Soils 101- Physical properties

Slides:



Advertisements
Similar presentations
Sedimentation Test of Soil Texture
Advertisements

Soil Texture and Structure Chris Thoreau February 24, 2012.
Contain have END SHOW. Soil is Important! Soil is the link between the rocky crust of the Earth and all life on the Earth’s surface. It is a subsystem.
Unit 1 Lesson 5 Soil Formation
Earth’s Surface Chapter 4 Section 2
Soils Plant Material Maintenance. Soil Soil is the top layer of the Earth’s crust.  Millions of years to make  Being lost at a rate of 5.2 tons/acre/year.
Properties of the Different Kinds of Soil
Components and Physical Properties of Soil Unit: Soil Science Lesson 3.
PHYSICAL PROPERTIES OF SOIL
 Necessary materials: PowerPoint Guide Teacher Information!
Soil 3 – Soil Composition. The ideal composition of soil, 25% Air, 25 % H 2 O, 45% Mineral Matter 5% Organic Matter.
Chapter 4: Soil Architecture and Physical Properties
Soil: A Renewable Resource PA Standards  C: Unifying Themes  B: Technological Devices  C: Ecosystems and their Interactions “Land,
Soil Types and Textures
Physical Properties of Soils Introduction to Agriculture.
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.
Physical Properties of Soil
ALL ABOUT SOIL.
Soil Physical Properties Used to Assess Soil Quality Field Exercise.
Soil Components Melissa Morris. Four Major Components Organic Matter Water Air Mineral Materials Exist in a close mixed condition Interactions among components.
Soil Topic 2052 Anna Blight. What is soil? Soil is the product of the rocks from which it was derived after weathering The top layer of the earth’s crust.
Physical Properties of Soil
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.
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.
Growing Plants : The Soil Profile. What is Soil Made up of?
 Different types of soil  Soil is made of four parts:  1) Sand  2) Silt  3)Clay  4)Humus.
Comparing soils Type of Soil Example of Test Jar
Growing Plants Hydroponically vs. In Soil:
Soils 102 – Chemical properties. It’s more than just salt...
Soil Structure. Soil Structure? ‘Arrangement of soil particles, pores and aggregates within a soil body’ Soil produces aggregates – clumps of soil that.
Lecture 7 b Soil Water – Part 2
Soils.
Soil Sand, Silt, Clay.
Soil Quality Explain the effects of soil quality on the characteristics of an ecosystem.
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.
Components of a fertile soil
Soil and Media % inorganic solids (rocks, sand, silt, clay) 1-10% organic solids (organic matter, residues, roots, microbes) 20-30% water or soil.
Drill (Pre-Lab) Soil Pre-Test: Take an “educated” guess!
The unknown ecosystem.  What is soil? What is it made of? Where do we get if from? What is your “definition” of soil.
Soil Chapter 2 Soil Physical Properties Pages 26 – 60.
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 & Soil Mediums April 4, 2014.
Essential Question- What is soil made of
Earth Matters: Investigating Soil. Where Does My Lunch Come From?
What is the best soil for growing plants? Loam soil that is made of almost equal parts of clay, sand, and silt is the best. This texture is important so.
Day 19 Objective You will learn about soil texture and composition in order to determine soil’s value as a resource and conservation measures. Warm-Up.
Lecture 7 b Soil Water – Part 2 Source: Dept of Agriculture Bulletin 462, 1960.
Properties of Soil TSW – Examine properties of soil including color and texture, capacity to retain water, and ability to support the growth of plants.
Soil Texture Testing Highland High School Property Ms. Norris Highland High School Earth Science 2015.
7-4.4 SOIL QUALITY. Soil is one of the most valuable abiotic factors in an ecosystem because everything that lives on land depends directly or indirectly.
Physical Properties of Soil. Soil Samples USESoil TypeWhy? Garden Livestock Pen Roadway Drainage Area Building Foundation Match the soil samples in the.
Leaving Certificate Agricultural Science
Soil Physical Properties Used to Assess Soil Quality
Soil Structure.
The unknown ecosystem THE DIRT ON SOIL.
Soil Texture.
Soil Formation and Components
Soil Structures.
Soil Science Written By Jim Melby Revised By Sam Behrends
Soil 7.EC.5A.2 Construct explanations of how soil quality (including composition, texture, particle size, permeability, and pH) affects the characteristics.
Soil Quality
Soil Structures.
7.EC.5A.2 Construct explanations of how soil quality (including composition, texture, particle size, permeability, and pH) affects the characteristics.
Soil Structures.
Soil moisture, percent organic matter and soil texture calculations
Soil Formation and Components
Soil Sand, Silt, Clay.
Presentation transcript:

