We present observations of 10 deuterated molecular species in the dark clouds TMC-1, L183, and the translucent object CB 17, as well as a subset of species in and other objects. With sensitive TMCNH 3 observations of the J 1¨0 and 2¨1 transitions of DCN, and DNC, we have been able to derive N 2 D‘, molecular constants that include the complex nuclear quadrupole hyper—ne splitting in these species, which is essential to determine accurate abundances. The spectroscopic results have required, in turn, new radiative transport techniques to handle the hyper—ne eUects. Our abundance determinations also utilize sensitive observations of secondary isotopomers involving 13C, 18O, and 15N. Compared with earlier molecular D/H ratios in the literature, these innovations have resulted in radically diUerent values in some cases in TMC-1 and in TMC-1; DCN/HCN in CB 17), (N 2 D‘/N 2 H‘ TMCNH 3 ;N H 2 D/NH 3 and important modi—cations in others in TMC-1). The new techniques usually produce (C 3 HD/C 3 H 2 deuteration ratios lower than those obtained earlier by simpler methods. Thus, in addition to the special cases noted above, our results are generally lower than previous ones by factors of typically 2. We also —nd that deuteration occurs only in regions of high density, while nondeuterated species generally reside at lower densities. A recently proposed model of translucent clouds as low-density objects containing embedded small, high-density fragments explains the observations. To study the chemistry of deuterated species, we have used the New Standard Model, modi—ed to include all monodeuterated species, and now containing 9930 reactions and 610 species. Our models explore the dependence of the molecular D/H ratios upon temperature, density, ionization rate, extinction, epoch, and elemental abundances. Within the uncertainties, we —nd agreement between observed and modeled ratios for nearly all species in nearly all sources. Our results generally agree with those of Roberts & Millar in a recent, similar study. We —nd signi—cantly higher ratios in L183 than in TMC, and intermediate values in CB 17. With our lower values in general, however, we believe that L183 is ii normal ˇˇ for a cold dark cloud, CB 17 is typical of a slightly warmer translucent object, and the TMC region is perhaps underdeuterated in general, certainly strongly so in the case of and These N 2 H‘ NH 3 . ii anomalous ˇˇ cases have no plausible single explanation in terms of gas-phase chemistry at this time. Grain processes are implicated. . .. . .. . ..
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