weathering, erosion and transport - msu billings · weathering, erosion, ... weathering –the...
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Weathering, Erosion and Transport
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Weathering, Erosion, and Transportation
• Rocks exposed at Earth’s surface are constantly changed
by water, air, temperature variations and other factors
• Weathering is the group of destructive processes that
change physical and chemical character of rocks at or
near Earth’s surface
• Erosion is physical picking up of rock particles by water,
ice, or wind
• Transportation is the movement of eroded particles by
water, ice, or wind
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The Nature of Weathering
• Weathering is the physical and/or chemical alteration of rocks and minerals where the lithosphere, hydrosphere, atmosphere, and biosphere meet
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Weathering and Earth Systems
• Hydrosphere – Water is necessary for chemical weathering
– Oxygen dissolved in water oxidizes iron and other metals in rocks
– Carbon dioxide dissolved in water creates carbonic acid
• Primary cause of chemical weathering
– Running water loosens and abrades particles
– Glacial ice removes and abrades particles
– Freeze/thaw cycling mechanically weathers
• Biosphere – Plant root growth widens cracks
– Animal movement and human activity mechanically weather
– Plant roots decaying organic matter in soils pump carbon dioxide into
the soil producing acids that dissolve the rock
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Products of Weathering
• Lithic (Rock) Fragments(granite, basalt, schist, etc.)
• Dissolved Ions(Calcium, Potassium, Sodium, etc.)
• Rust Minerals (Hematite, Goethite, etc.)
• Clay Minerals(Bentonite, Montmorillonite, etc.)
• Residual Minerals(Quartz, Orthoclase, Muscovite, etc.)
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Two Types of Weathering
• Chemical weathering– The decomposition of rocks and minerals as
chemical reactions alter them into new minerals stable at the Earth’s surface
• Physical (or mechanical) weathering– The disintegration or disaggregation of rocks by
physically breaking them apart
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Weathering
• Physical and chemical weathering are two distinct processes
• Usually work in tandem
• Chemical weathering is more significant in warm wet low land environments; Physical weathering is more important in in cold areas and high elevations
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Physical Weathering
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Physical Weathering
• Frost action– Mechanic effect of freezing (and
expanding) water on rocks
• Pressure release– Removal of overlying rock allows
expansion and fracturing
• Plant growth– Growing roots widen fractures
• Burrowing animals
• Thermal cycling– Large temperature changes fracture rocks
by repeated expansion and contraction
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But mostly physical weathering is a matter of things just
falling down. So in a sense, gravity, is the primary cause of
physical weathering.
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Physical Weathering in cold high altitude
environments
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Physical Weathering by running water
More on that later
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Sheeting
• Release of confining pressure on rocks formed deep within the Earth
• Development of fractures and joints caused by expansion
• Rocks break along fractures and joints
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Sheeting in granite
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Ice Wedging
• Freeze - Thaw cycles are effective at breaking apart rocks
–Water expands when it freezes
• Volume increases by 9%
– The stress of expansion breaks the rock
– Ice melts and the water percolates deeper into the newly expanded cracks
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Frost/freeze or Ice wedging
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Geometry of Weathering
• Spheroidal weathering
–Corners tend to be rounded during weathering
–Decomposition is most rapid at corners
–Rock’s shape approaches sphere
– Further weathering reduces size
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Spheroidal weathering in granites
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Spheroidal weathering in granites
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Other Forms of Physical Weathering
• Heat– Heat causes rocks (most solids) to expand
– Rocks are poor conductors of heat
– Outer layer of rock that expands breaks off (spall)
• Crystal Growth– Minerals precipitate along fractures
– Similar to ice wedging
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Other Forms of Physical Weathering
• Root Growth– Roots may exert enormous forces in growing
– Root tips pressures may exceed 10,000 kg per square meter
– Seeds gather in cracks in rock and germinate
– Growing plant and roots slowly wedge rock apart
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Geometry of Weathering
• Fractures in rock form from the reduction in load (pressure)
–Generally form in groups
• Parallel joints
• Intersecting joints
–Cut large blocks into smaller blocks
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Geometry of Weathering
• Surface Area is increased by fracturing
– The increase in surface area, increases the rate of weathering
• Both physical and chemical
– Surface area increases exponentially
y = 3e0.6931x
0
10
20
30
40
50
60
0 2 4 6
Series1
Expon.