Soils 101- Physical properties

Soils 101- Physical properties It’s more than just “dirt”

Introduction – Why should I care?

Introduction – Why should I care? Different soil types have unique properties

Introduction – Why should I care? Different soil types have unique properties Those properties, along with environment, affect tree survival and growth

Introduction – Why should I care? Different soil types have unique properties Those properties, along with environment, affect tree survival and growth Planting the wrong tree for the site is a waste of time and $

Introduction – Why should I care? Different soil types have unique properties Those properties, along with environment, affect tree survival and growth Planting the wrong tree for the site is a waste of time and $ Soil physical properties – the first thing to know about a site

Photos courtesy of Dave Hopkins, NDSU Barnes soil Photos courtesy of Dave Hopkins, NDSU

Photos courtesy of Dave Hopkins, NDSU Barnes soil Bowdle soil Photos courtesy of Dave Hopkins, NDSU

Soil components

Soil components Solids and pores

Soil components Solids and pores Solids – Minerals + Organic matter

Soil components Solids and pores Solids – Minerals + Organic matter Pores – Water + Air

Soil components Solids and pores Solids – Minerals + Organic matter Pores – Water + Air Ideal soil – Even mix of solids and pores ...

Mineral 45% Organic 5% Brady, 1990

Soil components Solids and pores Note: Solids – Minerals + Organic matter Pores – Water + Air Ideal soil – Even mix of solids and pores ... Note: Minerals – Sand (largest), silt, clay (smallest)

Soil components Solids and pores Note: Solids – Minerals + Organic matter Pores – Water + Air Ideal soil – Even mix of solids and pores ... Note: Minerals – Sand (largest), silt, clay (smallest) Pores – Even mix of water and air

Soil components Solids and pores Note: Solids – Minerals + Organic matter Pores – Water + Air Ideal soil – Even mix of solids and pores ... Note: Minerals – Sand (largest), silt, clay (smallest) Pores – Even mix of water and air Organic matter is good stuff ...

Organic matter Holds onto water Great source of nutrients Binds soil particles together into larger aggregates

Texture

Texture Relative amount of sand, silt and clay only

Texture Relative amount of sand, silt and clay only Lots of one part – soil named by that part

Texture Relative amount of sand, silt and clay only Lots of one part – soil named by that part e.g., 20% sand, 20% silt, 60% clay – clay

Texture Relative amount of sand, silt and clay only Lots of one part – soil named by that part e.g., 20% sand, 20% silt, 60% clay – clay e.g., 12% sand, 82% silt, 6% clay – silt

Texture Relative amount of sand, silt and clay only Lots of one part – soil named by that part Mixtures are called loams

Texture Relative amount of sand, silt and clay only Lots of one part – soil named by that part Mixtures are called loams e.g., 40% sand, 40% silt, 20% clay – loam

Texture Relative amount of sand, silt and clay only Lots of one part – soil named by that part Mixtures are called loams e.g., 40% sand, 40% silt, 20% clay – loam e.g., 33% sand, 33% silt, 34% clay – clay loam

Texture triangle

Example: 20% sand 60% clay 20% silt

Example: 20% sand 60% clay 20% silt

Example: 20% sand 60% clay 20% silt

Example: 20% sand 60% clay 20% silt

Example: 20% sand 60% clay 20% silt Clay soil

Example: 62% sand 15% clay 23% silt ???? soil

Example: 62% sand 15% clay 23% silt sandy loam soil

Texture Relative amount of sand, silt and clay only WHY SHOULD I CARE?

