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Tree/Soil  Relations &  Water Management
Scott Killpack Agronomy/Natural Resources
Introduction The relationship between tree root systems and the soils in which they grow has a greater influence on tree health than any other single factor.
Introduction Understanding soil is vital to arboriculture because soil is, quite literally, the foundation within which a tree grows.
Soil  Genesis
How it  All  Started
[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
[object Object],[object Object]
[object Object],[object Object],Significant Missouri Parent Materials
[object Object],[object Object],[object Object],[object Object],[object Object]
[object Object],[object Object],[object Object],Significant Missouri Parent Materials
[object Object],deposition occurred around 14,000 to 10,000 B.C.
[object Object],West East glacial till Missouri River Mississippi River prevailing wind loess
[object Object],[object Object],[object Object],[object Object],Significant Missouri Parent Materials
[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
[object Object],A top most mineral horizon - varying levels of organic matter - .5 to 4% in Missouri zone of maximum leaching/weathering - clay along with iron & aluminum oxides - light in color E zone of maximum accumulation - clay along with iron & aluminum oxides B ,[object Object],C
[object Object],Present in some soils Might find O horizon in heavy undisturbed forest or undisturbed prairie. O highly decayed organic material, not much mineral (sand, silt or clay)
Physical Properties
[object Object],Air 20 - 30% Mineral 45% Water 20 - 30% Organic 3-5% An ideal soil is 50% solids 50% pore space
[object Object],Silt 0.05 0.002 mm Clay < 0.002 mm Sand 2.0 - 0.05 mm
[object Object],[object Object],[object Object],1 gram samples (= 0.035 ounces)
[object Object],[object Object],[object Object]
External surfaces Diagram of a Silicate Clay Crystal K + Ca +2 Mg +2 Ca +2 Internal surfaces Surfaces have negative charge
silica  tetrahedron alumina octahedron Silicate Clay Structure oxygen aluminum silicon
 
