Effect of ammonium and phosphorus supply on h⁺ production in gel by two tropical forage grasses

Abstract

The effect of the supply of ammonium (NH₄ ⁺) and phosphorus (P) in gel on the amounts of hydrogen ion (H⁺) excreted from plant roots was studied with Brachiaria humidicola (a highly acid‐soil tolerant tropical grass) and B. brizantha (less acid‐soil tolerant) grown in soil in a glasshouse. The H⁺ production was measured over 24 h in agar gel containing full nutrient solution with a range of NH/‐N levels (0, 0.25, 0.5, and 5.0 mM NH₄ ⁺‐N). Highly soluble P, K₂HPO₄, or relatively insoluble P, rock P, was supplied at four concentrations (0, 11.5, 34.5, or 115 μM p) in the gel. Increasing NH₄ ⁺ concentration in the gel increased H⁺ production for both grasses, but there was some inhibition of growth for B. brizantha at the highest N concentration. For B. humidicola, but not B. brizantha H⁺ production was greater with 34.5 μM K₂HPO₄ than 11.5 μM K₂HPO₄. At 34.5 μM P for both grasses there was no difference in H⁺ production when P was supplied as rock P or K₂HPO₄. With 11.5 μM P both grasses produced less acid in the gel with the rock P compared with K₂HPO₄. The reduced H⁺ production is probably due to a lower availability of P in the rock P compared with K₂HPO₄. This effect was greater with B. brizantha than B. humidicola, implying that 11.5 μM rock P was not able to supply sufficient P for the growth of B. brizantha. Brachiaria humidicola was able to dissolve more rock P than B. brizantha or alternatively, the growth of B. humidicola was less adversely affected by the low P supply from rock P than B. brizantha. Plant‐induced acidity does not seem to occur as a response to a lack of available P, but rather these grasses only produce acid if there are enough nutrients for growth, i.e., both NH₄ ⁺ and P. If either N or P is limiting, growth is limited as is NH₄ ⁺ uptake, so that H⁺ production is curtailed.