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Over N fertilization is a common problem for the winter wheat ( Triticum aestivum L.)–summer maize ( Zea mays L.) rotation system in the North China Plain. A field experiment which included control (no N), conventional N (Con. N) fertilization, and optimized N (N min ) fertilization treatments, was conducted from 1999 to 2003 near Beijing, China. Soil nitrate (NO 3 ) dynamics were measured and N balance was calculated for the period of the eight successive cropping seasons. Soil NO 3 –N in the 0‐ to 90‐cm profile for the Con. N treatment ranged from 157 to 700 kg ha −1 during the eight successive cropping seasons, much greater than those in the no N and optimized N treatments. Large amounts of soil NO 3 –N were detected in the 90‐ to 200‐cm layer under the conventional N fertilization treatment, especially in the summer maize season. For the N min treatment, the total amount of N applied was 511 kg N ha −1 in the eight successive crops as compared with 2400 kg N ha −1 of the Con. N treatment. Grain yields were not different between the fertilized treatments except for maize in 2003. Soil NO 3 –N in the root zone under conditions of optimized N fertilization was maintained at a relatively low level as compared with the Con. N treatment, therefore dramatically decreasing NO 3 –N movement to deeper soil profile. This study indicates that soil NO 3 movement out of the effective crop root zone is an important pathway of N losses in this winter wheat–summer maize rotation system in the North China Plain and the optimized N fertilization by an improved N min method shows high potential of reducing N‐leaching losses.