Skip to main content

Understanding our Nitrogen Inputs

Page 1

Understanding our Nitrogen Inputs After some discussions with growers about Urea I believe there are a few misconceptions about how we can best utilise our Urea nitrogen applications and minimise nitrogen losses through volatilisation. It is interesting how a product that has been around for a very long time in agriculture still generates confusion about its best management strategy, however I believe much of this has to do with how it behaves in different soils, crops and environments. When our Urea is applied to our crops it must undergo a process in order to be converted into a form that the plant is able to use, and at each of these steps there is a risk of us losing the nitrogen that we’ve spent our hard-earned dollars on from the system.

The key step we have to be mindful of in this nitrification process for the Mallee Region is the loss of Urea through a urease enzyme in the conversion of Urea to Ammonia, commonly referred to as volatilisation. Many of the other steps when nitrogen losses can occur focus on leaching in high rainfall environments which are obviously unlikely to affect us. Volatilisation will almost always occur to some degree; however a variety of factors increase the rate of ammonia being gassed off to the atmosphere after application. These include; -​ Dry conditions post spreading -​ Wet soil surface at point of application -​ Dewy conditions after application -​ Windy weather -​ Applications at early crop stages with low canopy cover -​ Alkaline soils -​ High levels of soil carbonates -​ Sandy soil types -​ High levels of soil coverage by organic matter Unfortunately for us in the Mallee Region this list of unfavourable environments for the application of Urea are extremely familiar and we will likely be spreading in many if not almost all of these conditions. The biggest component that begins the volatilisation and nitrogen loss process is dry conditions after spreading, all other factors exacerbate how severe that rate of volatilisation is. So if we know that we’re guaranteed a significant rainfall event within a short time after application, regardless of conditions, we can expect volatilisation to be extremely low.

[DOCUMENT TITLE]


Turn static files into dynamic content formats.

Create a flipbook
Understanding our Nitrogen Inputs by MalleeSustainable - Issuu