Transcript PowerPoint

Sifting through
the Soil :
Determining London’s Local
Soils
Soil
Soil is like a skin over the earth’s
crust, and is essential in enhancing
life on earth.
There are six main contributors to
soil:
-
Parent rocks and sediments
Climate
Landscape
Vegetation and living creatures
Time
Man
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Parent Material
• Gradually rocks break down into smaller pieces under the effects of
rainfall, snow, freeze and thaw cycles.
• The parent rock or sediment is the main factor responsible for the
texture of the soil and is also important in determining the pH of
the soil and how rich it is in nutrients.
• For example
– Shale clay
– Sandstone sand
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Climate
• The two main climatic influences:
– Temperatures increase the rate at which the breakdown of
the underlying rock takes place and also the release of
nutrients into the soil.
– Rainfall and snowmelt break down rock to form soil and
distribute soil nutrients.
• In hot, wet climates such as the tropics soils tend to be deep.
• In cold, artic areas the soils tend to be thin and poorly developed.
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Landscape
• Landscapes generally affect the depth or thickness of soils.
• Steep slopes often have shallow soils because soil is easily
washed down the hillsides into the valleys below.
• Flat land such as that in valley bottoms, flood plains, or low
lying plains have deeper soils.
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Vegetation
• Vegetation aids in creating soils as acids released by the roots of some
plants act to breakdown the rock on which soil is forming.
• Once the rocks have been broken down into smaller materials, the
vegetation is able to supply its dying remains as a source of nutrients to
help enhance the soil while adding organic matter.
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Soil Organisms
• Organisms begin to set up their homes in the soil from the
moment it begins to form.
• The main role of organisms in soil is to recycle the organic
matter and release nutrients in what is called “castes.”
• Organisms also create pores within the soil to allow air
circulation and add architecture to the soil.
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Time
• It takes a long time for soils to develop from rock and existing
sediments.
• The oldest soils are currently located in South Africa.
Elsewhere, soil is relatively young due to periods of geologic
disturbance.
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Humans
• Farmers have cultivated the land for centuries and in most
cases the soil has been managed well.
• In some parts of the world however; soils have been
damaged. For example:
– Cutting down parts of the tropical rainforest, decreasing organic
material
– Cultivation of crops on steep slopes creating erosion
– Deterioration of natural nutrient content, as the focus is largely on
fertilizers in commercial agriculture
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Quick Quiz!
• Answer the following on a piece of paper:
1.
2.
3.
4.
5.
6.
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Name all of the soil forming factors.
What does parent material provide?
How does climate influence soil formation?
Why is vegetation important in soil formation?
How do humans influence soil?
Other than an earthworm, name a soil organism.
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Soil Horizons
• A soil horizon is
approximately parallel to the
surface, having distinct
characteristics produced by
soil forming processes.
• Soil horizons are used to
classify the soil and make
interpretations about its
quality and stability.
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O-Horizon
• Organic layers of decaying plant and animal tissues.
• Typically within a woodland area there are three
distinct organic layers:
1. Leaves, needles and twigs (Oi)
2. Partially decomposed layer (Oe)
3. Dark layer of decomposed humus (Oa)
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A-Horizon
• A mineral horizon at or near the surface in which an
accumulation of humified organic matter is mixed with
mineral material.
• This horizon exhibits obliteration of all or much of the original
rock structure.
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E-Horizons
• A horizon in the upper part of
the soil. It is light coloured and
leached.
• The light colour is due to the
natural colour of the dominant
quartz and sand grains.
• The main feature is the loss of
silicate clay, iron, or aluminum,
leaving a concentration of sand
and silt particles.
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B- Horizons
(Subsoil)
• Horizons which are dominated by the obliteration of all or
much of the original rock structure.
• Contain illuvial concentrations of clay, iron, aluminum, humus,
gypsum, silica, and other minerals.
• Well drained soils have the brightest colour development
within the B-Horizons.
• Usually 2-3 feet below the surface.
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C-Horizons
(Substratum)
• A horizon which excludes hard bedrock.
• Hardly affected by the soil forming processes and have
changed very little since the time they were deposited.
• This layer lacks colour, however, geologic layering or strata is
often present.
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R-Horizons
• Horizons containing
hard bedrock.
• Typically requires
large machinery to
break through.
• Common R-Horizon
materials consist of
granite, basalt,
quartzite, limestone
and sandstone.
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Activity
In groups of four, choose a local soil to research
during class. Using the internet, determine why
the soils are located where they are in London.
Assess the benefits and issues associated with
each type of soil. Present your findings to the
class.
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Soil Types
• There are various different types of soil in
London, all created from the eight factors
mentioned above:
•
•
•
•
•
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Alluvium
Clay
Organics
Sand-Gravel
Silt
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ACTIVITY
Characterizing Your Soil
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Plot the Soil Type
• Based on classmates
results and presentations
of their soil type, fill in the
map of London with the O
and A soil horizons found.
Be sure to pin point where
each sample came from.
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What did you think about the lesson?
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What did you learn?
What did you love?
What do you want to learn more about?
What was boring?
How would you make the lesson better?
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