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WHAT IS SOIL?
The upper layer of earth in which
plants grow, a black or dark brown
material typically consisting of a
mixture of organic remains, clay,
and rock particles
Physical properties of soil
1. Soil Texture
 Texture refers to the relative proportions of
particles of various sizes such as sand, silt
and clay in the soil
 Sand particles are the largest and clay
particles the smallest
 Most soils are a combination of the three.
The relative percentages of sand, silt, and
clay are what give soil its texture

 A clay loam texture soil, for example, has nearly
equal parts of sand, slit, and clay
Soil Structure
 Soil structure is the arrangement of soil
particles into small clumps, called peds
or aggregates
 Soil particles (sand, silt, clay and even
organic matter) bind together to form
peds
 Depending on the composition and on
the conditions in which the peds formed
the ped has a specific shape
 They could be granular (like
gardening soil), blocky, columnar,
platy, massive (like modeling clay)
or single-grained (like beach sand)
SOIL COLOR
 Soil color is influenced primarily by soil
mineralogy – telling us what is in a
specific soil
 Soils high in iron are deep orange-
brown to yellowish-brown
 Those soils that are high in organic
matter are dark brown or black

 Color can also tell us
how a soil “behaves” –
a soil that drains well is
brightly colored and
one that is often wet
will have a mottled
pattern of grays, reds,
and yellows
Chemical properties of soil
 Soil chemical properties including pH,
electrical conductivity (EC), cation
exchange capacity (CEC), C/N ratio of
added amendment, and organic matter
(OM) content can impact soil N supply
Acidity (pH)
 Acidity (pH) is a measure of the concentration
of free hydrogen ions (H+)
 A high concentration in the soil signifies a low
pH, whilst a low concentration equals a high
pH
 Soils and other substances with a pH below 6
are called acidic, whilst those with a pH above
6 are known as base or alkaline
Salt levels
 The salt level is the sum of all the mineral salts
that are present in the soil
 They can originate from the soil itself, fertilizer,
organic manure and in coastal areas from salt
marshes or tidal marshes.
CEC
 CEC is the abbreviation of cation exchange
capacity, which notes the amount of cations can
be bound to the soil
 These cations are mainly Ca2+, Mg2+, K+, Na+
and to a lesser extent NH4+ , Al3+, Fe2+, Mn2+
and H+
Macro-elements
 Macro-elements are the most important nutrients for
plants
 They occur naturally in the soil to some extent and
can be supplemented with fertilizers, manure and
compost
 The macro-elements are calcium (Ca), magnesium
(Mg), potassium (K), Sulphur (S), phosphate (P),
nitrogen (N), sodium (Na)
Micro-elements
 Trace elements are nutrients that plants
need in small doses
 The trace elements are boron (B),
copper (Cu), manganese (Mn), cobalt
(Co), silicon (Si), zinc (Zn), iron (Fe) and
molybdenum (Mo)

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Soil ecology

  • 1. WHAT IS SOIL? The upper layer of earth in which plants grow, a black or dark brown material typically consisting of a mixture of organic remains, clay, and rock particles
  • 2. Physical properties of soil 1. Soil Texture  Texture refers to the relative proportions of particles of various sizes such as sand, silt and clay in the soil  Sand particles are the largest and clay particles the smallest  Most soils are a combination of the three. The relative percentages of sand, silt, and clay are what give soil its texture 
  • 3.  A clay loam texture soil, for example, has nearly equal parts of sand, slit, and clay
  • 4. Soil Structure  Soil structure is the arrangement of soil particles into small clumps, called peds or aggregates  Soil particles (sand, silt, clay and even organic matter) bind together to form peds  Depending on the composition and on the conditions in which the peds formed the ped has a specific shape
  • 5.  They could be granular (like gardening soil), blocky, columnar, platy, massive (like modeling clay) or single-grained (like beach sand)
  • 6. SOIL COLOR  Soil color is influenced primarily by soil mineralogy – telling us what is in a specific soil  Soils high in iron are deep orange- brown to yellowish-brown  Those soils that are high in organic matter are dark brown or black 
  • 7.  Color can also tell us how a soil “behaves” – a soil that drains well is brightly colored and one that is often wet will have a mottled pattern of grays, reds, and yellows
  • 8. Chemical properties of soil  Soil chemical properties including pH, electrical conductivity (EC), cation exchange capacity (CEC), C/N ratio of added amendment, and organic matter (OM) content can impact soil N supply
  • 9. Acidity (pH)  Acidity (pH) is a measure of the concentration of free hydrogen ions (H+)  A high concentration in the soil signifies a low pH, whilst a low concentration equals a high pH  Soils and other substances with a pH below 6 are called acidic, whilst those with a pH above 6 are known as base or alkaline
  • 10. Salt levels  The salt level is the sum of all the mineral salts that are present in the soil  They can originate from the soil itself, fertilizer, organic manure and in coastal areas from salt marshes or tidal marshes.
  • 11. CEC  CEC is the abbreviation of cation exchange capacity, which notes the amount of cations can be bound to the soil  These cations are mainly Ca2+, Mg2+, K+, Na+ and to a lesser extent NH4+ , Al3+, Fe2+, Mn2+ and H+
  • 12.
  • 13. Macro-elements  Macro-elements are the most important nutrients for plants  They occur naturally in the soil to some extent and can be supplemented with fertilizers, manure and compost  The macro-elements are calcium (Ca), magnesium (Mg), potassium (K), Sulphur (S), phosphate (P), nitrogen (N), sodium (Na)
  • 14. Micro-elements  Trace elements are nutrients that plants need in small doses  The trace elements are boron (B), copper (Cu), manganese (Mn), cobalt (Co), silicon (Si), zinc (Zn), iron (Fe) and molybdenum (Mo)