Lecture 2: Formation of soils from parent materials Flashcards

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
Q

Secondary mineral

A

recrystallized products of the breakdown/alteration of primary minerals

26
Q

Resistance of primary minerals

A

primary minerals containing Fe (iron) and Mg (magnesium) are less stable. the more stable ones have Al (aluminum) and K (potassium)

27
Q

Resistance of secondary minerals

A

Aluminum silicates and minerals containing iron are more resistant and those containing calcium are less resistant.

28
Q

Physical Disintegration and examples

A

physical breaking of rock into smaller and smaller pieces without changing the mineralogy. (eg. jointing, thermal expansion, frost wedging)

29
Q

Chemical decomposition and examples

A

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
Q

Dissolution

A

minerals are soluble in water or weak acids. involves breaking relatively weak IONIC bonds

31
Q

Carbonate dissolution

A

acidic water dissolves calcite. this process dissolves limestone and carries the cations away. formation of caves and karst. dissolved products carried to ocean.

32
Q

Hydrolysis

A

H+ ion attacks minerals, replaces other cations in the crystal. Silicates react with acidic water to form: -secondary minerals -dissolved ions -dissolved silica

33
Q

Oxidation- Reduction

A

Formation of rust on metal

34
Q

Biogeochemical weathering

A

Chemical weathering enhanced by inorganic acids and organic acids.