PREPARATION OF NITROGEN FOLIAR FERTILIZERS

The microbial transformation of organic nitrogen to inorganic forms is referred to as mineralization. Common organic nitrogen substances are; soil humus, plant leaf clippings and root tissue, and sludge and manure based fertilizers. Generally, a complex and large molecule containing nitrogen is broken down into a simpler and smaller molecule and then into ammonium. Sometimes this process is referred to in two parts with the first part termed aminization and the second part ammonification.

Many different types of organisms can perform these reactions, some can do both steps while others can only perform one reaction or the other. Fungi and bacteria carry on most of the mineralization in soils. Because many different organisms can mineralize nitrogen in the conditions necessary for mineralization to occur are not highly specific. Warm, wet conditions, and soil pH greater than 5.5 enhance mineralization. Good soil aeration promotes mineralization, so water contents greater than field capacity tends to reduce the rate of nitrogen mineralization. One factor that can be altered by the turfgrass manager and greatly affects how fast nitrogen is released from an organic nitrogen source is the C: N ratio of the material.

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