August 2008 Soils Evaluation. August 2008 What good is it? teaches the practical application of the Soil Conservation Service soil classification system.

Slides:



Advertisements
Similar presentations
FactorInformation Needed Enterprise: Natural Resources Unit: Soil Judging I. Intro- duction A. Protecting resources, like soil, is an important career.
Advertisements

Soils and FFA Land Judging Jim Lathem Georgia Agricultural Education Curriculum Office Georgia Department of Education July 2005.
Soil Characteristics and Texture
KLASIFIKASI LANDUSE Bahan Kajian MK. STELA - Landuse Planing Smno.jurtnh.fpubdes2013.
Soil Science.
Land Classification and Use Chapter 8 Land is more than soil n Natural and artificial characteristics of an area to be used for agricultural or other.
 What is Depth of Soil?  The thickness of soil layers which have favorable permeability  What is permeability? The downward movement of water in soil.
Using Land Capability Classifications
Determining Soil Texture by Feel
1 Section:Plant & Soil Science Unit:Soil Management Lesson Title: Homesite evaluations.
Unit C. Basic Principles of Agricultural/Horticultural Science.
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 Texture Getting a feel for the soil!. Soil Texture Defined The relative proportions of the various size groups of individual soil grains (namely.
Chapter 3 Lesson 3 Essential Question: What is soil made up of? TYPES OF SOIL & PARTICLES.
What does the plant say to the worm who offered it a slice of pizza?
Land-Use Scorecard Landscape Characteristics Percent Slope -Percent slope is the rise and fall in 100 feet. -Subtract the difference between the two heights.
Land Evaluation and Classification Kevin Jump Bleckley County High School Compiled from the Land Judging Contest Guide originally prepared by Dr. Frank.
Soils Physical Properties Name______________ Date_________ Hour________.
Soils Physical Properties. Composition of Average Soil.
Growing Plants : The Soil Profile. What is Soil Made up of?
Growing Plants Hydroponically vs. In Soil: The Soil Profile.
Growing Plants Hydroponically vs. In Soil:
Soil Science Faculty of Agricultural and Applied Biological Sciences Ghent University.
Soil & Soil Judging Jeopardy Jeopardy With your host, Mr. C “Soils”
LAND JUDGING EVERYTHING YOU NEED TO KNOW BUT WERE AFRAID TO ASK EVERYTHING YOU NEED TO KNOW BUT WERE AFRAID TO ASK.
2006 Land Judging Contest Tifton, Georgia August 26, 2006 Photos Taken By Jeri Bozeman Slideshow Assembled By Kasey Bozeman.
NC STATE UNIVERSITY DEPARTMENT of SOIL SCIENCE NC STATE UNIVERSITY DEPARTMENT of SOIL SCIENCE Capability Classes.
Intro to Soils. Objectives Define terms relating to soil. Describe factors affecting soil formation. Describe soil weathering factors. Describe the procedure.
Properties of the Soil Wt. Tn. Workshop-Liberty July. 13, 2005.
Interest Approach Provide students with various samples of soil. One sample should be nearly all sand, one nearly all clay, and one nearly all silt. Ask.
SOIL-WATER RELATIONSHIPS: PERMEABILITY AND DRAINABILITY
Weathering and Soil Formation
Estimating Soil Moisture by Appearance and Feel
Understanding Soil Texture and Structure
LAND JUDGING. Land Classification The Soil Conservation Service uses a classification system to describe the capability of the soils to produce crops.
Soil An important resource. No Soil…No Life… WHAT is it??? Mixture of weathered/eroded rock, nutrients, decaying organic matter, water, air and…
Growing Plants Hydroponically vs. In Soil: The Soil Profile.
Physical Properties of Soil Denham Springs Freshman High Ag I.
LandJudging in Oklahoma
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.
Environmental Science: Soil
Soil Texture & Structure. Soil Texture What is Soil Texture? What is Soil Texture?  It is the proportion of three sizes of soil particles. The fineness.
Soil and It’s Importance Provides basic life needs –F–Food and Shelter Very limited resource.
Introduction to Land Evaluation Basic Soil Science AFNR-BAS-6: Describe soil formation and management and assess its relevance to plant/animal production.
Understanding Soil Texture and Structure McAllen FFA Mr. Leal.
 Soil is the lose covering of rock particles and decaying organic matter(humus)  Results from both physical and chemical weathering.
Soil! Video Notes #6. What are we going to learn… Soil-Why is it important? What is soil? Sand, Silt and Clay What’s a soil profile? Horizons? Not all.
Michael Teague. The best soils are used for growing crops Poorer soils are used for grazing.
Land Judging FFA CDE Linsey Fowler. Contest Review  An entry consists of four participants  Four fields to be judged  Additional information provided.
Components & Properties of Soil. Parent Material Unconsolidated mass of rock and mineral from which soil is formed Soil formation occurs where it is exposed.
It’s not DIRT! And it needs our lovin!
Soil Properties.
Soil & Land resources Objective: Evaluate soil properties that affect land use in agricultural and urban areas.
Soils Evaluation.
Soils and FFA Land Judging
Components and Properties of Soil

Land Evaluation Brewer FFA.
Land Judging FFA CDE.
Soil.
An Introduction to the Land Career Development Event
Land Career Development Event
Introduction To Soils.
Soil and It’s Importance
Soil
Land Career Development Event
Soils and FFA Land Judging
Soil.
Linking the Nonliving to the Living
Erosion, Deposition and Soil
Presentation transcript:

August 2008 Soils Evaluation

August 2008 What good is it? teaches the practical application of the Soil Conservation Service soil classification system and related land management practices.

