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Plant Nutrients
Nutrients required for plant growth are divided in macronutrients (primary &
secondary) and micronutrients based on the quantities of the nutrients needed. In
addition to these, the plant also needs Hydrogen, Oxygen and Carbon, which the
plant acquires from the air and from water.
Primary Secondary Micronutrients: Other elements with a
Macronutrients: Macronutrients: role in plant nutrition:
Nitrogen (N) Calcium (Ca) Iron (Fe) Sodium (Na)
Phosphorus (P) Sulfur (S) Manganese (Mn) Cobalt (Co)
Potassium (K) Magnesium (Mg) Zinc (Zn) Vanadium (V)
Copper (Cu) Silica (Si)
Boron (B) Aluminum (Al)
Molybdenum (Mo) Barium (Ba)
Chlorine (Cl) Nickel (Ni)
Titanium (Ti)
Photo credit: Scot
Nelson
Plant Nutrients
Essential nutrients Chemical form assimilated Average plant content
Carbon CO2 45%
Hydrogen HO 6%
2
Oxygen HO & O 45%
2 2
Nitrogen NH+ & NO - 1.5%
4 3
- 2-
Phosphorus HPO & HPO 0.2%
2 4 4
+
Potassium K 1.0%
Calcium Ca2+ 0.5%
2+
Magnesium Mg 0.2%
Sulfur SO2- 0.1%
4
Iron Fe2+ & Fe3+ 100 ppm*
2+
Manganese Mn 50 ppm
Boron HBO 20 ppm
3 3
2+
Zinc Zn & Zn(OH) 20 ppm
Photo credit: Scot
Nelson
2+ +
Copper Cu & Cu 6 ppm
Chlorine Cl- 100 ppm
Molybdenum MoO2- 0.1 ppm
4
* ppm = parts per million (100 ppm = 0.01 %)
pH
pH is a measure of how alkaline or
acidic the soil is. This is important,
because the pH affects the
availability of the nutrients in the
soil.
A nutrient may be present in the
soil, but it may not be available to
the plants because of chemical
reactions caused by the pH
conditions.
A pH of between 6.0 and 6.5 is the
optimal range where most
nutrients are most available for
plant use.
If not, the soil needs to be
amended with lime (for acidic Photo credit: Scot
soils). Gypsum can be used for Nelson
sodic soils with high alkalinity.
Soil Tests
Soil tests are essential for efficient plant nutrition. Not only do they show the levels of
nutrients in the soil, they also show other characteristics such as pH, percent organic
matter and cation exchange capacity (C.E.C.; i.e. how good the soil is at holding the
nutrients), which helps manage the soil for best results
Photo credit: Scot
Nelson
Soil Types
Cation Exchange Capacity
Soil types affect plant nutrition and fertilization. Clay soils and soils with a high
organic content hold a lot of nutrients (a high C.E.C. or cation exchange capacity). This
gives these soils a good buffering capability and they help ensure an efficient
fertilization. Sandy soils, on the other hand, have a low C.E.C. with low nutrient
holding capacity and little ability to prevent leaching of nutrients.
Soil Structure
An ideal soil for plant growth is one that has 50% solids and 50% pore space (filled
with 50% water and 50% air). [Did you know that the roots of a plant use about 10
times more oxygen than the leaves? This is because it takes a lot of energy for the
roots to extract nutrients from the soil. The oxygen in the air is needed for respiration,
which gives the roots the energy.]
For the efficient movement of air and water, a healthy soil should have a good
structure, which means that it should be organized into macro- and micro-aggregates.
Aggregates are groups of soil particles that ‘stick’ together due to organic material,
calcium and various natural carbohydrates and acids found in the soil. There are
different factors that affect the formation or breakdown of aggregates such as
Photo credit: Scot
cultivation techniques, levels of sodium and levels of organic matter.
Nelson
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