Premium
Influence of Nitrogen Source on Phosphorus Uptake by Corn from Soils Differing in pH 1
Author(s) -
Blair Graeme J.,
Mamaril C. P.,
Miller M. H.
Publication year - 1971
Publication title -
agronomy journal
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.752
H-Index - 131
eISSN - 1435-0645
pISSN - 0002-1962
DOI - 10.2134/agronj1971.00021962006300020012x
Subject(s) - chemistry , soil water , phosphorus , nitrogen , fertilizer , nutrient , agronomy , dry weight , soil ph , absorption (acoustics) , zoology , horticulture , biology , physics , organic chemistry , acoustics , ecology
The objective of this study was to test the hypothesis that reduction of pH at the soil‐root interface when NH 4 + ions were absorbed is the cause of the increased absorption of P in the presence of NH 4 + . The influence of addition of (NH 4 ) 2 SO 4 or KNO 3 to an MCP band on P absorption by corn was determined in a greenhouse study involving four soils ranging in pH from 4.2 to 8.2. The in‐situ activity of the corn plants was determined periodically during the growth, and the dry weight of tops and roots in the fertilizer zone as well as the nutrient content of the tops were determined after 17 days. Application of (NH 4 ) 2 SO 4 with MCP was found to increase fertilizer P uptake when compared to MCP alone on soils of pH 8.2, 7.4 and 5.5. No difference was measured on a soil of pH 4.2. Accumulations of Ca and P were found on the root surface of the plants grown in the alkaline soils. Ca, Fe and P was found on the root surface in a soil with a pH of 5.5. No root surface accumulation was found at a soil pH of 4.2. Fertilizer P uptake at 9 days was greatest where NH 4 + and least where NO 3 ‐ accompanied the P. Changes in the soil‐root interface pH and resulting changes in the H 2 PO 4 ‐ /HPO 4 = ratio at the root surface which are modified by the inherent soil pH are implicated in these findings.