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Soils 101- Physical properties
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Soils 101- Physical properties
It’s more than just “dirt”
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Introduction – Why should I care?
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Introduction – Why should I care?
Different soil types have unique properties
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Introduction – Why should I care?
Different soil types have unique properties Those properties, along with environment, affect tree survival and growth
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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 $
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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
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Photos courtesy of Dave Hopkins, NDSU
Barnes soil Photos courtesy of Dave Hopkins, NDSU
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Photos courtesy of Dave Hopkins, NDSU
Barnes soil Bowdle soil Photos courtesy of Dave Hopkins, NDSU
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Soil components
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Soil components Solids and pores
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Soil components Solids and pores Solids – Minerals + Organic matter
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Soil components Solids and pores Solids – Minerals + Organic matter
Pores – Water + Air
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Soil components Solids and pores Solids – Minerals + Organic matter
Pores – Water + Air Ideal soil – Even mix of solids and pores ...
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Mineral 45% Organic 5% Brady, 1990
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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)
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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
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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 ...
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Organic matter Holds onto water Great source of nutrients
Binds soil particles together into larger aggregates
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Texture
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Texture Relative amount of sand, silt and clay only
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Texture Relative amount of sand, silt and clay only
Lots of one part – soil named by that part
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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
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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
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Texture Relative amount of sand, silt and clay only
Lots of one part – soil named by that part Mixtures are called loams
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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
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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
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Texture triangle
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Example: 20% sand 60% clay 20% silt
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Example: 20% sand 60% clay 20% silt
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Example: 20% sand 60% clay 20% silt
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Example: 20% sand 60% clay 20% silt
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Example: 20% sand 60% clay 20% silt Clay soil
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Example: 62% sand 15% clay 23% silt ???? soil
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Example: 62% sand 15% clay 23% silt sandy loam soil
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Texture Relative amount of sand, silt and clay only WHY SHOULD I CARE?
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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 $
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Pore Space
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Pore Space Size matters
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Pore Space Size matters – macropores and micropores
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Pore Space Size Macropores – large, water drains easily
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Macropores Brady, 1990
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Pore Space Size Macropores – large, water drains easily
Micropores – small, water held tightly
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Macropores Micropores Brady, 1990
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Pore Space Size Texture effects
Macropores – large, water drains easily Micropores – small, water held tightly Texture effects
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Pore Space Size Texture effects
Macropores – large, water drains easily Micropores – small, water held tightly Texture effects Sands – lots of macropores
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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
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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
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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?
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McLaren & Cameron
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Steady infiltration rate inches/hour
Textural class Steady infiltration rate inches/hour Sands >0.8 Sandy loams Loams, fine sandy loams Clay loams, silty clay loams and clays Sodic clay soils <0.04 Hillel, 1982 An Introduction to Soil Physics
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Water drains out of macropores
Brady, 1990 Water drains out of macropores
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Water drains out of macropores
Brady, 1990 Water drains out of macropores Water held tightly in micropores
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Water drains out of macropores
Brady, 1990 Water drains out of macropores Water held tightly in micropores
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Water drains out of macropores
Brady, 1990 Water drains out of macropores Effect of soil texture on available water? Water held tightly in micropores
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Water drains out of macropores
Brady, 1990 Water drains out of macropores Water held tightly in micropores
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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?
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Brady, 1990
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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
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Bulk density = (Weight of soil particles)
(Volume of soil (solids + pores))
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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))
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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
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Pore Space Size Macropores – large, water drains easily Micropores – small, water held tightly Continuity – Water drains better if soil texture is consistent and continuous
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The sponge example The sponge example The sponge example
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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
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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”?
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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?
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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 $
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Applications
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Applications What trees can survive on sandy soils?
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Drought-tolerant deciduous shrubs
silver buffaloberry caragana common lilac silverberry
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Drought-tolerant hardwood trees
green ash Russian olive Siberian elm bur oak
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Drought-tolerant conifers
Rocky Mountain juniper ponderosa pine Eastern red-cedar
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Applications What trees can survive on sandy soils?
What species can survive on wet, poorly drained soils?
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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
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What species will NOT survive in wet, poorly drained soils?
Colorado (blue) spruce common lilac ponderosa pine
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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?
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Brady, 1990
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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
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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
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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.”
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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.”
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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.”
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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.
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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
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Soils 101- Physical properties
It’s more than just “dirt” Questions?
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Back to the canning jars ...
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Sand Clay Silt
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Back to the canning jars ...
Measure height of each component Fill in calculations Determine soil texture
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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%
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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)
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Before we even begin ...
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Before we even begin ...
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Before we even begin ... Place soil sample in jar
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Before we even begin ... Place soil sample in jar
Add 1 teaspoon of Calgon
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Before we even begin ... Place soil sample in jar
Add 1 teaspoon of Calgon Add water to within ~1/2” of top
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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
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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
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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 ...
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Soils 101- Physical properties
Introduction Components Texture Pore space Applications
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