Abstract
Aims. We test the use of three common molecular ions, ortho-H2D+ (oH2D+), N2H+, and DCO+, as probes of the internal structure and kinematics of a dense, starless molecular cloud core.
Methods. The pre-stellar core H-MM1 in Ophiuchus was mapped in the oH2D+(110 − N2H+(4 − 3), and DCO+ (5 − 4) lines with the Large APEX sub-Millimeter Array (LAsMA) multi-beam receiver of the Atacama Pathfinder EXperiment (APEX) telescope. We also ran a series of chemistry models to predict the abundance distributions of the observed molecules, and to estimate the effect of the cosmic-ray ionisation rate on their abundances.
Results. The three line maps show different distributions. The oH2D+ map is extended and outlines the general structure of the core, N2H+ mainly shows the density maxima, and the DCO+ emission peaks are shifted towards one edge of the core where a region of enhanced desorption had previously been found. According to the chemical simulation, the fractional oH2D+ abundance remains relatively high in the centre of the core, and its column density correlates strongly with the cosmic-ray ionisation rate, ζH2. Simulated line maps constrain the cosmic-ray ionisation rate to be low, between 5 × 10−18 s−1 and 1 × 10−17 s−1 in the H-MM1 core. This estimate agrees with the gas temperature measured in the core.
Conclusions. The present observations show that very dense, cold gas in molecular clouds can be traced by mapping the ground-state line of oH2D+ and high-J transitions of DCO+ and N2H+, despite the severe depletion of the latter two molecules. Modelling line emission of oH2D+ provides a straightforward method of determining the cosmic-ray ionisation rate in dense clouds, where the primary ion, H3+, is not observable.