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Soils

Soils form when processes of weathering reorganize the mineral content of the regolith into distinct horizon layers known as soil horizons. These horizons also gain organic material and stack vertically to form a soil profile.

AB
pedogenesisthe soil formation process
soil horizonthe horizontal layering formed during pedogenesis
soil profilethe vertical sequence of soil horizons
solumthe soil horizons known as the "true" soil
topsoilthe upper portion of the solum which contains humus
subsoilthe lower portion of the solum, lacking humus
humusdecayed and weathered plant debris
parent materialthe D-horizon, the presursor material of a soil profile
D-horizona soil profile's parent material
C-horizonpartially weathered parent material
B-horizonthe soil horizon gaining mineral material
hardpanwell-formed B-horizon that gains clay minerals
calichea well developed B-horizon that gains calcite
E-horizona soil horizon that loses minerals by eluviation
A-horizona soil horizon that loses minerals by chemical leaching
O-horizonuppermost soil horizon that has gains organic material
litterdecaying/weathering plant debris found in a forest
thatchdecaying/weathering plant debris found in a grassland
pedocalsoil type where calcite is found in the B-horizon
pedalfersoil type in which clays are found in the B-horizon
lateritesoil type in whcih oxides are found in the B-horizon


Holton Ag Ed

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