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The following parameters were measured on seven field plots at 3 sites which had been under organic farming for different periods of time: mineral nitrogen (N min) contents, in situ net nitrogen mineralization (N net), soil microbial biomass carbon (C mic), and nitrogen (N mic) contents, and extractable organic N contents. The measurements were conducted every three weeks from spring 1995/1996 to autumn 1997. The objective was to test whether, under organic farming: 1) temporal fluctuations of Nmic contents over the course of the year are indicative for a source‐and‐sink function for plant‐available N of the soil microbial biomass, and 2) temporal variations in Nmic content can be related with in situ Nnet or plant N uptake. Nmin contents gradually increased after ploughing in autumn until late winter. During intensive plant growth in spring, values rapidly declined. In situ Nnet fluctuated only moderately and reached high values during intensive plant growth (May—July) as well as after soil cultivation in autumn. The Cmic and Nmic contents generally were low in winter, increased in spring and reached maxima in late spring or summer. In spring, the increase in Cmic contents preceded the increase in Nmic contents, resulting in elevated Cmic:Nmic ratios until shooting of winter wheat. This corresponds to an uptake of available soil nitrogen by the plants at the expense of soil micro‐organisms. The subsequent increase in Nmic contents, coinciding with high plant N uptake rates, indicates an enhanced, plant‐induced N mobilization at that time. Possible mobilization mechanisms are discussed. Soil microbial biomass exerted a source‐and‐sink function for extractable organic N on some of the field plots. Estimates of in situ Nnet measurements were neither correlated significantly with soil microbial biomass N, Nmic flux, Nmic turnover, nor with plant N uptake. Lower Nmic turnover rates on 41 years versus 3 years organically managed fields indicate a stabilizing effect of organic farming on soil microflora. 相似文献