Title: Soils and Nutrition
1Soils and Nutrition
2Today
- Properties of soils
- Identifying nutrient deficiencies
- Container media
- Fertility management
3Properties of soils
- Physical properties
- Texture
- Permeability
- Water holding capacity
- Structure
- Porosity
- Bulk density
- Chemical properties
- Fertility
- Cation exchange capacity
- pH
- Salinity
- Biological Properties
- Soil biota
- Microorganisms
4Soil Management
- Tilling
- Ripping
- Maintain appropriate soil physical properties
5Properties of soils
- Physical properties
- Soil texture affects
- water retention
- aeration
- specific heat capacity
- fertility or cation exchange capacity
- tillage
6Properties of soils
- Physical properties
- Permeability
- the rate at which water moves through the soil
- Water holding capacity
- the ability of a soil to hold water for plant use
- Both are affected by the amount, size, and
arrangement of pores - Macropores control a soils permeability and
aeration - Micropores are responsible for a soils WHC
7Properties of soils
- Aeration
- Definition
- The process by which air in the soil is replaced
by air from the atmosphere. - Soil air mainly composed of
- Oxygen
- Needed for respiration by roots and
microorganisms - Carbon dioxide
- Byproduct of respiration
- Reduced aeration is a result of
- Waterlogging
- Soil compaction
- Crusted soils
8Properties of soils
- Bulk density (DB)
- Definition
- The mass of a known volume (including air space)
of soil - Compaction leads to an ? in DB
- Soil becomes more dense through a loss of pore
space - Measurement
- Soil volume is determined in place
- Dried to a constant weight
- DB soil DW / soil volume
- Causes
- Use of heavy equipment, esp. in wet soils
9Properties of soils
- Bulk density (DB)
- Consequences
- Impeded root penetration
- Reduced water infiltration
- Reduced water availability
- Reduced nutrient availability
- Reduced gas exchange
- Reduced availability of O2
- Greater accumulation of CO2
10Properties of soils
- Bulk density (DB)
- Indiana
11Properties of soils
- Physical properties
- Texture
- Permeability
- Water holding capacity
- Structure
- Porosity
- Bulk density
- Chemical properties
- Fertility
- Cation exchange capacity
- pH
- Salinity
- Biological Properties
- Soil biota
- Microorganisms
12Properties of soils
- Fertility
- Nutrients classified as macro or micro based
on concentration in plant tissue - Macronutrients
- N and K most often deficient in low fertility
soils - Micronutrients
13Properties of soils
- Methods for determination of soil chemical
properties - Saturated media extract (SME)
- Pour-through (PT)
- Typically values are half those of SME values
14Properties of soils
- Chemical properties
- Cation Exchange Capacity (CEC)
- capacity to hold cations
- Silicate and aluminosilicate clay particles are
negatively charged colloids. - Cations are bound ionically to the surface of
these colloid particles. - CEC is expressed as meq/100 g of soil.
- Cations with higher charge densities, ie, smaller
cations, will replace larger cations. - H will displace Ca
- Ca will displace Mg.
Typical CEC values by soil type
15Soil Management
- Cation Exchange Capacity (CEC)
- Definition
- A measure of the total amount of exchangeable
cations that a soil can hold.
- High in
- Clay
- Organic matter
- Alkaline soils
- Low in
- Sand
- Perlite
- Acid soils
16Soil Management
- Cation Exchange Capacity (CEC)
- Ion attraction to soil depends on
- Ion size
- Number of valence electrons
- Degree of hydration
- Concentration of salts
Na NH4 K Mg Ca H
Increasing attraction to soil
What about anions? PO4- NO3- SO4- Cl-
17Soil Management
- pH
- What is pH?
- What is the optimal pH for plants?
- How does pH affect nutrient availability?
