The Soil | Jamb Biology
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Time to Prepare for the Big Exam! As your academic landlord, I remind you that the rent for success is due,
and the currency is hard work and preparation. Keep your study room organized, review your resources, and
ensure every corner of your mind is ready for inspection. Pay this rent diligently, and you’ll secure your
place in the mansion of achievement! 📚💡
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In this post, you will be exposed to substantial number of points and summaries from the topic
The Soil which was extracted from the Jamb syllabus.
I would advice you pay attention to each of the point as you go through them.
Happy learning.
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Characteristics of Different Soil Types
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Sandy Soil
- Particle Size: Largest among soil types; particles are coarse and gritty.
- Porosity: High porosity; large spaces between particles.
- Water Retention: Poor; water drains quickly.
- Air Content: High due to large pores.
- Nutrient Retention: Low, as nutrients are leached away easily.
- Texture: Loose and easy to cultivate.
- Color: Light-colored, depending on mineral content.
- Capillarity: Weak due to large particle size.
- Humus Content: Low humus retention because organic matter drains with water.
- Examples of Crops: Cactus, groundnuts, and watermelons thrive in sandy soils.
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Loamy Soil
- Particle Size: Medium-sized particles; a mix of sand, silt, and clay.
- Porosity: Moderate; allows proper air and water balance.
- Water Retention: Good; retains adequate moisture without waterlogging.
- Air Content: Balanced; sufficient for root respiration.
- Nutrient Retention: High; rich in organic matter and minerals.
- Texture: Crumbly and soft, making it easy to work with.
- Color: Dark due to high humus content.
- Capillarity: Moderate, providing good water movement to plant roots.
- Humus Content: High, as it holds organic matter effectively.
- Examples of Crops: Suitable for most crops, including maize, rice, and vegetables.
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Clayey Soil
- Particle Size: Smallest particles; compact and sticky when wet.
- Porosity: Low; poor drainage due to tightly packed particles.
- Water Retention: High; retains water, often leading to waterlogging.
- Air Content: Low, making root respiration difficult.
- Nutrient Retention: High, as nutrients bind to particles.
- Texture: Heavy and hard to cultivate when dry.
- Color: Often dark or reddish, depending on mineral content.
- Capillarity: Strong, allowing water to rise efficiently.
- Humus Content: Moderate to low, depending on organic input.
- Examples of Crops: Rice thrives in clayey soils due to high water retention.
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Physical Properties of Soils
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Measurement Techniques
- Particle Size:
- Use sieves to separate sand, silt, and clay.
- Porosity:
- Measure how much water drains through a soil sample.
- Water Retention:
- Weigh soil before and after saturating it with water.
- Air Content:
- Observe bubbles released when soil is submerged in water.
- Humus Content:
- Burn a soil sample and measure the weight loss due to organic matter.
- Capillarity:
- Place soil in a dish of water and measure the height water rises over time.
- Texture Test:
- Rub soil between fingers to identify sandy, loamy, or clayey textures.
- pH Testing:
- Use litmus paper or pH meters to measure acidity or alkalinity.
- Temperature:
- Use a soil thermometer to assess heat retention.
- Compaction:
- Press the soil and observe how easily it crumbles.
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- Press the soil and observe how easily it crumbles.
Components of Soil
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Key Components
- Mineral Particles: Sand, silt, and clay form the foundation.
- Organic Matter (Humus): Decomposed plant and animal material, improving fertility.
- Water: Essential for nutrient dissolution and plant uptake.
- Air: Fills spaces between particles, supporting root and microorganism respiration.
- Microorganisms: Bacteria, fungi, and earthworms enhance nutrient recycling.
- Nutrients: Includes nitrogen, phosphorus, and potassium (NPK).
- pH: Determines nutrient availability; most plants prefer slightly acidic to neutral soil.
- Rocks and Minerals: Source of micronutrients like calcium and magnesium.
- Soil Structure: The arrangement of particles determines porosity and water retention.
