Title: Weather and Weathering
1Weather and Weathering
2(No Transcript)
3Plate Tectonic Wrap-up
- Locations of
- Basalt/Andesite/Rhyolite
4Hot spots
- Long-lived volcanic centers
- Many on mid-ocean ridges why?
- Stationary vs. apparent motion
5Hawaiian hot spot
6Yellowstone Hot Spot
- Eruptive pattern
- Bimodal volcanism
7Volcanoes and Climate
- Dust veil index
- Hemispheric cooling
- Case study Toba
8Volcanoes and Climate
- Dust veil index
- Hemispheric cooling
- Case study Toba
9Weathering weather climate
- Climate
- Water availability
- Temperature
10Weathering weather climate
- Climate
- Water availability
11Weathering weather climate
- Climate
- Water availability
- Temperature
12Weathering (Dis)Equilibrium
- Rock Environment
- Pressure high
- Temperature constant
- Water constant?
- Earth Surface Environment
- Pressure low
- Temperature variable
- Water variable
13Types of Weathering
- Chemical decomposition
- Interactions at the molecular level
- E.g., hydration
- Mechanical (Physical) disintegration
- Interactions at higher levels
- E.g., ice wedging
- Salt?
14Surface area
15Types of Chemical Weathering I
- Hydration
- Addition of water to the structure
- Swelling clays
- Hydration of biotite
- Grussification
16Types of Chemical Weathering II
- Hydrolysis
- Replacement of cations ( charge) with hydrogen
ions - Feldspars ? clay minerals
17Types of Chemical Weathering III
- Oxidation
- Oxygen accepts loose electrons (anion)
- Creates stronger cations
- Allows bonding to weak ions (e.g., OH-)
- E.g., Iron oxide (rust hematite/limonite) and
aluminum oxide
18Types of Chemical Weathering III
19Types of Chemical Weathering IV
- Chelation
- Biotic facilitation of weathering
- Physical chemistry models lie!
20Types of Chemical Weathering V
- Solution
- Polar water molecules bond more strongly to ions
than ions do to mineral structures - E.g., salts NaCl, CaCO3
21Relative Weatherability
22Relative Weatherability
23Relative Weatherability
- Goldich Stability Series
- But
24Weathering vs. Erosion
25Rates of Chemical Weathering
- Rates f(disequilibrium)
- Decrease at a decreasing rate
- With time, depth, temperature
http//www.usyd.edu.au/su/agric/ACSS/sphysic/pedog
enesis/pedogenesis.html
26Outside-in weathering corestones
- Because weathering f(depth)
27Weathering with Climate
28Results of Chemical Weathering
- Removal of unstable materials
- E.g., CaCO3
- Retention of stable materials
- E.g., quartz
- Creation of new stable material
- E.g., clay minerals
29Soil Formation
- Hans Jennys 5 soil-forming variables
- Parent mat.
- Topography
- Organisms
- Climate
- Time
30Soil Formation, Classification, Distribution and
Application
31Soil Horizons
- Building blocks
- O organic
- A OM-rich, leached
- B accum.
- C little altered
- Subdivisions
32USDA Soil Classification
- Descriptive language for communication
- Soil orders (n12)
- Based on one criterion
- Suborders (nhundreds)
- Secondary criteria
- http//soils.usda.gov/technical/classification/tax
_keys/index.html - Gradations
- Intergrades