Components of a fertile soil

Slides:



Advertisements
Similar presentations
Soils.
Advertisements

Soil Much more than "dirt".
Soil Characteristics and Texture
Unit 1 Lesson 5 Soil Formation
o Soils are a fertile, natural resource. o Soils develop / form from the weathering of rocks in one place and from re-deposited weathered materials.
SOIL PARTICLES Soil provides support and nutrients for plant growth.
Properties of the Different Kinds of Soil
Soil Much more than "dirt".
TYPES OF SOIL There are three major types of soil, namely; sandy soil, clay soil and loamy soil. SANDY SOIL. Any soil sample that contains sand particles.
Characteristics Texture Soil Profile Soil Types Threats to Soil
Soil 3 – Soil Composition. The ideal composition of soil, 25% Air, 25 % H 2 O, 45% Mineral Matter 5% Organic Matter.
Chapter 4: Soil Architecture and Physical Properties
Properties of Soil. Where does soil come from and how does it form? Most soils were originally created through the breaking down (weathering) of the solid.
Soil provides… nutrients for plant growth. Soil comes from: Rocks Minerals Decaying Organic Matter.
What's your type? Squeeze some soil between your fingers. Is it crumbly? Sticky? A soil's texture depends on the size of its particles. And living things.
What does the plant say to the worm who offered it a slice of pizza?
ALL ABOUT SOIL.
B. Describe how soil is formed, and define terms of formation; Begins when Parent Material or Rock is weathered Weathering: process when the climate breaks.
Growing Plants : The Soil Profile. What is Soil Made up of?
Types of soil Swati Lahamage Archana Lokare
Classification and Testing.  Understanding what type of soil is present is important because it determines what type of plant will be most suited to.
Soil 50% pores and 50% solids
Growing Plants Hydroponically vs. In Soil:
Our Soils CGR 4MI. What is Soil?  To the engineer, soil is a foundation to build.  To the ecologist, soil supports and connects ecosystems.  To the.
SOIL Medium: The soil mixture is the plant’s source for food, water, and support The soil mix will have effect on the health, vitality, and appearance.
Soil Structure. Soil Structure? ‘Arrangement of soil particles, pores and aggregates within a soil body’ Soil produces aggregates – clumps of soil that.
TEKS 4.7A The student is expected to examine properties of soils, including color and texture, capacity to retain water, and ability to support the growth.
That can be observed and measured to predict soil quality
Soils.
Chapter 4 Physical Properties of Soil. Texture Density Permeability Porosity Structure Tilth Compaction Temperature Color Soil physical properties are.
SOILS & SOIL TYPES. What is soil? Soil is one of the basic resources we need to survive – like air and water. the surface layer of the Earth that contains.
The unknown ecosystem.  What is soil? What is it made of? Where do we get if from? What is your “definition” of soil.
Soil Formation and Composition EQ: How do you scientifically describe soil? How is soil formed?
Soils. Formation of Soils Physical Weathering Rain, wind, abrasion Chemical Composition is not altered Influenced by climate Chemical Weathering Acid.
Soil is the growing medium for our food. Without it we could not survive. Soil purifies our waste. Soil is home to plants and animals. It may take up.
Soil Dirt is simply misplaced soil!. SOIL: A RENEWABLE RESOURCE Soil is a slowly renewed resource that provides most of the nutrients needed for plant.
Soil Chapter 2 Soil Physical Properties Pages 26 – 60.
Soil testing Volcano Dreaming Panel 4. Soil observation Place some soil between your thumb and forefinger Manipulate the soil to feel the texture The.
Soil Formation and Composition Biotic (living) Abiotic (nonliving) 1. Make a table and list 5 examples of each.
How Soil Forms WEATHERING AND SOIL. Soil is the loose, weathered material on Earth’s surface in which plants can grow. WHAT IS SOIL?
 Essential Question: How does soil form, and what purposes does it serve?  Objectives: 1. Describe the functions of soil 2. Describe the factors of.
AG-GH/PS-5 GROWING MEDIA. Read the story provided. Write a brief essay explaining the importance of soils in the production of food and fiber for our.
Weathering and Soil Formation Soil Composition:  Soil is a mixture of four materials:  Weathered rock particles (Main ingredient) (Main ingredient)
Understanding Soil Texture and Structure McAllen FFA Mr. Leal.
Soil Texture. Particle Size Distribution (Texture) Important for determining suitability for various uses Considered a basic property because it doesn’t.
Properties of Soil TSW – Examine properties of soil including color and texture, capacity to retain water, and ability to support the growth of plants.
Studying Soil Scientifically. Things plants need in order to grow: 1) Sunlight 2) Water 3) Air 4) Soil with proper nutrients.
Components & Properties of Soil. Parent Material Unconsolidated mass of rock and mineral from which soil is formed Soil formation occurs where it is exposed.
Soils.
Leaving Certificate Agricultural Science
Soil Texture.
The unknown ecosystem THE DIRT ON SOIL.
Soil Much more than "dirt".
Composition of Soils The ideal composition of soil, 25% Air, 25 % H2O,
Soil texture, structure & cultivation
Soil Structure.
SOIL.
Soil.
Soil components.
Soil Much more than "dirt".
Soil Structures.
Soil Structure Action movie.
Soil Structures.
Classification and Testing
8th Grade: The Dynamic Earth (Module E)
Soil Structures.
Linking the Nonliving to the Living
SOIL What is it?.
Soil Types!.
The Dirt on Dirt.
Presentation transcript:

