Organic Gardening - Introductory Study of Soils
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Introductory Study of Soils
For the Master Gardeners
Wendy Sue Harper, Ph.D.Vegetable and Fruit TA Advisor
Northeast Organic Farming Association of
Vermont
www.nofavt.org
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What We Will Cover Tonight
Introduction.
Ecological agriculture perspective tounderstanding the physical, chemical and
biological properties of soil for gardeners.
Compost basics for home and community
gardeners.
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Soil: the Foundation of
Gardening
WSH
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CEC
Air
MoistureMicrobes
OrganicM
atter
Structur
e
Texture
pH
Pollutants
Nutrients
A Simplified Soil Ecosystem
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Soil Fertility is
The ability of a soil to provide aphysical,
chemical, andbiological environment for
the plant that is health sustaining.
This is along term ecosystem based or
ecological agriculture perspective!
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Seven Principles to Maintain
Soil/Water/Plant Resource Base1. Maintain proper air/water balance
2. Maintain soil tilth
3. Prevent erosion
4. Maintain biological diversity
5. Maintain proper SOM levels
6. Maintain a proper pH7. Maintain a proper balance of nutrients
(A systems approach means you gotta do themall. Alone each will not build soil fertility.)
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A Good Loam Soil:
50% Solids
50% Pores
45% Mineral5% Organic Matter
25% Air
Big Pores
25% Water
Small Pores
So why is this important?
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Roots:
1 the plant
2 Absorb and
3 Exchange
4 Store and
5 Transform
6 Produce plant
7 Interact with
Support
water nutrients
gases
starches sugars
nutrients
hormones
microbes for disease suppression
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An Undisturbed Soil Profile:
Ap
Zone of accumulation
Zone of biological activity
Organic matter
Mix O + A + E = Ap A = topsoil p = plowed or disturbed
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Mountain Forest
Sandy Soils
O Organic Matter or
A Topsoil Layer
E Leached Layer
B Accumulations of
Iron, Aluminum and
Organic Acids
C Parent Material
(NRCS/USDA)
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Valley Clay Soils
Ap Topsoil Layer
(O Organic Matter tilled in)
E Leached Layer
B Clay Accumulations C Parent Material
(NRCS/USDA)
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1.Air/Water Balance Depends On:
1 Location on the landscape
2 Soil depth
3 Soil texture(lines=surface area)
4 Soil structure: inside vs. in-between
5 Soil organic matter content: it holds water!
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Soil Textural Triangle:
*Loam Soil: The influence of the sand, silt and clay on its physical
properties is equal. (Not the quantity or amount, but its influence!)
Here, amounts are equal.
(Brady and
Weil, 2002)
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Soil Particles That Make Up
Texture Feel: Sand
Silt
Clay
Not apart of Texture:
Organic Matter
Gritty
Smooth, like baking flour
Sticky
Greasy
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1.Air/Water Balance Depends On:
1 Location on the landscape
2 Soil depth
3 Soil texture(lines=surface area)
4 Soil structure: inside vs. in-between
5 Soil organic matter content: it holds water!
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Soil Structure
*Granular, Crumb
*Platy
*Subangular Blocky
Angular Blocky
*Prismatic
Columnar
*Structureless
1. Single grained2. Massive
Shape of individual peds
* Note: found in Vermont
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You worked your soil when it
was too wet?What did you get?
You get: CLODS
It is called: PUDDLING YOUR SOIL
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Promote Structure With OM Additions
And Thus:
Drainage in clay soils (macropores)
Water holding capacity in sandy soils (micropores)
*Cause it Creates the Pores You Aint Got!*
Macropore hold air and drain (in-between)
Micropores hold water (inside)
OM = Drought Prevention Insurance
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Soil Too Dry?Manage to Prevent Water Loss By:
Mulching to conserve moisturePrevent runoff
Build OM content to improve the water
holding capacity
Control weeds (competition) or used them
to your advantagePlant tolerant species
Water deeply and consistently
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Soil Too Wet?
Manage for water loss by:Raised beds
Shape of beds
Follow good Management Practices
Add OM to improve drainage (clays)
Dont work wet soil
Plant after soil warms up
Plan wet in early spring areas for late season cropslike tomatoes
Plant tolerant species
Put in a drainage system to drop the water table
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2. Soil Tilth:
All the Physical Properties of SoilRelated to Plant Growth
Including: structure, drainage, aeration,moisture holding capacity, bulk density.
Work a soil when it has dried out enough
Add OM to improve physical properties
Treat soil gently
Keep soil covered
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3. Prevent Erosion:Erosion is the process of detachment and
transport by wind or waterPrevent it by:
Make the wind or water less erosive by slowing it down.
Protect the soil from exposure to wind or water.
