Weathering and Soils Flashcards

1
Q

What is Weathering?

A

The break up (physical disintegration) and decomposition (chemical alteration) of solid rock by surface processes

Solid rock → loose unconsolidated sediment and/or dissolved ions (weathering does not involve transport)

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2
Q

where does weathering occur?

A

at interface: solid earth meets hydrosphere, atmosphere, biosphere

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3
Q

Why is weathering important?

A

Provides sediment
-Contributes to soil formation
-Wears down mountains built by plate tectonic processes
-Shapes landforms
Important role in carbon cycle (reactions consume CO2, produce carbonate)
Some weathering processes (e.g. of mining waste piles) lead to toxic run-off

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4
Q

what are some products of weathering?

A

Loose debris (regolith)
Secondary minerals
Ions in solution
Weathering also leads to rounded surfaces and is essential for most landform & landscape development

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5
Q

what are the two types of weathering processes?

A
1. Physical (disintegration → smaller pieces)
–no change in chemistry
–increases surface area
2. Chemical (decomposition/alteration)
–breaking of bonds
–reactions alter or ‘stabilise’ minerals

both processes often work simultaneously
water is usually required

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6
Q

Physical/mechanical weathering increases the surface area exposed for …

A

chemical weathering

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7
Q

what are the two main processes of physical weathering?

A

(1) Ice wedging

2) Pressure unloading (exfoliation

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8
Q

what is ice wedging?

A

Water seeps into fractures and other openings
Freezes → expands volume by 9%
–exerts huge amount of stress…
–wedging, heaving, shattering
Significant in climates with freeze-thaw cycles – with each freeze, the rock is wedged further apart

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9
Q

what is pressure unloading?

A

Rocks formed at depth expand & ‘relax’ when exposed at surface
‘Unloading’ → exfoliation
Sheeting, exfoliation
Rock layers break off like an onion

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10
Q

what is chemical weathering?

A

Breakdown of minerals through chemical reactions with the atmosphere or hydrosphere

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11
Q

what are the three main processes of chemical weathering?

A

(1) Dissolution
(2) Hydrolysis
(3) Oxidation

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12
Q

what are the products of chemical weathering?

A
soluble ions (e.g.Ca2+)
new secondary minerals e.g. clays, oxides
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13
Q

what is dissolution?

A

Minerals completely dissolve into soluble ions in the presence of water
e.g. calcite dissolves in weak acid

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14
Q

what is hydrolysis?

A

minerals react with water
H+ ‘attacks’ and replaces other cations in mineral
→ alteration to form new clay minerals

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15
Q

what is oxidation?

A

Iron (Fe) bearing minerals react with oxygen

e.g. rusting of solid iron → iron oxide

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16
Q

What minerals does oxidation affect?

A

Fe-bearing silicate minerals e.g. olivine, pyroxene, biotite, garnet
Sulfide minerals e.g. Pyrite FeS2 (when exposed to oxygen and water → sulfuric acid (H2SO4) + iron & hydrogen ions → acid mine drainage)

17
Q

what is biological weathering?

A

(physical/chemical)
Tree roots: wedge into rock fractures → growth exerts sufficient pressure to split rock
Animal burrowing, boring
Lichens: secrete acidic compound

18
Q

How does weathering shape landforms?

A

All landscapes experience weathering
Landforms result from differential weathering
–at the mineral scale up to rock outcrop scales
–more resistant ≈ ridges;
–weaker ≈ valleys

19
Q

what creates karst topography?

A

dissolution of carbonate

e.g. Limestone pavement, W. Ireland or Karst towers, S. China

20
Q

What controls weathering rates?

A

How susceptible is the rock?

Do the conditions promote weathering?

21
Q

what are the primary controls of weathering rates?

A

rock type & mineral composition

climate (temperature, precipitation)

22
Q

what are the secondary controls of weathering rates?

A
rock texture (grain size, porosity)
topography (relief, aspect, drainage)
vegetation & soil chemistry
23
Q

chemical weathering is strongest with…

A

high precipitation

high temp.

24
Q

physical weathering is strongest with…

A

moderate precipitation

low temp.

25
Q

What is Soil?

A

Thin veneer covering most land surfaces
Soil develops on regolith (rock and mineral fragments produced by weathering)
Interface in the Earth system: bridge between life and rocks
Supports the growth of plants and people

26
Q

how is Soil used as a resource

A
Medium for plant growth
Ecosystem habitat
Nutrient recycling
Water storage & filtration
Engineering medium
27
Q

What is soil made up of?

A

45% mineral matter
25% air
25% water
5% humus, decayed remains of plants & animals

28
Q

what are the controls on soil formation?

A
Parent Material
Climate - temperature and precipitation
Time
Topography - thin soils on steep slopes
Plants and animals - supply organic matter to the soil, fungi and bacteria active in decay
29
Q

what are the Soil horizons (O,A,E,B,C)

A

O: organic layer (humus) - decomposition of organic matter
A: organic and mineral matter - High biologic activity
E: zone of eluviation & leaching - Little organic matter
B: mineral ‘subsoil’…zone of accumulation
- deposition of clays, oxides, carbonates from A
- commonly red or brown in colour
- little organic matter – often rich in clays
C: Weathered parent material

30
Q

soil profiles are dependent on…..

A

climate

31
Q

what is an example of a soil profile in a cool and moist climate?

A

BC, Quebec & Maritimes: Coniferous forests
Strong leaching
O, A, E, B, C

32
Q

what is an example of a soil profile in an arid climate?

A

AB, SK: prairie ecosystems

O, A, B, C