We conducted a survey for (CO)-O-18, DCO+, and (HCO+)-C-13 J = 1 --> 0
emission in a sample of low-mass cores previously surveyed in CS, NH3
and C3H2. The DCO+ and (HCO+)-C-13 observations were used to test deu
terium fractionation chemistry models for TMC-1 type clouds. The [DCO/HCO+] fractionation ratio (0.045 +/- 0.014) was found to be in excell
ent agreement with current models. In addition, we did a multiple tran
sition study of DCO+ emission which revealed the presence of denser ga
s (n proportional to 10(5) cm(-3)) than most previous molecular line s
tudies of these cores had found. The observations also suggested that
those cores which are associated with young stars have slightly higher
densities on average than those cores which have no associated star.
We also found that DCO+ line-widths for the cores studied are signific
antly broader than the previously observed NH, line widths. The DCO+ l
ine width broadening does not appear to be entirely an opacity effect.
Instead, the broader line width suggests the presence inside the core
of a dense supersonic gas component not traced by NH3.