RE-EXAMINING LARSON'S SCALING RELATIONSHIPS IN GALACTIC MOLECULAR CLOUDS
The properties of Galactic molecular clouds tabulated by Solomon et al. (SRBY) are re-examined using the Boston University-FCRAO Galactic Ring Survey of 13CO J = 1–0 emission. These new data provide a lower opacity tracer of molecular clouds and improved angular and spectral resolution compared with previous surveys of molecular line emission along the Galactic Plane. We calculate giant molecular cloud (GMC) masses within the SRBY cloud boundaries assuming local thermodynamic equilibrium (LTE) conditions throughout the cloud and a constant H2 to 13CO abundance, while accounting for the variation of the 12C/13C with galactocentric radius. The LTE-derived masses are typically five times smaller than the SRBY virial masses. The corresponding median mass surface density of molecular hydrogen for this sample is 42 M☉ pc−2, which is significantly lower than the value derived by SRBY (median 206 M☉ pc−2) that has been widely adopted by most models of cloud evolution and star formation. This discrepancy arises from both the extrapolation by SRBY of velocity dispersion, size, and CO luminosity to the 1 K antenna temperature isophote that likely overestimates the GMC masses and our assumption of constant 13CO abundance over the projected area of each cloud. Owing to the uncertainty of molecular abundances in the envelopes of clouds, the mass surface density of GMCs could be larger than the values derived from our 13CO measurements. From velocity dispersions derived from the 13CO data, we find that the coefficient of the cloud structure functions, v° = σv/R1/2, is not constant, as required to satisfy Larson's scaling relationships, but rather systematically varies with the surface density of the cloud as ∼Σ0.5 as expected for clouds in self-gravitational equilibrium.
Memo
- 12CO J = 1-0は光学的に厚く、雲構造が隠され表面輝度プロファイルを平坦化するため、サイズや輝度の過大評価につながる
- 分子雲の特にエンベロープにおいては高い柱密度のH2領域を持っているものの13CO J = 1-0放射をしない成分が存在するため、LTE下でのCOとH2の存在比一定の仮定で導出された分子雲質量は本来の質量に対し過小評価される可能性がある
- 雲質量Mと表面密度Σから、ビリアル平衡下で以下のことが言える(Larson 1981)
- GRSでの13CO観測から導出されたサイズ、線幅、表面密度は上記の関係から逸脱していたものの、Σに対してσv/R^0.5が正の相関があるような一定のスケーリングを示している