Land-Use Scorecard Landscape Characteristics Percent Slope -Percent slope is the rise and fall in 100 feet. -Subtract the difference between the two heights.

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

August 2008 Soils Evaluation. August 2008 What good is it? teaches the practical application of the Soil Conservation Service soil classification system.
Student Learning Objectives
Soil Science.
Weathering and Soil Formation
 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
Physical Support Nutrients Water Aeration (O2).
FFA Land Judging Using the 2005 Scorecard and Guidebook Terence H. Cooper Dept. of Soil, Water, & Climate University of Minnesota, St. Paul.
Unit C. Basic Principles of Agricultural/Horticultural Science.
Unit C1 Basic Principles of Agricultural/Horticultural Science.
Understanding Soil Texture and Structure Mr. Pullom Fall 2011.
1 Section:Plant & Soil Science Unit:Soil Management Lesson Title: Homesite evaluations.
Unit C. Basic Principles of Agricultural/Horticultural Science.
Soil Texture Getting a feel for the soil!. Soil Texture Defined The relative proportions of the various size groups of individual soil grains (namely.
Soil provides… nutrients for plant growth. Soil comes from: Rocks Minerals Decaying Organic Matter.
Land Evaluation and Classification Kevin Jump Bleckley County High School Compiled from the Land Judging Contest Guide originally prepared by Dr. Frank.
Soils Information By: Becky McGuire. Soil A. outer layer of earth’s crust, renewable natural resource that supports life --takes 1000 years for 1 inch.
Animal, Plant & Soil Science Lesson D1-4 Soil Color.
Growing Plants : The Soil Profile. What is Soil Made up of?
Growing Plants Hydroponically vs. In Soil: The Soil Profile.
Lab 2 Soil Properties and Profiles. Activities for Today Texture: Determine texutral classes by feel, and identify textures of unknown samples; Soil Color:
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”
Unit C. Basic Principles of Agricultural/Horticultural Science.
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.
Properties of the Soil Wt. Tn. Workshop-Liberty July. 13, 2005.
Understanding Soil Texture and Structure. Soil Texture Soil Texture:  Fineness or coarseness of a soil What are the three soil particles? ◦ Sand ◦ Silt.
SOILS and PLANT NUTRITION
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.
Chapter 4 Physical Properties of Soil. Texture Density Permeability Porosity Structure Tilth Compaction Temperature Color Soil physical properties are.
Weathering and Soil Formation
Estimating Soil Moisture by Appearance and Feel
Horticulture Science Lesson 25 Understanding Soil Texture and Structure.
Understanding Soil Texture and Structure
Understanding Soil Texture and Structure. Objectives: Describe the concept of soil texture and its importance; Describe the concept of soil texture and.
Soil Classification Comparison Hall County, Georgia University of Florida Soil Pedology, Spring 2010 Prof: Willie Harris By: Sam Vacca 4/22/10.
Physical Properties of Soil Denham Springs Freshman High Ag I.
LandJudging in Oklahoma
Understanding Soil Formation Mr. Pullom Fall 2011.
Ga Ag Ed Curriculum Office, July 2002 Adapted for Colorado Soils Curriculum 2006.
Soil Project: Two Southeast Michigan Soils Ray Powe SWS 5716C.
Soil Structure, Density, and Porosity
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.
Recognizing Soil Texture & Structure
1 Soil Color Lesson Plan: NRES B Anticipated Problems 1. What physical features are used to differentiate between soils? 2. What colors are used.
Horticulture Science Lesson 24 Understanding Soil Color.
Essential Question- What is soil made of
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.
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.
How Is Soil Formed?  Have you ever squished your toes in a muddy garden?
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.
Studying Soil Scientifically. Things plants need in order to grow: 1) Sunlight 2) Water 3) Air 4) Soil with proper nutrients.
Soils and Growing Media
Physical Properties of Soil. Soil Texture What is Soil Texture? It is the proportion of three sizes of soil particles. Which are: Sand (Large) Silt (Medium)
It’s not DIRT! And it needs our lovin!
Soil & Land resources Objective: Evaluate soil properties that affect land use in agricultural and urban areas.
Soils Evaluation.
Basic Principles of Agricultural/Horticultural Science
Land Evaluation Brewer FFA.
Land Judging FFA CDE.
Soil and It’s Importance
Properties of Soil.
Rocks Weathering and Soil Components
Land Career Development Event
Presentation transcript:

Land-Use Scorecard Landscape Characteristics Percent Slope -Percent slope is the rise and fall in 100 feet. -Subtract the difference between the two heights and multiply by 4 if taken at 25 feet.

Landscape Characteristics Percent Slope  0-2 % Nearly level  2-5% Gently Sloping  5-10% Moderately Sloping  10-15% Strongly Sloping  15-20% Moderately Steep  20-30% Steep  More than 30% Very Steep

Thickness of Plow or Surface Layer, Degree of Erosion & Deposition  Directly related to % slope  Measure from the top of the profile down to where the subsoil starts  8” to 20” deposition (more likely 20” to 60”)  This will be the lowest of the sites, likely near a ditch or stream  The entire profile is topsoil, the lower half will be darker than the upper half

 Thickness of Plow Layer  More than 9”, no evidence of subsoil mixing; none to slight erosion  3” to 9”, may have up to 50% subsoil mixing; moderate erosion  Less than 3”, plow layer may be mostly subsoil; severe erosion  8” to 20” deposition layer of different color or texture than buried surface soil

