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)