In arid farmland, the soil water, heat, and salt movement tightly couple with crop growth. Accurately expressing the coupling relationships is essential to understanding the complex agricultural hydrological system and enhancing agricultural water productivity. A novel conceptual model coupling crop growth, soil water-heat-salt movement, and energy balance in arid area with shallow groundwater was developed which has potential for use in large heterogeneous irrigation districts. The model can calculate the crop-soil system through the effect of crop canopy and leaf area index (LAI) on potential evapotranspiration and the stress of soil moisture, temperature, and salinity status to root water uptake. The energy balance equation was used for calculating the upper boundary condition for soil temperature. The model was calibrated and validated using four years of field monitoring data for two crops located in a typical arid agricultural area in China. The model performed well in simulated field hydrology and crop growth processes. The model can capture soil water-heat-salt dynamics and model field evapotranspiration with RMSE below 1.14 mm/day, and crop transpiration with R2 of above 0.61. Furthermore, the model can accurately describe crop growth processes with R2 of 0.95 and RMSE of 0.49 for LAI, and R2 of 0.99, RMSE of 12.95 cm for crop height. With few parameters, our work supplies an alternative method for quantifying agricultural hydrological processes. In particular, the model has potential to simulate the regional crop growth and soil water-heat-salt processes for heterogeneous agricultural area. This method is helpful in determining the scientific irrigation management schedule.
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