Test 2 Flashcards
Weathering
The physical breakdown and chemical alteration of rock at earths surface
Mass Wasting
The transfer of rock and soil down slope under the influence of gravity
Erosion
the physical removal of material by physical agents i.e. water, wind, ice
Mechanical weathering
Physical forces breaking down rocks
Frost Wedging
caused by the expansion of water when it freezes in between cracks, repeated freezing and thawing causes the expansion
Unloading (sheeting)
reduction in pressure from erosion allowing rocks to expand, causing outer layers of rocks to crack, this can create an exfoliation dome
Biological Activity
Plants wedging in between cracks and spreading them apart, plants can also create acids eroding the rocks
Chemical Weathering
Chemically transforming rock into one or more new compounds
Hydrolysis
Where hydrogen ions replace other cations in minerals, causing minerals to breakdown and change into other minerals, ex: feldspar to clay
Dissolution
where solids are completely dissolved into ions by acids
oxidation
reaction where the elements loses electrons, this can cause rust on iron materials
Soil contains
A combination of minerals, organic material, water, and air 50/50
Differential weathering
different minerals weather at different rates
Parent Material
Source of weather material that soils develop from residual soils, transported soils
Rates of weathering is controlled by?
Mineral Composition
Climate
Particle size
Residual Soils
Soil developed from bedrock
Transported soils
soils developed on unconsolidated sediments
Formation of Soils is the product of?
Parent Material
Time
Climate
Plants and animals
topography
Time
The amount of time that weathering processes have been operating
Climate
Most control on soil, temperature and wetness of soil
Plants and animals
Amount of organic activity effecting the soil
topography
soil develops poorly on slopes
Soil profiles
O Horizon
A Horizon
E Horizon
B Horizon
C Horizon
Bedrock
O Horizon
Mostly organic materials, upper horizon is plant litter lower is decayed organic material
A Horizon
Largely organic material, lots of biological activity
E Horizon
Mostly Minerals
Eluviation
Leaching
Eluviation
As water percolates through the solid
Leaching
Water dissolves soluble materials carrying it downward
B horizon
Subsoil, materials removed from the E horizon is deposited into the B horizon
C Horizon
Partially altered parent material considered regolith not counted as true soil
Bedrock
Unweathered Parent Material
Sedimentary Rock sources
Weathering
Transportation
Sedimentation(Diagenesis)
Deposition
Sediment
Material derived from the mechanical and chemical weathering of rocks which is deposited on the surface of the earth
Sedimentary Rocks
Rocks formed from the calcification of sediments. They are the end products of mechanical and chemical weathering processes