Negatively Charged Colloids Attract Positively Charged Ions Cations K + Ca +2 Na + Ca +2 H + Mg +2 - - - - - - - - - Soil Colloid
[object Object],Classes based on relative proportions of sand, silt and clay Moderately Fine sandy clay loam, clay loam & silty clay loam Fine sandy clay, silty clay  & clay Coarse sand and loamy sand Moderately Coarse Sandy Loam Medium silt, loam and silt loam
[object Object],sand silt clay loamy sand sandy loam loam silt loam clay loam clay 85 65 45 20 28 25 10 25 40 60 37 30 5 10 15 20 35 45
Soil Textural Triangle
Soil Textural Determination 35 % sand 45 % silt 20 % clay
Pore Space
[object Object],Air 20 - 30% Mineral 45% Water 20 - 30% Organic 3%
[object Object],[object Object],[object Object]
Soil Pore Space -  Graphical Visualization
[object Object],macro pore micro pore
Relative Porosity Between Coarse and Fine Textured Soils Coarse Fine 35 - 50% 40 - 60% Micro Macro
[object Object],Virgin Tilled Micro Macro 34% 26% 35% 17%
Soil Structure
[object Object],The combination of soil particles and pore space
[object Object],[object Object],[object Object],[object Object],[object Object]
[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
[object Object],continuous corn corn in rotation meadow in rotation continuous bluegrass 9% 23% 42% 57%
[object Object],The mass of a given volume of dry soil -  a combination of the mineral, organic matter, and pore space. What happens when soil volume is compressed?
1.20 - 1.55 g/cm3  (75 - 97 lbs/cu ft) 1.30 - 1.70 g/cm3  (81 to 106 lbs/cu ft) Surface Sub-surface Bulk Density
[object Object],[object Object],loam, PA silt loam, IA silt loam, OH 1.07 0.93 1.05 1.25 1.13 1.31 uncropped cropped
Urban Soils  ,[object Object],[object Object],[object Object],[object Object]
[object Object],[object Object],How is it determined? (avg. B.D.- 1.36) x (wt. of cu ft of water  - 62.4 lbs)  x (volume of an acre 6.5 in. deep - 23,522 cu ft)
Organic Matter
[object Object],[object Object],[object Object]
[object Object],[object Object]
[object Object],water 75% dry matter 25%
[object Object],water 75% dry matter 25% carbohydrates 60% lignins 25% protein 10% other 5% Type of Compounds
[object Object],water 75% dry matter 25% carbon 44% oxygen 40% other 8% hydrogen 8% carbohydrates 60% lignins 25% protein 10% other 5% Elemental Composition Type of Compounds nitrogen phosphorus potassium sulfur calcium magnesium
[object Object],height of bars = to % of soil samples north bootheel < 1.0 1.0 to 1.9 2.0 to 2.9 3.0 to 3.9 > 3.9 4 40 42 12 3 12 55 26 6 2
[object Object],[object Object],[object Object],[object Object]
[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
[object Object],[object Object],[object Object],[object Object],[object Object]
[object Object],The relative composition of carbon and nitrogen within plant material
[object Object],Important in controlling: ,[object Object],[object Object],[object Object]
[object Object],animal manure legume residue wheat straw corn stalks sawdust soil 15:1 20:1 80:1 55:1 200:1 10:1
[object Object],activity of  organisms nitrate level  of soil Residues with high C/N ratio added here Residues with low C/N ratio remain
Soil  Water
[object Object],[object Object],[object Object],[object Object]
[object Object],[object Object],[object Object]
[object Object],[object Object],[object Object]
[object Object],0 10 20 30 40 sand sandy loam loam silt loam clay loam clay Field Capacity Available Water Wilting Point Unavailable Water
[object Object],[object Object],[object Object]
Soil Water Fundamentals The polarity of the water molecule results in the adsorption to negatively charged clay particles positive negative oxygen atom hydrogen atoms
[object Object],[object Object],Soil Water Capillary Fundamentals
[object Object],[object Object],silt loam
[object Object],[object Object],silt loam
[object Object],[object Object],silt loam water moves into the loamy sand only after the silt loam becomes saturated
[object Object],silt loam
[object Object],silt loam perched water table upon reaching the silt loam-clay interface water immediately moves into the clay layer due to the high attractive forces associated with clay-type soils
[object Object],[object Object],Types of Soil Water Movement
[object Object],Inches/foot of soil Soil Depth inches 1 1.5 2 2.5 3 0 10 20 30 40 50 60 70 Mexico Lindley menfro
[object Object],[object Object],silt loam Cotter loamy sand Sarpy silty clay Levasy Available Water for Several  Selected Soils 2.4 - 2.6 2.8 - 3.1 0.6 - 1.0 1.4 - 2.4 Bars = inches of water/ft of soil
[object Object]
Soil  Biology
[object Object],[object Object],[object Object],Soil Organisms - Fauna
