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igneous rock
form from magma
sedimentary rock
form from sediments are compressed over a long period of time
metamorphic rock
transformed rocks by intense heat, pressure
physical weathering
breakdown of rocks/minerals from water/wind/temperature variations
chemical weathering
breakdown of rocks/minerals by chemical reactions. ex: reactions w water, oxygen, etc…
what can dissolve rock?
acid rain
erosion
process of natural forces like water, wind, and ice breaking down and moving rocks and soil from one location to another
how does soil form?
Climate
Organisms
land shape
Parent Material (the original rock)
Time
benefits of soil
filters water
help plant growth
Habitat for a variety of organisms
Breaks down organic material & recycles nutrients
soil horizons in order to (from top to bottom)
O
A
E
B
C
R
O HORIZON
organic matter (humus)
A HORIZON
topsoil (rich in nutrients and organic matter, that is vital for supporting plant growth)
E HORIZON
Leaching: process where a substance, such as a mineral or pollutant, is dissolved or washed away
B HORIZON
subsoil:mineral material with very little organic matter
C HORIZON
weathered rock: least-weathered soil horizon
R HORIZON
bedrock
soil erosion
from contact against wind and water, as well as increases in human activity, affects on topsoil
How is soil productivity characterized?
water holding capacity
nutrient availability
porosity
the air space of soil
permeability
ability of water to move through the soil
most permeable to least permeable
sand, silt, clay
cation exchange capacity (CEC)
ability of a particular soil to adsorb and release cations (+ charged ionsnutrients and ions commonly identified in soils)
nutrients and ions commonly identified in soils
Nitrogen
Phosphorus
Potassium
Calcium
base saturation
proportion of soil bases to soil acids – too many acids can be harmful to plant nutrition.
biological soil properties
fungi, bacteria, and protozoans (single-celled eukaryotes)