Soil water deficit effects on soil inorganic nitrogen in alternate-furrow flood irrigated Australian cotton production systems

Abstract

Context Predicting the nitrogen (N) mineralisation from soil organic matter is a key aid to fertiliser decision-making and improving the N fertiliser use efficiency of a crop. Aims and methods Field experiments were conducted to assess the amount of inorganic N derived from soil organic matter mineralisation over two seasons (2017–2018 and 2018–2019) across treatments differing in irrigation frequency and amount. During both seasons, the plant line soil in each treatment was sequentially sampled at each irrigation event. Key results There was an effect of the soil water deficit on the measured accumulated soil inorganic N derived from mineralisation in both measurement years. It was observed that soil inorganic N accumulated in the plant line rather than in other hillside and furrow positions for all soil moisture deficit treatments in both years. In 2017–2018, N accumulated in the plant was significantly greater than the measured accumulated inorganic N (0–300 mm). Conclusions and implications The sequential soil sampling approach was challenging in irrigated systems and we propose a hybrid measurement of pre-season available soil N and/or plant N uptake in nil N fertiliser plots as a means of estimating N derived from soil organic matter mineralisation.

Beneficial Microorganisms Affect Soil Microbiological Activity and Corn Yield under Deficit Irrigation

“…The concentration of mineral nitrogen (N), as ammonium (NH 4 + ) or NO 3 − , increased due to the water deficit. In previous works, higher concentrations of mineral N were also observed in soil under water deficits [5,8,49]. Water restriction possibly decreased the rate of N absorption and accumulation by corn, providing higher levels of mineral N in the soil and decreasing the levels of this nutrient in the leaves.…”