2007ApJ...665..457A

High-resolution molecular line observations of CS (J=2⟶1), HCO⁺ (J=1⟶0), C¹⁸O (J=1⟶0), C¹⁸O (J=2⟶1), and N₂H⁺ (J=1⟶0) were obtained toward the starless globule FeSt 1-457 in order to investigate its kinematics and chemistry. The HCO⁺ and CS spectra show clear self-reversed and asymmetric profiles across the face of the globule. The sense of the observed asymmetry is indicative of the global presence of expansion motions in the outer layers of the globule. These motions appear to be subsonic and significantly below the escape velocity of the globule. Comparison of our observations with near-infrared extinction data indicate that the globule is gravitationally bound. Taken together, these considerations lead us to suggest that the observed expansion has its origin in an oscillatory motion of the outer layers of the globule, which itself is likely in a quasi-stable state near hydrostatic equilibrium. Analysis of the observed line widths of C¹⁸O and N₂H⁺ (J=1⟶0) confirm that thermal pressure is the dominant component of the cloud's internal support. A simple calculation suggests that the dominant mode of pulsation would be an l=2 mode with a period of ∼3x10⁵ yr. Deformation of the globule due to the large amplitude l=2 oscillation may be responsible for the double-peaked structure of the core detected in high-resolution extinction maps. Detailed comparison of the molecular-line observations and extinction data provides evidence for significant depletion of C¹⁸O and perhaps HCO⁺, while N₂H⁺ (J=1⟶0) may be undepleted to a cloud depth of ∼40 mag of visual extinction.