Delineating Soil Horizons. Soil as a Natural Body Parent Material Bedrock Additions Losses Translocations Transformations Differentiation Bedrock.

Slides:



Advertisements
Similar presentations
How do soils form? Soil Profiles
Advertisements

Soil Formation and Composition
Basic Principles of Agricultural/Horticultural Science
Horticulture Science Explaining a Soil Profile
Student Learning Objectives
Soil Physical Properties – Colour, Texture, Structure
What is weathering? Breaking down of rocks & other materials on Earth’s surface.
Earth’s Surface Chapter 4 Section 2
SOIL. WHAT IS SOIL? SOIL IS A MATERIAL THAT FORMS THE CRUST OF THE EARTH. IT COMES FROM THE WEATHERING OF ROCKS AND DECOMPOSITION OF ORGANISMS. IT IS.
Characterizing Soil Horizons Physical Properties of Soils.
How do soils form? Processes. 4 basic processes in the soil ADDITIONS LOSSES TRANSLOCATIONS TRANSFORMATIONS (MOVEMENT WITHIN THE SOIL) (ONE COMPONENT.
Unit C. Basic Principles of Agricultural/Horticultural Science.
HOMEWORK Text Book: Read pages Do questions 1-5 on page 266. Review Book: Read pages Do questions on page 85. Write out questions.
Hydric Soils Wetland criteria Hydrology Hydric soils Hydrophytic plants.
Soil Physical Properties
1 Important/significant foundation soil physical properties Color Redoximorphic features Texture Structure Consistence Coarse fragments Reaction.
Student Learning Objectives
Animal, Plant & Soil Science Lesson D1-4 Soil Color.
3G Science - Soils. 3 Layers of Soil Topsoil – top layer of soil. Has the smallest grains. Most humus. Richest layer of soil. Subsoil – Under the topsoil.
Soil Color GES 394 Revised by Mr. Brian Oram
Soil: More than just a bunch of dirt
Lab 2 Soil Properties and Profiles. Activities for Today Texture: Determine texutral classes by feel, and identify textures of unknown samples; Soil Color:
What is Soil?  Soil itself is very complex.  It would be very wrong to think of soils as just a collection of fine mineral particles (dirt.)  Soil.
Anyone who did not attend Lecture I, see me after class for materials and course basics.
Color Theory and Painting Vocabulary. Composition is the arrangement of the parts in a work of art, usually according to the principles of design.
Unit C. Basic Principles of Agricultural/Horticultural Science.
Weathering / Soils Weathering  The process by which natural forces break down rocks  Erosion: The break up and transport.
Soil Color. Soil Color… Has little effect on the behavior and use of soil –Exception: Soil warming Provides valuable clues, which helps scientists classify.
Soil Analysis Lab AP Biology November Properties of Soil Soil Texture –Determined by 3 soil components (listed largest to smallest) Sand Silt Clay.
Soil Science.  Used in much the same way as forensic geology  Soil represents a combination of geologic and biologic components  Classified much more.
Soils Up Close: The Soil Profile and Horizon Characteristics.
Soil Evolution Field Biology CCTI Mrs. Conway. Directions Read through the following slides while completing your lab packet. Be sure to answer all question.
Soil Origin and Development
SOIL COLOR. DETERMINANTS OF SOIL COLOR SOIL COLOR DETERMINANTS OF SOIL COLOR 1. Parent Material 2. Vegetation Prairie vs. Forest 3. Age 4. Topography.
Chapter 4 Physical Properties of Soil. Texture Density Permeability Porosity Structure Tilth Compaction Temperature Color Soil physical properties are.
Objective: Explain what soil consists of Describe the horizons of soil Essential Question: Why do soil horizons form the way they do? Earth’s Surface Text.
Soil Properties Willie Harris Acknowledgments:
12.2 Soil Key Ideas: Soil is made of weathered rock and organic material. Climate and other factors affect the composition of the soil.
1 Soil Color & Its Causes. 2 Factors that give soil color 1.Organic matter 2.Weathered mineral material composing the soil 3.Quantity and condition of.
SOIL HORIZONS Mrs. Wilson 9 th Grade Life Science.
Ga Ag Ed Curriculum Office, July 2002 Adapted for Colorado Soils Curriculum 2006.
Characteristics that differentiate soil horizons
Soil Profile, Classification and Physical Properties Soils & Fertilizers for Master Gardeners In-service Training June 9, 2008 Amy Shober UF/IFAS Gulf.
Soil Formation and Morphology Basics.
Soil Section 5.2.
SOIL PROFILE A vertical strip of soil stretching from the surface down to the bedrock and including all of the successive soil horizons.
Soil Morphology Willie Harris Acknowledgments:
Hue: the property of light by which the color of an object is classified as red, blue, green, or yellow in reference to the spectrum. Saturation: the.
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.
Origins- parent material; mixtures of eroded rock, mineral nutrients, decaying organic matter, and billons of living organisms (mostly decomposers)
 Soil Horizon. Horizon  Horizon is a side profile of the layers of soil  Soil is usually divided into 3 main layers, but will also include the layers.
 Vocabulary  Soil: Well weathered rocks and minerals mixed with decaying organic matter which covers much of earth’s land surface.  Humus: Soil containing.
Soil Horizon.
Soil Science Trace Evidence 2.
Soil Horizon.
Soil Color McIntosh Soil.
Soils Up Close: The Soil Profile and Horizon Characteristics
Soil Horizon.
Soil The following power point was adapted from Ryan P. Murphy. A full collection of his amazing power points can be found at:
How do soils form? Soil Profiles
Table of Contents Title: 7.3 Soil Texture, Fertility and Color
Soil Profiles.
Soil Horizon.
Warm Up 10/14/ Igneous rocks can be classified as intrusive and extrusive. Explain what that means in terms of form? 2. How are sedimentary rocks.
Soil Profiles.
5.2: Soil regolith: layer of rock and mineral fragments created from weathering soil: part of regolith that can support plant life.
Soils and Soil Science.
Soil Profile.
Soil and Soil Profiles.
Presentation transcript:

