The quantities, Y, of nitrogen taken up, and dry matter produced, at various times during the growth of six winter wheat crops at Rothamsted were shown to be related to thermal time, x, based on soil temperature, by a simple equationwhere A is the ultimate maximum of Y, n a shape factor and k a rate constant that is related to A and n through x', the inflexion point of the function. The value of n was 1.5 for both N uptake and dry matter. The value of A for N uptake, Au, was well described by a multiple regression on sowing data, t,, expressed as the number of days after August 31 st, and rainfall, R~pr, in the April before harvest, but no such regression could be found for the value of A for dry matter, AD. The rate constants, ks and ko, for N-uptake and dry-matter production respectively, could be related to the date of sowing and the weather through the corresponding inflexion points,x'N and x'o. Highly significant regressions were found, for x'u on the time, ts:, between sowing and the return of the soil to field capacity and for x'o on the reciprocal of t~. The function was used to generate N uptake curves from values of Au and ku (obtained from x'u) given by inserting the appropriate values of RApt, t~ and t,:in the regressions. These fitted measured N uptakes satisfactorily for the six crops used to obtain the regressions, and four grown subsequently, at Rothamsted, and also for six crops at Woburn. Values of Ao had to be set arbitrarily because no regression had been found to predict them, but using these arbitrary values in the function gave dry matter curves that fitted the measurements satisfactorily for all ten Rothamsted crops and two of the Woburn crops. Tests for seasonal and site effects showed that Au was influenced more by differences between the two sites than by seasonal differences other than those in RApt, whereas Ao was strongly influenced by these seasonal differencess and very little by those between the sites.