Exam 1 Flashcards
Define: soil
A dynamic natural body composed of minerals, organic materials, and living forms
Define rock
Mixtures of minerals
Define igneous rock
Rocks cooled from molten materials
Define sedimentary rock
Formed from the deposition of sediments followed by high pressure and a cementing agent
Define metamorphic rock
Formed from either igneous or sedimentary rocks through the action of intensive heat and pressure
Define physical weathering
Destructive process caused by atmospheric agents that breakdown rocks without change to e physical identity
Define chemical weathering
Weathering caused by atmospheric agents that change the chemical composition of rocks and minerals
O horizon
Organic horizon that forms above the mineral soil
A horizon
Mineral soil horizon, high biological activity . Zone of rapid mineral weathering and leaching
E horizon
Horizon in which large amounts of clay and iron have been leached or removed by water
Zone of eluviation
B horizon
Horizon that receives material leached from E and A horizons
Zone of illuviation
Define elluviation
Removal, exit, maximum leaching
Define illuviation
Deposition of materials eluviated from upper horizons
C horizon
Horizon of unconsolidated material that may or may not be parent material of the soil
R horizon
Consolidated hard rock
What are the five soil forming factors
Parent material, climate, relief, biota, time
Define colluvial
Transported by gravity
Define alluvial
Transported by stream
Define marine
Transported by ocean
Define lacustrine
Transported by lake
Define glacial
Transported with glacier
Define eolian
Transported by wind
What are the four soil forming processes
Additions, losses, transformations, and translocation
Entisols
Simple soils, no diagnostic horizon
Inceptisols
Soils with minimum development, little or no subsoil clay accumulation
Mollisol
Thick, soft, dark mineral soil of grasslands
Alfisol
Subsoil accumulation of clay, not strongly leached. Under deciduous forest or savanna vegetation
Spodosols
Subsoil accumulation of iron, organic matter, and aluminum, typically under coniferous forest vegetation
Ultisols
Subsoil accumulation of clay, highly leached soil
Oxisol
Extreme leaching, only iron and aluminum oxides and quartz are left
Gelisol
Soils with dark organic surface layer and mineral layers underlaid by permafrost
Aridisols
Soils of hot, dry,regions
Vertisols
Clayey soils with a high shrink swell potential. Distinct wet and dry periods throughout the year
Histosols
Dark organic soil, little mineral matter
Andisol
Mineral soil formed on volcanic ash parent material
Mollic
Has to be determined in lab. High base saturation
DSH
Umbric
Less than 50% base saturation
DSH
Melanic
Only found where volcanic eruptions occur. Black
DSH
Histic
Swampy soils formed under very wet conditions, lots of organic material
DSH
Ochric
Default. Fails to meet definition of other epipedons
DSH
Argillic
Semi arid and wetter.
Bt horizon associated with this
DSSH
Oxic
Tropics
Highly weathered, cation exchange is critical to plant nutrition.
DSSH
Spodic
Cool humid
Illuvial organic carbon, needs to be leached from the A or E horisons
DSSH
Albic
Basically and E horizon
Eluvial horizon free of clay, iron and aluminum oxides
DSSH
Cambic
Fails to meet definition of other diagnostic horizons
DSSH
Genetic horizon
Qualitative, descriptive, field descriptions
Diagnostic horizon
Quantitatively defined, used for taxonomy
Horizon a
Highly decomposed organic material
Associated with O horizon
Horizon b
Buried
Does not require pedogenesis
Horizon e
Intermediate decomposed organic material
Horizon f
Frozen
Horizon g
Gley: blue grey color, reduced Fe
In water logged soils
Horizon h
Illuvial accumulation of humus or organic matter
Horizon k
Illuvial accumulation of lime CaCO3
Horizon m
Cemented
Horizon p
Plowed
Horizon s
Illuvial accumulation of Fe and Al oxides
Associated with B
Horizon t
Illuvial accumulation of clay
Horizon w
Weak development
Associated with B
Hydrolysis
Breaking down of a water molecule during the reaction producing either H+ or OH-
Hydration
The addition of water
Water does not disassociate
Carbonation
Acid base reaction, with carbonic acid or some acid being a source of protons
Oxidation-reduction
Reactions involving the exchange of electrons or change in oxidation state of an element
Dissolution
Reactions in which minerals dissolve in water
Complexation or chelation
Breakdown of a mineral is accelerated by an organic molecule acting as a chelate
Composition breakdown of soil
45% mineral, 25% water, 25% air, 5% organic matter