[object Object],[object Object],[object Object],[object Object]
[object Object],Bacteria  -  one of the simplest, smallest and most important  forms of soil microbial life  ,[object Object]
[object Object],[object Object],[object Object]
[object Object],height of bars are in lbs/acre-furrow slice actinomycetes fungi algae bacteria 2,200 4,500 275 2,200
[object Object],Protozoa Nematodes Earthworms Others height of bars are in lbs/acre-furrow slice 15 - 150 10 - 100 100 - 1000 15 - 150
Mycorrhizae – “Fungus Roots”  ,[object Object],[object Object],[object Object],[object Object]
Rhizosphere  ,[object Object]
Soil Chemistry
[object Object],The  &quot;exchange&quot;   between a cation in the soil solution and another cation on the surface of negatively charged material such as clay or organic matter.
Negatively Charged Colloids Attract Positively Charged Ions Cations K + Ca +2 Na + Ca +2 H + Mg +2 - - - - - - - - - soil colloid H + H + K + Ca +2 NH 4 + soil solution soil solution soil solution Fe +2 - - - Al +3 H + H +
[object Object],Na + K + Ca 2+ Mg 2+ Al 3+ H + NH + Fe 3+
Negatively Charged Ions Are Called Anions Chemical Ionic Nutrient symbol form Chloride Cl Cl - Nitrate N NO 3 - Sulfate S SO 4 - 2 Borate B BO 4 - 3 Phosphate P H 2 PO 4 -
[object Object],[object Object],[object Object],[object Object]
[object Object],[object Object],sand sandy loam loam silt loam clay loam 3 6 14 18 27 height of bars = millieq./100g of soil
Clay and Organic Matter have Greatest Influence on CEC Clay - 10 to 150 meq/100g OM – 200 to 400 meq/100g
[object Object],[object Object],height of bars = to % of soil samples north bootheel < 5 5 to 10 10 to 18 18 to 24 > 24 0 16 70 12 2 11 36 29 14 10
[object Object],[object Object],[object Object],[object Object]
[object Object],[object Object],humid semi-arid arid 65 90 100 height of bars = %
[object Object],height of bars = % Calcium Magnesium Potassium Sodium 43 18 6 3
[object Object],height of bars = lbs/acre Calcium Magnesium Potassium 3,500 210 320
Soils and pH  Two cations largely responsible for acidity ,[object Object],[object Object]
Understanding pH ,[object Object],6 vs 7 = factor of  10 5 vs 7 = factor of  100
[object Object],4 5 6 7 8 9 10 11 very strong strong very strong mod- erate mod- erate slight slight strong Neutral Alkalinity Acidity pH Scale common range for Missouri soils
pH and Plant Nutrition ,[object Object],[object Object],[object Object]
pH & Nutrient Availability
pH Preferences of Some Common Plants  Alkaline loving  >7.0 Pin Oak, Magnolia Pine, Juniper Holly,  Birch Sweet Gum,  Spruce Ash, Beech Dogwood, Maple Spruce, Yew Cedar, Elm Juniper, Poplar Redbud, Willow Tuliptree Poplar, Willow Black Walnut Junipers, Redbud Elm, Maple Hickory Medium Range 6.0 - 7.0 Acid Loving <6.0
Alter Soil pH ,[object Object],[object Object],[object Object]
pH Can be Difficult to Alter ,[object Object],[object Object],Resistance to change - buffering capacity
Plant Water Needs ,[object Object],[object Object],What part of the plant plays a role in water loss or transpiration rate? Leaf stomatas
The Leaf
Leaf Stomata apple corn black oak sunflower None 39,000 None 55,000 250,000 64,000 375,000 100,000 Number of stomata per square inch plant  upper   lower
Irrigation Principles ,[object Object],[object Object],[object Object],[object Object]
Irrigation Principles ,[object Object],[object Object],[object Object]
Irrigation Principles ,[object Object],[object Object],[object Object],[object Object],[object Object]
Irrigation Methods ,[object Object],[object Object],[object Object],[object Object],[object Object]
Irrigation Methods Minimum irrigation ,[object Object],[object Object],[object Object],[object Object]
Irrigation Methods Recycled water ,[object Object],[object Object],[object Object],[object Object]
Drainage ,[object Object],[object Object],[object Object]
Let’s review some test questions
[object Object]
Plant Nutrients
Major Nutrients ,[object Object],[object Object],[object Object]
Secondary Nutrients ,[object Object],[object Object],[object Object],[object Object]
Micro Nutrients ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
[object Object],[object Object],[object Object],[object Object],Nitrogen (N)
Nitrogen and Plants ,[object Object],[object Object],[object Object]
Immobilization Mineralization Nitrogen in the Soil Organic Nitrogen Pool (proteins, etc.) Inorganic Nitrogen Pool (ammonium and nitrate)
[object Object],[object Object],[object Object],[object Object],[object Object],Nitrogen - Potential Sources
Nitrogen - Uptake by Plants Nitrate -- NO 3 - Ammonium -- NH 4 +
 
