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LA Master Gardener
Soils, Soil Moisture and Nutrition
Chapter 5 J Stevens
Associate Professor/SpecialistSoil Fertility/Nutrient Management
Still daylight in California.
Did You Read Chapter 5?If so, do you have any “burning”
questions?
This presentation is a combination of information from 4-5 courses in Soil
Fertility,Advanced Soil Fertility, Micronutrients,
Soil Chemistry, and Soil Classification.
Soil Fertility is actually Soil Chemistry.
So, What is Soil?
A living dynamic resource that supports plant
life.
Contains mineral particles, organic matter, air,
water, and organisms.
Biological, chemical and physical properties that
are always changing.
Soil CharacteristicsA medium in which plants grow.
An ideal garden soil is fertile, deep, easilycrumbled, well drained and fairly high in
organicmatter (O.M.)
Soil fertility is vital to a productive soil. A
fertile soil is not necessarily a productive soil.
Poor drainage, insects, weeds, drought and other
factors can limit production, even when fertility is
adequate.
Soil Composition
Soil is made up of:Mineral matter- sand to clay 45%Organic matter 5%Water - in the pore spaces 25%Air - in the pore spaces 25%
These are the proportions in a loam-textured
soil & they vary from time to time and place to
place.
Soil Formation The exposed surfaces of rocks,
gravel,sand and silt particles are constantlybeing broken down by physical andchemical weathering.
As soils are formed during the weathering
process, some minerals and organicmatter are broken down to
extremelysmall particles.
Important Physical Properties of SoilColor- determined by O.M., drainage,
and degree of oxidation/weatheringTexture- amounts of different sized particlesStructure- arrangement of soil
particles into aggregatesDrainage- water movement in/on the
soilSoil Depth- vertical distance into a
soil to layer that restricts root
growth
Soil Color- GeneralizationsLight (topsoil) - low O.M., coarse texture, leached
Dark (topsoil) - more O.M., could be parent
material
Red/Brown (subsoil) - relative free movement
of water and air
Yellow (subsoil) - drainage impediment
Gray (mottling) - too much water/ too little air
Poor drainage - notice the gray color
O
High water in bed – notice the plasticNot a desirable situation!
O
Soil TextureRelative amounts of sand, silt and clayRefer to the soil textural triangle (Figure
5-2)
Sand is the coarser particles, feel rough when
rubbed between the thumb and fingersSilt when dry feels smooth/floury; wet-
smooth,not slick or stickyClay particles are fine textured. Smooth
whendry; slick and sticky when wet
Eight or nine textural classes generally used.
Soil Textural Triangle
Notice the direction of the arrow
Maui Gulf of Mexico White SandsNew Mexico
Sand
Clay
Structure of Clay,1:1 non-expanding lattice clay
Structure of Clay, 2:1 expanding lattice clay
Soil StructureRefer to Table 5-1Arrangement of primary soil particles intoaggregates. Principal forms are- platy,prismatic, columnar, blocky and granular.Structure is closely related to air and
watermovement. Water, air and plant roots
movemore freely through soils that have blockystructure than those with platy structure.
Watercan enter a soil with granular structure
morerapidly.
MulchingSimply placing a layer of organic or
inorganicmaterial on top of the soil. Shredded pine
barkor compost can reduce extremes in soil temperature and moisture levels. Dense
mulchcan be effective in controlling weeds.
Mulch that decomposes can be incorporated
into the soil to improve soil structure, water
holding capacity, rainfall infiltration, and raise
soil nutrient levels.
What is Composting?Composting occurs naturally nearly everywhere! Leaves
drop, grassclippings after the lawn is cut, plants and animals die.
Over time, these organic materials breakdown and decompose.
The rich, dark, soil-like material that results is called compost.
Microorganisms such as bacteria and fungi and small soil animals
do much of the work in breaking organic residues down to form
compost.
Microorganisms use the organic materials as food sources.
Nutrients are released back into the soil, to be used by plants.
This is nature’s way of composting and recycling!
Why Compost?You can help the composting cycle work even better than
innature. The organic waste you put back into the soil can be
usedby other things.
Instead of it going to a landfill or garbage-burning plant, itbecomes a valuable resource.
Yard waste and food scraps account for 20 to 30 % of garbage. By
composting these organic materials you send less garbage to the
landfill.
Gardeners use compost, as it allows the soil to hold more water,
and it adds nutrients to the soil.
