Ion-Neutral Drift Velocity as a Diagnostic of Dust Growth and Magnetic Field in Star-Forming Environments
Haruka Fukihara, Yusuke Tsukamoto, Hiroyuki Hirashita, Doris Arzoumanian, Yoshiaki Misugi
TL;DR
This paper investigates how dust growth via accretion and coagulation influences ion–neutral drift in star-forming environments, with ambipolar diffusion linking dust microphysics to magnetic field evolution. Using self-consistent dust evolution and ionization chemistry in one-zone molecular cloud and dense-core models, the authors compute ambipolar resistivity $\eta_A$ and the resulting drift velocity $v_{\rm drift}$, finding that core-scale $v_{\rm drift} \sim 100$ m s$^{-1}$ is achievable only if grains grow substantially and the magnetic field is $\sim 2\times 10^2$ μG. They further show that cloud-scale drift is more degenerate with dust growth and $B$, limiting its diagnostic power at those scales. The results support using ion–neutral drift measurements as a diagnostic to constrain the dust size distribution and magnetic field strength in cores, consistent with observations like coreshine and the L1544 core, while highlighting the need for multi-dimensional, time-dependent modeling to capture realistic contraction and coagulation histories.
Abstract
Recent observations have revealed that the ion-neutral drift velocity in star-forming molecular clouds and dense cores is on the order of 100 m s^-1. Theoretical studies have shown that, in ambipolar diffusion, the process responsible for the differential motion between ions and neutrals, the dust size distribution has a significant impact on the magnetic resistivities. In this study, we perform simulations to investigate how dust growth through accretion and coagulation affects the ion-neutral drift velocity in molecular clouds and cores. We find that, on core scales, both dust growth and a magnetic field strength of 200 microgauss are required to reproduce the observed drift velocity. We suggest that measurements of ion-neutral drift velocity, particularly on core scales, may serve as a new diagnostic to constrain the dust size distribution and magnetic field strength in such environments.
