Перейти к основному содержанию
AkademIndex

Продукты

Для разработчиков

AkademBaseОткрытый API экосистемы
Статья

Re-examining Larson’s Scaling Relationships in Galactic Molecular Clouds

M. H. HeyerDepartment of Astronomy, University of Massachusetts, Amherst, MA 01003-9305, USAColeman KrawczykDepartment of Astronomy, University of Massachusetts, Amherst, MA 01003-9305, USAJulia Román-DuvalInstitute for Astrophysical Research, Boston University, Boston, MA 02215, USAJames M. JacksonInstitute for Astrophysical Research, Boston University, Boston, MA 02215, USA
2013en
ABI

Аннотация

The properties of Galactic molecular clouds tabulated by Solomon et al. (1987) (SRBY) are re-examined using the Boston University-FCRAO Galactic Ring Survey of 13 CO J=1-0 emission. These new data provide a lower opacity tracer of molecular clouds and improved angular and spectral resolution compared to previous surveys of molecular line emission along the Galactic Plane. We calculate GMC masses within the SRBY cloud boundaries assuming LTE conditions throughout the cloud and a constant H2 to 13 CO abundance, while accounting for the variation of the 12 C / 13 C with Galacto-centric 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 13 CO 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 giant molecular clouds could be larger than the valued derived from our 13 CO measurements. From velocity dispersions derived from the 13 CO data, we find that the coefficient of the cloud structure functions, v ◦ = σv/R 1/2, is not constant, as required to satisfy Larson’s scaling relationships, but rather systematically varies with the surface density of the cloud as ∼ Σ 0.5 as expected for clouds in self-gravitational equilibrium.

Перевод пока недоступен

Цитирования и источники

Цитирований: 2Использованных источников: 0