The North China Plain (NCP) is one of the major crop production areas in China. However, severe water shortage is the primary limiting factor in this area. Quantifying evaporation loss under different cover types will make a huge contribution to reduce water consumption. This research estimated the evaporation from pan, bare soil, and irrigated winter wheat–summer maize field in the NCP using the isotope method. The results showed that the evaporation from the pan was the highest, followed by bare soil, while that from the soil surface with crop cover was the lowest. Water loss associated with soil particles and crop cover was decreased for 9 %∼77 %. The source of soil moisture was primary groundwater during the wheat season (April–June) and precipitation in the maize season (July–September). The crop field soil evaporation depth was 0–30 cm, which will be beneficial in determining the subsurface drip irrigation depth. This research will provide a scientific basis for developing an agricultural water-saving strategy for the NCP.