Carbon dioxide (CO) is among the most abundant interstellar ices and has been observed by JWST in water-rich mixtures and pure CO environments. Astrochemical models adopt binding energies (BEs) measured on water ice because few BEs are available for CO ice. We calculate BE distributions for twelve adsorbates (N, CH, HCl, CH, HS, HF, HCN, HCO, HCOOH, HNC, CHOH, HO) on CO clusters containing two to five molecules using DFT calibrated against CCSD(T)/CBS, a coupled-cluster treatment extrapolated to the complete-basis-set limit. Binding strength depends on whether the adsorbate requires the surface to donate a hydrogen bond (H-bond). CO can accept an H-bond but cannot donate one, and all six species compared with water ice from Ahmad et al. (2026) bind more weakly on CO. The ratio of the BE on CO to water ice ranges from 0.66 for HCO and 0.75 for HO to 0.87 for CHOH, 0.89 for HCOOH and 0.92 for CH. Formaldehyde is predicted to desorb near 57 K from CO-rich ice, compared with 85 K from water-rich ice, and could contribute to cold gas-phase HCO. Although the mean binding energies are changing with cluster size for several species, the differences can be traced to local binding interactions likely to remain important in larger ice models. The BEs vary by more than 500 K between sites, while the desorption peaks range from 11 K for CH to 132 K for HCOOH. The limited H-bonding capacity of CO may favour separation of mixed HO:CO ice into CO-rich domains.

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