2025-04-01 null null 74(卷), null(期), (null页)
The soil water content at field capacity, theta(FC), is a fundamental variable for irrigation and agriculture. This study determines the optimal tension (-33 or -10 kPa) of deriving theta(FC) which best matches the in situ field measurements following the Veihmeyer procedure. The Veihmeyer method refers to a profile water status for which there is a negligible drainage rate of bare soil without evaporation. In addition, we derive a set of linear and nonlinear pedotransfer functions (PTFs) which estimate theta(FC). theta(FC) was measured in 69 plots in north-western Iran, which has a cold semi-arid climate. The soil properties used for developing PTFs include texture, bulk density, and organic matter. The results show that theta(FC) cannot be derived at a fixed tension. We therefore developed PTFs with satisfactory performance in reproducing in situ measured theta(FC). The findings show that PTFs developed at a fixed tension consistently underestimate theta(FC) derived in situ. It was also speculated that tension less than -10 kPa could yield improved predictions of in situ theta(FC).