- Most nutrient imbalances are due to pH, not the
amount of nutrient present. - Example Hydrangea flower color
18Soil Management
- pH and nutrient availability
- Most nutrients more available at low pH
Most available
19Soil Management
- pH and nutrient availability
- Example Fe and Mn
- Both are available at low pH
- Availability declines with ?pH
- Some Indiana soils are pH 8
- Combination of high pH and acid-loving plants
- Fe or Mn deficiencies
- Problem in oaks in IN (prefer pH of 4.5-6.0)
20Soil Management
- pH and nutrient availability
- Soil pH can be modified
- increase pH
- lime
- lower pH
- sulfur
- Degree of change depends on
- Soil texture
- Organic matter
- For of modifying substance to be used
- Rate of change depends on
- Temperature
- Moisture
21pH and nutrient deficiency
- Modifying soil pH
- Degree of change depends on
- Soil texture
- Organic matter
- Form of modifying substance to be used
22pH and nutrient deficiency
- Modifying soil pH
- For ornamentals in IN soils, we sometimes want to
? pH - Quick fixes
- Aluminum sulfate
- Ammonium sulfate
- Urea
- Longer term
- Sulfate (gypsum)
- Time how long will it take?
- Area how much of the root zone can we actually
change?
23Soil pH
- Sources of soil acidity
- Hydrolysis of aluminum
- Alumino-silicate clay dissociations
- Organic matter breakdown
- Carbonation
- Nitrification
- Sulfur oxidation
Hydrolysis of aluminum Al3(soln.) H20 ?
Al(OH)2 H Al(OH)2 H20 ? Al(OH)2
H Al(OH)2 H20 ? Al(OH)3 H
Nitrification Nitrosomonas 2 NH4 3O2 ? NO2-
2H2O 4H Nitrobacter 2NO2- O2 ? 2NO3-
24Soil pH
- Neutalizing soil acidity
- Calcium carbonate (lime)
- Magnesium carbonate
- Calcium-magnesiu carbonate
- Calcium oxide (CaO)
- Calcium hydroxide
- Wood ash
Calcium carbonate CaCO3 H ? Ca2
HCO3 HCO3 H ? CO2 H20
25Soil Management
- pH and nutrient availability
- Species dependent
26Plants tolerant of high pH
27Properties of soils
- Physical properties
- Texture
- Permeability
- Water holding capacity
- Structure
- Porosity
- Bulk density
- Chemical properties
- Fertility
- Cation exchange capacity
- pH
- Salinity
- Biological Properties
- Soil biota
- Microorganisms
28Properties of soils
- Roles of OM in soil
- Attracts and holds elements in an available state
- reducing leaching losses
- Binds soil particles into aggregates
- increasing aeration
- increasing capillary water movement
- increasing root penetration
- Increases water-holding capacity
29Properties of soils
- Roles of soil organisms
- fix N2 from air
- mineralization
- form symbiotic relationships with roots
- increased mineral uptake
- create tunnels in soil
- increased aeration, water penetration, etc
- prey on plant pathogens
- produce CO2
30Soil Management
- Soil sterilization
- Steam
- Soil temp 76F
- With steam 180F
- Methyl Bromide
- Exemption ends soon
31Soil Management
- Many nursery practices contribute to loss of soil
productivity - Digging
- Erosion
- Clean cultivation
- Working on wet soils
32Soil Management
- Fallow (bare-ground)
- Decrease habitat for pests and diseases
- Cover-crop
- Increase organic
- matter content
- Organic matter added
- Sawdust
- Compost
- Manure
33Container media
- Ideal characteristics
- Free of weeds, pests, and disease
- Heavy enough to avoid tipping over
- Light enough for efficient handling shipping
- Well drained
- High water holding capacity
- Other factors
- Price
- Availability
- Consistency
34Media selection
- Physical properties
- Related to container size
- Air space
- Available water
- Not related to container size
- Porosity
- Bulk density
35Media selection
- Physical properties
- Normal ranges for container media
- Total porosity 50 - 85
- Air space 10 - 30
- Available water 25 - 30
- Bulk density 0.19 - 0.52 g/cc
36Media selection
- Physical properties
- Water holding capacity
- Aeration
- Bulk density
- Chemical properties
- Fertility
- pH
- Cation exchange capacity
37Container media organic amendments
- Peat moss
- Plant material (usually Sphagnum spp.) that has
decomposed under partial exclusion of oxygen - High WHC
- High CEC
- Low nutrient levels
- Low pH (3.0 - 4.5)
- Hydrophobic
38Container media organic amendments
- Softwood bark
- Pine bark stripped from trees and screened into
various sizes. May be fresh, aged, or composted. - Hardwood bark
- Less acid than softwood bark. May contain
leachable organic acids (toxic)
39Container media organic amendments
- Sawdust and wood chips
- CN ratio is extremely high and therefore not
recommended.
