Michigan State University Extension
Soils & Soil Management - Fertilizer - 05209708
07/10/97

Iron

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Secondary and Micronutrients for Vegetables and Field       
Crops                                                       
Extension Bulletin E-486, Revised August 1994               

By M.L. Vitosh, D.D. Warncke and R.E. Lucas                 
Department of Crop and Soil Sciences                        
Michigan State University Extension                         

Iron is a constituent of many organic compounds in          
plants. It is essential for synthesizing chlorophyll,       
which gives plants their green color. Iron deficiency can   
be induced by high levels of manganese. High iron levels    
can also cause manganese deficiency.                        

Iron Deficiency Symptoms                                    

Deficiency symptoms are marked and show up first in         
terminal leaves as a light yellowing. The symptoms are      
very similar to those of manganese deficiency (Vis. 26).    
A lack of iron in field and vegetable crops is not common   
in soils with pH below 7.0.                                 

Iron deficiency is common in the western states, where      
the soils contain considerable sodium and calcium. In       
Michigan, woody plants such as pines, pin oaks, roses,      
certain ornamentals and acid-demanding plants such as       
blueberries, azaleas and rhododendrons may need iron.       
Lawns, particularly putting greens on golf courses,         
sometimes show a lack of iron because of high pH and high   
levels of phosphorus.                                       

Iron deficiency in many woody plants appears when they      
are grown in soils low in organic matter and high in pH.    
Mixing in organic materials such as manure or acid peat     
will help increase the availability of the iron.            

Sphagnum peat moss in mixtures with sand, perlite or        
vermiculite intensifies the need for iron fertilizer in     
the production of petunias, snapdragons, tomatoes and       
other bedding plants.                                       

Correcting Iron Deficiency                                  

Soil treatments usually require applications of iron        
chelates at a rate equivalent to « to 1 pound of iron per   
acre. Often it is difficult to correct iron deficiency      
with soil applications when soils are alkaline. Soil        
applications are effective if soils are acid or neutral     
in reaction. Under alkaline soil conditions, foliage        
sprays are recommended. Use iron sulfate, iron chelates     
or iron citrate according to the supplier's                 
recommendations. Wet foliage thoroughly. Iron chelates,     
though more expensive than iron sulfate, persist longer.    

Sometimes the best cure for Fe deficiency is to grow        
varieties that are not sensitive to Fe deficiency. For      
instance, some soybean varieties are more sensitive to Fe   
deficiency than others. For bedding plant production, use   
1 to 2 ounces of elemental iron per cubic yard of soil      
mix.                                                        

To help prevent an iron problem, avoid using excessive      
amounts of lime or phosphate. Apply chemicals or            
fertilizers to increase the soil acidity and add organic    
matter.                                                     

Iron Toxicity                                               

Injury due to high soil iron concentrations is not common   
under neutral or high pH soil conditions. Toxic             
situations occur primarily on acid soils (< pH 5.0) and     
where excess soluble iron salts have been applied as        
foliar sprays or soil amendments. The first symptoms of     
iron toxicity are necrotic spots on the leaves.             

An unusual form of iron toxicity has been observed in       
Michigan on organic soils and high organic sands. Some      
iron-rich, low pH, low manganese soils create an            
environment in which an interaction between the iron and    
manganese in the soil reduces manganese uptake by plants.   
The symptoms observed on the plants are of manganese        
deficiency, but the low plant uptake of manganese is        
caused by excessive available iron in the soil. The         
addition of iron chelates or manganese chelates, which      
rapidly convert to the iron form under these soil           
conditions, aggravates the situation by increasing the      
amount of available iron and without solving the            
manganese deficiency problem.                               

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Iron-deficient corn - 31K
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