Build the soils resistance to erosive forces. (Brady and Weil, 2002)
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Seven Principles to Maintain
Soil/Water/Plant Resource Base1. Maintain proper air/water balance
2. Maintain soil tilth
3. Prevent erosion
4. Maintain biological diversity5. Maintain proper SOM levels
6. Maintain a proper pH7. Maintain a proper balance of nutrients
i i i di i
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4. Maintain or Create Biodiversity
& SOIL
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& SOIL
DFW
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4. Maintain or Create BiodiversityRotate Crops
Plant Mixtures of Species
Interplant, Under-sow, Companion Plant, PolycultureAdd Compost
Mulch
Plant Biological or Ecological IslandsHabitat and Food For Beneficials
Selective Weeding
Change Tolerance Levels for Pest
Use IPM
Cautions?..
4 M i i C Bi di i
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4. Maintain or Create BiodiversityProvide Diverse Food: Organic Matter
Add Organic Residues
Add Manure or Compost
Grow Cover Crops
Provide Diverse HabitatRotate Crops; Include Cover Crops
Plant Mixtures of Species
Interplant, Under-sow, Companion Plant, Polyculture
Plant Biological or Ecological Islands; Habitat and Food ForBeneficial Organisms
Bio-strips, Flower Strips, Beetle Banks, Strip InsectaryIntercropping, Vegetative Corridors, Hedge Rows orSelective Weeding
Use Mulches; Reduce Tillage and Bare Land
Change Tolerance Levels for Pest
Reduce Chemical Inputs: Use Integrated Pest Management
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Biological or Ecological Islands
www.sare.org
Syrphid Fly
Lacewings
Parasitic Wasp
www.attra.orgwww.sare.org
www.sare.org
NCSU-IPM
NCSU-IPM
NCSU-IPM
www.sciencemuseum.org.uk
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H d R H bi
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Hedge Rows as Habitat
Wind Shelter Belt
Vegetation Barriers
Vegetative Corridors
Spined Soldier Bug
Praying Mantis
USDA/NRCS/NAC
National Corn Growers Association
Texas A&M University
University of Idaho
www.sare.org
l h bi
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Mulch as Habitat
Ground Beetles
Spiders
DFW
DFW
B l B k B i i
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Beetle Banks: Britain
Ground Beetles
and other
Predatory Beetles
http://www.orc.govt.nz/
Oregon State University Extension
www.snh.org.uk/
DFW
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Time for..
A. Questions?
B. A Break?
C. A Nap?
D. A Snack? Some Compost Tea?
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5. How Can You Get OM Into
Your Soils?
Animal Manures
Composts
Cover Crops
Mulches
Peat Moss
Others?
Any Cautions? C:N Ratio or Carbon to Nitrogen Ratio
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What is Compost?
Compost is the biological reduction of
organic wastes to humus. (Golueke)
MICROBIAL ROT
Scientific American, 1991
P i i l f C ti
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Principles of Composting
C:N Ratios Recipe
Moisture Balanced with Oxygen
Recipe Particle Size
Temperature
Recipe
Size of pile
Microbes and Macrobes
Time
Management
Assess Your Level of Interest
C:N Ratio
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C:N Ratio If hot compost is desired, the ratio preferred is
about 25-30:1, but 20-40:1 is acceptable.
High C Materials: straw, hay, woody materials,
dried corn stalks, paper wastes. Not are Carbon behaves the same.
High N Materials: manures, green material, food
wastes.
Start with 1 handful of N wastes to 3 of C wastes.
Cornells WWW site for recipe design: http://compost.css.cornell.edu/science.html
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Moisture Balanced with O2
If hot compost is desired, a range of 50-60% ispreferred, but 40-65% is acceptable.
Field Test: Compost should feel like a dampsponge. Moist, but you cant ring water out of it.
Generally, if the C:N ratio is OK, moisture will beOK too.
Cornells WWW site for recipe design http://compost.css.cornell.edu/science.html
Particle size and thus pile porosity areimportant too!
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Temperature
Thermophilic over 105o
F Recipe more critical Size is important
Quicker
More management More labor
Destroys weed seeds
Destroys pathogens
Mainly microorganisms:Mostly BACTERIA,
Some fungi andactinomycetes
Less disease suppression
Mesophilic 50-105o
F Recipe less critical Size is not important
Slower
Less management Less labor
May not destroy weed
seeds and pathogens
Diversity of both micro
and macro-organismsinvolved
More disease suppression
SMB
SMB
SMB
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Troubleshooting Hot Compost
Wet and stinky?
Dry not working?
No heat when turned?
Add C materials and turnin sunny weather. Shapeto shed water. Break upmatting or compaction.
Add N materials and turnwhen raining. Shape to
hold water. Look at material if dark
and crumbly with goodearth smell, may becuring. No? Check sizeand consider additions.
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Management
VS.
.
Compost a Recipe for Trouble!
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Gardeners Easy Practical Compost Method
In bins or free standing. Build pile by adding 1 handful
of green/wet stuff for every 3
handfuls of brown/dry stuff,added overtime.
