what is soil
natural bodies having depth and surface area
products of destructive/synthetic forces
alive, internally structure into layers/horizons
soils processes (pedogenic processes)
inputs
losses
translocations
transformations
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what is soil
natural bodies having depth and surface area
products of destructive/synthetic forces
alive, internally structure into layers/horizons
soils processes (pedogenic processes)
inputs
losses
translocations
transformations
soil inputs
enrichments, mainly from above
soil losses
removals
types of soil losses
erosion
removal of solutes to groundwater
plant uptake
leaching
minerals trickling down thru soil via force of gravity
translocation
vertical mvmt of materials in soil
types of translocation
eluviation and leaching
illuviation
eluviation n leaching
when water moves materials down and out of upper of soil
illuviation
when leached materials from uppermost soil recrystallise in lower part of soil
transformation
decomposition of minerals n organic matter into other forms
soil profile
vertical organisation of soil into layers visible in cross section
layers/horizons
horizon
layer that’s homogeneous within
reflects processes of decomposition, weathering, translocation
organic horizons
O, L, F, H
mineral horizons
A, B ,C
A horizon
at/near surface
organic matter accumulates
materials removed in percolating rainwater
B horizon
materials added via illuviation
prismatic columnar structures
stainings or coatings
distinct in colour bc of enrichment
C horizons
comparatively unaffected by pedogenic processes
soil colour
tells about composition and chemistry
black soil
organic content
high fertility
white/pale soil
silica n aluminum oxides
reds/yellow
iron oxides n minerals
soil forming factors
organisms
topography
time
climate
parent material
climate
determines speed and intensity of:
mineral weathering, organic matter decomposition
parent material
underlying geologic material that soil forms on
determines:
composition, structure, texture
acidity, nutrients
two major types of parent materials
consolidated: residual
unconsolidated: transported