations are suggestive of obliquity excitation through secular resonance -- a process where the precession of a hot Neptune becomes locked onto a forcing frequency, and is slowly guided into a perpendicular state. Previous models of resonant capture have involved the presence of companion perturbers to the star-planet-disk system, but in most cases, such companions are not confirmed to be present. In this work, we present a mechanism for exciting Neptunes to polar orbits in systems without giant perturbers, where photo-evaporation is the self-contained mechanism. Photo-evaporation opens a gap in the protoplanetary disk at ~1 au, and the inner disk continues to viscously accrete onto the host star, precessing quickly due to the perturbation of the outer disk. As the inner disk shrinks, it precesses more slowly, and encounters a resonance with the J2 precession of the Neptune, quickly exciting it to a polar configuration. While likely not applicable to more massive planets which trigger back-reactions onto the disk, this mechanism reproduces the obliquities of small planets in multiple respects.
