Transcript 5.0 Soils

Mrs. Schratwieser
Horticulture I
Growing Media

 Peat Moss
 Vermiculite
 Perlite
 Organic Matter
 Compost
 Bark
 Sphagnum moss
Peat Moss

 Organic (natural)
 Partially decomposed material mined from swamps
 Good moisture holding properties
Vermiculite

 Inorganic
 Mica mineral matter
 Commonly used to start seeds & cuttings
 Holds moisture
 Neutral pH
Perlite

 Inorganic
 Natural volcanic ash
 Aids with aeration & water holding capacity
Organic Matter

 Dead plant or animal tissue
 Contains carbon
Compost

 Decaying organic matter
 Soil conditioner
 Fertilizer
Bark

 Organic
 Larger matter added to some media to promote
drainage
 Adds weight to soilless mixtures
 Widely used in tree and shrub production
Spagnum Moss

 Organic
 Dehydrated remains of acid bog plants
 Hold moisture
 Very acidic
 Commonly used to line wire hanging baskets
Advantages of Soilless
Media

 Sterile
 pH is neutral
 Disease & weed free
 Good form starting disease sensitive seeds (tomato)
 Easy to control the nutrient content of soil
 Improves crop uniformity
 Easy to create soil for particular needs
Disadvantages of
Horticulture Soils

 Expensive
 Light weight
Additional Materials
Used

 Sawdust
 Wood shavings
Sawdust & Wood
Shavings

 High carbon to Nitrogen ratio
 N is unavailable for plant use
Soil Profile

 Soil layers – Horizons
 O Horizon
 A Horizon
 B Horizon
 C Horizon
 R Horizon
O Horizon

 Rich in organic matter
 Various stages of decomposition
 Dark in color
 Most fertile layer in the soil profile
A Horizon

 Topsoil
 Just below the O horizon
 Earthworms and soil organisms
 Brown in color due to organic matter
B Horizon

 Subsoil
 Clayey soil high in mineral content
 Usually brown or reddish (clay)
C Horizon

 Parent material
 Mainly clumps of un-weathered rocks
R Horizon

 Bed rock
 Cannot be dug by hand
 Very few roots can penetrate bedrock
Soil Structure

 “how the soil particles fit together”
 Sandy soils – looses structure
 Silty/loam have a granular structure
 Clayey soils have a blocky/platy soil
 Granular soil structure is the best
Soil Texture

 Sand – largest particles (low moisture & nutrient
holding capacity)
 Silt – medium size particles (good moisture &
nutrient holding capacity)
 Clay – smallest particle size (high water & nutrient
holding capacity)
 Loam – almost equal parts of all three textures (ideal
texture for most outside/non container plants)
Soil pH

 Measure of acidity or alkalinity of the soil
 0-14 (range)
 0-6.9 (low pH - Acid)
 7 (neutral)
 7.1-14 (high pH – alkaline)
 Lime raises pH
 Calcium or Sulfur lowers pH
 Ideal pH for vegetable garden soils 5.5-7.0 pH
Physical Properties of
Soil

 Permeability – rate at which water moves through
 Water holding capacity – ability to hold water
 Porosity – amount of air space between particles
Ideal Soil Makeup

 50 % - pore space
 50% - soil
 Pore Space: 25% water, 25 % air
 Soil: 45% mineral matter, 5% organic matter
Soil Sample

 Testing for accurate fertilizer recommendations
 Growing plant
 Should be done 1 growing seasons before planting
Soil Sample Procedures

 Create a visual grid of area to be planted (5-10
subsamples from the site)
 Use a stainless steel soil-sampling probe
 4” for lawns, 6-8” crops
 Mix soil samples together
 Remove any grass, rocks, other materials than soil
 Avoid unusually spots, separate box
 Place in soil sample box (Extension office), fill our sample
information sheet
 Mail box and information to Agronomic Division Soil Test
Lab in Raleigh (free)