Soil Profile Characteristics  Color and percent of organic matter in plow (surface) layer  Moisten 2 inches from the top-get some moistened soil on the color chart chips and match the nearest chip  See chart next slide

 Color  Very dark  Dark  Moderately dark  Light  Very light  Ave. % O. M. 55  3 ½  2 ½ 22  1 ½ Organic Matter Content

 Presence of Grayish E Horizon  A 2”to 6” layer between the topsoil & subsoil  Primarily found in forest soils  If WET it will appear as a grayish, ashy, pasty material  If DRY it will be a reddish brown,with a platy structure

Soil Profile Characteristics  Grayish E horizon present  Grayish E horizon not present  Note: A 2 horizon was its previously known letter designation

Soil Profile Characteristics  Subsoil color  Measure from the top of the profile down to 24”  If there are gray mottles above 24” it will be gray and brown mottled  If there are gray mottles below 24” will be brown or yellowish brown; gray or gray mottling below 24”

 If there are NO gray mottles in the subsoil it will be brown or yellowish brown; no gray mottling  Note: Don’t confuse Gray substrata with Gray subsoil Subsoil Color

Soil Profile Characteristics  Texture  a. Fine-textured a ribbon forms easily and remains long and flexible.  b. Moderately fine-textured a ribbon forms but breaks into pieces ¾ to 1 inch long.

 c. Medium-textured no ribbon forms. The sample breaks into pieces less than ¾ inch long. The soil feels smooth and talc-like.  d. Moderately coarse-textured no ribbon forms. The sample feels gritty and lacks smoothness.  e. Coarse-textured no ribbon forms. The sample is composed almost entirely of gritty material and leaves little or no stain. Texture (cont.)

Soil Profile Characteristics  Texture  Wet CLAY (fine texture) will leave a “stain” on your hands  A profile with NO TRUE TOPSOIL could have a moderately fine topsoil and a moderately fine subsoil

 Texture  Peat & muck soils will be very black with black dust that leaves black on your fingers & it’s spongy to walk on  Substrata-first determine if it is present  Go to the bottom 1 foot of the profile = is the soil a different texture or color than the subsoil?

 Texture  Substrata is usually gray-moist-pasty- has no structure-will not break on even planes-no roots, and no dark coatings. It is highly that this type of substrata has a medium texture  A reddish tinted soil at in the bottom foot that ball & bounces easily will have a fine texture

 Texture  If the texture in the bottom foot is the same as the subsoil texture = the substrata in not present

Soil Structure  Types of Soil Structure  Single grain = sand  Massive = won’t happen  Granular = plowlayer (if it’s not a true topsoil)  Platy = clods come out of the profile more Horizontal than Vertical

Soil Structure (cont.)  Blocky = (subsoil) clods break on irregular shape planes  Prismatic or Columnar = clods come out of the profile more Vertical than Horizontal

Soil Structure  A plowlayer with NO TRUE TOPSOIL could easily have a Blocky structure  Determine Structure by how the clods chip out of the profile walls.

Associated Soil Features  Internal Drainage and Aeration  This is a DIRECT MATCH with your SUBSOIL COLOR selection.  If you miss Subsoil Color your also going to miss Internal Drainage & Aeration.

Internal Drainage and Aeration  Example: If you choose a Gray and Brown mottled for you subsoil color than you will choose Somewhat poorly drained for your internal drainage and aeration.

Surface Runoff  Combine the finest of the topsoil/subsoil Textures with the % Slope on the front #I.  Use Table #1 to determine the surface runoff  Area subject to ponding = will this be the last spot where water drains after a rain?  Area subject to flooding = this area must be next to a continuous running stream.

Permeability  The ease of water and air movement  Match with Subsoil texture:  Rapid = coarse / moderately coarse  Medium = medium / moderately fine  Slow = fine or bedrock

Soil Depth  Measure to the lowest roots  Bedrock is the only thing that will cause the soil depth to be shallow

Available Water Holding Capacity  Use Table #2  Use a 60 inch profile  If you can only see the A and B horizon then add the two thicknesses of each horizon and subtract the total from 60 to get the C horizon.  Usually very high in Central Illinois

Figuring C-Value  Given:% Slope  Slope Length  Z Factor  The percent slope in NOT the site’s actual % slope. The C-Value information does NOT necessarily pertain to the site.

C-Value Procedure  1. Combine the % Slope and the slope Length on Table #4  2. Take the Table # 4 number & divide it into Z. (Z always goes in the calculator first)  3. Just write down the first two numbers past the decimal point and drop all other numbers. (do not round up)

Procedure (cont.)  4. The answer you get by dividing is the C-Value.  5. On each of the five horizontal rotation/tillage choices = X the exact C-Value number or the next LOWEST number.

Procedures (cont.)  In order for YES to be checked for restricted use = you must have checked all four rows as DOES NOT APPLY  If C-Value is.02 or higher = NO will always be checked for restricted use

Nonagricultural Use  Use Tables 6 (Home site) & 7 (Septic Tank)  O = None to Slight  M = Moderate  S = Severe  You must have filled the scorecard out first in order to record this information. Look up the information from your scorecard.

Nonagricultural Use  The only difference between the two charts is that “somewhat poorly drained” for home site is considered moderate but “somewhat poorly drained” for septic tank is considered severe. All the other answers will be the same for both.

Degree of Limitation  You just place an X for the highest degree used in the home site and the highest degree used for the septic tank.  Severe is the highest, Moderate is second and Slight is the lowest degree of limitation.