Mj. Barlow et al., FIRST RESULTS FROM THE UHRF - ULTRA-HIGH-RESOLUTION OBSERVATIONS OF ATOMIC INTERSTELLAR LINES TOWARDS ZETA-OPHIUCHI, Monthly Notices of the Royal Astronomical Society, 272(2), 1995, pp. 333-345
We present ultra-high-resolution observations of optical interstellar
lines towards zeta Oph obtained during the commissioning phase of the
new Ultra-High-Resolution Facility (UHRF) at the AAT. The UHRF has ach
ieved its design resolving power of R approximate to 10(6), and has ve
ry clearly resolved hyperfine splitting in three of the 11 identified
Na I D-line velocity components towards zeta Oph. In addition, the int
rinsic line profiles of the 3s-4p Na I doublet at 3302 Angstrom have b
een measured for the first time. 12 velocity components are identified
in the interstellar Ca II K-line absorption profile, of which seven h
ave definite velocity counterparts in the Na I profile. Three of the N
a I velocity components have b-values which correspond to a gas temper
ature of about 200 K, for the case of pure thermal broadening. The str
ongest component in the sightline (-14.8 km s(-1)) was found to have a
b-value of 0.6(-0.1)(+0.2) km s(-1), corresponding to a temperature o
f 500 K. If a true gas kinetic temperature of 54 K is assumed to apply
to this component, from the H-2 rotational excitation temperature pre
viously measured for the zeta Oph sightline, then the observed Na I an
d Fe I line profiles both imply an rms turbulent velocity of 0.4 km s(
-1) within the cloud, just less than the local sound speed. The observ
ed Ca II linewidths are all significantly larger than those of the cor
responding Na I components. The Ca II components are interpreted as ar
ising from warm neutral material (intercloud medium) surrounding coole
r clouds, while half of the Na I components arise from cool clouds and
half arise from warm intercloud material. The measured Na I/Ca II col
umn density ratios, and the inferred temperatures, are consistent with
a model in which calcium is heavily depleted on to grains in cool clo
uds but is restored to the gas phase by impact desorption in the warm
intercloud medium.