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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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