The document discusses key soil chemical properties including organic matter, pH, and nutrient retention. Soil organic matter is made up of living and decaying residues and humus, which improves soil structure and nutrient levels. Soil pH indicates acidity or alkalinity on a scale of 0-14 and affects plant nutrient uptake. Various soil particles also retain nutrients through adsorption. Maintaining proper organic matter, pH, drainage, and fertilizer use is important for soil health and plant growth.
The document discusses key soil chemical properties including organic matter, pH, and nutrient retention. Soil organic matter is made up of living and decaying residues and humus, which improves soil structure and nutrient levels. Soil pH indicates acidity or alkalinity on a scale of 0-14 and affects plant nutrient uptake. Various soil particles also retain nutrients through adsorption. Maintaining proper organic matter, pH, drainage, and fertilizer use is important for soil health and plant growth.
The document discusses key soil chemical properties including organic matter, pH, and nutrient retention. Soil organic matter is made up of living and decaying residues and humus, which improves soil structure and nutrient levels. Soil pH indicates acidity or alkalinity on a scale of 0-14 and affects plant nutrient uptake. Various soil particles also retain nutrients through adsorption. Maintaining proper organic matter, pH, drainage, and fertilizer use is important for soil health and plant growth.
The document discusses key soil chemical properties including organic matter, pH, and nutrient retention. Soil organic matter is made up of living and decaying residues and humus, which improves soil structure and nutrient levels. Soil pH indicates acidity or alkalinity on a scale of 0-14 and affects plant nutrient uptake. Various soil particles also retain nutrients through adsorption. Maintaining proper organic matter, pH, drainage, and fertilizer use is important for soil health and plant growth.
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Soil Chemical Properties
Soil Chemical Properties
Minerals originate from slow breakdown of parent material
Mineral salts from soil particles dissolve in soil water
Inorganic salts required by plants for nutrition
Hence study of Soil Chemical Properties
Chemical Properties The main properties of concern to us are:
1. Soil Organic matter
2. Soil pH
3. Soil particle – soil nutrient relationships
Soil Organic Matter Living organisms together with decaying residues Decaying residues known as Humus Humus is dead organic matter in state of continuous decomposition promotes activities of soil organisms (as host and food source) adds nutrients to the soil improves structure e.g. binds sandy soils conserves soil moisture prevents erosion Soil pH Term used to express of degree of acidity and alkalinity Measured on a scale from o-14 Neutral on scale = 7 < 7 is acidic > 7 is alkaline Testing done to measure soil acidity or alkalinity Soil pH Testing Use of a soil indicator to test acidity or alkalinity An indicator is a substance that allows changes in colour Colour changes compare to chart that allows you to measure soil acidity Effect of pH on plant growth Incorrect pH prevents soil from taking up nutrients Crops sensitive to pH changes Each crop has a minimum, maximum and optimum pH Minimum – pH below which crop would not grow Maximum – pH above which crop will not grow Optimum – middle of minimum and maximum and ideal for crop growth Most crops have a ideal range of pH 5.5 - 7 Correcting soil acidity Soil acidity caused by: Leaching – excess water washing away ions Nutrient uptake – plant growth and removal Fertilizers – excessive use of acid fertilizers Sulphur – soils with high S resulting in sulphuric acid and can be corrected by: Application of lime (limestone) Proper drainage Use of appropriate fertilizers Soil particle – soil nutrient relationship Soils can retain nutrients due to the presence of: Clay Organic matter (OM) Aluminum and iron compounds
These substance are responsible for the ‘adsorption
complex’ Adsorption is the attraction to a solid surface Clay and OM have a layer of negative charges Some soil nutrients have positive charges resulting in attraction Nutrient content of the soil – There are 16 essential elements needed for proper plant growth, Hydrogen, Carbon and Oxygen come from the air
MACRO PRIMARY SECONDARY MICRO OR TRACE
NUTRIENTS NUTRIENTS NUTRIENTS NUTRIENTS Nitrogen N Nitrogen Calcium Iron Fe Phosphorous P Phosphorous Magnesium Manganese Mn Potassium K Potassium Sulphur Copper Cu Calcium Ca Boron B Magnesium Mg Molybdenum Mo Sulphur S Zinc Zn Chlorine Cl Macro nutrients NITROGEN (N) PHOSPHOROUS (P) POTASSIUM (K)
Absorbed as nitrate or Absorbed as phosphate ions Absorbed as potassium
Lack of nitrogen Lack of phosphorous causes; Lack of potassium
causes; stunted growth, purple green leaf color, poor causes drying of leaves yellowing of leaves and root development, stunting of from the tip backward, leaf drop green parts mottling of leaves and premature falling of buds Soil Chemical Properties - Review Minerals originate from slow breakdown of parent material and dissolve in soil water
Inorganic salts required by plants for nutrition
Hence study of Soil Chemical Properties
1. Organic matter 2. Soil pH 3. Soil particle – soil nutrient relationship Assessment 1. What is soil pH?
2. Jim is a vegetable farmer who received a soil pH
tester, however is unsure of its worth to his farm. Briefly provide advice to Jim as his Extension Officer.
3. Explain the causes of soil acidity and how it can be
corrected in agricultural soils. Answer 1 A measure on a scale of 0-14, the acidity or alkalinity of a soil
Back Answer 2 Used to determine the pH of the soil.
plant vegetables suitable to their pH range thereby
facilitating plant uptake of up nutrients.
maintain the soil pH so that the vegetables would grow in
optimum pH conditions.
Efficient use of appropriate fertilizers to minimize soil acidity
Back Answer 3 Soil acidity caused by: Leaching – excess water washing away ions Nutrient uptake – plant growth and removal Fertilizers – excessive use of acid fertilizers Sulphur – soils with high S resulting in sulphuric acid and can be corrected by: Application of lime (limestone) Proper drainage Use of appropriate fertilizers Keep on learning!