Nitrogen Loss from Soils ,[object Object],[object Object],[object Object],[object Object]
Nitrogen Fertilizer Sources ammonium nitrate 34 ammonium sulfate 21 calcium nitrate 15 potassium nitrate 13 urea 46 Fertilizer Material % Nitrogen
Phosphorus and Plants ,[object Object],[object Object],[object Object],[object Object],[object Object]
Phosphorus Sources in the Soil ,[object Object],[object Object],[object Object],[object Object]
Phosphorus - Uptake by Plants phosphate -- H 2 PO 4 -
 
Phosphorus Fertilizer Sources single superphosphate 20 triple superphosphate 46 monoammonium phosphate (MAP) 48-55 diammonium phosphate (DAP) 46 Ammonium polyphosphates 34-37 Fertilizer Material % P 2 O 5
Potassium and Plants ,[object Object],[object Object],[object Object]
Potassium and Plants ,[object Object],[object Object],[object Object],[object Object]
Potassium - Uptake by Plants potassium -- K + can be influenced by CEC
 
Potassium Fertilizer Sources potassium chloride 60 potassium sulfate 50 potassium nitrate 44 Fertilizer Material % K 2 O
Fertilization
Fertilizing many products available 32-3-5 Miracle Grow 29-3-4 Scott’s 18-24-6 Pennington 29-3-4 K-Gro
Which Brand? ,[object Object]
Fertilizing ,[object Object],46-0-0 CO-OP nitrogen 0-46-0 CO-OP phosphate 0-0-60 CO-OP potassium
Fertilizer numbers ,[object Object],nitrogen only blend = 23 lbs/bag = 14.5-1.5-2 lbs/bag 46-0-0 CO-OP 50 lbs 29-3-4 Scott’s 50 lbs
Applying the Correct Amount ,[object Object],18-24-6 Pennington 32-3-5 Miracle Grow 29-3-4 Scott’s
Applying the Correct  Amount 18-24-6 Pennington
Applying the Correct  Amount ,[object Object],[object Object],[object Object],18-24-6 Pennington
Soil Testing: Procedure ,[object Object],[object Object],[object Object],[object Object]
[object Object],[object Object],[object Object],[object Object],Soil Testing: Procedure
Review Soil Test Reports

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Basic soils arborist version - 2010

Notas do Editor

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  126. 12/29/10 Nitrogen can also be converted from inorganic to organic forms by microorganisms, a process called immobilization. It is the reverse of mineralization. Immobilization occurs when crop residues high in carbon (C) and low in N content are incorporated into the soil.
  127. 12/29/10 All N sources ... commercial, legumes, crop residues, soil organic matter, and animal manures ... are readily converted to NO 3 -N. All are subject to leaching if they are not utilized by the growing crop or retained in the ammonium- N form.
  128. 12/29/10 All N sources ... commercial, legumes, crop residues, soil organic matter, and animal manures ... are readily converted to NO 3 -N. All are subject to leaching if they are not utilized by the growing crop or retained in the ammonium- N form.
  129. 12/29/10 Nitrogen produces a green color in plant leaves due to the concentration of chlorophyll. A deficiency of N causes a yellowing (chlorosis) of leaves because of declining chlorophyll. Symptoms first appear on older leaves, then as the deficiency becomes more severe, yellowing begins to appear on younger leaves. This is a typical N deficiency on corn. Grain sorghum develops identical N deficiency symptoms.
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  134. 12/29/10 All N sources ... commercial, legumes, crop residues, soil organic matter, and animal manures ... are readily converted to NO 3 -N. All are subject to leaching if they are not utilized by the growing crop or retained in the ammonium- N form.
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  139. 12/29/10 All N sources ... commercial, legumes, crop residues, soil organic matter, and animal manures ... are readily converted to NO 3 -N. All are subject to leaching if they are not utilized by the growing crop or retained in the ammonium- N form.
  140. 12/29/10 One of the most common K hunger signs is scorching or firing along leaf margins. The symptom first appears on older leaves of most plants, especially grass-type crops. These K deficiency symptoms on corn are a classic example. Potassium deficiency shows up in many other ways as well.
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