Soil Fertility

PLANT NUTRIENTS
and
SOIL

 

Essential Plant Nutrients (Elements uniquely required by plants for metabolism and life)

Primary Nutrients:

Secondary Nutrients:

Micronutrients:

Nitrogen (N)

Magnesium (Mg)

Boron (B)

Phosphorus (P)

Calcium (Ca)

Zinc (Zn)

Potassium (K)

Sulfur (S)

Manganese (Mn)

 

 

Iron (Fe)

 

 

Copper (Cu)

 

 

Molybdenum (Mo)

 

 

Chlorine (Cl)

 

Important terms:

CEC: Cation Exchange Capacity - The ability of a soil to hold cations such as potassium, magnesium and calcium, on the surfaces of colloids in the soil. Is usually expressed in meq/100g soil. The higher the number, the more cations a soil can hold on exchange sites. Cations held on exchange sites are readily available to the soil solution and, therefore, the plant. Sandy soils usually have low CEC’s of less than 5.

Nitrogen
Soil Persistence:

The primary forms of inorganic N in soil are nitrate ions (NO3-) and ammonium ions (NH4+). Nitrates do not persist in soil. They are easily leached through soils and they are also converted to nitrogen gases by denitrification under anaerobic conditions (wet or compacted soils). While NH4 may be held by clay soils to some degree, they are readily nitrified (converted to NO3) in warm, well-drained soils, especially when pH and fertility are maintained at favorable levels. Once in the NO3 form, they may be more easily leached from the rooting zone of most crops.

Deficiency Symptoms:

Yellowing of older (lower) leaves and stunting of the plant are characteristic of nitrogen deficiency. Leaves will begin to die at the tips and will eventually die completely.

Phosphorus
Soil Persistence:
Phosphorus is not very mobile in soils (except coarse sands and muck soils), but it can be lost by water runoff and erosion. Phosphorus is readily fixed in the soil to unavailable forms. Soils with low levels of P may fix more of the applied fertilizer than soils that are high in P, thus affecting application methods. Since P is relatively immobile in the soil, root growth is even more important to uptake by the plant. Factors limiting root growth (such as cold soil temperatures, compaction, etc.) may increase the chance of having a P deficiency.

Phosphorus availability in soil increases as pH increases from 5.0 to 7.0.

Deficiency Symptoms:

Plants may be stunted and have fewer leaves with less flowers. Phosphorus deficient cotton may be stunted and a darker green. Most obvious P deficiency symptom is purpling of leaves. This often occurs in spring when temperatures remain cool.

Other:

At pH’s above 6.5, may have interaction between P and Ca resulting in a Ca induced P deficiency. Sandy Coastal Plains soils can have P induced Zn deficiency at high pH’s and high P levels. Can also have P induced Fe deficiency at high pH’s (iron chlorosis in turf).

Potassium
Soil Persistence:

More mobile in soil than P, but less than nitrate. The potassium cation (K+) is held on exchange sites in soil, so leaching is more of a problem on very sandy soils.

Deficiency Symptoms:

Leaf margins may turn brown in K deficient plants. Increased lodging may occur in grain crops. Deficient plants are less drought tolerant. In pastures with legumes and grasses, legumes can be expected to suffer more than grasses from low K levels. Potassium deficiency may also allow greater incidence of some diseases.

Other:

In sandy soils, may see Ca induced K deficiency if soil is limed heavily to raise pH from a low pH to a pH of about 6.5.

Magnesium
Soil Persistence:
Similar to K for most Alabama soils.
Deficiency Symptoms:

Magnesium deficiency may cause interveinal chlorosis in older leaves (N deficiency yellows in middle of leaves, Mg on the edges). May exhibit purple color similar to P. Deficiencies occur most readily on sandy, low CEC soils.

Deficiencies may be more likely when using high rates of NH+ and K+ on low CEC soils.

Calcium
Soil Persistence:
Similar to Mg.
Deficiency Symptoms:

A key symptom of Ca deficiency is death of the growing point (bud), although this is rare. Calcium deficiencies are also involved in excessive "pops" in peanuts and blossom end rot of tomatoes and watermelons. Deficiencies occur on sandy soils most often. Poor root growth (nematode damage, cold wet soils, compacted layer in soil, low pH, herbicide damage, etc.) also contributes to Ca deficiency.

Sulfur
Soil Persistence:

Sulfur is converted in the soil to the sulfate anion (SO42-) which is easily leached from the rooting zone (though not as easily as NO3-). Sulfur accumulates in clay subsoil, therefore deficiencies are more common in the early part of the season.

Deficiency Symptoms:

Sulfur deficiency may include yellowing of younger leaves. There is greater need for S fertilizer today because of increased use of P fertilizers that do not contain S and because there is less S air pollution.

Boron
Soil Persistence:

Boron is easily leached from soil. Recommendations for B are very crop specific. What is needed by one crop may be toxic to another.

Deficiency Symptoms:
A common B deficiency is hollow heart in peanuts. Peanuts, cotton and vegetables respond well to B applications.
Interactions with other nutrients:

High Ca or K and low B may result in B deficiency. Low K and high B can lead to B toxicity.

Zinc and Manganese
Soil Persistence:

Zinc and Mn are more available to plants at lower pH’s. Care should be taken when planting crops that are sensitive to high Zn levels behind crops that respond to Zn fertilization (e.g. planting peanuts behind corn).

Buds of young plants turning white or light yellow demonstrate Zn deficiency in corn.  Yellow bands on either side of the leaf midrib can also occur.

Mn deficiency is more common in high water table soils with pH>6. Soybeans with Mn deficiency exhibit interveinal chlorosis.