Flowers, vegetables, trees, shrubs, house plants, lawns and
container plants benefit greatly.
Best Ever CompostLike baking a cake- just follow the recipe! Add the ingredients,
stir, “bake” and out comes compost!
There are a few basic steps to follow. Here are the necessary ingredients
and general directions for composting:
IngredientsKitchen Compost Yard or Garden Compost Add a mixture of some or all of these ingredients
Vegetable peels and seeds Hay or straw
Eggshells Wood chips/sawdustFruit peels and seeds Weeds and other wastesNutshells Grass clippings & leavesCoffee grounds Manure (not dog/cat)
Other vegetable or fruit scraps Ashes, shredded newspaper
Do not add meat scraps, bones, dairy products, oils or fats- Attract pests.
Directions1. Choose a composting bin; buy one for $$ - $$$ or make one.2. Place kitchen or yard waste in the bin; chop or shred
organics.3. Spread soil or “already done” compost over the pile This
layercontains the microorganisms that do the work; can do this in layers.
4. Adjust the moisture. The materials should be damp to the touch,but not so wet that drops come out when it’s squeezed.
5. Allow the pile to “bake”. It should heat quickly and reach a desiredtemperature of 90 to 160 degrees F in four to five days.
6. Stir the compost as it “bakes” if you want to speed the process.
7. The pile will settle down from its original height. This is good signthat the compost is “baking properly”.
8. If you turn or mix the pile every week, it should be done, or readyto use in 1 to 2 months. If you don’t turn it, the compost should be ready in 6 to 12 months.
9. Your compost should look like dark, crumbly soil; earthy/sweet.
10. Use the compost to mix into the soil to “feed” hungry plants.
Microbes Need a Balanced DietMicrobes normally live in the soil and eat small
tidbits oforganic matter where they get their nutrition.
They need carbon for energy and nitrogen to help build
their bodies. Carbon to Nitrogen ratio; C:N
Some wastes high in Carbon:Paper, sawdust, wood chips, straw, and leaves
Some wastes high in Nitrogen:Food scraps, grass clippings, legumes, and manures.
Be sure to include a mixture of wastes high in Nitrogen
in your compost pile.
Air, Water and WarmthMicrobes need oxygen, which if low, microbes
die-offand other microbes that don’t need oxygen
breakdownmaterial and give off nasty odors.
Compost piles should be as moist as a sponge that has
just been wrung out. If the pile is too dry, add water; if
too wet, add straw or dry sawdust to soak-up excess
moisture.
Microbes like temperatures of 90 to 140 degrees F. If
the temperature is too low, microbes will die-off and the
pile will take longer to reach the compost stage. Build
pile at least 3’ X 3’ X 3’ to help keep it warm.Shred the organic material, as it’s easier for
microbes to work with smaller pieces and decompose it
faster.
Which Composting System?System Used Cost Rate of
CompostingYard Waste
Compost mound None Slow not turned; fast
Holding unit Low SlowTurning unit High/Low Fast, minimum 6
wksCommercial bin High Fast, minimum 2
wksKitchen Waste
Garbage can Low Slow; faster if mixed
Worm compost bin Medium Fast, minimum 4 wks
Turning unit High Fast, minimum 6 wks
Kitchen/yard wastes combined may attract rodents.
Compost Pile Isn’t WorkingSymptom Problem How to Fix It
Pile is wet/ smells of Not enough air Turn the pile
rancid butter, vinegar, Too much N Add straw, sawdust,
and rotten eggs Too wet and chips
Pile doesn’t heat up Pile is too small Make pile larger
Pile is too dry Add water
Pile is damp and sweetsmelling, won’t heat up Not enough N Add grass
clippings or other sources of N
Center is dry, containstough materials Not enough water Add water and
turnPile attracts animals Meat and other Keep meat
and otheranimal products animal
products out;have been added enclose pile in
¼ inch hardware cloth
What To Do With My Compost1. Spread it on garden and mix it in with tillage.
2. Place or bury between the rows; roots will find nutrients.
3. In flower gardens, dig it in around the plants.
4. Use it as a mulch for shrubs, trees, and plants.
5. When transplanting, mix compost into the soil.
Don’t use compost to sprout tender seed. The seed may be killed by a fungus in the compost that causes a damping-off disease.
Organic Material vs. Organic Matter
Fresh/Partially decomposed OrganicMaterial:
Manures, grass clippings, leaf mold, oldsawdust and straw are good examples.
