Soils Soils are the result of weathering Mechanical Chemical Critical resources for food, timber, textiles... Waste filters Understanding soils is important for land-use planning, and engineering Zone of Leaching Idealized soil profile from a humid climate at middle latitudes Horizon Development and Climate Soil textural classes Topsoil ecosystem in a temperate climate Porosity and Permeability Water saturation and air space Nutrients to plant roots The Water Table The level below which the soil is saturated with water (no air space) Soil water Representative water budgets Deficiencies can be remedied by storage and irrigation Effect of climate on soil development The Principal Soil Types Effect of climate on soil types Temperature hot laterites hot pedocals pedalfers tundra soils cold undra soils low 50 cm/yr Precipitation cool high Principal soil types in the USA Effect of climate on soil types A typical pedocal with white caliche (CaCO3) deposits in a shallow B horizon Effect of climate on soils Making laterite bricks Tundra soil Laterite Temple at Angkor Wat Cambodia (700 yrs old) A Newer Classification of Soil Types Pf Pc Pf Pf, Pc L Pf, L 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 Universal Soil Loss Equation A = RKLSCP A = long-term average annual soil loss for site R = long-term rainfall runoff erosion factor K = soil erodibility index L = hill slope/length factor S = hill slope gradient (slope) factor C = soil cover factor P = erosion-control practice factor 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 Woods Grass Corn Fallow Soil Erosion for Various Uses Soil Lost (tons/km2/yr) % runoff ~0 0.12 10 6.5 18087 42 17050 49 Soil Erosion Number of dust storms during the month of March, 1936 Effects of logging in Madagasgar 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 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 Soil Erosion Salt accumulation due to irrigation in an arid climate: San Fernando Valley Worldwide Distribution of Salt-affected Soils Chemical Contamination of Soils Grain production levels off while population continues to grow Cleaning Up Chemical Contamination Combating Soil Degradation Combating Soil Degradation Combating Soil Degradation Strip-cropping and Contour plowing Combating Soil Degradation Rice terraces in Asia Combating Soil Degradation No-till Farming Soil Surveys and Adequate Planning