Transcript File

 20
ESSENTIAL NUTRIENTS
Different chemical elements have been
identified in plants.
 Only 16 chemical elements are essential to
plant growth and development.
 Non-Mineral essential nutrients
 Carbon
 Hydrogen
 Oxygen
 Hydrogen and Oxygen are supplied to
plants from carbon dioxide and water
through photosynthesis
ELEMENT-A simple form of matter that
cannot decompose by ordinary
chemical means.
 FERTILIZER-
product added to growing
material to supply essential macro and
micro nutrients.
Nitrogen-General Facts
 One
of the most abundant and mobile nutrients
 Part of every plant cell
 Soils may contain as much as 5,000 lbs of nitrogen
per acre.
 The air we breathe contains 37,000 tons (78% by
weight) over each acre
 Origin for ALL nitrogen sources
 Part of chlorophyll-gives the green color
 Loss of nitrogen results in loss of color-turns yellow
 Lack of nitrogen causes spindly, weak stems and
growth is slowed.
 Production
of nitrogen starts with ammonia
 This is a gas
 Combo of atmospheric nitrogen and hydrogen
from natural gas and/or fossil fuels.
 Can be applied directly as a gas or further
processed into a liquid or solid fertilizer.
Common Sources of Nitrogen
Urea
Ammonium
Nitrate
Nitrogen Solutions
Nitrogen and the Environment
 Nitrification
 Changes
to Nitrate—NO3
 Decomposed organic materials or inorganic
fertilizers are converted to N03
 NO3 can get trapped into clay particles of soil
 Bacteria aids in nitrification
 Nitrate is available for plant use
 Nitrate can also be tied up and not available to
the plant. Can be as much as 50%
 Leaching-When
water passes through the
soil profile and removes chemical
compounds or nutrients in solution from soil.
 Nitrate
nitrogen is the form most subject to
leaching
 Nitrates are only bound loosely to the clay
particles in soil so they move easily with water.
 Ammonium binds tightly and does not leach
 Leaching during growing season and in fine to
medium soil texture is minimal-less then 5%
 Leaching is more likely in course soils
 Erosion-the
removal of soil material by
wind or water moving over the land.
 Run-off
water
 Sediment loss
 Denitrification
 Only
happens when soil is fully saturated or
flooded
 No oxygen in the soil pores
 Bacteria converts nitrate to elemental N2-this is
a gas
 15-30% loss during heavy water situations
 Volatilization
 Happens
under warm and moist conditions.
 Urea is converted to ammonium carbonate
 Ammonium carbonate is converted to ammonia
gas
 Ammonia gas is then released to the
atmosphere
 Happens most commonly when urea (usually in
an organic form)is applied to a warm moist
surface.
 If the urea is NOT incorporated into the ground
shortly after application and is allowed to dry on
the surface-can be 10-30% loss of nitrogen into
the atmosphere.
Nitrogen Cycle
 In
order to be used by the plant-nitrogen must be
plucked from the atmosphere.
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Nitrogen goes through several changes in the soil
before returning to elemental form
The cycle is atmospheric nitrogen to usable nitrogen
and back to elemental nitrogen
 Nitrogen
Fixation-the process by which elemental
nitrogen is removed from the atmosphere by soil
bacteria called rhizobia.
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Bacteria lives on roots of legumes. (Alfalfa, clover,
peas, beans)
Produce their own nitrogen and do not usually need
other sources
Organic Matter (Humus)
 As
plants die they decompose (break down) into
soil organic matter.
 The rate of decomposition and the amount of
nitrogen released into the soil is determined by
the carbon:nitrogen ratio
 With ratios of about 25:1or less, organic nitrogen is
quickly converted to usable nitrates.
 Mineralization happens most is legumes, animal
manures and municipal sludges.
 If greater the 25:1 ratio then nitrogen is tied up
and actually take nitrogen from soil during a slow
decompostion.
 Materials
such as straw, sawdust and bark are very
high in carbon and break down slowly and may
actually cause soil to be deficient in nitrogen.
 Organic matter that has completely decomposed
and is stable with the surrounding soil environment
is called humus with a C:N ratio of 12:1
 Humus is responsible for nitrogen release control
 Average amount of nitrogen in humus is 5%.
