SUMMARYWe investigated interactions between the effects of elevated atmospheric carbon dioxide concentrations g and soil water availability on root biomass, root length and nutrient uptake by spring wheat {Triticum aestivum cv. Tonic). We grew plants at 350 and 700/^mol mol"^ COg and with frequent and infrequent watering ('wet' and ' dry' treatments, respectively). Water use per plant was 1-25 times greater at 350 than at 700 /^mol COg mol~^, and 1-4 times greater in the 'wet' tban in the 'dry' treatment. Root biomass increased with [COJ and with watering frequency. Elevated [COg] changed tbe vertical distribution of tbe roots, witb a greater stimulation of root growtb in tbe top layers of the soil. These data were confirmed by tbe video data of root lengths in the 'dry' treatment, which showed a delayed root development at depth under elevated [COg]. The apparent amount of N mineralized appeared to be equal for all treatments. Nutrient uptake was affected by [COg] and by watering frequency, and there were interactions between these treatments. Tbese interactions were different for N, K and P, which appeared to be related to differences in nutrient availability and mobility in the soil. Moreover, these interactions changed witb time as tbe root system became larger with [COJ and witb watering frequency, and as fluctuations in soil moisture contents increased. Elevated [COg] affected nutrient uptake in contrasting ways. Potassium uptake appeared to be reduced by the smaller mass flow of water reaching the root surface. However, this might be countered with time by the greater root biomass at elevated [COJ, by tbe greater soil moisture contents at elevated [COg], enabling faster diffusion, or botb. Pbosphorus uptake appeared to be increased by tbe greater root biomass at elevated [CO2]. We conclude that plant nutrient uptake at elevated [COJ is affected by interactions witb water availability, tbough differences between nutrients preclude generalizations of the response.