Soil Formation and Morphology Basics - University of Floridasoillab.ifas.ufl.edu/SOS 3022/Lectures...
Transcript of Soil Formation and Morphology Basics - University of Floridasoillab.ifas.ufl.edu/SOS 3022/Lectures...
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Soil Formation and Morphology
Basics
AdditionsLossesTranslocationsTransformations
Processes
Pedogenesis:
The process of soil formation as the resultof the combination of soil forming factorsleading to addition, loss, transformation and translocation of materials
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Soil Forming Factors
ClimateOrganisms
ReliefParent Material
Time
Soil Forming Factors
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ClimateClimate involves both local (microclimatic) and global (macroclimatic) considerations. The key components of climate in soil formation are moisture and temperature.
Temperature speeds reactionsWater promotes translocation
Organisms
The soil and the organisms living on and in it comprise an ecosystem. The active components of the soil ecosystem are the vegetation, fauna, including microorganisms, and man.
Grassland Forest Pineland
Organisms: Vegetation
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Organisms: Meso-/Macrofauna
EarthwormsTermites
AntsBeetles
ArthropodsRabbitsMoles
Organisms: microorganisms
BacteriaVirusAlgaeFungi
Actinomycetesprotozoa
Relief/Topography
solar radiation slope direction aspect overland and subsurface flow, velocity and runoff rate gradient slope climate, vegetation type, potential energy elevation Altitude
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Parent Material
in situ weathering of consolidated rock
superficial deposits, which may have been transported by ice, water, wind or gravity
organic sediments
Time acts on soil formation in two ways:
The extent of a pedogenetic reaction depends on the time for which it has operated.
The value of a soil forming factor may change with time (e.g. climatic change, new parent material).
Time
Soil as a Natural Body
Parent Material
Bedrock
Additions
Losses
Translocations
Transformations
Differentiation
Bedrock
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Soil Horizons
Roughly parallel layers in the soil with varying composition and properties
Soil Profile
Soil Profile – 2D representation of a vertical section of soil from the surface to its deepest layers or horizons.
The Essentials of Soils
Soil Horizons
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Soil Horizons
Roughly parallel layers in the soil with varying composition and properties
Definitions:
Eluviation: the loss of materials including clays,organic matter, oxides of Fe and Al.
Illuviation: accumulation of materials resultingfrom eluvial horizons.
Master HorizonsMaster Horizons
A horizon [
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A horizon• topsoil/plow layer.• Accumulates organic
material• Often darker than soil
below.• high in plant roots,
biotic activity• Zone of gas and water
exchange
The A HorizonThe A Horizon
A horizon
Master HorizonsMaster Horizons
A horizon E horizon
- Zone of EEluviation
The E horizonThe E horizon
E horizon
A horizon
Elluviation = exitIlluviation = into
•Organic matter•Clay•Carbonates•Fe, Al oxides•color
(Illuvial)
(Elluvial)
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Master HorizonsMaster Horizons
A horizon
B horizon[E horizon
- Accumulates material lost from above, or forms in place.(translocation, transformation)
- Zone of Illuviation (translocation).
- Maximum expression of soil development.
• clays, O.M., Fe/Al• soil structure• Strong color development• Potentially high reactivity
B horizon
The B HorizonThe B Horizon
Master HorizonsMaster Horizons
A horizon
B horizon
C horizon [
E horizon
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-Weakly altered by soil forming processes.
-Closely resembles parent material C horizon
The C horizonThe C horizon
Master HorizonsMaster Horizons
A horizon
B horizon
C horizon
E horizon
R HorizonFlorida?
R horizon
The R HorizonThe R Horizon
limestone
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O Horizon
• Surface Horizon• Organic horizon
Very high in organic matter
Usually dark-colored
• Often called peat, muck
• Some are very fertile, valuable
• In some countries, O horizon used as fuel.
The O HorizonThe O Horizon
Master HorizonsMaster Horizons
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