Performance assessment of the FAO AquaCrop model for soil water, soil evaporation, biomass and yield of soybeans in North China plain

Los índices de Flesch y Flesch-Kincaid también se utilizaron en otro estudio que trató de medir el grado de dificultad del TCLE o los años de estudio necesarios para su

Since the calculation of the irrigation water depth involves the knowledge of the actual soil water content before irrigation, of the soil water content at field capacity, and of

The first signs of declining soil water are leaf rolling and sto- Figure 2 – Relationship between the normalized transpiration rate (NTR) and the fraction of transpirable soil

The performance of the CROPGRO-Drybeans model for the prediction of soil water balance, as well as growth components and bean crop yield, was assessed using data from two

The values of latent heat flux (LE) and sensible heat flux (H) followed the distributions of rainfall, stored soil water and LAI (Figures 1D-F); in periods with low soil

This study investigated water potentials in the soil (matric, osmotic and total) and in bell pepper plants (osmotic and total) irrigated with water of six levels of

The soil samples were used to estimate the soil microbial biomass carbon and nitrogen, soil basal respiration, metabolic quotient and soil enzymatic activity, through hydrolysis

The performance of the CROPGRO-Drybean model for the prediction of soil water balance, as well as growth components and bean crop yield, was assessed using data from two