Soils
Soils
Characteristics
Characteristics
Texture
Texture
Soil Profile
Soil Profile
Soil Types
Soil Types
Threats to Soil
Soil Characteristics
Soil Characteristics
3 characteristics of soil that affect its value for 3 characteristics of soil that affect its value for
farming and growing vegetation a
farming and growing vegetation are:re:
1.
1.
Organic Content
Organic Content
2.
2.
Mineral Content
Mineral Content
3.
Soil Characteristics
Soil Characteristics
1.
1.
Organic Content
Organic Content
- A soil's fertility is determined as a ratio
- A soil's fertility is determined as a ratio
of the organic content to the content of
of the organic content to the content of
ground bed rock. Amount of dead and
ground bed rock. Amount of dead and
Soil Characteristics
Soil Characteristics
2.
2.
Mineral Content
Mineral Content
- Varies with precipitation because
Soil Characteristics
Soil Characteristics
3. Soil Texture (pg. 138)
3. Soil Texture (pg. 138)
-
-
refers to the mixture of fine particles
refers to the mixture of fine particles
(sand),
(sand),
very fine particles
very fine particles
(silt)
(silt)
and
and
extra fine particles
extra fine particles
(clay).
(clay).
The best
The best
texture for agriculture is an even
texture for agriculture is an even
mixture of each
Triangular graph of
Triangular graph of
Soil Texture
Soil Texture
Soil Profile
Soil Profile
(pg. 135-136)
(pg. 135-136)
O Horizon – “Organic”O Horizon – “Organic” HUMUS:HUMUS: dead or dead or
decaying plant matter,
decaying plant matter,
leaf litter and other
leaf litter and other
organic material
organic material lying lying on the surface
on the surface..
darkdark because of the because of the
decomposition.
decomposition.
decompose into decompose into
nutrients
nutrients that enrich the that enrich the soils.
Soil Profile
Soil Profile
A Horizon – “Topsoil”A Horizon – “Topsoil” darker than the lower darker than the lower
layers.
layers.
looseloose and and crumblycrumbly with with
varying amounts or
varying amounts or
organic matter.
organic matter.
most most productiveproductive layer of layer of
soil.
Soil Profile
Soil Profile
B Horizon – “Subsoil”B Horizon – “Subsoil” Light coloredLight colored, dense, , dense,
and
and low in organiclow in organic matter
matter..
materials materials leached from leached from
the topsoil
the topsoil accumulate accumulate here.
Soil Profile
Soil Profile
C Horizon – C Horizon –
“Weathered Parent
“Weathered Parent
Material”
Material”
transition areatransition area between between
soil and parent material.
soil and parent material.
Partially disintegratedPartially disintegrated
parent material.
parent material.
mineralmineral particles.particles.
Soil Formation/Advancement
Soil Formation/Advancement
Differentiate among the terms
Differentiate among the terms humushumus, , leachingleaching, , eluviation
eluviation and and capillary actioncapillary action..
HumusHumus is the accumulation of dead and decayed plant and animal is the accumulation of dead and decayed plant and animal
matter that makes up the
matter that makes up the organic nature of soilorganic nature of soil. Occurs where . Occurs where there is substantial
there is substantial plant and animalplant and animal growth. growth.
LeachingLeaching is the process where nutrients are washed down through is the process where nutrients are washed down through
the soil with the
the soil with the movement of water downmovement of water down the soil profile. Occurs the soil profile. Occurs where there is substantial rainfall.
where there is substantial rainfall.
EluviationEluviation is the lateral or is the lateral or downward movement of clay and downward movement of clay and other fine materials
other fine materials in suspension. Occurs where there is in suspension. Occurs where there is
substantial rainfall substantial rainfall..
Capillary actionCapillary action results when water molecules are attracted to clay results when water molecules are attracted to clay
particles and
particles and drawn upwarddrawn upward through the soil profile. Occurs where through the soil profile. Occurs where it is
it is substantially drysubstantially dry. .
Using the triangular graph of soil texture, which combination would make the poorest soil?
Using the triangular graph of soil texture, which condition would make the
Using the triangular graph of soil texture, which condition would make the
least favourable soil for farming?
least favourable soil for farming?
(A) 40% sand, 20% clay, 40% silt
(A) 40% sand, 20% clay, 40% silt (B) 30% sand, 10% clay, 60% silt(B) 30% sand, 10% clay, 60% silt (C) 25% sand, 60% clay, 15% silt
Using the triangular graph of soil texture, a soil texture combination of
Using the triangular graph of soil texture, a soil texture combination of
20% sand, 10% clay and 70% silt would constitute which soil type?
