XU Rong-yan, WANG Yi-ning, JIANG Peng, ZHOU Chao, DING Yu-tong, ZHANG Mei-na, GAI Yong-wei, WANG Zhen-long
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In order to investigate the relationship between the changing law of phreatic evaporation of summer maize in sandy ginger black soil and yellow tidal soil of Huaibei Plain and the meteorological factors and burial depth, the meteorological observation and evapotranspiration meter data of Wudaogou Experimental Station from 2011 to 2022 were selected, and the correlation analysis between phreatic evaporation and meteorological factors during the growth period of summer maize was carried out, and multiple linear regression was performed by the stepping method, and the independent variables of the model were analyzed by the pass-through analysis to reveal the main influencing elements of maize phreatic evaporation, and a regression model was established. We also proposed a nonlinear fitting function between phreatic evaporation coefficient and 0.2-5.0 m burial depth. The results show that: ①in the sandy ginger black soil, the phreatic evaporation coefficient was significantly correlated with the water vapor pressure difference at the burial depths of 0.2 m and 0.4 m; with water vapor pressure difference and absolute humidity at the burial depths of 0.6 m;with water vapor pressure difference, sunshine hours, and relative humidity at the burial depths of 1 m. In the yellow tidal soil, the phreatic evaporation coefficient was significantly correlated with the water vapor pressure at the burial depths of 0.2 m, 0.4 m and 1.0 m; with water vapor pressure difference, absolute humidity, and average temperature at the burial depths of 0.4 m. ②The regression models of maize evapotranspiration and meteorological factors were constructed under different soil qualities and burial depths, and the models met the accuracy requirements (R 2>0.810 for the model of sandy ginger and black soil, and R 2>0.800 for the model of yellow tidal soil). ③The nonlinear fitting of the phreatic evaporation coefficient to the burial depth showed a logarithmic function relationship (R 2>0.75) for sand-ginger black soil maize; an inverse function relationship (R 2>0.800) for yellow tidal soil maize at the early and late stages, and an exponential function relationship (R 2>0.950) for the developmental stage and the middle stage. ④The maximum burial depth Zm of summer maize in sandy ginger-black soil was in the range of 2.7~3.1 m; Zm in yellow tidal soil was in the range of 3.5~4.6 m. The calculation model meets the accuracy requirements and can be used for the calculation of phreatic evaporation of maize during the growing period.