40Container media organic amendments
- Manures
- Potentially high in soluble salts
- Fine particle size
- Weed seeds
- Nutrient contribution
- Plant-based composts
- Particle size may be too fine or too large
- Degree of degradation (CN) important
41Container media inorganic amendments
- Perlite
- Silicaceous material
- Volcanic origin
- Improves aeration
- Very low mass
- High water holding capacity
- (3 4 its weight)
- Low cation exchange capacity
- No nutrient content
- Neutral pH
42Container media inorganic amendments
- Vermiculite
- Hydrated Mg-Al-Fe silicate
- Improves aeration
- Low bulk density
- High water holding capacity
- 5 its weight
- High cation exchange capacity
- Neutral pH
- Contains K and Mg
43Stock types
44Container media typical mixes
- Greenhouse
- Commercial (premixed) mixes
- Consistent product quality
- Content the same
- Expensive
- Not tailored to specific plant type
- Custom mixes
- Typically peat, vermiculite, and perlite
- Nursery
- Typically bark, peat, sand, and soil
- Typical recipe
- 80 bark
- 10 peat
- 10 sand
45Media selection
- Composts
- Add CEC and nutrients to substrates
- reduce adding minor nutrients
- provide starter nutrients
- high soluble salts
- Raise pH
- no lime addition necessary
- Lack course particles
- Increase water holding capacity
- Further decomposition is a concern
- Limit to 10-30 container volume
46Goals of Nutrient Management
- Supply adequate amount of nutrients for
- Maintained shoot growth
- Healthy root growth
- Protection from insects disease
- Over-fertilization results in
- Excessive growth
- Increased costs
- Environmental damage
47Factors to consider when developing a
fertilization program
- Nutrient availability
- Relative proportion of nutrients to each other
- Timing of application
- Moisture availability
48How to identify a nutrient deficiency
- Soil and plant tissue test
- Annual growth
- Deficiency symptoms
49Soil Management
- Tests for nutrient status
- Plant tissue tests
- Timing
- Sampling methods
- Soil tests
- Monitor nutrient status
- Adjust fertilizer formulations
- Timing
- Conduct in conjunction with tissue tests
- Water tests
- pH
- Nitrates
- Soluble solids (salts)
50Soil Management
- Tests for nutrient status
- AL Great Lakes Lab, Inc.
- Fort Wayne, IN
- Ag Source Belmond Labs
- Belmond, IA
- Agri Labs, Inc
- Bronson, MI
- Brookside Farms Lab
- New Knoxville, OH
- Cal Mar Soil Testing Lab
- Westerville, OH
- CLC Labs
- Westerville, OH
- Ingrams Soil Testing Center
- Sullivan, IN
- Land O Lakes, Inc.