Broken down similar to composting, by micro-organisms in the soil, with adequate moisture, temperature, and nitrogen availability, to ultimately become Organic Matter (O.M.).
Soil Organic Matter Organic matter was once a living,
breathing organism, either plant or animal. Organic materials breakdown into humus under favorable temperature, oxygen and moisture conditions. What we measure in a soil sample as organic matter is the end product of decomposition. As earthworms, insects, bacteria, fungi and microbes feed on organic matter, nutrients are released that are available for use by growing plants.
Benefits of Soil Organic Matter
Improves soil physical condition, soil tilth
Increases water infiltration and water
holding capacityImproves soil structure and aerationStorehouse of plant nutrients - N, P,
S,Zn, etc.Increases exchange capacity
Cation Exchange One teaspoon of clay particles has a
surface area that will cover an acre of land. For the same measure, sand particles will have a surface area about equal to a sheet of paper in your manual.
The clay and organic fraction of the soil are referred to as colloids. These colloids have a negative (-) charge, attracting positively (+) charged particles.
This soil property is important, as it enables
a soil to hold positively charged nutrients;negatively charged nutrients will leach
throughthe soil.
Cation Exchange Capacity
The net total negative charge of a soil (or it’s capacity toexchange one cation for another) is referred to as cationexchange capacity, abbreviated as CEC.
Table 5-2 shows the CEC of soils from seven soil areas inLouisiana. Numbers increase with > amounts of clay.
Basic Cations include: Calcium, Ca ++, Magnesium, Mg ++, Sodium, Na+, Potassium, K+ and Ammonium, NH4
+
Acidic Cations: Aluminum, Al+++, Hydrogen, H+; maydominate exchange sites in highly weathered, acidic soils.
Selected Soil Areas in LASoil Area Soil Texture CEC
(meq/100 g)
Coastal Plains sl 4vfsl 6
Mississippi Terrace sil 8 – 10Coastal Prairies vfsl 8
sil 10cl 15
Miss., Red, Ouachita sl 4River Alluvial vfsl 8
sil 10 -15sicl/c 20/25
Clay or Organic MatterParticle(Colloid)
Ca++
- -Mg ++
- -Na +
-
- H+
-K+
-NH4
+- - -Al+++
NO3 -
HPO4-2
Lime reaction:
Step 1. Al +3 + CaCO3 + OH- ----> Ca +2 + Al(OH)2 + OH- + CO2
Step 2. H+ + OH- ----> HOH (pH goes up)
Cl-
SO4-2
Exchangeable Soil solution Fertilizer
(NH4)2SO4
NH4NO3
H3PO4
KCl
NH4+
K+
Na + Ca +2 Mg +2
Soil Water TermsGravitational water- available to plants
Capillary water- available to plants
Hygroscopic water- referred to as unavailable water.
Associated with soil moisture content at or below the
wilting point.
Field capacity- water a soil will hold against gravity
when allowed to drain freely.
Soil Moisture Storage
Figure 5-4 illustrates the relationship between soil texture and
soil moisture content.Size and total volume of pore space are a function of soiltexture and structure. Both available and unavailable water increases as claycontent increases. Thus, sands have a a much lower waterholding capacity than clay soils.Soil water holding capacity is important for irrigationamounts and frequency. Table 5-5 lists numerical values ofwater storage capacities for six common soil textures.
Remember, most garden and landscape soils have been
modified, so the values in this table may vary significantly.
Fertilizer or Food?Fertilizers contain plant nutrients. Fertilizers are not plant food.Plants produce their own food usingwater, carbon dioxide, and energy
fromthe sun to produce sugars andcarbohydrates, which, combined
withplant nutrients, do produce proteins,amino acids, enzymes, and vitamins,
asthe building blocks essential for
plantgrowth and development.
Plant Nutrients Plants need 16 elements for plant growth.
These arecalled the essential elements.
Carbon, C from carbon dioxide; Hydrogen, H from
water and Oxygen, O from water and the air, as O2.
These are the non-mineral nutrients.