Texture Relative amount of sand, silt and clay only WHY SHOULD I CARE? Different soil types have unique properties Those properties, along with environment, affect tree survival and growth Planting the wrong tree for the site is a waste of time and $

Pore Space

Pore Space Size matters

Pore Space Size matters – macropores and micropores

Pore Space Size Macropores – large, water drains easily

Macropores Brady, 1990

Pore Space Size Macropores – large, water drains easily Micropores – small, water held tightly

Macropores Micropores Brady, 1990

Pore Space Size Texture effects Macropores – large, water drains easily Micropores – small, water held tightly Texture effects

Pore Space Size Texture effects Macropores – large, water drains easily Micropores – small, water held tightly Texture effects Sands – lots of macropores

Pore Space Size Texture effects Macropores – large, water drains easily Micropores – small, water held tightly Texture effects Sands – lots of macropores Clays – lots of micropores

Pore Space Size Texture effects Macropores – large, water drains easily Micropores – small, water held tightly Texture effects Sands – lots of macropores Loam – mixture of macro- and micropores Clays – lots of micropores

Effect on infiltration and water availability? Pore Space Size Macropores – large, water drains easily Micropores – small, water held tightly Texture effects Sands – lots of macropores Loam – mixture of macro- and micropores Clays – lots of micropores Effect on infiltration and water availability?

McLaren & Cameron

Steady infiltration rate inches/hour Textural class Steady infiltration rate inches/hour Sands >0.8 Sandy loams 0.4-0.8 Loams, fine sandy loams 0.2-0.4 Clay loams, silty clay loams and clays 0.04-0.2 Sodic clay soils <0.04 Hillel, 1982 An Introduction to Soil Physics

Water drains out of macropores Brady, 1990 Water drains out of macropores

Water drains out of macropores Brady, 1990 Water drains out of macropores Water held tightly in micropores

Water drains out of macropores Brady, 1990 Water drains out of macropores Water held tightly in micropores

Water drains out of macropores Brady, 1990 Water drains out of macropores Effect of soil texture on available water? Water held tightly in micropores

Water drains out of macropores Brady, 1990 Water drains out of macropores Water held tightly in micropores

Pore Space Size Texture effects Where do roots grow? Macropores – large, water drains easily Micropores – small, water held tightly Texture effects Where do roots grow?

Brady, 1990

Pore Space Size Texture effects Where do roots grow? Macropores – large, water drains easily Micropores – small, water held tightly Texture effects Where do roots grow? “Bulk density” – an indicator of pore space

Bulk density = (Weight of soil particles) (Volume of soil (solids + pores))

Bulk density = (Weight of soil particles) High bulk density Low pore space Low bulk density High pore space Bulk density = (Weight of soil particles) (Volume of soil (solids + pores))

Pore Space Size Texture effects Where do roots grow? Macropores – large, water drains easily Micropores – small, water held tightly Texture effects Where do roots grow? “Bulk density” – an indicator of pore space Compaction – Decreases pore space, esp. macropores Increases bulk density

Pore Space Size Macropores – large, water drains easily Micropores – small, water held tightly Continuity – Water drains better if soil texture is consistent and continuous

The sponge example The sponge example The sponge example

Pore Space Another way to look at it is Size Macropores – large, water drains easily Micropores – small, water held tightly Continuity – Water drains better if soil texture is consistent and continuous Another way to look at it is Water does not move well from one soil texture to another

Pore Space Another way to look at it is Size Macropores – large, water drains easily Micropores – small, water held tightly Continuity – Water drains better if soil texture is consistent and continuous Another way to look at it is Water does not move well from one soil texture to another Ever heard of the “teacup effect”?

Pore Space Size Texture effects Where do roots grow? Macropores – large, water drains easily Micropores – small, water held tightly Texture effects Where do roots grow? “Bulk density” – an indicator of pore space WHY SHOULD I CARE?