- Indianapolis, IN
- Midwest Laboratories
- Omaha, NE
- Mowers Soil Testing Plus, Inc
- Toulon, IL
- Spectrum Analytical, Inc
- Washington Courthouse, OH
- Southern Illinois Soil Lab
- Hamel, IL
- United Soils, Inc
- Fairbury, IL
- Waters Agricultural Labs
- Camilla, GA
51- Deficiency symptoms
- Roles of essential nutrients
- Nutrients that are part of carbon compounds
- N, S
- Nutrients that are important in energy storage or
structural integrity - P, Si, B
- Nutrients that remain in ionic form
- K, Ca, Mg, Cl, Mn, Na
- Nutrients that are involved in redox reactions
- Fe, Zn, Cu, Ni, Mo
52- Deficiency symptoms - Nutrient mobility
- Highly mobile
- N, P, K, Mg, Zn, Mo
- Deficiencies occur in older leaves
- Immobile
- Ca, S, Fe, B, Cu
- Deficiencies occur in younger leaves
53- Deficiency symptoms Nutrient mobility
- Highly mobile
- N, P, K, Mg, Zn, Mo
- Deficiencies occur in older leaves
- Immobile
- Ca, S, Fe, B, Cu
- Deficiencies occur in younger leaves
54Nitrogen
- Most required nutrient in plants
- Forms
- Nitrate (NO3-)
- Preferred source for plants
- Uptake most rapid in low pH soils
- Ammonium (NH4)
- Uptake most rapid in neutral pH soils
- Uptake of both forms is temperature-dependent
55Urea ((NH2)2CO)
56Nitrogen
- Deficiencies
- required in greatest amounts
- amino acids, nucleic acids, chlorophyll
- symptoms
- Uniform chlorosis
- Small leaves
- Occurs in old leaves
57Nitrogen
- Molybdenum (Mo) is essential for N conversion
from ammonium to nitrate in plants - Therefore, Mo deficiency can result in N
deficiency symptoms - Especially true in conifers
- Typically found on acid soils
- Treatment
- Granular or foliar sodium molybdate
58Nitrogen
- Which form to apply?
- Decision based on
- Soil pH
- Weather
- Moisture dependence
- Solubility
- Fast or slow release
- Leaching potential
- Other nutrition needs
- Toxicities
- Dry soils
- Cold
- Poorly drained soils
59Nitrogen
- Sources of quick-release N for woodies
- Availability is not dependent on moisture or warm
temperatures
60Nitrogen
- Sources of urea-N for woodies
61Nitrogen
- Sources of organic N for woodies
- Sources
- Composted leaf litter, animal manures, etc.
- Slow release
- Very dependent on moisture and temperature
- Added benefits
- Improve soil structure
- May provide protection against diseases
62Nitrogen
- Potentially harmful if released into the
environment - How do you minimize amount of nitrogen released?
- Timing of application(s)
- Method of application
- Cultural practices
- New methods
- e.g. defoliants
- You MUST understand the physiology of the crops
you are working with
63Phosphorus
- Deficiencies
- Required in relatively high amounts
- nucleic acids, ATP
- Deficiencies occur on acid soils
- Symptoms
- Small leaves
- Weak, stunted plant
- Bronze to purple tinge
- Occurs in old leaves
64Phosphorus
- Forms
- Inorganic
- Superphosphate (0-20-0)
- Triple superphosphate (0-46-0)
- Phosphoric acid
- Ammonium phosphate (11-48-0)
- Di-ammonium phosphate (18-46-0)
- Organic
- Compost
- Leaf litter
- Bone meal
65Phosphorus
- Application
- Apply prior to planting if possible.
- Phosphorus is available for several years.
