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what are two influences of infiltration rate
water{ porosity and permealbility)
what are the four primary processes on soil horizonation
transformation, translocation, additions, losses
transformations in soil horizonation
-chemical/physical weathering
- the breakdown of stuff within the soil column profile
- formation of peds
translocation in soil horizonation
moves within soil profile
additions in soil horzonation
new stuff coming into soil profile from the outside
losses in soil horzonation
leaving soil
Three components of total water potential
matric potential( suction)
gravitational potential( gravity)
osmotic potential (degree of movement)
what mineral group has the greatest shrink swell capacity
phyllosilicates
least mobile water
negatives
Which horizon is the zone of accumulation
B horizon
e horizon
-lighter in color
-higher concentration of coarse particles
-associated with acidic soils
The b horizon
shows little evidence of original parent material
must have subhorizon designation
high in minerals( inorganic)
elluvial
stuff leaves
illuvial
accumulations