Nutrient availability

Nutrient availability and soil pH

Some generalizations can be made regarding the availability of nutrients to plants in relation to soil pH. Deficiencies of zinc, manganese, and iron are more common on alkalines soils while deficiencies of molybdenum, calcium, and magnesium occur more commonly on acid soils. For other nutrients such as potassium and sulfur, there is little association between soil pH and availability to plants. Toxicities of aluminum and manganesse occur almost exclusively on acid soils.

Effects of other nutrients on nutrient uptake

There are many effects of one nutrient upon the uptake of another nutrient (see table). As well as these interactions, any conditiont that decreases root growth (e.g. aluminum toxicity, calcium deficiency, boron deficiency, and toxicity of hydrogen ions per se) will decrease nutrient uptake.

Table. Effect of other nutrients and liming on uptake and transport of nutrients.

Nutrient Uptake decreased by Uptake increased by Transport to growing point decreased by
Calcium
  • Ammonium-nitrogen
  • Magnesium
  • Potassium
Potassium
  • Ammonium-nitrogen
  • Magnesium
  • Calcium
Magnesium
  • Ammonium-nitrogen
  • Calcium
  • Potassium
Sulfur Nitrogen
Chloride Bromides
Molybdenum Sulfate
  • Phosphate
  • Liming
Zinc
  • Copper
  • Liming
  • Calcium
  • Magnesium
Nitrogen
Boron Liming
Copper Zinc Nitrogen
Manganese
  • Calcium
  • Magnesium
  • Iron
  • Liming
Ammonium-nitrogen
Iron
  • Manganese
  • Calcium
  • Magnesium
  • Liming
Ammonium-nitrogen Phosphate