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4 parts of soil
Minerals
Organic Matter
Water
Air
Functions of soil
Medium for plant growth
Water storage and purification
Serves as a habitat
Modifies the atmosphere
Soil storages
Organic matter
Organisms
Nutrients
Minerals
Air
Water
Transfers within soil
Biological mixing - redistribution of soil materials.
Translocation - soil forming materials move in the profile
Leaching - water moving nutrients thru the soil profile
Salinization - salt content moving into the soil profile
Translocation
Movement of soil particles in suspension
Leaching
Minerals dissolving in water moved in soil
Evaporation
Drawing soil out of water
Decomposition
Breaking down organic matter into the soil
Weathering
Breakdown of parent/rock material
Salinization
Water evaporates and salt content is left behind
What are the layers of the Soil Profile
Made up of 5 vertical layers
O
A
B
C
R
O layer
Organic layer with dead organic matter (DOM)
A layer
Top soil/mineral layer
High organic matter with high biological activity
Zone of leaching
B layer
Subsoil layer
Plant roots are most often found here
C layer
Decomposed parent material and weathered rock
R layer
Parent material layer (can be bedrock or other forms)
Soil texture
Based on the ratio of clay sand and soil
Figured out via the soil triangle
Sandy soil properties
Large particles
Good drainage but poor water retention
Limited biota
Poor GPP/NPP
Poor organic matter retention
Clay soil properties
Small particles (low porosity)
Good water retention but poor drainage
Limited biota
Poor GPP/NPP
Poor organic matter retention for plants
Loam soil properties
Medium particles
Good water retention and drainage
Good GPP/NPP
Good organic matter retention
Good biota
Best for plant growth
What is the soil structure
Good soil is crumbly
Poor soil is coarse with no structure
Porosity
Measure of Air spaces in the soil
Permiability
The ability for water to flow through the soil
Soil as a dynamic ecosystem
Soil has both abiotic and biotic components that work together