The root zone soil water content at field capacity, BFC, is often crucial for irrigation scheduling and soil-plantatmosphere modelling. Although BFC is traditionally determined using methodologies based on matric head or when water flux at the bottom of the root-zone equal to a prescribed negligible flux, these approaches can be problematic for some soils and applications. In this study, a novel water storage approach was used to estimate BFC for 11 soil texture classes in southeastern Australia (northwest Victoria) by employing the Soil-WaterAtmosphere-Plant (SWAP) model to simulate gravity drainage from saturation in the active root zone (top 60 cm). Field capacity was specified as the average root zone water content corresponding to a 1% relative change in daily soil water storage. We have also estimated flux-based BFC when prescribed flux at the bottom of the rootzone was 0.1 cm d-1. Three new empirical equations were developed to estimate storage-based BFC as a function of SWAP-simulated drainage flux out of the root zone, the n parameter of the van Genuchten function, and the saturated soil hydraulic conductivity, Ks, or the soil water content at - 100 cm matric head. We have evaluated these three new equations in addition to nine published equations for estimating BFC. The three new equations were found to be better predictors of BFC than most of the nine popular equations reported in the literature when compared to flux-based BFC values. Based on findings from this study the new equations are considered to be effective for irrigation scheduling and crop/climate modelling on the dryland soils of Victoria. Future studies will assess the applicability of the new equations to other parts of Australia.