unit 3 Flashcards
top surface litter layer, decomposed leaves and organic matter, normally brown or black, rich in bacteria, fungi, insects and earthworms
o horizon
topsoil layer, humus and minerals. roots are in this area, also rich in living organisms, if dark brown or black: rich in nitrogen and organic materials, ***if gray/yellow/red: low in organic material, bad for crops
a horizon
subsoil layer, mostly inorganic materials, clay particles, receives material from A horizon through illuviation, may be colored by iron oxides (red), aluminum oxides (yellow), or white due to calcium carbonate, leaching, lots of humus
b horizon
weathered parent material, consists of broken fragments of parent rock, caco3 and mgco3 accumulates here forming a hard impenetrable layer
c horizon
breaks rocks into smaller pieces (water, machinery, wind, etc)
mechanical weathering
change mineral makeup of a rock, chemical reactions between minerals in the rock and the environment
chemical weathering
both mechanical/chemical in some ways, but always involves living organisms (ex: lichen secrete acids into rocks that break down its minerals)
biological weathering
diameter greater than 0.05 mm, high permeability, poor water capacity, poor nutrient capacity, good aeration, good workability, low porosity (cannot hold water)
sand
between 0.002 and 0.05 mm, medium levels of all characteristics
silt
less than 0.002 mm, low permeability, good h20 capacity, good nutrient capacity, poor aeration, poor workability, high porosity
clay
relatively equal portions of sand, silt, clay (ideal soil for farming)
loam
the degree to which soil resists pressure; important when considering how land should be managed
soil consistence
mass/volume, expresses how much soil weights per unit volume depending on amount of pore space and density of soil particles
bulk density
reduces permeability of soil to water and air, if soil is subjected to pressure, pore spaces can collapse, decreasing pore space
compaction
can help determine whether a piece of land should be planted w/ grass, trees, etc., or if it can be used for homes, lots, landfills, septic tanks, etc.
slope of the land
presence of gullies, examination of surfaces of soil
signs of erosion
character and chem. composition directly impacts soil chemistry and properties (ex: coarse grained parent material=coarse grained texture soil)
parent material
content of soil (clay, silt, sand)
soil texture
how particles are organized/clumped
soil structure
water holding capacity, very porous soil has more spaces, and can hold more water
porosity
rate of percolation, related to porosity
permebility
ability of air to move through soil
aeration
magma cools and solidifies, bulk of crust (ex: granite)
igneous rock
sediments “cement” under pressure, weathering forms sediment (ex: contains fossils)
sedimentary rock