Source Smith, 1986
66Phosphorus
- Excessive application
- Results in deficiencies of other nutrients
- Copper, iron, zinc, calcium
- Can leach into ground water
67Potassium
- Deficiencies
- Required in relatively high amounts
- Water uptake, stomatal opening
- Deficiencies in woodies are rare
- Symptoms
- Weak, stunted plant
- More susceptible to disease
- Occurs in old leaves
68Potassium
- Forms
- Inorganic
- Potassium chloride (0-0-60)
- Potassium sulfate (0-0-60)
- Potassium nitrate (13-0-44)
- Organic
- Manure
- Seaweed
69Potassium
- Application
- Apply prior to planting
- Potassium levels may be low at the end of the
growing season
Source Smith, 1986
70Iron (Fe)
- Most common micronutrient deficiency in woody
plants - Most common in high pH soils
- Some species especially susceptible
- Pin oak, white pine, sweet gum
- Loss of roots leads to deficiency
- Some nutrients in excess cause Fe deficiency
- Phosphorus, zinc, manganese, copper
- PFe ratio should be about 291
71Iron (Fe)
- Deficiency treatment options
- Soil treatment
- Typically not practical to modify soil pH for
trees - Chelates
- Sequestar 6 Iron chelate, Sequestrene 138
- Usually only last 1 year
- Foliar spray
- Iron chelates or iron sulfate
- Apply early in the season
- Response is quick, but often spotty
- Trunk injection
- Ferric ammonium citrate (iron citrate) or iron
sulfate - Apply just after leaf expansion
- Uptake improved if holes are drilled in root
flares - Lasts for approximately 2 years
72Iron (Fe)
- Chelates
- Iron application
- Fe supplied as FeSO4 or Fe(NO3)2
- FeOH precipitate forms
- Fe(PO4)2 may also form
- Chelators form soluble complexes
- ionic rather than covalent bonds
- common chelators
- ethylenediaminetetraacetic acid (EDTA)
- diethylenetriaminepentraacetic acid (DTPA)
73Manganese (Mn)
- Also a common micronutrient deficiency in woody
plants - Most common in high pH soils
- Some species especially susceptible
- Maples, cherry
- Cold, wet periods
- Can be applied as manganese sulfate (MnSO4)
74- pH and nutrient availability
- Example Fe and Mn
- Both are available at low pH
- Availability declines with ?pH
- Some Indiana soils are pH 8
- Combination of high pH and acid-loving plants
- Fe or Mn deficiencies
- Problem in oaks in IN (prefer pH of 4.5-6.0)
75Fertilizer Application
- Not just amounts, but ratios
- Some elements compete at the root surface
76Timing of Application
- Spring
- Major application
- Have nutrients available before growth begins
- Fall
- Increase N reserves (foliar spray)
- Avoid extremely high applications late in season
- Not effective during or after onset of cold
weather - Think about solubility and speed of release
77Timing of Application
- Effect of plant growth stage (trees and shrubs)
- Stage 1 Planting to newly planted
- Approx. 1 lb actual N per 1000 ft2
- Broadcast quick release N do not add to
planting hole - Stage 2 Young trees and shrubs
- Rapid growth usually desired
- Approx. 2 to 4 lb actual N per 1000 ft2
- Split applications for plants surrounded by turf
- Stage 3 Mature trees and shrubs
- Growth rate slows
- Goal is maintaining plant health
- Approx. 1 lb actual N per 1000 ft2
78Timing of Application
- Effect of plant phenology
- Roots active in early spring and fall
79Timing of Application
- Effect of soil type
- Sandy soils
- Nutrients in solution and therefore more
available - Nutrients move more quickly through soil
- Quick response
- Leaching potential is higher
- Split applications
- Clay soils
- Nutrients more bound to soil particles
- Nutrients move slowly through soil
- Slow response
- Leaching potential is lower
- Split applications not necessary
80Fall Fertilization
- Why?
- Some nutrients limiting at the end of the season.
- Spring rain may leach soil nutrients.
- Optimal timing of spring fertilization is tricky.
- Potential effects
- Increased cold hardiness.
- Increase nutrient reserves to draw upon in
spring.
81Fall Fertilization
- Which fertilizer to use?
- Based on soil test
- Low in N
- High in K
- Potentially micros as well
- How much?
- Rule of thumb 1 lb per 1000 ft2
82Fall Fertilization
- Nitrogen
- Avoid applying high N fertilizer, even if soil
test indicates slight deficiency. - Application can lead to maintained growth and
decreased cold acclimation. - Can also create imbalances with other nutrients
(e.g. K)
83Fall Fertilization
- Potassium
- Low availability in some areas at the end of the
growing season - Apply in fall for enhanced spring growth
- Use a potassium source low in nitrogen and
phosphorus - 5-3-15, 5-5-30, or 5-0-20
- Apply late Aug to early Sept to allow for uptake
- Application rate of 1 lb K per 1000 ft2
- N is required for efficient uptake of K, so check
soil tests and apply accordingly
84- Factors affecting plant nutrient uptake
- Nutrient
- availability
- mobility
- competition
- Plant
- species
- cultivar
- phenology
- stress
- Environment
- water
- ionic status
- pH
- temperature