(5) + (6) Weathering Flashcards

1
Q

Weathering

A
  • Breaks down rock into loose particles : Creates sediment & soil & dissolved ions in water
  • Change phys. & chem. character of rock
  • Surficial process
  • Leads to development of sediment & sedimentary rock : Major Earth material at surface ; Minor in total Earth crust
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2
Q

Two types of weathering

A
  • Mechanical (or) Physical [physical disintegration, no chemical change]
  • Chemical (rock decomposes due to exposure to water and gases in atmosphere)
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3
Q

Weathering Is progressive

A
  • Weathering along joints (fractures)
  • Rounded corners
  • Increases towards the surface
  • Greater surface area speeds weathering
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4
Q

Mechanical Weathering

A
  • Intact rocks break into pieces
  • Major types:
  • Frost action **
  • Pressure release **
  • Plant growth (roots in the cracks of rocks)
  • Burrowing animals (burrow into the rock)
  • Temperature changes, expansion and contraction (fire suddenly put out, hot interior, cool exterior causes them to explode)
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5
Q

Frost Action

A
  • Freeze-thaw cycle
  • Expanding water when it freezes
  • Boulders created by frost wedging
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6
Q

Pressure Release

A
  • Most effective of mechanical weathering
  • The rock breaks apart along these joints and exfoliates
  • Rock breaks into sheets
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7
Q

Where will mechanical weathering be most intense?

A
  • Cool, with abundant water (Freeze thaw)

- Steep slopes (Gravity assists)

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8
Q

Chemical Weathering

A
  • Also ‘rock decomposition’
  • Rocks react with water and air to produce new chemical products (Makes new minerals and ions in solution. Many of these reactions prefer warm, wet conditions)
  • Remember equilibrium? (Will break down without it. Mineral stability)
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9
Q

Agents of chemical weathering (Oxygen)

A
  • Interaction of water with rocks
  • Abundant in atmosphere: chemically active (oxidation)
  • If Fe present, yields Fe-oxide and Fe-hydroxide minerals
  • If Al present, yield Al-oxide minerals
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10
Q

Agents of chemical weathering (Carbonic Acid)

A
  • Most important natural source of acid: carbon dioxide dissolved in water
  • Weak acid, but abundant
    Rainwater; water percolating through soil
  • Aids dissolution (dissolving minerals)
  • Aids hydrolysis (breakdown of minerals from reactions with water)
  • Can cause the formation of new minerals
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11
Q

Chemical Weathering: Calcite

A
  • Form caves
  • Discolour and dissolve marble and limestone statues, monuments
  • Where do the ions go?
    • Hard water
    • Seawater is a product of weathering carrying dissolved ions into the ocean
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12
Q

Chemical Weathering: Quartz

A
  • Forms smaller particles of quartz +
  • Dissolved silica ion
    • Forms common cement in sedimentary rock
  • Quartz is rock-forming mineral LEAST susceptible to chem weathering
    • Strength of bonds in crystal lattice
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13
Q

Chemical Weathering: Feldspars

A
  • Clay minerals +
  • Ions of SiO2, NA, Ca, K
    • Note cations from K-feldspars and plagioclase: Na, Ca, K
    • Effects of carbonic acid
    • Slow, complex reaction
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14
Q

Chemical Weathering: Ferromagnesian minerals

A
  • Clay and minerals +
  • Ions of SiO2, Mg, Na, Ca, K +
  • Fe oxide minerals
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15
Q

Yellowish-reddish soils are rich in Fe oxides (examples)

A
  • Limonite, goethite (yellow)

- Hematite (red)

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16
Q

After complete weathering what is left?

A
  • Solids: Clays, quartz, iron oxides, aluminum oxides
  • Ions : including Ca2+ SiO2, HCO-3
    o Ions become cement for sediment reactions
    o Calcite, silica common elements
17
Q

Chemical weathering and climate

A
  • Most intense where there is abundant liquid water

- Most intense where warm

18
Q

Soil

A
  • Layer of weathered, unconsolidated material on top of bedrock
    o Some definitions: Contains organic matter and can support plant growth
  • Role of clay, quartz
    o Clay holds water plant nutrients
    o Quartz: sand grains drainage
19
Q

Mature soil is layered (soil horizons) in…

A

Appearance and chemical composition

20
Q

Soil Formation

A
  • Takes long time to form (thousands of years)
  • Depends on:
    o Climate: (rainfall, temp)
    o Parent rock composition
    o Organisms (type of vegetation, different root systems)
    o Relief (slope, topography)
    o Drainage
    o Time
21
Q

Soil Formation: Climate

A
  • Most important factor determining soil type
  • Dry climate
    o Thin soil
    o Little leaching
    o Little humus
    o Upward movement of soil water (Evaporation and Capillary action)
  • Wet climate
    o Form thicker soils
    o Strong leaching
    o Downward movement of soil water
    o High Al and Fe oxides
    o Abundant humus
22
Q

Bauxite (Aluminum Oxide)

A
  • Least soluble of all the weathering products
  • Source of aluminum
  • Formed in tropical weathering conditions
  • Laterite soils
  • Highly leached
  • Only insoluble oxides remain
23
Q

Weathering produces: Sediment

A
  • Loose, solid particles
  • Classified by size:
  • Gravel (includes boulders and cobbles)
  • Pebbles
  • Sand
  • Silt
  • Clay
  • (mud = wet silt and clay)
24
Q

Transportation of Sediments: Agents of transportation

A
  • Running water
  • Glaciers
  • Waves
  • Wind
25
Q

Transportation of Sediments: Rounding

A
  • Particles hit and scrape each other during transport
  • Gets rid of irregular surfaces
  • Rounding vs angular (gradational)
26
Q

Transportation of Sediments: Sorting

A
  • By size
  • Poorly sorted well sorted (mixing of sizes uniform) sizes
  • Running water – a good sorting agent
27
Q

Deposition of sediment

A
  • Transported materials settle
    o Occurs when agent loses energy and can no longer transport its load
  • Chemical or organic sediment accumulates on the sea or swamp floor
    o Dead organisms accumulate
    o Evaporation and precipitation (ex. Salt))
    o Change in temperature, pressure, chemical of solution – can cause precipitation
28
Q

Preservation of sediments

A
  • Not all sediments are preserved as sedimentary rock

o Marine sediments most easily preserved

29
Q

Lithification of sediment

A
  • Process that converts loose sediment into sedimentary rock
  • Compaction and cementation (results in clastic sedimentary rock)
    o Pressure
    o Usually buried under more sediment
  • OR crystalize minerals directly from solution (chemical sedimentary rock)