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What is a soil profile?
Vertical arrangement of soil horizons
What is a soil pedon?
Smallest unit of soil that can be studied that contains all soil properties
What is a soil horizon?
Layers formed over time with soil development and as a product of soil forming factors and processes
What are the 6 master horizons?
Most common horizons present in developed soils:
O - Organic materials
A - Topsoil
E - Loss of material; eluviated zone
B - Subsoil; accumulation zone
C - Weathered rock
R - Solid rock
What are the differences between an O and A horizon?
O = organic horizon vs. A = mineral horizon with decomposed OM
What processes form E horizons?
Losses (eluviation of clays)
What processes form B horizons?
Additions and translocations (illuviation of nutrients)
How are E and B horizons different?
E = mineral horizon leached (eluviated) of clays, OM, Fe, Al, and other mobile constituents
B = mineral horizon of alteration or accumulation of materials from overlaying horizons
What is the main difference between a C and R horizon?
Both dominated by parent material, but C is the layer of parent material (not bedrock), little affected by soil formation vs. R is hard bedrock
What is a W horizon?
Water (frozen or liquid)
What is a V horizon?
dominated by vesicular pores
What is a M horizon?
human-made layer (i.e. asphalt)
What is a L horizon?
biologically produced material deposited in water
horizon subordinate distinctions: p
plowed
horizon subordinate distinctions: w
weak or change in soil structure
horizon subordinate distinctions: g
gleying - prolonged soil-water saturation —> Fe reduction and gray color
horizon subordinate distinctions: k
accumulation of CaCO3
horizon subordinate distinctions: s
illuvial accumulation of Fe and Al oxides with OM
horizon subordinate distinctions: f
frozen
horizon subordinate distinctions: l
slightly decomposed OM
horizon subordinate distinctions: e
intermediately decomposed OM
horizon subordinate distinctions: a
highly decomposed OM
horizon subordinate distinctions: m
cemented
horizon subordinate distinctions: ss
slickenslides
horizon subordinate distinctions: h
humus - accumulation of OM
What are the factors of soil formation? Write an equation that shows the relationship between soil properties and the soil forming factors.
S = f (cl, o, r, p, t)
Climate (i.e. when temp and precip increase, weathering increases)
Organisms (i.e. soil engineers– earthworms– mix the soil)
Topography (i.e. steep slope = low infiltration into soil vs. flat slope = high infiltration)
Parent material (i.e. felsic or mafic = different particle size, mineralogy, and weathering rates)
Time (i.e. all factors are relative to time–soil in hot/wet climate or on bottom of slope = more weathering over longer periods of time)
What is the main factor that drives the formation of an andisol?
Volcanic ejecta and ash
What is the main factor that drives the formation of gelisols?
Permafrost
What are some morphological features of vertisols?
Self-churning soils by shrink-swell processes
How are Mollisols formed? What are some of the main characteristics of Mollisols?
Thick surface accumulation of soil organic matter; grassland soils transition to arid climate
General properties of Entisols
soils with little or no profile development
General properties of Inceptisols
soils with subtle profile development
General properties of Ultisols
highly weathered soils with subsurface accumulation of clay and low base saturation
General properties of Alfisols
soils with subsurface accumulation of clays
General properties of Spodsols
common in boreal forests
General properties of Oxisols
completely weathered soils
Residuum
Bedrock
Eolian
Transported by wind
Alluvium
deposited by streams and rivers
Till
transported by glaciers
Colluvium
Transported by gravity
Lacustrine
Lake deposits - tend to have beds oriented parallel to surface
Contrast the properties of basalt and granite and explain why these rocks are different
Basalt - Mafic (heavy elements), dominated by small-grains, extrusive, easily weathered, nutrient rich minerals (fertile)
Granite - Felsic (light elements), course-textured, intrusive, low fertility
What is aspect in the context of topography?
direction a slope is facing, like north or south. It’s relevant to soil because it has an effect on temperature/moisture (south-facing slopes get more sunlight, making them warmer and drier) and impacts the vegetation that grows, all of which affect soil
What are the five hill slope components? How does water and sediment movement vary among the five components?
From top to bottom: summit, shoulder, backslope, footslope, toeslope. As you move from the summit to the footslope, infiltration decreases and erosion increases. Runoff and eroded material accumulates at the toeslope.
main attributes and outcomes of the soil forming processes: melanization
Accumulation of organic matter in the upper soil horizons | Formation of dark A horizons (from humus enrichment) |
main attributes and outcomes of the soil forming processes: calcification
Accumulation of calcium carbonate in the soil in dry climates | Alkaline soil, formation of Bk horizons (k = calcium carbonate) |
main attributes and outcomes of the soil forming processes: podzolization
Fe, Al, and humus leaching caused by organic acids | Bleached E (elluviation) horizon, high acidic soil (pH 4-5), reddish-brown Bh/Bs horizons from Fe/Al/humus accumulation |
main attributes and outcomes of the soil forming processes: lessivage
Downward movement of clay particles | Bt horizons with clay films (argillians) on ped faces, E horizon lacking clay |
main attributes and outcomes of the soil forming processes: laterization
Intense leaching leaving behind high concentrations of Fe/Al oxides | Poor soil fertility, clay-poor and Fe/Al-rich, reddish in color, very hard |
main attributes and outcomes of the soil forming processes: gleization
Prolonged saturation leads to reduction of Fe | Gray/blue/greenish color, indicator of waterlogged conditions |
Bt
the illuviation of clay in the B horizon
Bk
accumulation of carbonate (k = ‘karbonate’)
Bs
illuvial accumulation of Fe/Al oxides (s = sesquioxide)
Bh
organic matter (humus) accumulation (h = humus)
Bqm
cemented silica formation (q = ‘siliqa’, m = ceMented)
Bo
residual accumulation of sesquioxides
Bw
reddening of soil
Bss
slickensides present (ss = slickensides)
Bg
gleyed
Name the six categorical levels of Soil Taxonomy. Which level provides the most general information about soils? Which level provides the most specific information about soils?
Order → Suborder → Great Group → Subgroup → Family → Series
(most general) → (most specific)
What is the California state soil?
San Joaquin
What is the California state rock?
Serpentinite