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21 Cards in this Set

  • Front
  • Back
swidden agriculture
slash and burn
soil degradation
negative changes in soil due to
Deforestation
Overgrazing
Overcultivation
detritivore
energy flows through these organisms, they feed on detritus-dead or decaying matter; Detritivores quickly break down organic matter and recycle nutrients back to the soil; Detritus nibbled by countless bacteria, fungi, protists
These in turn help feed the larger detritivores - insects, pill bugs, earthworms, millipedes.

They are important because they:
Break up detritus into smaller particles for bacteria and fungi to decompose
Constantly aerate the soil as they tunnel through it
humus
leftover small organic particles that make up the O horizon
soil structure
the physical characteristics of the soil (ex. particle size, pore spaces, how the grains clump together etc.)
soil horizons
a specific layer in the soil which differs from the layers above it and below it
soil profile
all the layers visible when you take a section through the soil (the sequence of layers)
O horizon
humus
A horizon
topsoil, still contains some humus
top soil
A horizon; important protective layer of all soil-Soil loses most of its organic content and nutrients when humus is removed and underlying soil can no longer hold water; acts like a sponge and holds water long enough for plants to be hydrated
E horizon
below the A horizon, zone of leaching
B horizon
subsoil; either red or yellow due to oxides of minerals in the ground like iron or aluminum
subsoil
B horizon; either red or yellow due to oxides of minerals in the ground like iron or aluminum
C horizon
Basic mineral soil, no organic matter
parent material
c horizon; starting point in the formation of new soil
Forms by:
Volcanic deposition
Glacial deposition
Natural weathering of bedrock
no-till farming
relies on special plowing disks - one set opens the soil, seed is dropped in, last set zips the soil back up
desertification
healthy soils are turned into sterile soils, with no organic content, no soil structure
salinization
Increase in soil salinity, caused by irrigated agriculture;When fresh water evaporates, leaves minute amount of salt behind
Salt gradually builds up in irrigated fields, eventually can no longer grow crops
Dust Bowl
Higher grain prices during World War I convinced farmers that wheat was more lucrative than cattle
Plowed up healthy rangeland to plant wheat
Just in time for a prolonged drought
windbreaks
we planted trees to act as windbreaks to erosion of the topsoil
contour plowing
helped hold remaining topsoil in place