 Soil with 1% organic matter has about one 1000 lbs
of nitrogen per acre.
 Only about 2% of that amount is released annually
for crop use.
PHOSPHORUS
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Phosphorus is NOT like nitrogen and does not travel
through soil easily.
It moves with soil particles so is lost through plant use or
erosion.
Very little phosphorus moves through the soil
Phosphorus is most important to new seeds and plants
Most effective in high amounts near root area
Soil pH greatly effects phosphorus-too high or too low
pH converts phos to unusable compounds.
Sources for phos-Diammonium phosphate and triple
superphosphate, animal manures, sludges, plant
residues, ground rock phosphate and apatite
Potassium
 Second
only to nitrogen in amount used by
plants
 Relatively immobile in soil.
 Moves in sandy soils
 Most common sign of deficiency is scorching or
browning on leafs.
 Highest nutrient found in soil
 Low amounts available to plants
 Bound in clay soil particles
 Comes from mined waters. Largest deposit is in
Saskatchewan, Canada.
Secondary Nutrients
 The
difference between secondary and
primary nutrients is simply that the plant
uses them in smaller amounts. Still essential
to plant growth and development.
 There are three secondary nutrients: Sulfur,
Calcium and Magnesium.
 Sulfur
 Becomes
available after decomposition of
organic matter and plant residues.
 The available form is SO4—Sulfate and behaves
in soil much like nitrate
 Sulfur
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Continue
Water logged soils may make sulfur unavailable
Can be supplied by rainwater
Is a fertilizer impurity
Adding gypsum will add sulfur
Is an ingredient of many proteins, enzymes and
amino acids of the plant
Interesting fact-helps give mustard, onion and garlic
it’s flavor
 Calcium
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Supplied to plants by soil minerals, organic materials,
fertilizers and liming materials.
Because of cation exchange-soil is very attracted to
calcium.
 Calcium
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Continued
Essential for plant cell-wall structure, element
transport and retention and strength in the plant.
Exist in a balance with Magnesium and Potassiumtwo much of any one of them results in harmful
insufficiencies of the other two.
 Magnesium
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Supplied to plants through soil minerals, organic
material, fertilizers and limestone.
Strong positive cation exchange and acts like
Calcium and Potassium
Is essential for photosynthesis
Activates enzymes for plant growth
Very mobile-goes where it is needd
Micronutrients
7
0f the 16 essential plant nutrients that are
required in small amounts.
 They are: Iron (Fe), Manganese (Mn), Zinc (Zn),
Copper (Cu), Boron (B), Molybdenum (Mo) and
Chlorine (Cl).
 Will limit plant growth under the following
conditions:
 Highly leached acid sandy soil
 Muck Soils
 Soils high in pH or lime content
 Soils that have been heavily cropped and
heavily fertilized with macronutrients
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Iron
 Part of many organic compounds
 Essential for chlorophyll-gives plants their green color
 Highly reactive with Manganese
Copper
 Essential for growth and activates many enzymes
 Lack of will effect proteins in plant
 Too much copper causes shortages in Iron
Manganese
 Basically absorbed by plants
 Activates enzymes
Zinc
 Essential for plant growth
Molybdenum
 Required in minute amounts
 Aids in Nitrate fixation and reduction
 Boron-regulates
metabolism
Nutrient Availability and Plant Uptake
 Available
nutrients are located near the surface of
soil particles. Roots come in contact with nutrients
and take them up into the plant.
 Soil may and does contain large amounts of
nutrients but only a small percentage is available
for the plant to take up.
 Some nutrients will simply stay in the soil until
converted to usable forms
 Some amount of nutrient is lost through erosion,
leaching or volatilization
 Nutrient
Unavailability
 Insoluble chemical compounds-phosphorus and
micronutrients included in many of these (does
not dissolve in water)
 Unweathered or undecomposed soil minerals or
rock fragments-most nutrients included
 Organic matter or plant residues-the main ones
are nitrogen and sulfur
 Trapped by soil particles-potassium and some
ammonium
 Soil pH greatly influences nutrient availability. Too
high or too low can make nutrients unavailable
by converting them to insoluble chemical
compounds
Soil pH
 Soils
contain both acids and bases and the
amounts are expressed as pH
 Scale ranges from 0 to 14
 Soils below 7 contain acid and are acidic
or sour
 Soils above 7 are base and are alkaline or
sweet
 Soils that are 7 are neither acidic or alkaline
 These differences effects how nutrients are
taken up by the plant.
