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Soil Composition & Ferterlizers Northridge Garden Guild June 29, 2010 Materials are a condensed version of information provided by the USU extension service
Soil Composition Jerry L. Goodspeed Utah State University Extension
USDA NRCS Soil – what’s in it?
Why is soil important? Like humans, plants thrive in a healthy environment Good soil provides nutrients, oxygen and water to plants without stress Weak plants are more susceptible to disease and insects
Components of Soil (by volume) (Transpiration and nutrient transport) (Primary soil particles and nutrients for plants) (Soil structure and nutrients for plants) (Oxygen to roots)
Different soil profiles What does your soil look like?
Topsoil-subsoil Characteristics -high organic matter -low salts -high nutrients “Topsoil” -low organic matter -high clay and/     or lime -high salts -high pH “Subsoil”
Individual Soil Properties
Soil Texture The Percentage of sand, silt and clay in the soil
The Effect of Particle Size Sand particles Clay particles Air flow Water flow
Determining Soil Texture By feel Soil test jar method Fill a 1-quart jar ¼ full of soil Fill the jar ¾ full of water Shake very well to suspend soil Place on a flat surface and allow soil to settle
Clay Silt Sand
Texture Effects on Soil’s Physical Properties Textureavailable waterAerationDrainageCompaction Sand Loam Silt loam Clay loam Clay
Treating Soil Texture “Problems” Too much sand? You are lucky Adjust irrigation accordingly Select drought tolerant plants Too much clay? Good luck! Select plants tolerant of poor drainage, lack of oxygen Either case: induce soil structure
Introduction of Organic Matter The combination of sand, silt and clay  combined with organic matter creates secondary particles called aggregates
Compaction Destroys soil structure Seals off soil surface Water runs off instead of into soil – drought results Air can’t enter or escape soil -       suffocation Roots can’t penetrate the soil Stress – plants die
Soil Compaction
Preventing Compaction Grates, bricks, sidewalks in high-use areas
Treating compaction Eliminate the cause: Fence, hedge, signs Add organic matter to soil Aerate or till the soil
Aeration Hollow Tine Aerator “Instant air spaces” for water and oxygen  movement into the plant root zone
Soil Drainage
Poor Drainage Problem Prevent compaction? Add organic matter Install subsurface drainage system  Provide drainage ditches Develop raised beds Use precise water management
Excessive Drainage Problem Very sandy soil Consider sunken beds Add extra organic matter Precise water management
Amending Soil with Organic Matter Benefits: Improves drainage Improves water-holding capacity Reduces compaction Provides nutrients to plants Improves soil “tilth”  	 (ease of tillage, working with a soil) Lowers soil pH
How much organic matter should I add? How much is already there? Native Utah soils ~ 0.25 to 2.0% Ideal soils 5-10% Are you satisfied with the current condition of your soil? Add some organic matter to maintain soil conditions Should I add sand to my clay soil?
Adding/Preserving Organic Matter Grow plants Mulch around perennials Add extra organic matter to gardens and other annual planting areas
Sources of Organic Matter Wood Residues Chips/sawdust/bark materials  Add 1  to 2 lbs of nitrogen per 100 lbs of material Grass clippings or green residues Can’t go wrong with these Allow to dry Composts and animal manure ,[object Object],[object Object]
Summary  Understand what you have Figure out what you need Texture Compaction Drainage
Fertilizers Basic Master Gardener  Training Jerry L. Goodspeed Utah State University Extension
16 Essential nutrients Macronutrients (large quantities): oxygennitrogen		phosphorus hydrogenpotassium		sulfur carbon		calcium		magnesium Micronutrients (small quantities):	 zinciron 		copper		manganese 		chlorine		molybdenum 		boron	         nitrogen       		  Phosphorus	            Potassium
Sources of nutrients Inorganic/Synthetic fertilizers Organic Fertilizers Manures composts, and other organic materials Green manures (legumes and others)
Fertilizer label  Three numbers always appear on the label 	1.	% Nitrogen  (N) 	2.	% Phosphorus (P) 	3.	% Potassium (K)
Just A few N-P-K labels out there 34-0-0 21-0-0 29-3-4 26-3-3 28-4-4 25-3-5 20-2-4 26-3-3 25-3-5 32-3-5 24-6-12 16-4-8 16-16-16 12-12-12 22-4-11 22-4-14 20-27-5 18-5-9 5-10-10 9-17-9
Selecting a fertilizer What nutrients are needed? Soil test What ratio of nutrients are needed? Nitrogen alone or a “complete” fertilizer? Established landscapes need nitrogen annually;  few landscapes need other nutrients Are extras needed? cost factor:  extras increase cost
Soil testing
Soil testing… …prior to planting:  ensures good success – especially in new landscapes …diagnose problems …every 2 to 3 years to monitor soil environment
Soil sampling Sample areas with different soils 6-inch depth in turf 12-inch depth around woody vegetation and in gardens Combine 4 to 6 sub-samples from the area for each sample submitted
Soil Test Report