There are 13 other elements (nutrients) that aregrouped into three categories:
Major nutrientsSecondary nutrientsMicronutrients
The Major Nutrients
Nitrogen, NPhosphorus, PPotassium, K
Plants require these in larger quantities;
Most likely to be deficient.These are the three elements on afertilizer label. ( N – P2O5 – K2O)
NitrogenDark green color of leaves; usually responsible
more forincreasing plant growth than any other element.Proteins & DNA/RNA
Excess- succulent growth, weak spindly plants, few fruit
Deficiency- yellowing of the leaves, reduced growth
Plants can absorb their N in the form of ammonium or
nitrates, with nitrates being the largest quantity.
Mobile in the plant; nitrates may leach in sandy soil.
Phosphorus
No other nutrient can be substituted for it. Contained in
proteins and amino acids. Without it, plants could not
convert solar energy to chemical energy for synthesis of
sugars, starches and proteins.
Excess- micronutrient deficiencies of Zinc and Iron
Deficiency- reduced growth, purpling in foliage or veins of some plants
Fixed by Al, Fe and Mn in acid soils; fixed by Ca in alkalinesoils. Important in root development of young plants.
Mobile in plant; doesn’t leach except in organic mixes.
Applied as a fertilizer in the phosphate form.
PotassiumInvolved in photosynthesis, sugar transport,
water and nutrient movement, protein synthesis, and starchformation. Improves tolerance to disease, water
stress,winter hardiness and uptake efficiency of othernutrients.
Excess- causes N deficiency and may affect uptake of
other positively charged nutrient elements.
Deficiency- marginal burn or scorch affecting photosynthetic activity. Short
internodes, weak stalks.
Involved in photosynthesis, plant-water relations,disease tolerance, and quality in fruits and
vegetables.Mobile in the plant/leaches in the soil
The Secondary NutrientsCalcium, CaMagnesium, MgSulfur, S
These are not any less essential than the major
nutrients, only being used in a smaller quantity.
Lime, if needed to raise soil pH, will supply
Calcium and/or Magnesium. Calcitic orDolomitic lime; there are other liming
materials(Hydrated lime and Quick lime ; Pelletized
lime)Gypsum is not a liming material, not
effect pH.Gypsum (Calcium sulfate) contains Ca and
S.
CalciumImportant in the structure of the plant cell walls.Stimulates root and terminal bud development.
Excess- interferes with Mg absorption; replaces K, Na
and NH4+ on soil complex; causes high soil pH-
micro’s
Deficiency- inhibition of bud and root tip growth,blossom-end rot on vegetables
Important in pH control by reducing acidity. Limited
mobility in the plant; moderately leachable.
MagnesiumCentral element of the chlorophyll molecule, so
it’sactively involved in photosynthesis, energy
metabolism,and is required for protein formation.
Excess: interferes with Ca uptake
Deficiency: reduced growth, marginal chlorosis, interveinal chlorosis starting at leaf
tips at lower to mid-plant.
Leaches from soils, is mobile in the plant. Foliage plants
susceptible. Epsom salts or Dolomitic lime, if pH is low.
SulfurComponent of some amino acids that are
importantin building proteins.
Excess: over-application of S to lower soil pH
Deficiency: symptoms are general yellowing of
younger leaves or the entire plant
High N rates may induce S deficiency. Is not mobile
in the plant, but sulfate-S is leachable in the soil.
The Micronutrients
Boron, B; Copper, Cu; Manganese, Mn ; Zinc, Zn; Iron,
Fe; Molybdenum, Mo and Chlorine, Cl
Micro meaning small; at one time called minornutrients, but not of minor importance. Soilavailability depends on pH with deficiencies
likelyabove a soil pH of 6.8
Many micronutrients are enzyme activators. Used in
smaller quantities than major or secondary nutrients.
IronImportant in chlorophyll and protein formation,
enzymesystems, respiration, photosynthesis and energytransfer.
Deficiency: interveinal chlorosis on younger tissue that
may change from yellowish to white.
Conditions for deficiency include soils high in Ca, poorly
drained soil, high soil pH, high soil P, Cu or Zn.
Acid loving plants: azaleas, blueberries, camellias,
roses, etc. need iron and will show symptoms.
Can be corrected with chelated forms of iron and other
type fertilizers containing iron , as well as amendments
that lower soil acidity; Aluminum sulfate & sulfur.Caution!
Iron deficiency- Crepe myrtle
Iron deficiency- Elm
Hydrangea- Iron deficiency
Soil pHThe term pH defines the relative acidity or
alkalinity of a substance.
The pH scale ranges from “ 0 ” to “ 14 ” , with a pH of
“ 7 ” being neutral.
