Weathering and Soils
Steven Dutch, Professor Emeritus, Natural and Applied Sciences, University of Wisconsin - Green Bay
The Rock Cycle
The Ideal Rock Cycle
- Igneous rocks form when molten rock (magma) invades the crust.
- They break down by weathering and the breakdown products are transported by erosion.
- The breakdown products are deposited to form sedimentary rocks
- Sedimentary rocks are buried, subjected to heat, pressure, and the action of fluids
- Heat, pressure, and the action of fluids change rocks, forming metamorphic rocks.
- Metamorphic rocks may eventually be heated enough to melt, forming a new generation of igneous rocks.
Anything can happen in the Rock Cycle
- Igneous rocks can be subjected to heat, pressure, and the action of fluids to form metamorphic rocks.
- Igneous rocks can be re-melted, forming a new generation of igneous rocks.
- Sedimentary rocks can be weathered and eroded to form a new generation of sedimentary rocks.
- Sedimentary rocks may eventually be heated enough to melt, forming a new generation of igneous rocks (although technically they'd be metamorphic by the time they melted).
- Metamorphic rocks can be weathered and eroded to form sedimentary rocks.
- Metamorphic rocks can be subjected to heat, pressure, and the action of fluids to form a new generation of metamorphic rocks.
Breakdown of Rock near the Surface Due to Surface Processes
- Chemical Alteration (Often Addition of Water)
- Solution & Leaching
- Biological Action
- Frost - Wedging
- Plant Roots
- Salt Crystal Growth
- Expansion of Hydrated Minerals
Movement of Large Amounts of Material Downhill under Gravity
Surface Area and Weathering
Imagine a cube of rock one meter on a side:
- Divide the edges by 2, total area increases 2 times
- Divide the edges by 3, total area increases 3 times
- Divide the edges by n, total area increases n times
For a one-meter block crushed into 0.1 mm pieces, the edge length is divided by 10,000, and the area multiplied by 10,000. 10,000 square meters is over 100,000 square feet or 2-1/2 acres.
The smaller we subdivide particles, the more surface area is exposed. Things that happen at surfaces, like heat transfer or chemical reactions, happen faster. Some common applications of this fact:
- Crushed ice cools faster than an ice cube
- Granulated sugar dissolves faster than a large lump
- A carburetor or fuel injector sprays a fine mist of gasoline into an engine cylinder
A more serious example:
Flour in a sack in your kitchen is about as inert as a material can get. Grain dust (which is what flour is) dispersed in the air is highly combustible, even explosive. Every year a couple of dozen people in the U.S. die in grain elevator explosions caused by suspended dust. Coal dust in mines can be even deadlier.
How Surface-Volume Ratio Affects Weathering
||Hence: corners of blocks weather fastest, then edges, then faces. The interior is immune as long as the surrounding material is intact.
What Determines Soil Type
- Parent Material
- Residual - Transported
- Least Important Factor for Mature Soils
Strongest Influence Is Parent Material
Strongest Influences:Climate, Vegetation, Drainage
Leaching from Surface
Accumulation beneath Surface
- Al, Fe in Humid Climates
- Ca in Arid Climates
Soil Horizons and Profiles
Layers in Soil
Not Deposited, but Zones of Chemical Action
Suite of Layers at a Given Locality
Principal Soil Horizons
O - Organic (Humus) Often Absent
A - Leaching
K, Mg, Na, Clay Removed
E - Bleached Zone - Present Only in Certain Soils
B - Accumulation
Absent in Young Soils
Distinct in Old Soils
Al, Fe, Clay (Moist)
Si, Ca (Arid)
C - Parent Material
Limits of Soil Formation
- Balance Between:
- Downward Lowering of Surface
- Downward Migration of Horizons
- If erosion rapid or soil evolution slow, soils may never mature beyond a cetrain point.
- Extremely ancient soils may have lost everything movable
First Systems Russian
- Chernozem (Cherny + Zemlya) Black + Earth
- Serozem (Sery, Gray + Zemlya)
- Podzol (Pod + Zola) Beneath + Ash
- This is how words are often formed in Russian
Early US Names
- Pedalfer (Al + Fe in Subsoil)
- Pedocal (Ca in Subsoil)
- Laterite - Intensely Weathered Tropical Soils
- Caliche - Calcite - Cemented Arid Subsoil
This may be the most difficult classification problem in science because of the many factors involved.
Genesis & Evolution
- Most Effective Use
- Slope Stability
- Expansion and Shrinkage
- Stability of Excavations
Varied Bases for Classification
- Parent Material
- Constituent Material
- Climate & Vegetation
"The 7th Approximation"
US Soil Conservation Service
12 Soil Orders
|No B Horizon
||Weak B Horizon
||Distinct B Horizon
||Very Deep Horizons
|Soils Classified on Basis of Horizon Development
Dry Climate Soils
B Horizon Clay Rich
B Horizon Fe-Rich
Old Temperate Soils
Old Tropical Soils
|Soils With Special Characteristics - Lack of B Horizon Not Related to Maturity
|Very young ash soils are so distinctive they have their own soil order.
|No B Horizon due to internal churning by swelling and shrinking clays
|No B horizon: A Horizon is organic debris resting on subsurface materials.
|No B horizon: A Horizon resting on permafrost.
Soils of the U.S.
- Weakly-Developed Soils
- Mostly on young alluvium in the West where climate is dry and chemical weathering is slow. The large area in Nebraska is the Sand Hills, former Pleistocene sand dunes. Some in the East on very young deposits.
- In drier parts of the West
- Mostly on mountain slopes where weathering and erosion are about equal. Some on young glacial deposits. Imply somewhat wetter climate than entisols.
- Well-Developed Soils
- Mostly in the Midwest and West in grasslands, often on wind-blown deposits (loess).
- Mostly in the Midwest and East in deciduous forest areas. Some in the West at higher elevations in deciduous forest areas.
- Coniferous forest areas in northern Wisconsin, Michigan, New York and New England. Also high mountains in the Northwest with conifer forests.
- In the Southeast where warm climates and stable conditions allow extremely long times for soil development. A few areas in the far West. Note in the Oregon Cascades how ultisols occur at low elevations but mollisols at higher, cooler elevations. Still higher, alfisols occur. The final stage of soil evolution, oxisols, do not occur in the continental U.S. but do occur in Hawaii and Puerto Rico.
- Soils With Special Characteristics
- Occur mostly in flood plains in clay deposits, and along outcrop belts of certain shales where the right clay minerals occur.
- Form on volcanic deposits in the Northwest.
- Cold-climate peat bogs in Minnesota and northern Michigan, coastal swamps in the Southeast.
- Abundant in Alaska, not found in the continental U.S. except perhaps in a few very high mountain areas.
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Created February 3, 1997, Last Update 23 January 2001
Not an Official UW-Green Bay Site