Methods of application Broadcast – evenly distributed on surface Banding – applied in a narrow band on surface or in furrow opened adjacent to plant row Foliar – applied in liquid form
Spreaders
Organic nutrient sources Much lower concentration of nutrients Example: 2-2-2 for composts Good sources of organic matter May need to supplement with inorganic nitrogen fertilizer
Green manures Plants grown for the sole purpose of “storing” nutrients or producing nutrients (nitrogen) and organic matter for later use in the garden Examples: Legumes (peas, beans, vetch, alfalfa) Small grains (rye, oats, barley, wheat)
Other considerations Combine inorganic and organic nutrients  Practice crop rotation in garden Return as much organic matter as possible to annual planting areas
Soil pH and Iron Chlorosis
Soil pH Soil pH: the degree of acidity or alkalinity of soil The pH scale: 		  2	  4	   6	    8	     10		12 Neutral   (7.0) acidic alkaline
Causes of iron chlorosis High lime soils  Buffer pH in 7.8-8.0+ range Planting acid-loving plants in Utah “Aggravating factors” Cold soils Over-irrigation Soil compaction Over-fertilization Other stresses
Major pH problem:iron chlorosis
Solutions to iron chlorosis problem Select iron efficient plants Treat with iron Change soil pH?
pH tolerant = iron efficient plants
Soil salinity
Soil salinity = soluble salts in soil Salts inhibit plant growth Salts cause “chemical drought”  Visual diagnosis: salt crusting/salt burn Soil test diagnosis: Electrical conductivity (EC)  EC > 2 deciSiemens/meter is a saline soil for horticulture uses
Examples
Sources of salts Residual salts in new development areas Irrigation water natural sources water softeners Deicing salts (road throw and sidewalks) Over-application of fertilizers and/or manures and composts
Solutions to salt problems Control the source: water, fertilizer, manure runoff, other? Clean up the problem: Remove salts by leaching with water
Mg soil   ferterlizer

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Mg soil ferterlizer

  • 1. Soil Composition & Ferterlizers Northridge Garden Guild June 29, 2010 Materials are a condensed version of information provided by the USU extension service
  • 2. Soil Composition Jerry L. Goodspeed Utah State University Extension
  • 3. USDA NRCS Soil – what’s in it?
  • 4. Why is soil important? Like humans, plants thrive in a healthy environment Good soil provides nutrients, oxygen and water to plants without stress Weak plants are more susceptible to disease and insects
  • 5. Components of Soil (by volume) (Transpiration and nutrient transport) (Primary soil particles and nutrients for plants) (Soil structure and nutrients for plants) (Oxygen to roots)
  • 6. Different soil profiles What does your soil look like?
  • 7.
  • 8.
  • 9. Topsoil-subsoil Characteristics -high organic matter -low salts -high nutrients “Topsoil” -low organic matter -high clay and/ or lime -high salts -high pH “Subsoil”
  • 10.
  • 12. Soil Texture The Percentage of sand, silt and clay in the soil
  • 13. The Effect of Particle Size Sand particles Clay particles Air flow Water flow
  • 14. Determining Soil Texture By feel Soil test jar method Fill a 1-quart jar ¼ full of soil Fill the jar ¾ full of water Shake very well to suspend soil Place on a flat surface and allow soil to settle
  • 16.
  • 17. Texture Effects on Soil’s Physical Properties Textureavailable waterAerationDrainageCompaction Sand Loam Silt loam Clay loam Clay
  • 18. Treating Soil Texture “Problems” Too much sand? You are lucky Adjust irrigation accordingly Select drought tolerant plants Too much clay? Good luck! Select plants tolerant of poor drainage, lack of oxygen Either case: induce soil structure
  • 19. Introduction of Organic Matter The combination of sand, silt and clay combined with organic matter creates secondary particles called aggregates
  • 20. Compaction Destroys soil structure Seals off soil surface Water runs off instead of into soil – drought results Air can’t enter or escape soil - suffocation Roots can’t penetrate the soil Stress – plants die
  • 22. Preventing Compaction Grates, bricks, sidewalks in high-use areas
  • 23. Treating compaction Eliminate the cause: Fence, hedge, signs Add organic matter to soil Aerate or till the soil
  • 24. Aeration Hollow Tine Aerator “Instant air spaces” for water and oxygen movement into the plant root zone
  • 26. Poor Drainage Problem Prevent compaction? Add organic matter Install subsurface drainage system Provide drainage ditches Develop raised beds Use precise water management
  • 27. Excessive Drainage Problem Very sandy soil Consider sunken beds Add extra organic matter Precise water management
  • 28. Amending Soil with Organic Matter Benefits: Improves drainage Improves water-holding capacity Reduces compaction Provides nutrients to plants Improves soil “tilth” (ease of tillage, working with a soil) Lowers soil pH
  • 29. How much organic matter should I add? How much is already there? Native Utah soils ~ 0.25 to 2.0% Ideal soils 5-10% Are you satisfied with the current condition of your soil? Add some organic matter to maintain soil conditions Should I add sand to my clay soil?