 Causes
of Acid Soil
 Removal of calcium, magnesium and potassium
from a soil profile will allow soil acids to move in.
 Conversion of ammonium fertilizers to nitrates
 Adjusting Soil pH
 Soil can be adjusted-AFTER soil test
 Lime is used to adjust pH upward-neutralizer
 Sulfur lowers pH
 2 lbs/1000ft2 for each .1 unit of pH
 Iron and Aluminum can also lower pH
 Lime Sources
 Most common is agricultural Limestone
 Contains calcium and magnesium-positive
cations
 Functions
of Lime
 Sweetens the soil
 Improves the availability of plant nutrients
 Increase the effectiveness of applied
nitrogen, phosphorus and potassium.
 Increase the activity of microorganisms,
including those responsible for nitrogen
fixation in legumes and the
decomposition or organic matter.
 Improves plant growth and crop yields.
Beans
6.0-7.5
Lettuce
6.0-7.0
Blueberry
4.0-6.0
Onion
6.0-7.0
Cabbage
6.0-7.5
Potato
4.5-6.0
Cantaloupe
6.5-7.5
Rhubarb
5.5-7.0
Carrot
5.5-7.0
Strawberry
5.0-7.5
Grape
6.0-7.0
Tomato
5.5-7.
Azalea
4.5-6.0
Junipers
5.0-6..5
Carnation
6.0-7.5
Petunias
6.0-7.5
Chrysanthemum
6.0-7.0
Pansies
5.5-7.0
Daffodil
6.0-6.5
Roses - Hybrid Tea
5.5-7.0
Geraniums
6.0-8.0
Roses - Climbing
6.0-7.0
Hydrangea - blue
4.0-5.0
Spruce
4.5-5.5
Hydrangea - pink
6.0-7.0
Rhododendron
4.5-6.0
Soil Sampling
 Before
attempting to adjust pH or add fertilizers,
soil samples must be taken.
 Sample must be representative of the soil that is to
be treated.
 Take cores from several areas throughout total
field, lawn or garden
 Soil probes, shovel, bucket
 Mix all the core samples together well
 Take one sample from composite to test
Foliar Symptoms
 Foliar
systems-abnormalities in leaves, stems or
petals that show nutrient deficiencies, insect issues,
disease, drought and pesticide damage.
 Tissue Testing-Rapid and Dry
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Rapid Tissue Testing
 Green
tissue is used
 Chemicals are used
 Quick but not always accurate
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Dry Tissue Testing
 Dried
leaves or plants
 Whole is ground up and sample taken
 Reliable and repeatable
 Not recommended for fertilizer needs
Fertilizer Placement
 Proper
placement of fertilizer is very important to
the effectiveness of the nutrients.
 Characteristics of the soil, kind of crop and the
nature of the fertilizer have to be taken into
consideration.
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Provide adequate quantities of plant nutrients with
the root zone.
Irregular distribution can lower fertilizer efficiency
Early stimulation of the seedling is usually
advantageous. Placement in root zone is good.
The rate and distance of fertilizer movement
depends upon the character of the soil. Nutrient
elements may move upward during dry periods and
may be carried downward by rain or irrigation water.
 Soil-supplied
nutrients when in dry soils are of little
or no benefit to the plant. Excessive amounts of
fertilizer can be injurious. Crops vary in tolerance to
soluble salts.
 Important to place phosphorus near roots as it
travels slowly and is most effective at roots
 Fertilizer needs to be watered in to reduce risk of
salt injury
 Foliar Fertilization
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Feeding plant through leaves and stems
Supplemental feeding
Not effective
Used for rapid intake of a particular nutrient to
correct a deficiency problem
Animal Manure
 Plant
nutrient content is generally low but contains
most of the essential nutrients
 Even in small amounts manure can supply enough
of especially micronutrients to fill in the gaps.
 Nutrient amount is variable and dependent on
many factors: age and kind of animal, feed
consumed, amount and kind of litter/bedding
used and handling methods.