August 2008 Land Capability Classes in Georgia Class I- They may be used for the production of cultivated crops with few limitations. Class IIThese soils may also be used for cultivated crops but they have some limitations that require moderate conservation practices. Class IIIClass III land has severe limitations that require special conservation practices and may reduce the choice of crops. Class IVThese soils are used for cultivated crops but have very severe limitations that restrict the choice of plants and require special management.

August 2008 Georgia Land Capabilities Class VIThese soils have such severe limitations that they are unsuited to cultivated crops and are restricted to pasture, woodland, or wildlife feed and cover.

August 2008 Georgia Land Capabilities Class VIIThese soils have very severe limitations and their use is restricted to forestry and wildlife.

August 2008 FACTORS AFFECTING LAND CLASS Slope Topsoil thickness Erosion Topsoil texture Permeability of the subsoil Drainage Effective depth

August 2008 Slope Slope refers to the steepness of the field. It is determined by the amount of fall in feet per 100 feet and is expressed in percent. If measured over a 100 foot distance, it is easy to convert the fall in feet to percent. Example: if the fall is 12 feet over a distance of 100 feet (12 divided by 100) the slope is 12%

August 2008 Some Methods of determining slope Clipboard & Pencil Hand & Arm

August 2008 SOIL FACTORS Best Land Class For Slope (North Georgia) Catagories of slope % of slopeBest Land class Nearly Level0-2 %I Very Gently2-6%II Gentle6-10%III Sloping10-15%IV Strongly Sloping15-25%V! Steep25-60%VII Very SteepOver 60%VII

August 2008 SOIL FACTORS Best Land Class For Slope (South Georgia) Catagories of slope % of slopeBest Land class Nearly Level0-2 %I Very Gently2-5%II Gentle5-8%III Sloping8-12%IV Strongly Sloping12-17%V! SteepOver 17%VII Very SteepNot ApplicableVII

August 2008 Topsoil thickness 1. Extremely thick -- over 40 inches 2. Very thick to 40 inches 3. Thick to 20 inches 4. Moderate -- 5 to 10 inches 5. Thin -- less than 5 inches

August 2008 Erosion 1.None to slight - less than 25% eroded 2.Moderate - 25 to 75% eroded 3.Severe - Over 75% eroded

August 2008 Topsoil Texture At the contest, students will determine texture by feeling the topsoil.

August 2008 Topsoil Textures - A fine textured soil is smooth and sticky when wet. The particles feel as fine as flour. When balled in the palm of your hand, it holds its shape and shows finger marks. A long ribbon of soil can be formed by rubbing the soil between the thumb and fore finger.

August 2008 Topsoil Textures Medium - A medium textured soil is a mixture of sand, silt and clay particles. It is between fine and coarse. The ball will show some finger marks and hold its shape. A short thick ribbon can be formed.

August 2008 Topsoil Textures Coarse - Coarse textured soils are made up of mostly sand particles. Sand feels gritty and particles are large enough to be easily seen. The ball breaks in your hand and almost no ribbon can be formed.

August 2008 Permeability of the Subsoil Permeability is the ability of air and water to move through the subsoil. Permeable soils (rapid) are often described as "loose" and impermeable soils (slow) as "tight."

August 2008 Permeability 1.Rapid -- Due to a coarse texture greater than 20 inches. 2.Moderate -- Subsoils of fine or medium texture; well defined nut-like structure; visible pores of varying size. 3.Slow -- Subsoils of fine texture; sticky or plastic clay subsoils; few pores visible.

August 2008 Drainage Drainage refers to surface and internal drainage. As a general rule, the more quickly soil can be tilled safely following a good rainfall, the better the drainage.

August 2008 Drainage 1.Excessively drained -- Coarse textured, sandy material that continues to depths of more than 40 inches. 2.Well-drained -- No gray mottles found in top 30 inches of profile. 3.Moderately well- drained -- No gray mottles found in top 20 inches of profile

August 2008 Drainage 4.Somewhat poorly drained -- No gray mottles found in top 10 inches of profile. 5.Poorly drained -- Gray matrix or gray mottles found in top 10 inches of profile. Soil may be gray completely to the surface. 6.Very wet -- Surface water remains for extended periods.

August 2008 Effective Depth Effective Depth is that depth to which plant roots can easily penetrate.

August 2008 Effective Depth 1. Deep -- Over 40 inches 2. Moderate to 40 inches 3. Shallow to 20 inches 4. Very Shallow -- Less than 10 inches