  • 30. Adding/Preserving Organic Matter Grow plants Mulch around perennials Add extra organic matter to gardens and other annual planting areas
  • 31.
  • 32. Summary Understand what you have Figure out what you need Texture Compaction Drainage
  • 33. Fertilizers Basic Master Gardener Training Jerry L. Goodspeed Utah State University Extension
  • 34. 16 Essential nutrients Macronutrients (large quantities): oxygennitrogen phosphorus hydrogenpotassium sulfur carbon calcium magnesium Micronutrients (small quantities): zinciron copper manganese chlorine molybdenum boron nitrogen Phosphorus Potassium
  • 35. Sources of nutrients Inorganic/Synthetic fertilizers Organic Fertilizers Manures composts, and other organic materials Green manures (legumes and others)
  • 36. Fertilizer label Three numbers always appear on the label 1. % Nitrogen (N) 2. % Phosphorus (P) 3. % Potassium (K)
  • 37. Just A few N-P-K labels out there 34-0-0 21-0-0 29-3-4 26-3-3 28-4-4 25-3-5 20-2-4 26-3-3 25-3-5 32-3-5 24-6-12 16-4-8 16-16-16 12-12-12 22-4-11 22-4-14 20-27-5 18-5-9 5-10-10 9-17-9
  • 38. Selecting a fertilizer What nutrients are needed? Soil test What ratio of nutrients are needed? Nitrogen alone or a “complete” fertilizer? Established landscapes need nitrogen annually; few landscapes need other nutrients Are extras needed? cost factor: extras increase cost
  • 40. Soil testing… …prior to planting: ensures good success – especially in new landscapes …diagnose problems …every 2 to 3 years to monitor soil environment
  • 41. Soil sampling Sample areas with different soils 6-inch depth in turf 12-inch depth around woody vegetation and in gardens Combine 4 to 6 sub-samples from the area for each sample submitted
  • 43. Methods of application Broadcast – evenly distributed on surface Banding – applied in a narrow band on surface or in furrow opened adjacent to plant row Foliar – applied in liquid form
  • 45. Organic nutrient sources Much lower concentration of nutrients Example: 2-2-2 for composts Good sources of organic matter May need to supplement with inorganic nitrogen fertilizer
  • 46. Green manures Plants grown for the sole purpose of “storing” nutrients or producing nutrients (nitrogen) and organic matter for later use in the garden Examples: Legumes (peas, beans, vetch, alfalfa) Small grains (rye, oats, barley, wheat)
  • 47. Other considerations Combine inorganic and organic nutrients Practice crop rotation in garden Return as much organic matter as possible to annual planting areas
  • 48. Soil pH and Iron Chlorosis
  • 49. Soil pH Soil pH: the degree of acidity or alkalinity of soil The pH scale: 2 4 6 8 10 12 Neutral (7.0) acidic alkaline
  • 50. Causes of iron chlorosis High lime soils Buffer pH in 7.8-8.0+ range Planting acid-loving plants in Utah “Aggravating factors” Cold soils Over-irrigation Soil compaction Over-fertilization Other stresses
  • 52. Solutions to iron chlorosis problem Select iron efficient plants Treat with iron Change soil pH?
  • 53. pH tolerant = iron efficient plants
  • 55. Soil salinity = soluble salts in soil Salts inhibit plant growth Salts cause “chemical drought” Visual diagnosis: salt crusting/salt burn Soil test diagnosis: Electrical conductivity (EC) EC > 2 deciSiemens/meter is a saline soil for horticulture uses
  • 57. Sources of salts Residual salts in new development areas Irrigation water natural sources water softeners Deicing salts (road throw and sidewalks) Over-application of fertilizers and/or manures and composts
  • 58. Solutions to salt problems Control the source: water, fertilizer, manure runoff, other? Clean up the problem: Remove salts by leaching with water