0 ------------------------7-----------------------14 Acid Alkaline
pH is defined as the negative logarithm of the hydrogen
(H+) concentration.
pH - Hydrogen Ion ActivitySoil pH is expressed in logarithmic terms, not a
linearscale! Each pH unit change means a tenfold
changein acidity or alkalinity. Ex: pH 4 is 10 times as
acidic aspH 5
Older literature spoke of a soil being sour (acid) or
sweet ( basic or alkaline)
pH is one of the most important soil chemical reactions
Soil pH has a profound effect on availability of
nutrients and microbial activity. (Refer to page 5-11)
I
II
Don’t lime to this level Never happen
Need to lime
Need to lime
Need to lime
Adjusting Soil pHBase it on a Soil Test!!!! Lime or Sulfur
requirement.
Lime raises the soil pH; Sulfur reduces soil pH, more
acid. The old adage “ if a little is good, more is better”
willget you in a bind if you over-apply either of thesematerials.
Raise pH – Ag Lime, Dolomitic lime, Hydrated lime
(caution)
Lower pH- Elemental sulfur, Aluminum sulfate (caution)
Soil TestingPurpose - supply clients with enough
information tomake a wise choice regarding applications of
soil amendments and fertilizers.
Measures the plant-available portion of soil nutrients.
Soil test results form the basis for nutrientrecommendations.
Routine soil test from the LSU AgCenter Soil Testing
and Plant Analysis Laboratory costs $10, provides a soil
texture, soil pH, Calcium, Magnesium, Phosphorus,
Potassium, Sodium, Zinc, Copper, and Sulfur plus a lime
or sulfur requirement, if needed, to adjust pH for the
crop (s) listed.
No Reliable Soil Test For Nitrogen Availability* In all soils there is considerable intake
and outgo of nitrogen in the course of a
year. This is accomplished by many complex transformations. * The Nitrogen cycle is an interlocking succession of largely biochemical
reactions.* Total N encompasses all phases of N, but
available N is like a snapshot of something in
motion.
Philosophy of Soil Test Fertilizer Recommendations1. Base them on soil test results, every 3
years
2. Recommend that lower testing soils be built up to higher test levels by adding fertilizer
3. Apply maintenance amounts of plant nutrients to higher testing soils to keep them there and keep productivity high (Vegetables and high value crops)
4. Do not apply specific nutrients to soils testing very high in these nutrients
Using the Soil Test Results
Need to understand the information on the
Soil Test Results Sheet that is mailed toyou from the Soil Lab with Soil Test
Results.
*Soil Test Results and ratings (interpretations)
*Fertilizer and lime recommendations*Fertilizer management practices or
concerns (Soil Test Information Sheet)
Soil Area
*Soils are classified into two areas, upland &
alluvial. Upland soils are those in the Coastal Plains (hill soils) and the
Loessial, silt loam-textured soils, like the Macon Ridge or the Grand Coteau Ridge.
*The alluvial soils are those in the river bottoms, not creek bottoms.
Soil pH ( Soil Reaction)*Soil pH indicates the level of active
acidity.*Maintaining a soil pH between 5.7 to 6.5
will generally provide a favorable
environment for growth and development of many
plants.*Lime recommendations are made to
correct problems with soil acidity; H, Mn &Al*Recommendations are based on the soil
pH, soil texture and the crop to be grown.*Two types of lime: Calcitic or Dolomitic*Look at soil test Ca and/or Mg levels.
Soil Test Ratings
Soil testing labs use some form of rating scale within which
soil test values are placed. What do these ratings mean?
An example of this :
Very Low < 50% crop potential, with no fertilizerLow 50-75% crop potential, if not fertilizedMedium 75- perhaps 95% of the crop potentialHigh no fertilizer is needed, soil can supply allVery High no fertilizer is needed, just more cost;
potential for environmental issues
Phosphorus- P*In LA, P is extracted using the Mehlich III soil testing extractant. *Test results given as ppm of Extractable
P, a measure of the relative availability of
P.
*Not a measure of total phosphorus.
*Recommendations as lbs. of Phosphate/Ac
( P2O5 ); oz./bush; oz or lb./100 or 1,000 sq. ft., based on the crop.
Calcium, Magnesium,Potassium, Sodium, Copper, Sulfur, Zinc* Cations are extracted by the Mehlich III
soil test extractant.* Reported as Extractable nutrients, as
ppm.
