Terrestrial environment Flashcards
soil
Loose outer material of earth’s surace
Soil layers
O horizon
A horizon
B horizon
C horizon
O horizon
At the surface, composed of undecomposed plant material
A horizon
Most M growth, rich in organic material and nutrients
Plant roots release nutrients in exchange for ecosystem function
B horizon
subsoil where organic material leached from A gather, little M activity
C horizon
base that is directly above bedrock and forms from bedrock
No O2 and all microbes strictly chemolithotrophs
Soil groups
Mineral soil
organic soil
Mineral soil
Derived from rock weatherig and other inorganic material
Organic soil
Derived from sedimentation in bogs and marshes
soil composition
40% inorganic mineral
5% organic matter
50% air and water
5% M and macro organisms
Soil formation
Formed by interdependant physical, chemical and biological processes
-CO2 is formed by respiring organisms that form Carbonic acid that breaks down rock
-Physical processes such as freezing and thawing break apart rocks, allowing plant roots to penetrate and form an expanded rhizosphere
Rhizosphere
Area around plant roots where plants secrete sugars and other compounds, is rich in organic matter and microbial life
water availibility
It is variable and dependant on rainfall, plant coverage, drainage and soil composition
Soil solution
Soil water has many dissolved materials
soil and water
Well-drained soils have O2 availibility while waterlogged soils are typically anoxic, with O2 being consumed by soil M