The rate coefficients for the removal of O(¹D) by N₂, O₂, N₂O, CO₂, O₃ and n-butane were measured between 210 and 370 K. The appearance of O(³P) was observed following photolytic production of O(¹D) in an excess of the reactants. The measured rate coefficients in this study, in units of 10⁻¹⁰ cm³ molecule⁻¹ s⁻¹, are: k₁(N₂) = (0.195 ± 0.020)exp((125 ± 20)/T); k₂(O₂) = (0.365 ± 0.023)exp((22 ± 10)/T); k₃(N₂O) = (1.17 ± 0.20)exp((40 ± 50)/T); k₄(CO₂) = (0.79 ± 0.07)exp((110 ± 20)/T); k₅(O₃) = (2.65 ± 0.35)exp((−20 ± 40)/T); k₆(n-C₄H₁₀) = (5.00 ± 1.55)exp((−10 ± 90)/T). The quoted uncertainties include estimated systematic errors and are at the 95% confidence level. Our results are compared with previous measurements, particularly the very recent data from Strekowski et al. (this issue) and Blitz et al., (this issue), to produce a set of rate coefficients most appropriate for use in atmospheric calculations. The newly recommended rate coefficients, in units of 10⁻¹⁰ cm³ molecule⁻¹ s⁻¹, are: k₁(N₂) = (0.21 ± 0.02)exp((115 ± 10)/T); k₂(O₂) = (0.312 ± 0.025)exp((70 ± 10)/T); k₃(N₂O) = (1.11 ± 0.11)exp((17 ± 40)/T); k₄(CO₂) = (0.74 ± 0.07)exp((133 ± 40)/T); k₅(O₃) = (2.37 ± 0.36)exp((6 ± 15)/T); k₆(n-C₄H₁₀) = (5.35 ± 0.54)exp((−33 ± 32)/T).