India is the second largest producer of rice (Oryza sativa L.) in the world and rice is an essential component of the diet for a majority of the population in India. However, detailed studies aimed at the evaluation of radionuclide transfer factors (F v ) for the rice grown in India are almost non-existent. This paper presents the soil to rice transfer factors for natural ( 226 Ra, 228 Ra, 40 K, and 210 Pb) and artificial ( 137 Cs) radionuclides for rice grown in natural field conditions on the West Coast of India. A rice field was developed very close to the Kaiga nuclear power plant and the water required for this field was drawn from the cooling water discharge canal of the power plant. For a comparative study of the radionuclide transfer factors, rice samples were also collected from the rice fields of nearby villages. The study showed that the 226 Ra and 228 Ra activity concentrations were below detection levels in different organs of the rice plant. The soil to un-hulled rice grain 40 K transfer factor varied in the range of 6.5 × 10 −1 to 2.9 with a mean of 0.15 × 10 1 , and of 210 Pb varied in the range of <1.2 × 10 −2 to 8.1 × 10 −1 with a mean of 1.4 × 10 −1 , and of 137 Cs varied in the range of 6.6 × 10 −2 to 3.4 × 10 −1 with a mean of 2.1 × 10 −1 . The mean values of un-hulled grain to white rice processing retention factors (F r ) were 0.12 for 40 K, 0.03 for 210 Pb, and 0.14 for 137 Cs. Using these processing retention factors, the soil to white rice transfer factors were estimated and these were found to have mean values of 1.8 × 10 −1 , 4.2 × 10 −3 , and 3.0 × 10 −2 for 40 K, 210 Pb, and 137 Cs, respectively. The study has shown that the transfer of 40 K was higher for above the ground organs than for the root, but 210 Pb and 137 Cs were retained in the root and their transfer to above the ground organs of the rice plant is significantly lower.