Equations and tables are presented from which accurate values can be obtained, in any of several sets of units, for the concentration of oxygen dissolve11 in freshwater in equilibrium with the atmosphere from 0" to 40°C and 0.5 to 1.1 atm. The y are based on values for the Henry coefficient of oxygen, k,,, which have an estimated accuracy of 0.02%. Equations are derived which relate k, to equilibrium concentrations in natilral waters. The equations include corrections for molecular interactions in the vapor pha.;e. Uncertainty about the best way to correct for these interactions limits the estimated act Iracy of the derived values to about & 0.07% at 0°C and 0.04% at 4O"C, but the new results are much more accurate than values from the UNESCO tables. Within their random errors, previous measurements agree very well with the new results. Under equilibrium conditions, and between 0" and 6O"C, the per mil difference between the 340,:3202 abundance ratio in t le dissolved gas and the air is given by 6 = -0.730 + (427/T), where T is in kelvin and the standard deviation is <0.02%0.