Carbon dioxide is abundant in ice mantles of dust grains; some is found in the pure crystalline form as inferred from the double peak splitting of the bending profile at about 650 cm −1 . To study how CO 2 segregates into the pure form from water-rich mixtures of ice mantles and how it then crystallizes, we used Reflection Absorption InfraRed Spectroscopy (RAIRS) to study the structural change of pure CO 2 ice as a function of both ice thickness and temperature. We found that the ν 1 + ν 3 combination mode absorption profile at 3708 cm −1 provides an excellent probe to quantify the degree of crystallinity in CO 2 ice. We also found that between 20 and 30 K, there is an ordering transition that we attribute to reorientation of CO 2 molecules, while the diffusion of CO 2 becomes significant at much higher temperatures. In the formation of pure crystalline CO 2 in ISM ices, the rate limiting process is the diffusion/segregation of CO 2 molecules in the ice instead of the phase transition from amorphous to crystalline after clusters/islands of CO 2 are formed.