Glossary

 

0-9   A B C D E F G H I J K L M N O P Q R S T U V W X Y Z

Ground water

That portion of the water below the surface of the ground at a pressure equal to, or greater than, that of the atmosphere. See also water table.


Gully

Channel resulting from erosion and caused by the concentrated but intermittent flow of water during and immediately following heavy rainfall; gullies are deep enough (usually >0.5 m) to interfere with, but not obliterated by, normal tillage operations.


Horizon

Single layer in soil profile with similar properties or material but which differs at least in one property, e.g. colour or texture from adjacent horizons above or below in the profile; diagnostic horizon: Dominant soil property or material defines name of horizon, e.g. gypsic horizon having distinct calcium sulfate (gypsum: CaSO4) enrichment; genetic horizon depending on the type of pedogenesis.


Humification

Process whereby the carbon of organic residues is transformed and converted to humic substances through biochemical and abiotic processes.


Humus

Organic compounds in soil, exclusive of undecayed plant and animal tissues, their partial decomposition products, and the soil biomass; a term often used synonymously with soil organic matter, its structure is amorphous, specific weight is low and surface area high. Humus is important for soil fertility, and helps to bind soil particles and aggregates together.


Hydromorphic soils

Formed under conditions of poor drainage in marshes, swamps, seepage areas or flats.


Infiltration

The downward movement of water into the soil. lt is largely governed by the structural condition of the soil, the nature of the soil surface including presence of vegetation, and the antecedent moisture content of the soil.


Ion

Electrically charged atom or group of atoms.


Karst

Topography with sinkholes, caves and underground drainage that is formed in limestone, gypsum or other rocks by dissolution (dissolving).


Landslide

A general term for a mass movement landform and a process characterized by moderately rapid to rapid (greater than 30 cm per year) downslope transport by means of gravitational stresses, of a mass of rock and regolith that may or may not be water saturated.



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