Michigan State University Extension
Soils & Soil Management - Fertilizer - 06109728
07/10/97

Phosphate Fertilizers


N-P-K Fertilizers                                           
Extension Bulletin E-896, October 1990                      

by M.L. Vitosh                                              
Extension Specialist, Crop and Soil Sciences                

Rock phosphate has virtually disappeared from the market    
because of its very low water solubility and high           
transportation costs. Rock phosphate may, however, supply   
sufficient P for good crop growth where soils are           
moderately acid and where decomposing organic matter is     
abundant. Application of 1,000 to 2,000 pounds per acre     
may be necessary for good plant growth if soil test         
levels for P are low. On fields with high soil tests for    
P. broadcasting rock phosphate to replace crop removal      
may be acceptable, but rock phosphate is not acceptable     
for a starter fertilizer because of its low water           
volubility. Today, rock phosphate is generally processed    
before it is used as a fertilizer.                          

Normal superphosphate (20% P2O5), also referred to as       
ordinary superphosphate, is no longer used in large         
quantities. Because of its lower analysis and high          
transportation costs, it has been replaced by               
concentrated superphosphate (46% P2O5,) and the ammonium    
phosphates. One of the advantages of normal                 
superphosphate was its significant sulfur content.          
As consumption of this material has slowly decreased,       
concerns over the need for sulfur have come primarily       
from the fertilizer industry. Currently, sulfur from the    
atmosphere is keeping pace with crop removal.               

Concentrated superphosphate (46% P2O5), also known as       
triple superphosphate, is being used in Michigan in         
direct application as well as in granulated processes and   
in bulk blending with other materials. Consumption has      
decreased in recent years due to the competitiveness of     
diammonium phosphate (18-46-0) and monoammonium phosphate   
(11-48-0). These materials have better storage properties   
and are more desirable for bulk blending, particularly      
where N is required in the final product.                   

Diammonium phosphate (18-46-0) is a dry material being      
used extensively for bulk blending and for direct           
application where soils do not need K or where K is         
broadcast. It has the advantage of being highly water       
soluble, having a high analysis and often a price           
advantage. Diammonium phosphate has an acid effect upon     
the soil similar to anhydrous ammonia. Because of the       
high ammonia content, this material can cause germination   
injury if used in direct contact with the seed.             

Monoammonium phosphate (11-48-0) is a dry material being    
used for bulk blending or direct applications.              
Monoammonium phosphate has a lower ammonia content and      
may be less injurious to germinating seeds than             
diammonium phosphate. The general agronomic effects of      
diammonium and monoammonium phosphates are equal for most   
soils.                                                      

Polyphosphate differ slightly from the more common          
orthophosphate fertilizers. Nearly all of the liquid        
fertilizers containing P are of the polyphosphate type.     
Polyphosphate are composed of a series of orthophosphate    
molecules connected by the process of dehydration           
(removal of water). Commercial ammonium polyphosphate are   
usually a mixture of ortho- and polyphosphate. With         
prolonged storage, polyphosphate will hydrolyze to          
orthophosphates. Solutions of ammonium polyphosphate most   
commonly made are 10-34-0 and 11-37-0. The most common      
dry polyphosphate is 13-52-0.                               

In the soil, polyphosphate converts to orthophosphate by    
hydrolysis (adding on water). The time required for         
hydrolysis to occur varies with soil conditions. In some    
cases, 50% of the polyphosphate hydrolizes to               
orthophosphate within two weeks. Under cool, dry            
conditions, hydrolysis may take longer.                     

Some claims have been made that polyphosphate will make     
certain unavailable micronutrients in the soil more         
available for plant uptake. Due to the rather rapid         
conversion of polyphosphate to orthophosphates in the       
soil, it is not likely that such complexes would be         
available for any significant length of time. Research at   
Michigan State University and Kansas State University has   
shown that micronutrient uptake is not enhanced by          
polyphosphate materials. The efficiency of polyphosphate    
is considered to be equal to, but not better than, the      
orthophosphates with more than 80 percent water             
solubility.                                                 
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