Components of a fertile soil

What makes up a fertile soil? A fertile soil is one that will maintain life, and is made up of minerals, organic matter, water, air and living organisms.

Mineral Components Sand Formed by physical weathering Feels gritty Does not hold together Easy to cultivate Called ‘light soils’ Have large spaces between the grains (pores) so water moves through quickly Dry out quickly Warm up quickly in spring Need irrigation in warm dry weather

Advantages and Disadvantages of Sandy Soils Warm up earlier Less damaged by compaction Less expensive to cultivate Disadvantages Dry out quickly Low water storage capacity so crops growing on them suffer droughts Too well aerated, this tends to destroy organic matter Tends to be more leached (nutrients leave the soil with the movement of water)

Clay Formed by chemical weathering Particles stick together so they feel sticky ‘heavy’ to work Swell when wet and shrink when dry Absorb water easily Slow to warm in spring Clays hold some elements essential to plant growth e.g. calcium, magnesium, potassium and sodium. Particles clump together or FLOCCULATE in the presence of lime – this provides larger spaces for the water to drain through.

Advantages and Disadvantages of Clay soils Good water holding capacity Rich in plant nutrients Disadvantages Water does not drain through readily Slow to warm up in spring Puddle when wet and set like concrete when dry Expensive to cultivate In high rainfall areas may develop an iron pan or a clay pan which leads to water logging Susceptible to damage from stock and implements especially when very wet or very dry

Silt Consists of particles in size between sand and clay Has a slippery or silky feel Pure silt soils erode easily as they do not have good structure Have properties between sandy and clay soils Silt soils have the ability to retain large amounts of moisture Silt soils are well aerated

Loam Soils Contain sand, silt and clay in balance Do not feel gritty when rubbed between the fingers Have properties between sandy soils and clay soils Usually well drained and well aerated Have the ability to hold moisture and plant nutrients

Typical characteristics of a sandy loam: Drainage and aeration Free draining due to the relatively large particle size and the lack of water holding finer particles. Easily leached (washed away) because water can move freely through it and it lacks a lot of the nutrient holding clay particles. Free gas exchange results in good gaseous environment in the soil promoting good root growth and good mining of resources resulting in good growth

Water holding capacity Large pore space allows water to drain freely to lower levels causing moisture stress in dry weather. Reduces the rate of photosynthesis and poor structure due to reduced turgidity therefore less plant growth Temperature Warms quickly due to lack of temperature moderating moisture and free air movement. Allows the soil to warm quickly resulting increased chemical reaction rate in roots and earlier plant growth in the spring

Typical characteristics of a clay loam: Drainage and aeration Poor drainage due to the small particle size and micropores. Water is held tightly so tends to retain nutrients. Gas exchange is restricted in the soil preventing respiration in the roots. Water holding capacity Small pore spaces prevent water from draining freely preventing water stress in dry weather. Temperature Warms slowly because the temperature is moderated by moisture and lack of air movement. Because the soil is slow to warm the sped of chemical reactions in roots is reduced and crops will be harvested later due to later planting (sowing) in the spring.

Below is a sample of garden loam magnified under the microscope Below is a sample of garden loam magnified under the microscope. Copy the diagram and label: air spaces, coarse gravel, water, earthworm, fine sand, and dead organic matter.

Copy out the table below and fill it in correctly SIZE GROUPING OF MINERAL PARTICLES IN SOIL NAME PARTICLE DIAMETER Bigger than 200 mm 20 -200 mm 2- 20mm 0.2 – 2mm 0.02 – 0.2mm 0.002 -0.02mm Less than 0.002mm Write in the following names where you think they should go. CLAY BOULDERS FINE SAND SILT GRAVEL COARSE SAND STONES

What do the following words mean? Mineral Matter Nutrients Infertile Light soils Heavy soils Leaching Loam

SOIL REVISION QUESTIONS Name the main components in soil. Explain what the following terms mean Chemical Weathering Physical Weathering Name three of the five factors that affect the rate of soil formation. Define the following rock types. Igneous Sedimentary Metamorphic