Cr 1−x Ti x O 2 (0 ≤ x ≤ 1) solid solution was synthesized by a high-pressure and high-temperature method, whereafter systematic experimental and computational studies were conducted on the Cr 1−x Ti x O 2 system. The crystal structure of the samples where 0 ≤ x ≤ 0.4 and x = 1 was of a rutile structure (P4 2 /mnm), while samples where 0.5 ≤ x ≤ 0.9 crystallized in a CaCl 2 structure (Pnnm). The structural transformation from rutile-type to CaCl 2 -type structure should be due to the combined action of positive chemical pressure and physical pressure. The saturation magnetization of the Cr 1−x Ti x O 2 samples decreased linearly with the increase of x because Ti 4+ is nonmagnetic. In addition, the Curie temperature of the Cr 1−x Ti x O 2 samples also decreased noticeably with the increase of x. When nonmagnetic Ti 4+ randomly replaced Cr 4+ and occupied its position, the net exchange coupling in Cr 1−x Ti x O 2 would decrease. When Ti 4+ occupied the majority in the system, Cr 4+ ions would be separated by nonmagnetic Ti 4+ ions far enough for the long-range ferromagnetic order to weaken or even disappear with the increase of x, causing the Cr 1−x Ti x O 2 system to finally approach a paramagnetic state. Density functional theory calculations were performed for the Cr 1−x Ti x O 2 system, and the predicted trends of the magnetic properties agreed well with the experimental results. These calculations also showed that Cr 1−x Ti x O 2 was still half-metallic until x reached 0.6.