20% sand, 10% clay and 70% silt would constitute which soil type?
(A) sandy clay
(A) sandy clay (B) sandy loam(B) sandy loam (C) silty clay
Using the triangular graph of soil texture below, which combination would
Using the triangular graph of soil texture below, which combination would
make the most favourable soil for farming?
make the most favourable soil for farming?
(A) 10% sand, 15% clay, 75% silt
(A) 10% sand, 15% clay, 75% silt (B) 15% sand, 55% clay, 30% silt(B) 15% sand, 55% clay, 30% silt (C) 20% sand, 70% clay, 10% silt
Which process transports insoluble inorganic matter downward through the soil?
A) accumulation of humus B) capillary action
C) eluviation D) leaching
Which term refers to the process by which particles of insoluble inorganic matter are transported downward through the
soil?
(A) accumulation of humus (B) capillary action
Which refers to the upward movement of soluble material Which refers to the upward movement of soluble material
through the soil by water? through the soil by water?
(A) capillary action (A) capillary action (B) eluviation (B) eluviation (C) erosion (C) erosion (D) leaching (D) leaching
Which term refers to the process by which minerals and Which term refers to the process by which minerals and
dissolved salts are transported upward through the soil? dissolved salts are transported upward through the soil?
(A) accumulation of humus (A) accumulation of humus (B) capillary action
(B) capillary action (C) eluviation
3 types of Soil
3 types of Soil
pg. 136-137
pg. 136-137
1.
1.
Latosol
Latosol
2.
2.
Podzol
Podzol
3.
Latosol
Latosol
Typically in Typically in tropical rainforesttropical rainforest.. Very deep, very well drained, Very deep, very well drained,
homogeneous.
homogeneous.
InfertileInfertile due to…. due to….
- Highly
- Highly weatheredweathered and and
leached
leached soils because of high soils because of high amounts of
amounts of rainfallrainfall. .
They tend to have medium to They tend to have medium to
very high
Podzol
Podzol
Typically found in the Typically found in the Boreal Boreal
forest
forest..
Extends immediately Extends immediately south south
of the tundra
of the tundra regions of the Northern regions of the Northern Hemisphere.
Hemisphere.
Gray in color, ashy appearance.Gray in color, ashy appearance. Often Often severely leachedseverely leached and and
highly acidic.
highly acidic.
They are They are low in agricultural low in agricultural
value, forests
Chernozem
Chernozem
Rich in organic matter in the Rich in organic matter in the
form of
form of humushumus. .
True chernozem is True chernozem is black in black in
color.
color.
They are found in They are found in grasslandsgrasslands
which are
which are semi-aridsemi-arid……
Resulting in Resulting in less leachingless leaching and a and a
mineral rich soil
mineral rich soil. .
It is It is very suitable for very suitable for
agriculture
Threats to Soil
Threats to Soil
Environmental
Environmental
Factors:
Factors:
1. Temperature
1. Temperature
- affects
- affects humus humus (low temps. slow the (low temps. slow the decay
decay of organic matter).of organic matter).
2.
2.
Precipitation
Precipitation
- affects
- affects mineral contentmineral content (rain causes (rain causes minerals to be eluviated).
Threats to Soil
Threats to Soil
pg. 140-143
pg. 140-143
• Poor soil managementPoor soil management
- agricultural areas and
- agricultural areas and
grasslands.
grasslands.
• Urban ExpansionUrban Expansion
- settling in rich farmland
Threats to Soil
Threats to Soil
•
Desertification
Desertification
–
–
the spread of desert-like
the spread of desert-like
conditions in semi-arid environments
Threats to Soil
Threats to Soil
•
Flooding
Flooding
Reducing Soil Erosion
Reducing Soil Erosion
Pg. 142
Pg. 142
Soil Erosion can be reduced by:
Soil Erosion can be reduced by:
1. Strip cropping
1. Strip cropping
• Alternating strips of open-growing crops and close-growing crops.
Reducing Soil Erosion
Reducing Soil Erosion
2. Cover cropping
2. Cover cropping
• When soil is ready to use, this crop gets ploughed back into the soil, increasing the humus content. • Planting close-growing
Reducing Soil Erosion
Reducing Soil Erosion
3. Contour ploughing
3. Contour ploughing
• Respects the natural shape of the land and
forms
Reducing Soil Erosion
Reducing Soil Erosion
4. Terracing
4. Terracing
• Constructing steps or shelves in the sides of hills or sloping land to reduce water run-off and retain