* Calcium/ Magnesium levels – type of lime
* Recommendations for K as lbs. Potash/Ac
( K2O ); oz./bush or 100 or 1,000 sq. ft.
Organic Matter*Expressed as a percentage*No rating system*Measures the resistant state of
O.M. in soilConsider this:
An acre of soil measured to a depth of six and 2/3 inches weighs about 2,000,000 pounds, meaning that 1% organic matter in the soil would weigh about 20,000 pounds. It takes about 10 pounds of organic material to decompose to 1 pound of organic matter, so it takes at least 200,000 pounds (100 tons) of organic material applied to the soil to add 1% stable organic matter under favorable conditions.
Know the Size of the Plot** 1 Acre = 43,560 square feet AND** Anything at ~ 45 lb/1,000 sq. ft. = 1
Ton/Ac
Ex: Length in feet X Width in feet = Square feetGarden is 20 ft. X 50 ft. = 1,000 sq. ft.
1,000 sq. ft. divided by 43,560 sq. ft. = 0.023 Ac and
0.023 Ac X 2000 lb Lime (1 ton) = 46 lb of lime (rounded)
Use this type equation to figure lime/sulfur rates on
small areas of less than one acre.
Additional Soil Tests- STPALSoil Organic Matter $4/sample
Micronutrient Test Zn, Fe, Mn and Cu. , $5/sample
Heavy Metal Test As, Cd, Pb, and Zn., $5/sample
Optional Soil Tests Al, B, S, Soluble salts and Extractable oil; $5 for each analysis; separate
Flood Test EC, Salts, SAR, Cl, Na, etc.; $6/sample
Soil-less Routine Ca, K, Mg, P, pH, conductivity (E.C)for potting mixes nitrates ; $10/sample
The soil tests offered are not for environmental assessment purposes.
Heavy metals should be determined by labs using EPA approved methods, which determine and report these elements as totals or
semi-total values.
The W. A. Callegari Environmental Lab will run totals.
Fertilizer
Produces results that are considered desirable; applied
to obtain some desired plant response; appliedwhenever you expect to get a desired plant
response;that’s where the ratings/interpretations come in.
Fertilizer needs should be based on soil test results ~ 3
years.
A properly taken soil sample, analyzed by a soil testing
lab will give you recommendations on the fertilizer
nutrient needs of the crop (s) you will be growing.
Fertilizer SelectionRecognize the plant response you are seeking
Contains the needed nutrient (s)
Releases the nutrients when needed
Cost effective
Safe and convenient to use
Environmentally friendly
LA Fertilizer Law
Louisiana Dept. of Agriculture and Forestry- State LawRequiring fertilizer manufacturers to guarantee the
claimedfertilizer analysis on the label on a bag of fertilizer.
Nutrient analysis is based upon a percentage of weight. The
analysis is sometimes called the “grade.”
All fertilizers are labeled with three numbers that give the percentage by weight of nitrogen, phosphate and
potash.
All fertilizers are based on 100 pounds.
Example: 8-8-8 contains 24 lb. of nutrients per 100 pounds of
fertilizer.
Common Nitrogen FertilizersFertilizer material % NitrogenAmmonium nitrate 34
Ammonium sulfate 21
Urea 45-46
Potassium nitrate 13
Calcium nitrate 15
Common Phosphate Fertilizers
Fertilizer material % P2O5
Triple superphosphate (TSP) 46
Ordinary superphosphate 20
Bone meal 22 - 30
Common Potash FertilizersFertilizer material % K2O
Muriate of potash 60
Potassium sulfate 52
Potassium nitrate 44
Sulfate of potash magnesia 21also known as K Mag
Complete/Incomplete/Balanced FertilizersComplete- contains the three major
nutrients; N, P and K Ex: 12-6-6
Incomplete- lacks one of the major nutrients
Ex: 34-0-0 ; 0-0-60 ; 18-46-0
Balanced- contains the three major nutrients,
in the same proportions Ex: 8-8-8 ; 13-13-13
Incomplete to Complete FertilizerFertilizer Analysis AmountUrea 45-0-0 100 lb
Triple superphosphate 0-46-0 100 lb
Muriate of potash 0-0-60 100 lb
Produces 45-46-60 300 lb
With a grade of ~ 15-15-20 for every 100 lb
Slow- Release Fertilizers
Slow release of nutrients at a controlled rate, with a
balance of nutrients throughout the growth cycle.
