Soil Flashcards
Soil
the natural product formed from weathered rock by the action of climate and living organisms.
pedon
a three-dimension soil body large enough to study all physical and chemical properties and all horizons
soil profile
any vertical cut through a body of soil or pedon
horizons
apparent layers of soil
spodosol
is found in cool humid regions; coniferous forests
O
the “o” horizon is the surface layer, formed above the mineral layer and composed of fresh or partially decomposed organic material that has not mixed into mineral soil
A
the “A” horizon is the upper layer of mineral soil with a high content of organic matter
It is characterized by an accumulation of organic matter and the loss of some clay, inorganic minerals and soluble matter
E
the “e” horizon is the zone of maximum leaching
characterized by the development of granular, platelike, or crumblike structures
leaching
is the loss of minerals due to water
B
the “b” horizon is the zone of illuviation, or collection of leached material
it accumulates silicates, clay, iron, aluminum, and humus
C
the “c” horizon contains weathered material, either like or unlike the material from which the soil is presumed to have developed
this layer is little affected by soil formation
R
bedrock
Soil texture
determined by the proportion of particle size classes
-sand .05 to 2.0mm
-silt .002 to .05
-clay less than .002mm
which soil holds the most water
clay
loess
soil is transported by wind
alluvial
soil transported by streams
till
soil transported by ice
lacustrine
soil developed in a lake
marine
soil developed in an ocean
how is soil formed?
formation of soils begins with the weathering of rocks and their minerals
mechanical weathering
under the action of water, wind and temperature change the rock surface flakes and peels away
lichens and plants colonize the weathered material
plant roots penetrate and further break down the parent material
plant debris enables bacteria, fungi, earthworms, and others to colonize the area
animals like earthworms consume fresh material and leave partially decomposed products
compounds break down into inorganic products
humus remains
aluminosilicates
calcium, potassium, and sodium
humus
is chemically complex organic material. the formation of humus in soil is strongly influenced by the climate
Fossorial animals
rodents of the family Bathyergidae which made these mounds are the African mole rates and all are fossorial
All soil development processes will occur faster in
warm wet climates than in cool dry climates