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Weathering and Soils. Granite headstone in Southern Vermont. Weathering and Soils. Marble headstones in Southern Vermont. Weathering and Soils. Mechanical Weathering- the physical breakdown of rocks Chemical Weathering- reaction of rocks with water, acids, oxygen, etc.
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Granite headstone in Southern Vermont Weathering and Soils Marble headstones in Southern Vermont
Weathering and Soils Mechanical Weathering- the physical breakdown of rocks Chemical Weathering- reaction of rocks with water, acids, oxygen, etc.
Mechanical Weathering Tectonic Jointing
Exfoliation Mechanical Weathering
Exfoliation Mechanical Weathering
Exfoliation Mechanical Weathering
Limestone dissolves readily CaCO3 + 2 H+ (aq) = Ca+2 + CO2 + H2O gas Chemical Weathering Solution: H2O + CO2 = H2CO3 ( H+ + HCO3- ) in air (acid rain) acid
Solution: Karst Topography Chemical Weathering
Solution: Karst Topography Chemical Weathering
Karst Sinkhole- Florida Chemical Weathering
Karst Sinkhole- Florida Chemical Weathering
Tower Karst - China Chemical Weathering
Oxidation: Fe2SiO4 + ½ O2 = Fe2O3 + SiO2 Chemical Weathering
Chemical WeatheringDifferential Weathering Weathering can preferentially dissolve out mafics & increase the sialic component in sediments to yield “granite”
What happens when granite is weathered? • The biotiteand hornblende will undergohydrolysis to form • clay,andoxidation to form iron oxides. Chemical Weathering • The feldspars will undergo hydrolysis to form kaolinite (clay) and release Na+ and K+ ionsinto solution The quartz (and muscovite, if present) will remain as residual minerals because they are very resistant to weathering.
Idealized soil profile from a humid climate at middle latitudes Zone of Leaching
Chemical Weathering Transported Soils
hot hot laterites Temperature pedocals pedalfers tundra soils cool cold low 50 cm/yr high Precipitation Effect of climate on soil types tundra soils
Effect of climate on soil types A typical pedocal with white caliche (CaCO3) deposits in a shallow B horizon
Tundra soil Laterite Effect of climate on soils Making laterite bricks Temple at Angkor Wat Cambodia (700 yrs old)
Pf Pc Pf Pf, Pc L Pf, L A Newer Classification of Soil Types
Rates of soil formation: Central USA: ~ 1 cm/100 years in very porous and permeable rock Humid N. Carolina: ~ 1 cm/5 years “ Granite may require over 1000 years for a cm
Both Ends of the Erosion Problem Serious soil erosion and gully formation related to diversion of water runoff over a few months in central California Sediment pollution following heavy rains in North Carolina
Soil Degradation • Erosion • Deforestation • Agricultural depletion • Contamination - Pollution • Salinization • Pesticides • Chemical additions and spills • Urbanization • Desertification • Overgrazing
Soil Erosion Raindrop impact: millions in a single shower hit at ~ 30 mph
Soil Erosion Rill-wash and gullying in loose and poorly-consolidated soils
Soil Erosion Number of dust storms during the month of March, 1936
Soil Erosion Figure 3.12: (a) a natural forested slope (b) the same slope following a clearcut
Soil Erosion Figure 3.12: (c) the same slope after conversion to farmland (b) the same slope following urbanization
Soil Erosion 1968 motorcycles first come to Deer Creek near Bakersfield, CA 1972 after only 4 years of ORV use little vegetation or topsoil remains
Soil Erosion ORV users increased from 21 to 38 million between 1982 and 1992 ATVs rip through a marsh in West Virginia Great Grizzly Hike, Montana
Soil Erosion 1985 photo of bulldozer and jeep tracks in Alaskan tundra made in 1946