(Series1)
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Chemical Weathering
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Chemical Weathering
• Minerals are destroyed or altered by chemical reactions
–Dissolution
–Hydrolysis
–Oxidation
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Chemical Weathering
• Oxidation
– Chemically active oxygen from atmosphere
– Iron oxides are common result
• Soil and sedimentary rocks often stained with
iron oxides
• Acid dissolution
– Hydrogen cations replace others in minerals
– Carbonic acid from atmospheric CO2 dissolved
in water
– Sulfuric, hydrofluoric acids emitted by volcanic
eruptions
– Some minerals, such as calcite, may be totally
dissolved
– Human activity, such as mining and burning of
fossil fuels, produces acids
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Chemical Weathering
• Feldspars
– Most common minerals in crust
– Slightly acidic rain water attacks feldspar
– Clay minerals produced
• K+, Na+, Ca++ ions released into water
• Other minerals
– Ferromagnesian minerals
• Clays, iron oxides, Mg++ ions produced
– More complex silicate bonds lead to lower weathering susceptibility
• Olivine most susceptible, quartz least
• Warm, wet climatic conditions maximize weathering
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Chemical Weathering
• Most igneous and metamorphic rocks and minerals are formed at high temperatures and pressures– They are in a state of equilibrium at the
Temperature (T) and Pressure (P) of formation
– At the Earth’s surface, rocks and minerals are subject to chemical weathering
– Secondary minerals formed at the T and P common to the Earth’s surface
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Chemical Weathering (cont)
• Sedimentary Rocks: –Limestones and Dolomites are formed in
the ocean and are easily dissolved by water, especially if it is acidic
–Evaporites (Halite, Gypsum and Anhydrite) are precipitated from seawater and easily dissolved in water even if it is not acidic
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Dissolution
• Some minerals are soluble in water
–e.g., Halite - NaCl
–Minerals dissolve into constituent ions
– Ions removed with water by leaching
– Solubility of compound controls leachability
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Acid Hydrolysis
• CO2 mixes with water to produce carbonic acid, H2CO3
• Decaying organic matter produces acid
• Roots pump CO2 into the soil producing very high concentrations of carbonic acid
• Anthropogenic sources of acid (CO2 and SO2)– Acid rain
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Acid Hydrolysis
• H+ attacks minerals by replacing other ions in the mineral structure
• Promotes dissolution
– Calcite hydrolysis by carbonic acid solution
CaCO3 + H2CO3 Ca+2 + 2HCO3-
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Acid Hydrolysis
• New “secondary” minerals may be created by this process
– H+ ion replaces the K+ ion in the feldspar structure
– K+ ion goes into the water solution
– Kaolinite, a clay mineral, formed
2KAlSi3O8 + 2H2CO3 + 9H2O =
2K+ + 2HCO3- + 4H4SiO4 + Al2Si2O5(OH)4
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Oxidation
• Valence state increases
–Often associated with free O2 in the environment
• Iron is usually found as the Fe+2 ion in silicate minerals
• Exposed to the atmosphere it will oxidize to the Fe+3 ion
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Oxidation
• Change in valence state disrupts crystal structure
• Oxidation works in combination with hydrolysis and dissolution
2FeSiO4 + 4H2O + O2 = 2 Fe2O3 + 2H4SiO4
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Trends in Chemical Weathering
• Alkali and alkaline earth elements removed into solution
• Al and Si are enriched in secondary minerals
• Fe is enriched in insoluble ferric oxides
• Warm wet climates increase chemical weathering rates
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Weathering of Rocks
• Relative stability of minerals varies widely
• Minerals composition is primary control
• Rock texture influences role of water in weathering
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Relative stability of minerals
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Inorganic Carbon CycleWhat controls CO2 concentrations on geologic timescales
– Carbon dioxide present as trace
gas in atmosphere (380ppm)
– Combines with water to form
carbonic acid (H2CO3)
– Weathers rocks and provides
CaCO3 to marine animals and
plants so they can make shells.
