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Desiccation
removal or loss of moisture
Water balance
maintaining balance of water between organisms and their surroundings environment
Gravitational forces
the need to remain erect gravitational forces in terrestial environments
Cellulose and Lignin
the kelp cannot support its own weight under the forces of gravity
80%
The percentage of its biomass to supportive and conductive tissues
Variability
temperature that is higher in air than water
Solar Radiation
the amount if light at any depth in the canopy is affected by the number of leaves above
Soil
medium for plants and controls the fate of water
SoiL
stratum below the vegetation and above hard rock
Mechanical Weathering
water, wind, and temperature without influencing their composition
Chemical Weathering
H2O, O2 and acids fom soil organisms and organic matter
5 factors of Chemical Weathering
Parent Material
Climate
Biotic Factors
Topography
Time
Parent Material
From which soil develops
Parent MateriaL
underlying bedrock; glacial deposits; sand and wind gravity sediments
Climate, temp, precipitation, and wind
responsible for breaking down parent material
Leaching
movement of solutes through the soil and movements of weathered materials
Topography
influences the weathering process
Topography Time
Accumulation
Decomposition
Mineralization of Organic Material
Loss of minerals from the upper surface
Downward movement of minerals
Color
can indicate the chemical composition of the rocks and minerals from which the soil was formed
Texture
partly inherited from parent material and partly a result of the soil-forming process
TexturE
affects oire space in the soil and movement of air and water
Depth
organic matter added to the soil
Soil Horizons
Organic
Topsoil
Eluviation Layer
Subsoil
Parent Rock
Bedrock
Topsoil
Mineral with humus
Eluviation Layer
Leached minerals and organic matter
Subsoil
deposited materials and metal salts
Parent Rock
Partly weathered rock
Bedrock
unweathered parent rock