The aim of this controlled environment experiment was to quantify the distribution of leaffed-15 N and canopy fed-13 C within nodulating, nonnodulating or N fertilized non-nodulating Cicer arietinum L. and in their surrounding rhizosphere soil, excluding soil+root respiration. Nodulating chickpea partitioned 32% of its total N and 27% of its total recoverable C below-ground, of which only 50% of N and 36% of C were in the clean root fraction. Non-nodulating chickpea allocated equal recoverable C but slightly less N (28%) below-ground but lost less C from plant induced below-ground respiration. The importance of this below-ground partitioning for crop systems C and N balances is highlighted by their large (45% and 33%, for N and C, respectively) contribution to the total plant derived residue (recyclable) fraction. Recovered 15 N and 13 C were greater (P<0.05) in the outer-rhizosphere (459µg 15 N and 3.2 mg 13 C core −1 ) than in the inner-rhizosphere soil (detached from roots during freeze-drying; 18µg 15 N and 67µg 13 C core −1 ) in relation with the relative size of these compartments. This highlights the significance of the outerrhizosphere soil when estimating C and N budgets and quantifying rhizodeposition, and the benefit of a double ( 15 N, 13 C) isotope approach to determine this flow against large background soil C and N pools.