Categorized by the way the fertilizer is released:1. materials that dissolve slowly2. materials from which nitrogen is released by
microorganisms3. granular materials with membranes made of resins
or sulfur that control the rate of nutrient release
from the granules into the soil
Ex: Sulfur-coated Urea and Osmocote
Slow Release - Pros and Cons
AdvantagesFewer applicationsLow burn potentialRelease varies based on fertilizer characteristicsComparatively slow release rate
DisadvantagesUnit cost is highAvailability limitedRelease rate governed by factors other than plant need
Conventional Fertilizer – Pros and Cons
AdvantagesFast actingSome are acid-formingLow cost
DisadvantagesGreater burn potential (fertilizer salts)Solidifies in the bag when wetNitrogen leaches readily
Manures/Sewage Sludge – Pros and Cons
AdvantagesLow burn potentialRelatively slow releaseContains micronutrientsConditions the soil
DisadvantagesSalts may be a problemBulky; hard to handleOdorExpensive per pound of actual nutrientWeed seeds may be a problemHeavy metals in sewage sludge
Organic FertilizersRefers to nutrients contained in fertilizer - type
productsderived solely from the remains (or a by-product)
of aonce living organism.
Cottonseed meal, blood meal, bone meal, fish emulsion
and all manures are examples of organic fertilizers. If
sold as a fertilizer, it will have a fertilizer analysis
stated on it.
Many times sold as a soil conditioner, without aguaranteed fertilizer analysis. Some have
fertilizeradded to them.Depend on soil organisms to break them down.
Manure is a Complete FertilizerLow in the amount of nutrients it can supply.
Varies in nutrient content according to the animal
source, what the animal has been eating and storage
method.
Manures are best used as soil conditioners.
Fresh manure should not be used in contact with tender
plant roots.
Application rates may vary from a moderate 70 lbs/1,000 sq. ft. to as much as 1 ton/1,000 sq. ft.
“Weed and Feed”CAUTION IS ADVISED!!!!
We use them for convenience and reduced labor.However, a big concern is that the herbicides
used onthe lawn area will be taken up by tree and shrub
rootsand severely affect or kill what we don’t want todisturb. Different herbicides control different
weedspecies.
Need to check on which herbicides are used in the
“Weed and Feed” products. Ask your County Agent!
Keep these fertilizers away from shrubs, flower beds,
and trees.
Soluble SaltsFertilizers don’t burn or damage plants if applied
correctly.
Fertilizers are salts: nitrates, sulfates, phosphates, chlorides,
carbonates, bicarbonates, borates, etc.
Consider table salt ( Sodium chloride); we have afertilizer material, Muriate of potash (Potassium
chloride.)
Fertilizer applied to the soil dissolves in the soil moisture
and diffuses out into the soil. Tender roots near fertilizer
have water drawn from them and the surrounding soil; roots
begin to dehydrate and collapse if the salt concentration is
too high, roots “burn” and plants may die or suffer severe
damage.
Salt ProblemsContainers- salts accumulate on top of the soil; white crust
or ring of deposits at soil line or the drain hole. Clay pots- inside and/or outside of the pot.
Fertilizer applied repeatedly without sufficient water to leach or wash accumulated salts through the soil.
Container plants should be leached every 2-4 months. Do this
prior to fertilizing the plant, with an amount of water twicethe volume of the container.
Do not allow leached water to remain in contact with containers.
Problems do occur in gardens, with excess fertilization, since all
fertilizers are one type of salt or another. Fertilizer salts.
Fertilizer salts- Strawberry field
Gypsum for Sodium ProblemsGypsum is calcium sulfate, a neutral salt.
Does not increase or decrease the soil pH.
Soil areas should receive an application of gypsum to
dislodge the Na on the soil exchange sites.
Thorough watering/irrigation, will move Na somewhat
deeper into the soil (away from the active rooting zone)
or out of a pot. If it’s a clay soil, salts will not move.
Calcium is left on the soil exchange sites.
Gypsum does not improve soil tilth; does not alleviate
compaction problems, unless Na is the problem!
Fertilizer Application Methods
Broadcasting
Banding
Starter solutions
Side-dressing
Foliar feeding
Wishing you the best with your gardening adventure!
Thanks for your attention!
Are there any questions?
STPAL website
http://www.lsuagcenter.com/soiltest