– Returns to the mantle during
subduction
– Released back to atmosphere by
volcanic eruptions
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On geologic timescales volcanism controls CO2 concentrations.
The negative feedback mechanism on this is the rate of weathering which
increases because of warmer climates due to higher CO2 concentrations.
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Climate & Weathering
• Climatic conditions strongly influence weathering reactions
–Amount of rainfall
• Most reactions need water
–Average temperature
• Increase of 10oC doubles reaction rate
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Rates of Weathering
• Rates of weathering are linked to climate zones
–Human structures are useful gages for measuring rates
– Thickness of soil profile is controlled by weathering rates
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Climate and weathering
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From Sediment to Sedimentary Rock
• Transportation– Movement of sediment away from its source, typically by
water, wind, or ice
– Rounding of particles occurs due to abrasion during transport
– Sorting occurs as sediment is separated according to grain size
by transport agents, especially running water
– Sediment size decreases with increased transport distance
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Distinguishing Characteristics of Clastic Sediments (cont.):Sorting - Well-sorted sediment indicates prolonged reworking by wind or water; poorly sorted
sediment may indicate rapid deposition, or deposition by ice or mass movement.
Angularity/Roundness and Shape – Well rounded sediment also indicate prolonged reworking
by transporting agent; the shape of grains often indicates the transport system, but also may
be related to the type of mineral or rock fragment
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Mass Movement:landslides, debris flows,
avalanches, lahars, mudflows and creep
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Types of Mass Movement
• Includes all types of slope failures
• Classified by
– Type of motion
– Type of material
–Rate of movement
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Creep
• Extremely slow movement of soil and regolith - 1 to 10 mm/yr
• Combination of factors cause creep
–Heaving of soil - expansion & contraction is the primary cause
• Wet-dry cycles
• Freeze-thaw cycles
Types of Mass Movement
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Creep
• Other factors adding to creep
–Plant root growth - displaces soil
–Burrowing animals - displaces and loosens soil
–Undercutting - streams, earthquakes, human activity
Types of Mass Movement
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Debris Flows
• Mixtures of water, mud and rock
– Liquified soil flows downhill
• Up to 50 km/hr
–Water lubricates mass of soil and rock
– Large boulders, building etc. may be carried by viscous fluid
Types of Mass Movement
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Lahars
• Volcanic debris flows
–Common is loose pyroclastic material
–Rain or melting snow saturates soil and rock
– Explosive eruptions and associated earthquakes can be triggers
–Very fast flowing - up to 150 km/hr
Types of Mass Movement
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Mudflows
• Debris flows consisting of slit and clay sized particles
–Usually associated with heavy rain
–High water content - up to 30%
–Usually follow stream valleys
Types of Mass Movement
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Landslides
• Mass movement along well defined slippage plane
• Landslide block moves as a single or group of units
• Rock type, orientation and water content influence events
Types of Mass Movement
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Yellowstone River valley
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A landslide
DebrisFlow_Moscardo.mov
A debris flow
A flash flood
DebrisFlow_simualted.mov
Simulated debris flow: graded
bedding
http://www.searchles.com/links/show/youtube.com%2Fwatch%3Fv%3Dyoqkplxjalk&feature%3Dplaylist&p%3D9b1d99fb0c4dd21b&index%3D4
Banda Aceh Tsunami