Chapter 2 - Soil origin and classification Flashcards
Igneous Rock
Solidified, molten lava; slow to break down
Sedimentary Rock
Formed from particles that settle, such as from minerals deposited from suspension in water
Metamorphic Rock
Formed from other rocks, such as continental plates moving and other pressures; tends to create stronger rock (granite, slate)
Weathering
Chemical and physical breakdown and/or synthesis of particles
Biogeochemical Weathering
Weathering by
- water
- oxygen
- biological agents
- acids and bases (H+, OH-) produced by micro org and plant roots
Factors influencing soil formation
1) Parent material
2) Climate
3) Biota
4) Topography
5) Time
Soil formation - parent material
Formed in place or moved to a new location
Residual Parent Material
Developed in place from underlying rock
Weathered and breaks apart
Colluvial Materials
Rock fragments that are above a deposit of soil
Rocks carried down a slope - gravity
Alluvial Materials
Moved by water Flood plains, delta deposits, coastal sediment Ice movement (glaciers)
Eolian Movement
Wind
One of the biggest movers of soil
Builds dunes and loess
Volcanic ash
Loess
Silt-sized particles moved by wind
Organic deposits - examples/attributes
Marshes, swamps
Slow degradation
Creates peat
Soil formation - climate: factors
Precipitation/moisture (including humidity) - needed for most chemical reactions Seasonal rains Evaporation Leaching Hydrolysis Temperature
Hydrolysis chemical reaction
Addition of H2O to make a reaction occur to break down material
Ex: starch (carbohydrates) + H2O -> breaks down into glucose(s)