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

Context. Predicting the nitrogen (N) mineralisation fromsoil 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.

Automated summary

The study found that soil water deficit had a significant impact on the inorganic nitrogen derived from soil organic matter mineralization, with inorganic nitrogen primarily accumulating in the plant line. Through sampling and measurement, it was observed that the nitrogen accumulation in plants was significantly greater than the inorganic nitrogen in the soil.