What limits nitrate uptake from soil?

Abstract. An accepted view, that unless nitrate concentrations in the soil solution are very low (e.g. below 0.1–0.2 mol m^?3) the growth of high-yielding crops is not limited by the availability of nitrogen, is challenged. Conventional analyses of nutrient supply and demand, based on calculations of apparent inflow rates (uptake rates per unit total root length) are invalid. Apparent inflow rates are inversely proportional to root length. The convention of using total root length grossly overestimates the fraction of the root system active in nutrient uptake. Consequently, inflow rates based on total root lengths underestimate the true values, indicating unrealistically low nutrient concentration differentials between bulk soil and root surfaces required to drive uptake. An alternative method of analysis is suggested. This is based on total nutrient uptake rather than on inflow rate. Measurements of the former do not depend on estimates of active root length and can be made directly and reliably. The method was applied to data obtained from a pot experiment using spring wheat (Triticum aestivum L., cv. Wembley) grown in soil without nitrogen fertilizer (N₀) or with nitrogen fertilizer equivalent to 200kg N ha^?1 (N⁺). Soil nitrate concentrations calculated using the conventional method based on total root length, suggested that any increases in concentration above those measured in the N⁰ treatment should not have resulted in increased uptake and growth. However, the N⁺ plants were always bigger than those in the No treatment, refuting this suggestion. Theoretical uptakes of nitrogen (calculated initially on the basis of a fully active root system) were adjusted, by reducing the effective root length incrementally, until the theoretical uptake matched the measured net uptake of nitrogen. The mean fractions of the root systems likely to have been involved in nitrate uptake were 11% and 3.5% of the total lengths of root in the N⁰ and N⁺ treatments, respectively.     

Micronutrient Cation Sorption by Roots and Uptake by Plants

The sorption of ferric iron, copper, zinc and manganese by wheatseedling roots and by discs of cellulose filter paper was measured.The magnitude of sorption at pH 5-0 was Fe(III) > Cu(II)> Zn(II) > Mn(II). Sorption of Cu(II), Zn(II) and Mn(II)increased with increasing pH whilst sorption of Fe(III) decreased.The patterns of sorption are discussed in the light of our knowledgeof the hydrolysis of the metal ions. It is suggested that metalsadsorbed on root surfaces may be remobilized by organic ligandswhich leak from the root cells. Where an external liquid diffusionpath away from the root does not exist, soluble metal ligandcomplexes might accumulate in the water free space and superficialwater film of the root, thus facilitating their uptake intoroot cells and translocation within the plant. Under such conditionsthe amounts of metal translocated to the shoots of wheat seedlingsare shown to be related to the amounts of metal adsorbed bytheir roots. Key words: Adsorption, Micronutrients, Roots