SIMBAD references

The sulfur chemistry in protoplanetary disks influences the properties of nascent planets, including potential habitability. Although the inventory of sulfur molecules in disks has gradually increased over the last decade, CS is still the most commonly observed sulfur-bearing species, and it is expected to be the dominant gas-phase sulfur carrier beyond the water snow line. Despite this, few dedicated multiline observations exist, and thus, the typical disk CS chemistry is not well constrained. Moreover, it is unclear how that chemistry-and in turn, the bulk volatile sulfur reservoir-varies with stellar and disk properties. Here, we present the largest survey of CS to date, combining both new and archival observations from the Atacama Large Millimeter/submillimeter Array, Submillimeter Array, and Northern Extended Millimeter Array of 12 planet-forming disks, covering a range of stellar spectral types and dust morphologies. Using these data, we derived disk-integrated CS gas excitation conditions in each source. Overall, CS chemistry appears similar across our sample with rotational temperatures of ≈10-40 K and column densities between 10¹² and 10¹³ cm^–2. CS column densities do not show strong trends with most source properties, which broadly suggests that CS chemistry is not highly sensitive to disk structure or stellar characteristics. We do, however, identify a positive correlation between stellar X-ray luminosity and CS column density, which indicates that the dominant CS formation pathway is likely via ion-neutral reactions in the upper disk layers, where X-ray-enhanced S⁺ and C⁺ drive abundant CS production. Thus, using CS as a tracer of gas-phase sulfur abundance requires a nuanced approach that accounts for its emitting region and dependence on X-ray luminosity.