“…Availability of K to the tree from the soil is not limited to total soil K concentration, but is dependent on soil structure and irrigation, form of K, method of application (McKinnon and Lilleland, 1931;Robbins et al, 1982), equilibrium effects (Carlson and Uriu, 1981;Lilleland, 1946;Lilleland and Brown, 1939), and rootstock and cation balance (Rosen and Carlson, 1984a). Finetextured soils impede uptake of K (Lilleland, 1946), and, as these soils are poorly draining, K may not penetrate deeply into soils without the addition of gypsum (Carlson et al, 1974) or deep auguring (Robbins et al, 1982). The positional availability of K above all other nitrogenous compounds, a substance that has been used experimentally to induce K deficiency symptoms (Forshey and McKee, 1970).…”