Soils Evaluation.

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

Soil Characteristics.
Soils and FFA Land Judging Jim Lathem Georgia Agricultural Education Curriculum Office Georgia Department of Education July 2005.
August 2008 Soils Evaluation. August 2008 What good is it? teaches the practical application of the Soil Conservation Service soil classification system.
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
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.
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.
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.
Estimating Soil Moisture by Appearance and Feel
LAND JUDGING. Land Classification The Soil Conservation Service uses a classification system to describe the capability of the soils to produce crops.
Growing Plants Hydroponically vs. In Soil: The Soil Profile.
Physical Properties of Soil Denham Springs Freshman High Ag I.
LandJudging in Oklahoma
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.
To be the best you have to beat the best!. Part 1 Physical Characteristics of the Soil.
Components & Properties of Soil. Parent Material Unconsolidated mass of rock and mineral from which soil is formed Soil formation occurs where it is exposed.
Soil and Water Resources WATER RESOURCES.
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.
Soil AG-BAS-17-(a – c), ELA10RC2 (a), SSWG8 (d), SES3
Soil Objective: I will be able to explain what soil is and why it is important by creating an illustration.
Soils and FFA Land Judging
Soil An important resource.
Chapter 6 Lesson 2 Soil Pages
Soil Much more than "dirt".
Soil Science Objectives: Identify the major soil areas of Alabama. Identify the layers in a soil profile. Determine the texture of different soil samples.
Components and Properties of Soil

Non- Agricultural Land Uses
Land Evaluation Brewer FFA.
Land Judging FFA CDE.
Soil Texturing Flow Chart
Soil.
An Introduction to the Land Career Development Event
Land Career Development Event
Soil A recipe for soil.
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:

Soils Evaluation

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

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

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

Georgia Land Capabilities Class VII These soils have very severe limitations and their use is restricted to forestry and wildlife.

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

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%

Some Methods of determining slope Clipboard & Pencil Hand & Arm

SOIL FACTORS Best Land Class For Slope (North Georgia) Catagories of slope % of slope Best Land class Nearly Level 0-2 % I Very Gently 2-6% II Gentle 6-10% III Sloping 10-15% IV Strongly Sloping 15-25% V! Steep 25-60% VII Very Steep Over 60%

SOIL FACTORS Best Land Class For Slope (South Georgia) Catagories of slope % of slope Best Land class Nearly Level 0-2 % I Very Gently 2-5% II Gentle 5-8% III Sloping 8-12% IV Strongly Sloping 12-17% V! Steep Over 17% VII Very Steep Not Applicable

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

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

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

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.

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.

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.

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."

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.

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. Closed depression subject to ponding, located in the Great Plains.

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

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.

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

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