“…It operates over short distances, and is especially important for the macronutrients P and K that often limit crop production (Hinsinger et al 2011). The mass flow of a mineral element to the root surface is determined by its concentration in the soil solution and the transpiration-driven movement of water to the root surface (White and Greenwood 2013). It is important for the acquisition of essential mineral elements with large concentrations in the soil solution, such as N, K, S, Ca, Mg and Cl in agricultural soils, and for mineral elements that are required in relatively small quantities by plants, such as Fe, Mn, Zn, Cu, Ni, B and Mo (White et al 2013a).…”