Michigan State University Extension
Soils & Soil Management - Fertilizer - 06029704
07/10/97

Soil Testing Procedures


Fertilizer Recommendations for Field Crops in Michigan      
Extension Bulletin E-550A, March 1992                       

D. R. Christenson, D. D. Warncke, M. L. Vitosh, L. W.       
Jacobs and J. G. Dahl, Department of Crop and Soil          
Sciences                                                    

The following is a brief discussion of the procedures       
used in the Michigan State University Soil Testing          
Laboratory.                                                 

Soil pH of mineral soils is measured using a 1:1            
soil-to-water suspension; on organic soils, a 1:2           
soil-to-water suspension is used. Lime requirement for      
mineral soils is determined using the SMP Buffer method.    
On organic soils, lime requirement is based on soil pH.     

Available phosphorus is measured using the Bray-Kurtz P1    
(weak acid) extractant while exchangeable potassium,        
calcium and magnesium are extracted using 1.0 N neutral     
ammonium acetate. Recommendations for phosphorus,           
potassium and magnesium are based on soil test values       
from these extractants.                                     

The Bray-Kurtz P1 test does not extract all of the          
available phosphorus on soils which contain free calcium    
carbonate. These soils can be identified as having pH       
values above 7.2 and a Bray-Kurtz P1 test of less than 20   
lb/acre. Soils in this case are extracted with sodium       
bicarbonate (referred to as Olsen P). This test was         
designed for soils with free calcium carbonate.             

Available manganese and zinc are extracted with 0.1 N HCl   
and copper with 1.0 N HCL using a 1:10 soil-to-extractant   
ratio.                                                      

Mineral soil samples submitted to the MSU Soil Testing      
Laboratory are extracted using weighed samples. The         
amounts of nutrients are expressed as parts per 2 million   
or pounds per acre, which assumes that one acre of a        
loamy soil 6 2/3 inches deep weighs 2 million pounds.       

Organic soil samples are measured by volume because such    
materials usually have much lower densities than mineral    
soils. Results for organic soils are expressed on a         
volume acre furrow slice basis (volume of an acre 6 2/3     
inches deep).                                               

Available phosphorus, calcium and magnesium are expressed   
as pounds of element (P, K, Ca, Mg) extracted. Available    
zinc, manganese and copper are expressed as parts per       
million (ppm). Some laboratories express all elements as    
parts per million. To convert parts per million to pounds   
for mineral soils, multiply by 2 (i.e., 2 X ppm =           
lb/acre). The exact conversion varies with bulk density     
of the soil, but organic soils have a wider variation       
than mineral soils. For example, for an organic soil with   
a bulk density of 0.34 g/cm3, 1 ppm = 0.5 lb/acre. For      
soils with a bulk density of 0.68, 1 ppm = 1 lb/acre.       

Some laboratories express phosphorus and potassium in       
terms of P2O5 and K2O. The factors to convert between P     
and P2O5 or K and K2O are:                                  

lbs P X 2.3 = lbs P2O5; lbs P2O5 X 0.44 = lbs P             

lbs K X 1.2 = lbs K2O; lbs K2O X 0.83 = lbs K               

The fertilizer recommendations are given in pounds of       
phosphate (P2O5) and potash (K2O) per acre because          
fertilizers are expressed and sold in these terms.          


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