Michigan State University Extension
Soils & Soil Management - Fertilizer - 06039712
07/10/97

Nitrogen Losses From Soil


Tri-state Fertilizer Recommendations for Corn, Soybeans,    
Wheat and Alfalfa                                           
Extension Bulletin E-2567 (New), July 1995                  

M.L. Vitosh, Michigan State University; J.W. Johnson, The   
Ohio State University; D.B. Mengel, Purdue University;      
Co-editors                                                  

Nitrogen (N) can be lost from the field through three       
principal pathways: denitrification, leaching and surface   
volatilization.                                             

The form of N a farmer chooses should depend on how         
serious a problem he has with the above N losses. Cost of   
N, labor, equipment and power availability are other        
considerations when choosing a fertilizer source.           

Denitrification occurs when nitrate N (NO3-) is present     
in a soil and not enough oxygen (O2) is present to supply   
the needs of the bacteria and microorganisms in the soil.   
If O2 levels are low, microorganisms strip the oxygen       
from the nitrate, producing N gas (N2) or nitrous oxide     
(N2O), which volatilizes from the soil. Three conditions    
that create an environment that promotes denitrification    
are wet soils, compaction and warm temperatures.            

Leaching losses of N occur when soils have more incoming    
water (rain or irrigation) than the soil can hold. As       
water moves through the soil, the nitrate (NO3-) that is    
in soil solution moves along with the water. Ammonium       
(NH4+) forms of N have a positive charge and are held by    
the negative sites on the clay in the soil; therefore,      
NH4+ forms of N leach very little. In sands where there     
is very little clay, ammonium forms of N can leach.         
Coarse-textured sands and some muck soils are the only      
soils where ammonium leaching may be significant            

One way to minimize N leaching and denitrification is to    
minimize the time the N is in the soil before plant         
uptake. This cuts down on the time when conditions are      
favorable for losses. Most of the N is needed by corn       
after the plant is 3 to 4 weeks old (June 1).               

Surface volatilization of N occurs when urea forms of N     
break down and form ammonia gases and where there is        
little soil water to absorb them. This condition occurs     
when urea forms of N are placed in the field but not in     
direct contact with the soil. This situation can occur      
when urea is spread on corn residues or 28 percent is       
sprayed on heavy residues of cornstalk or cover crop.       

The rate of surface volatilization depends on moisture      
level, temperature and the surface pH of the soil. If the   
soil surface is moist, the water evaporates into the air.   
Ammonia released from the urea is picked up in the water    
vapor and lost. On dry soil surfaces, less urea N is        
lost. Temperatures greater than 50 degrees F and a pH       
greater than 6.5 significantly increase the rate of urea    
conversion to ammonia gases. Applying urea-type             
fertilizers when weather is cooler slows down N loss. If    
the surface of the soil has been limed within the past      
three months with 2 tons or more of limestone per acre,     
DO NOT apply urea-based fertilizers unless they can be      
incorporated into the soil.                                 

To stop ammonia volatilization from urea, the urea must     
be tied up by the soil. To get the urea in direct contact   
with the soil requires enough rain to wash the urea from    
the residue or placement of urea-based fertilizer in        
direct contact with soil by tillage, banding or             
dribbling. If the residue is light (less than 30 percent    
cover), 0.25 to 0.5 inch of rain is enough to dissolve      
the urea and wash it into the soil. If the residue is       
heavy (greater than 50 percent cover), 0.5 inch or          
greater of rainfall is required.                            

Ammonia volatilization of N may also occur when ammonium    
forms of N--ammonium sulfate (AS), ammonium nitrate (AN),   
diammonium phosphate (DAP), monoammonium phosphate (MAP)    
and ammonium polyphosphate (APP)--are surface applied to    
calcareous soils (soil pH greater than 7.5). The extent     
of loss is related to the reaction products formed when     
ammonium fertilizers react with calcium carbonate.          
Ammonium fertilizers that form insoluble precipitates       
(AS, DAP, MAP and APP) are subject to greater ammonia       
volatilization losses than AN, which forms a soluble        
reaction product. To prevent ammonia volatilization,        
ammonium fertilizers should be knifed in or incorporated    
on calcareous soils.                                        


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