Lecture 2: Formation of soils from parent materials Flashcards

(34 cards)

1
Q

Climate (Cl-O-R-P-T)

A

-most influential factor on parent material because it determines what kind and how intense the weathering will occur in that area
-temperature: every 10 degree rise in temp double the rate of biochemical rxns
-effective precipitation: water must penetrate the regolith to be effective in soil formation

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2
Q

Organisms (Cl-O-R-P-T)

A

the type of vegetation that is growing in that area, as well as the land use, affects the soil layers. (eg. a plowed field vs a forest)

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3
Q

Relief (Cl-O-R-P-T)

A

Soils on a slope LOSE material due to gravity. Soils in flat areas GAIN materials especially from the fallen materials of the slope.

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4
Q

Time (Cl-O-R-P-T)

A

Younger soils typically have less layers than older soils. Older soils also may not have as many nutrients.

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5
Q

When does pedogenesis begin?

A

When horizons that are not present in the parent material begin to appear in the soil profile

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6
Q

What is pedogenesis?

A

Soil formation

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7
Q

The 4 basic processes of pedogenesis

A

-Additions
-Losses
-Translocations
-Transformations

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8
Q

Topsoil Letters

A

A (or E)

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9
Q

Subsoil

A

B

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10
Q

Regolith

A

C (or R)

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11
Q

Topsoil: A Horizon

A

-darker
-mineral soil + organic matter
-water flows through (loses minerals bc of this)

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12
Q

Topsoil: E Horizon

A

-grey to white
-mostly sand
-zone of intense leaching
-Fe- and Al- oxides have been eluviated
-common under forest because of HUMIDITY and ACIDIC soil pH

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13
Q

Subsoil: B Horizon

A

-accumulation of mineral particles leached from topsoil like clay and salts
-less organic matter
denser
-more difficult for plant roots and water to penetrate
-usually red, brown, or orange

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14
Q

Regolith: C Horizon

A

-most like parent material
-very little biological activity and weathering
-can be dug with a shovel

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15
Q

Regolith: R Horizon

A

-hardpan (compacted)
-composed of compacted and/or cemented clay with calcium carbonate, iron oxide, manganese or silica
-unaltered parent material, consolidated bedrock
-impermeable
-can’t be dug with a shovel

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16
Q

Compared to the B horizon, the A horizon is likely to be higher in ___

A

Organic matter

17
Q

Master Horizons Order

A

O
A or E
B
C or R

18
Q

O Horizon

A

-organic layer
-not usually in grasslands
-most common in forests

19
Q

Oi

A

surface- undecomposed leaves and twigs

20
Q

Oe

A

middle-partially decomposed

21
Q

Oa

A

bottom- very dark, well decomposed (soapy)

22
Q

Minerals

A

naturally occurring inorganic element or compound with repeating structure.

23
Q

Rocks

A

made up of a bunch of different minerals

24
Q

Primary mineral

A

solidified from molten magma/lava

25
Secondary mineral
recrystallized products of the breakdown/alteration of primary minerals
26
Resistance of primary minerals
primary minerals containing Fe (iron) and Mg (magnesium) are less stable. the more stable ones have Al (aluminum) and K (potassium)
27
Resistance of secondary minerals
Aluminum silicates and minerals containing iron are more resistant and those containing calcium are less resistant.
28
Physical Disintegration and examples
physical breaking of rock into smaller and smaller pieces without changing the mineralogy. (eg. jointing, thermal expansion, frost wedging)
29
Chemical decomposition and examples
breaks down rock components and internal structures of minerals. converts primary minerals to secondary and releases plant nutrients in soluble form (eg. hydrolysis, dissolution, oxidation) *needs water and acids
30
Dissolution
minerals are soluble in water or weak acids. involves breaking relatively weak IONIC bonds
31
Carbonate dissolution
acidic water dissolves calcite. this process dissolves limestone and carries the cations away. formation of caves and karst. dissolved products carried to ocean.
32
Hydrolysis
H+ ion attacks minerals, replaces other cations in the crystal. Silicates react with acidic water to form: -secondary minerals -dissolved ions -dissolved silica
33
Oxidation- Reduction
Formation of rust on metal
34
Biogeochemical weathering
Chemical weathering enhanced by inorganic acids and organic acids.