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Soil texture
the relative proportions of different sized grains of sand, silt, and clay in soil
Soil organic matter
plant, animal, and microbial residues in various states in decomposition
Soil Horizon O
Horizon containing a high percentage of soil organic matter
Soil A Horizon
horizon darkened by the accumulation of organic matter
Soil E horizon
horizon formed through the removal (eluviation) of clays, organic matter, iron, or aluminum
Soil B Horizon
broad class used for subsurface horizons that have been transformed substantially by a soil formation process (color and structure)
Soil C Horizon
A horizon minimally affected or unaffected by the soil formation process
Soil R Horizon
bedrock
Salinization
A build up of salts in soils to the point that they destroy the soil's physical and chemical properties and plants are not able to take up water due to the high salt concentration; often associated with improper irrigation
plant available water
the portion of water in the soil that plants can actually absorb and use for growth
percolation
the downward movement of water through soil and porous rock layers under the influence of gravity
field capacity
the amount of water a soil holds after excess water has drained away
permanent wilting point
the soil moisture level at which plants can no longer extract water, even though some water is still present in the soil
salinity
a measure of the dissolved matter within seawater
density
the weight of a substance for a specific volume
temperature
a physical property representing the average kinetic energy of a parcel of water
absolute salinity
the modern measure of salinity in a parcel of water
subsurface lateral flow
the movement of water horizontally through the soil profile typically in high porosity soil
macropores
larger pores into the lower soil profiles (gopher holes, plant roots, earthworm holes)
micropores
smaller pores into the lower soil profiles (natural pores)
vertical percolation
runoff
evapotranspiration
Aquic
Udic
Ustic
Xeric
Aridic
mollisols
water potential