Pore Space Size Texture effects Where do roots grow? Macropores – large, water drains easily Micropores – small, water held tightly Texture effects Where do roots grow? “Bulk density” – an indicator of pore space WHY SHOULD I CARE? Different soil types have unique properties Those properties, along with environment, affect tree survival and growth Planting the wrong tree for the site is a waste of time and $

Applications

Applications What trees can survive on sandy soils?

Drought-tolerant deciduous shrubs silver buffaloberry caragana common lilac silverberry

Drought-tolerant hardwood trees green ash Russian olive Siberian elm bur oak

Drought-tolerant conifers Rocky Mountain juniper ponderosa pine Eastern red-cedar

Applications What trees can survive on sandy soils? What species can survive on wet, poorly drained soils?

Native trees and shrubs commonly found in wet, poorly drained soils. American elm green ash boxelder American linden willows cottonwood ironwood (hophornbeam) chokecherry redosier dogwood juneberry False indigo

What species will NOT survive in wet, poorly drained soils? Colorado (blue) spruce common lilac ponderosa pine

Applications What trees can survive on sandy soils? What species can survive in wet, poorly drained soils? What happens to pore space when a soil gets compacted?

Brady, 1990

Applications What trees can survive on sandy soils? What species can survive on clay soils? What happens to pore space when a soil gets compacted? Bulk density increases (total pore space decreases) Greater percentage of micropores

Applications What trees can survive on sandy soils? What species can survive on clay soils? What happens to pore space when a soil gets compacted? Bulk density increases (total pore space decreases) Greater percentage of micropores Soil compaction  reduced tree health Might need to break up compacted soils

Colorado blue spruce in the yard at a rural farmstead Colorado blue spruce in the yard at a rural farmstead. And whatever is killing this tree is “moving down the row.”

Colorado blue spruce in the yard at a rural farmstead Colorado blue spruce in the yard at a rural farmstead. And whatever is killing this tree is “moving down the row.”

Colorado blue spruce in the yard at a rural farmstead Colorado blue spruce in the yard at a rural farmstead. And whatever is killing this tree is “moving down the row.”

Colorado blue spruce – the issue is soil fill from construction of the new home resulted in the roots of these trees being covered, thus killing the roots, and therefore the trees.

Applications What trees can survive on sandy soils? What species can survive on clay soils? What happens to pore space when a soil gets compacted? Bulk density increases (total pore space decreases) Greater percentage of micropores Soil compaction  reduced tree health Might need to break up compacted soils

Soils 101- Physical properties It’s more than just “dirt”  Questions?

Back to the canning jars ...

Sand Clay Silt

Back to the canning jars ... Measure height of each component Fill in calculations Determine soil texture

Component Height (inches) Component Percent Sand Clay Silt A B +C _____ D (A/D) x 100 ________% (B/D) x 100 (C/D) x 100 +______% 100%

Soil samples Sample Soil type WSG % clay A Williams/Bowbells loam 3 (1) 18-27 B Bowdle/Lehr loam 6G 10-27 C Bearpaw/Zeeland loam 4 D Parnell silty clay loam 2 27-40 E Zahl/Williams loam 10 (3) F Heimdal loam ? G Greenhouse loam N/A H Play sand I (G + H)

Before we even begin ...

Before we even begin ...

Before we even begin ... Place soil sample in jar

Before we even begin ... Place soil sample in jar Add 1 teaspoon of Calgon

Before we even begin ... Place soil sample in jar Add 1 teaspoon of Calgon Add water to within ~1/2” of top

Before we even begin ... Place soil sample in jar Add 1 teaspoon of Calgon Add water to within ~1/2” of top Fasten lid and band

Before we even begin ... Place soil sample in jar Add 1 teaspoon of Calgon Add water to within ~1/2” of top Fasten lid and band Shake for ~1/2 minute

Before we even begin ... Place soil sample in jar Add 1 teaspoon of Calgon Add water to within ~1/2” of top Fasten lid and band Shake for ~1/2 minute LET IT SIT ...

Soils 101- Physical properties Introduction Components Texture Pore space Applications