Delineating Soil Horizons

Soil as a Natural Body Parent Material Bedrock Additions Losses Translocations Transformations Differentiation Bedrock

Soil Horizons Roughly parallel layers in the soil with varying composition and properties

Master Horizons

Criteria for Characterizing Soil Horizons ColorTextureDensityStructure Organic matter MineralogyChemistry

Soil Color

Mineralogy of the soil/parent material Relative amount of organic matter Hydrology of the soil Soil chemistry Soil Microbes Soil Color Determinants

Coloring Agents in Soils Organic Matter Grey to Black coloration particularly in topsoil or A horizon material. Can be found in the sub-soil as an accumulation Elements and Compounds Iron, manganese Reddish to yellow-brown Purplish black

Soil Color Determination

Value Chroma Hue Munsell Soil Color dominant spectral color; related to the wavelength of light. Related to the proportions of red to yellow. In soils we only use 1/5 of the color chips available. related to total amount of light reflected. measure of the strength of spectral color

0 2.5YR 5YR 7.5YR 10YR Y 5Y 10R

Hue 10 R 2.5 YR 5 YR 7.5 YR 10 YR 2.5 Y 5 Y RedYellow Increasingly dominated by yellow spectral color Pages Florida soils dominated by 7.5 YR and 10 YR pages

Soil Color

Hue = 10 YR Value = 6 Chroma = 3 Munsell Color 10 YR 6/3

10 YR 2/1 10 YR 5/6

Pale Red Red Weak Red light Red Pink Dark Red

Summary A horizon – mid/low value - low chroma E horizon – high value - low chroma B horizon – ? value - ? chroma

Water table depth Oxygen status Development decisions

Hue 10YR or Yellower Value≤ 3 Chroma ≤ 1 Hydric Soil Classification “Black Histic”

MineralFormulaSizeMunsellColor goethiteFeOOH(1-2 m m)10YR 8/6yellow goethiteFeOOH(~0.2 m m)7.5YR 5/6strong brown hematiteFe 2 O 3 (~0.4 m m)5R 3/6red hematiteFe 2 O 3 (~0.1 m m)10R 4/8red lepidocrociteFeOOH(~0.5 m m)5YR 6/8reddish-yellow lepidocrociteFeOOH(~0.1 m m)2.5YR 4/6red ferrihydriteFe (OH) 3 2.5YR 3/6dark red glauconiteK(Si x Al 4- x )(Al,Fe,Mg)O 10 (OH) 2 5Y 5/1dark gray iron sulfideFeS 10YR 2/1black pyriteFeS 2 10YR 2/1black (metallic) jarositeK Fe 3 (OH) 6 (SO 4 ) 2 5Y 6/4pale yellow todorokiteMnO 4 10YR 2/1black humus 10YR 2/1black calciteCaCO 3 10YR 8/1white dolomiteCaMg (CO 3 ) 2 10YR 8/2white gypsumCaSO 4× 2H 2 O 10YR 8/3very pale brown quartzSiO 2 10YR 6/1light gray

Low Value Low Chroma Low Value high Chroma High Value

Criteria for Characterizing Horizons ColorTextureDensityStructure Organic matter MineralogyChemistry

Jon Demps Melissa Odal Grant Baysinger Daniel Kristiansen Markihe Anderson Percy Harvin See the Teaching Assistants Before Leaving: Also anyone who has not received a student number