Add soil/old compost for odor
control. Turn and rebuild pile in fall,
mix in garden cleanup debris.
Wait 2-3 years before using.
Do not add weeds gone to seedor plants infected with viruses.
ORGANIC MATERIALS
ORGANIC MATERIALS - Grass, leaves, weeds, etc.
ORGANIC MATERIALS
1-2 manure
Cross Section of Layering in Compost Bin
1-2
6-8
SOIL
SOIL
SOIL
SOIL
LINE
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What Composting Does for You!
1. Decrease bulk of the pile (CO2 gas)
2. C:N ratio3. Odor
4. Hot composting kills weed seeds & pathogens
5. Cool composting provides disease resistance6. Humified (turning to humus) material is a slow
release fertilizer
7. Wastes become useful material
gardeners brown gold
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6. Maintain A Proper pH
Which is: pH
7. Maintain A Proper Balance of the
Nutrients
How to Know?
ESSENTIAL ELEMENTS FOR PLANT GROWTH
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Plant Available Major Source
Form of Nutrients
MACRO-NUTRIENTS
Carbon CO2 AirOxygen O2 Air
Hydrogen H2O Water
Nitrogen NO3-, NH4
+ Soil OM
Phosphorus H2PO4-, HPO4
2- Soil OM
Potassium K + Soil Minerals
Calcium Ca2+ Soil Minerals
Magnesium Mg2+ Soil Minerals
Sulfur SO42-
, SO2
(gas) Soil OM, Air
ESSENTIAL ELEMENTS FORPLANT GROWTH
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ESSENTIAL ELEMENTS FORPLANT GROWTH
MICRO-NUTRIENTS
Iron Fe2+ Soil Minerals + OM
Manganese Mn2+ Soil Minerals + OMCopper Cu2+ Soil Minerals + OM
Zinc Zn2+ Soil Minerals + OM
Boron H3BO3 Soil Minerals + OM*Molybdenum MoO4
2- Soil Minerals* + OM
Chlorine Cl- Soil Minerals + Rain*
Cobalt Co2+ Soil Minerals + OM
Nickel Ni2+ Soil Minerals + OM
OTHERS??
Sodium, Selenium, Silica, Vanadium, Iodine, Fluorine???
Plant Available Major Source
Form of Nutrients
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Soil Solution:
The Thin Skins of Water that CoatEverything.
Roo
tHair
C ti
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Cation
ExchangeCapacity +
++
+++ We arepositive!
Cations
K+ Mg2+ Ca2+ H+ Al3+
pH near neutral Acid pH
NO3-
A id
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The pH of
things in ourlives.
* Distilled water or rain water = pH 5.6
0
1
2
3
4
5
6
7
8
9
10
11
12
13
14
pH Acid
Basic
Neutral
Soils
Lemons
Lye
Ammonia
Milk of Magnesia
SeawaterBicarb of Soda
Vinegar, Grapefruit, Wine
Grass silage
TomatoesBeerBoric Acid
Human bloodManure
Cows milk
Distilled water
H+ + OH- = HOH = H2O
Acid + Base = Water
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pH Effects on Nutrient Availability
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pH
Prefere
ncesfo
rS
elec
ted
Pla
nts
(Foth, 1992)
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DO
YOUKNOW
Whats
In YourDirt
?
pH??
HeavyMetals??
N-P-K??
%OM??
Micron
utrients??
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http:/
/pss.uvm.
edu/ag_t
estin
g/forms.h
tml
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S il T t
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Soil Test
Report Soil Test Results
Recommendation Limestone
Nitrogen Phosphorus
Potassium
Management Info
Who to call
O k
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On Back
Interpretation of soil
test results to help
you figure out what
all this soil test
information means.
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Useful Soil Resources
Start with the Soil: The Organic Gardeners Guide toImproving Soil for Higher yields, More Beautiful Flowers, and
a Healthy Easy Care Gardenby Grace Gershuny.Rodale Press. 1993.
The Nature and Properties of Soilsby Nyle
C. Brady and Ray R. Weil. Prentice Hall.2002.
http://pss.uvm.edu/ag_testing/forms.html
U f l C t R
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Useful Compost Resources
The Rodale Book of Composting
by Deborah L. Martin & Grace Gershuny.
Rodale Press. 1992.
On-Farm Composting Handbook
by Robert Rynk. NRAES-54. 1992.
Cornells WWW site:
http://compost.css.cornell.edu/Composting_homepage.html
http://compost.css.cornell.edu/science.html
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Biological Slide References
DFW: The Decomposer Food Web: Ecologyof organisms of compost and soil litter by
Dr. Daniel Dindal, Professor Emertius, SoilEcologist, SUNY-Syracuse
SMB: Soil Microbiology and Biochemistryfrom Soil Science Society of America
WSH: Wendy Sue Harper, Ph.D.
More Questions on Soils or Compost?
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More Questions on Soils or Compost?
WSH
WSH
WSH
WSH
WSH
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The End