23 Flashcards
(12 cards)
factors of soil formation (5 factors)
parent material - bedrock/deposits from which soil develops, residual vs. transported
climate - precipitation,evapotrasnpiration determine soil moisture, temperature and moisture influence chemical reaction rate
organisms - bacteria and fungi decompose organisms and nutrients , larger organisms like earthworms or terminates mix aerate the soil
time - slow process disturbance can take centuries to repair
topography - slope and aspect direction affect moisture and temperature , soil erosion on slopes
aspect - downslope direction measured in degrees
active energy supplying factors
climate and organisms
passive energy receiving factors
topography, parent material and time, cannot form soil without active factors
soil profile horizons
horizon - distinct layers of soil that make up the soil profile differing in color, texture and organic content
common horizon - LFH uppermost layer of exclusively organic matter
a - upper layer of minerals and organics
b - mineral layer receives material from above layers
c- actively weathering parent material
soil components
Mixture of organic matter and weathered minerals and rocks with variable proportions of air and water, can have distinct layering an dits development is influences by climate and living organisms, supports plant growth
water, air, minerals and organic material
soil texture
particles size - sand (2-0.05mm), silt (0.05-0.002mm) clay <0.002mm)
determines propensity, permeability and field capacity
field capacity
ability to hold water against gravity
soil structure- 4 basic structures
PED naturally occurring clumps of soil
4 basic structures
platy , prismatic, blocky angular and spheroidal granular
soil stability
affected by soil texture, parent material and amount of organic material
Soil water movement
influenced by soil texture, structure and pore size
sand - water moves quickly , silt and clay - more slowly
water moves in any direction but gravity move sit downward, bedrock may aug eat to move laterally
capillary moves water n unsaturated soils
gravity moves water in saturated soils
unsaturated vs saturated soil
Saturated conditions occur when all of the voids, spaces, and cracks are filled with water. Unsaturated conditions occur when the voids, spaces, and cracks between soil, sand, gravel, or rock are filled with a combination of air and water.
Canadian soil orders
10 orders in the Canadian system of soil classification
- considers the entire soil profile, specific to Canadian soils and based on soil properties and oil forming processes