Layers of soil (soil horizons) soil profile

Slides:



Advertisements
Similar presentations
The Nature of Soil Chapter 7, Section 2.
Advertisements

Chapter 15 Soil Resources
Soil Portfolio By Tim Butterfield. What is soil? Soil is the medium in which crops are grown to feed human and other living things. It is also is a loose.
Chapter 15, Section 2: Crops & Soil Standards: SEV4a, b, c
Weathering and Soil.
The Nature Of Soil Ms. Scerra
Soil: A Renewable Resource PA Standards  C: Unifying Themes  B: Technological Devices  C: Ecosystems and their Interactions “Land,
Soil It’s not just DIRT.
Rocks, Weathering, and Soil Information
The Nature of Soil Essential Question:
Soil Resources Soil Erosion, Degradation, and Conservation.
Processes that break down rock.  Rock is broken apart but not changed chemically.
Soil and Soil Conservation
Chapter 7 Weathering and Soil
Crops and Soil.
Unit 4 Soil Science. Importance of Soil What is soil? Holds water and nutrients for plants Natural filter Stores and recycles nutrients Fertile soil =
Soils CharacteristicsTexture Soil Profile Soil Types Threats to Soil.
Soils.
SOIL. What is soil? The loose covering of broken rock particles and decaying organic matter (humus) covering bedrock.
The Soil System Topic 3 The Soil System and Food Production Students will be able to: - to outline how soil systems integrate aspects of living systems.
Soil Formation and Composition
Earth’s Changing Surface
The Ground Beneath Our Feet
*UNPACKED STANDARDS: FOR TEACHER USE ONLY!* Forces deep inside Earth and at the surface produce a slow cycle that builds, destroys, and changes the rocks.
BIG IDEA: Abiotic & biotic factors influence the environment
From Bedrock to Soil.
Soil. Soil Formation Over many years, weathering and erosion will cause the formation of soil. Soil is the loose, weathered material on the Earth’s surface.
How Much Fertile Soil Does Earth Have?
O.
Soil Chapter 7, Section 3 & 4. Soil  A loose mixture of rock fragments, organic material, water, and air that can support the growth of vegetation.
Weathering and Soil Formation Notes. Weathering Two types – Mechanical Weathering Ice Abrasion Wind, Water, Gravity Plants Animals Chemical Weathering.
Soils 2015 is the Year of Soil Soils 2015 is the Year of Soil.
ROCK CYCLE. IGNEOUS ROCK Formed when –magma cools underground EX: granite –Or above ground EX: lava rock/pumice.
The Nature of soil. Dirt is what you find under your fingernails. Soil is what you find under your feet. Think of soil as a thin living skin that covers.
Soil Formation.
Soil as a System. Soil formation is slow and complex Parent material—base geological material in a particular location, can include lava or volcanic ash,
Soil is a System. How do soils form? Mineralization: decomposition or oxidation of the chemical compounds in organic matter into plant-accessible forms.
SOIL.
Characteristics of Soil 5.2 Soil  Soil is part of the regolith that supports the growth of plants. Regolith is the layer of rock and mineral fragments.
Instructions for using this template. Remember this is Jeopardy, so where I have written “Answer” this is the prompt the students will see, and where.
Soil horizons Farming Techniques Erosion Soil Particles.
Are these examples of weathering, erosion, or both?  1. Ice breaking rock  2. Wind breaking away and moving rock  3. A river moving sediment  4. Tree.
Soil Formation and Composition
Weathering  It is surface processes that break down rock  Breaks rocks into smaller and smaller pieces  Ex.) Sand, silt, clay  The formation of soil.
What Are Some Types of Soil?
Soil Formation and Composition.  I. Soil Formation –A. When bedrock is exposed, it weathers. –B. Particles of rock mix with other material. –C. Soil.
NOVEMBER 4, 2015 Silently title your notes: LAYERS OF SOIL
Soil ..
The Nature of soil.
The Nature of Soil Essential Question:
Soil as a System.
The Nature of Soil Essential Question:
Soils of Canada.
The Ground Beneath Our Feet
Soil Formation How Soil Forms.
Soil 7.EC.5A.2 Construct explanations of how soil quality (including composition, texture, particle size, permeability, and pH) affects the characteristics.
The Nature of Soil Essential Question:
All About Soil.
Characteristics Texture Soil Profile Soil Types Threats to Soil
Soil Regolith – layer of rock and mineral fragments produced by weathering Soil – part of regolith that supports plant growth.
How is Soil Formed? Over many years, weathering and erosion will cause the formation of soil. Soil is the loose, weathered material on the Earth’s surface.
7.EC.5A.2 Construct explanations of how soil quality (including composition, texture, particle size, permeability, and pH) affects the characteristics.
Mechanical Weathering
What is happening in numbers 1, 2, 3 and 4
Chapter Soils.
Soil Formation Soil – The loose, weathered material on Earth’s surface in which plants can grow. How is soil formed? Mechanical and chemical weathering.
It provides minerals and other nutrients for plants.
Soil Formation How Soil Forms
Week 3: Lesson 2 and 3 Soils and Relationships
Presentation transcript:

Layers of soil (soil horizons) soil profile Surface litter – fallen leaves and partially decomposed organic matter Topsoil – organic matter, living organisms, and rock particles Zone of leaching - dissolved or suspending materials moving downward, minerals may leach quickly and deprive plants of nutrients Subsoil – larger rock particles with organic matter, and inorganic compounds Weathered parent material – rock that has undergone weathering Bedrock – solid rock layer

Topsoil is richer in organic matter than the other soil layers; without it plants cannot grow Particle size increases down

Soil Characteristics Color Texture Darker soils means richer in humus and nutrients Use as indicator of soil’s fertility Texture Based on particle size Clay, silt, and sand (smallest to largest) Loam – even mixture of the 3 particle sizes Influences workability because of how porous it is Finer the particle size, less space and harder for air and water to travel through Silty soil or loamy material is best for plant growth

Soil Characteristics (continued) Structure Arrangement of particles – “clumpiness” Clumpy soil has more humus and is more rich in nutrients Too clumpy may prevent plant roots from growing pH Plants die if soil is too acidic or too alkaline Acid precipitation and leaching can affect pH

Learning Target To understand ways to prevent soil degradation and why they will prevent soil degradation

Land degradation occurs when human activity or natural processes damage land so that it can no longer support plant growth or other ecosystem services

Erosion #1 cause of land degradation Can help create soil through deposition Takes away the topsoil Humans cause this through overgrazing, clearing forests on slopes, clear-cutting, and leaving soil bare after harvests

Farming Practices for Soil Conservation Plants slow wind and water roots hold soil in place and absorb water Intercropping Crop rotation Cover crops Shelterbelts Conservation tillage Terracing Contour farming soil conservation

Intercropping Planting crops in mixed arrangements More plant cover Less vulnerable to insects and disease

Crop rotation Alternate crops grown in a field Returns nutrients to soil Breaks disease and pest cycles Prevents erosion