- Soil Horizons: Layers like topsoil, subsoil, and bedrock vary in composition and fertility.
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Soil Characteristics and Plant Growth
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Soil Types and Plant Health
- Sandy Soil:
- Poor nutrient retention affects plant growth.
- Requires organic matter addition to improve fertility.
- Loamy Soil:
- Ideal for healthy plant growth due to balanced properties.
- Clayey Soil:
- High water retention may cause root rot in some plants.
- pH Balance:
- Alkaline soils need acidifying agents like sulfur; acidic soils need lime.
- Humus Addition:
- Boosts fertility and improves soil structure.
- Crop Selection:
- Match plants with suitable soil types (e.g., rice for clayey soil).
- Drainage:
- Poorly drained soils require amendments like sand or raised beds.
- Aeration:
- Essential for oxygen-dependent roots; improve with tilling.
- Fertilizer Use:
- Replace depleted nutrients for optimal plant growth.
- Mulching:
- Conserves moisture and prevents erosion in sandy soils.
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- Conserves moisture and prevents erosion in sandy soils.
Soil Fertility and Its Loss
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Causes and Solutions
- Loss of Inorganic Matter:
- Overharvesting removes essential minerals; replenish with fertilizers.
- Compaction:
- Heavy machinery compresses soil, reducing aeration.
- Leaching:
- Excessive rainfall washes nutrients away; combat with organic mulches.
- Erosion:
- Wind and water remove topsoil; prevent with cover crops.
- Repeated Cropping:
- Monoculture depletes specific nutrients; use crop rotation to restore balance.
- Soil Salinization:
- Excess irrigation leads to salt accumulation; solve with proper drainage.
- Acidification:
- Overuse of fertilizers increases acidity; counteract with lime.
- Pest Infestations:
- Degrade soil quality; control with integrated pest management.
- Organic Matter Depletion:
- Happens with overuse of chemical fertilizers; add compost or manure.
- Desertification:
- Excessive deforestation or grazing turns fertile land into deserts.
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- Excessive deforestation or grazing turns fertile land into deserts.
Renewal and Maintenance of Soil Fertility
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Techniques
- Crop Rotation: Alternating crops replenishes nutrients.
- Cover Crops: Prevent erosion and add organic matter.
- Composting: Enriches soil with humus and nutrients.
- Green Manuring: Plowing plants like clover into the soil improves fertility.
- Reduced Tillage: Minimizes soil disruption, conserving structure and moisture.
- Organic Mulching: Conserves water, suppresses weeds, and adds nutrients.
- Terracing: Prevents soil erosion on slopes.
- Contour Plowing: Reduces water runoff, conserving topsoil.
- Water Management: Prevents leaching and salinization through proper irrigation.
- Biosolids Application: Recycles nutrients from treated waste.
- Soil Testing: Determines nutrient deficiencies and pH for targeted amendments.
- Fertilizer Application: Use balanced NPK fertilizers based on crop needs.
- Biochar: Enhances soil structure and retains nutrients.
- Microbial Inoculants: Boosts beneficial microorganisms in the soil.
- Reforestation: Restores degraded lands with trees.
- Agroforestry: Combines crops and trees to improve fertility.
- Leguminous Crops: Fix atmospheric nitrogen, enriching the soil.
- Integrated Farming: Combines crop and animal farming to recycle nutrients.
- Education and Awareness: Train farmers in sustainable practices.
- Monitoring: Regularly assess soil health for timely interventions.
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After publishing this post I have this feeling that whoever study this post sincerely will come back to "share testimony"
about their Jamb UTME score. If you are a prospective Jambite and you think this post is resourceful enough, I
enjoin you to express your view in the comment box below. I wish you success ahead. Remember to also give your
feedback on how you think we can keep improving our blog posts.
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I recommend you check my Post on the following:
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- Biology Tutorial on 'Humans and Environment' for Jamb(UTME Candidates)
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This is all we can take on "Jamb Biology Tutorial on the Soil for UTME Candidates"
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