Let’s dish some dirt! Please get out paper for notes. Please read the board. Dishing the dirt! Soil Resources complex mixture of inorganic minerals (clay, silt, sand), decaying matter, & living organisms. • potentially renewable resource; • typically 200–1000 years to form 2.5 centimeters (1 inch) of topsoil. © Brooks/Cole Publishing Company / ITP Soil formation Physical Freeze/thaw cycle Weathering/erosion Biological Lichen action Decomposition The granite rock cracks and breaks off as it is heated and cooled each day and season. This is the first step in the formation of soil. Physical: Freeze/thaw cycle Decomposition: adding carbon, N,P,K during soil formation Soil Food Webs are complex! • soil food webs complex; • figure shows simplified soil food web. Fig. 13–15 © Brooks/Cole Publishing Company / ITP Soil Nutrient Cycling pathways of nutrients in soils Fig. 5–15 © Brooks/Cole Publishing Company / ITP Generalized Soil Profile • O horizon: leaf litter • A horizon: topsoil • B horizon: subsoil • C horizon: parent material bedrock © Brooks/Cole Publishing Company / ITP Examples of Soil Profiles Fig. 13–17 a & b © Brooks/Cole Publishing Company / ITP More Examples of Soil Profiles Fig. 13–17 c & d © Brooks/Cole Publishing Company / ITP Ecosystem comparison! – rich soil (deep, lots of humus, nutrients) Tropical Rainforests – poor soils! Rapid decomposition increases rate of nutrient uptake! Prairies Soil types determined by Particle size Chemical composition (bedrock material) Color pH Soil texture Sand Silt Clay Landfills? Wetlands? Soil Texture determined by particular mix of clay, silt, & sand Fig. 13–18 © Brooks/Cole Publishing Company / ITP Erosion movement of soil, especially litter & topsoil, from one place to another • makes soil less fertile & less able to hold water; • topsoil eroding faster than it forms in about one–third of the world's cropland. © Brooks/Cole Publishing Company / ITP Soil Erosion Fig.13–20 © Brooks/Cole Publishing Company / ITP 1930s Dust Bowl Fig.13–21 © Brooks/Cole Publishing Company / ITP Desertification causes: • overgrazing; • deforestation & devegetation; • surface mining; • poor irrigation; • salt buildup; • farming unsuitable terrain; Fig.13–22 • soil compaction. © Brooks/Cole Publishing Company / ITP Problems of Irrigation • Salinization: salts build up to levels that decrease yields or prevent cultivation • Waterlogging excess irrigation water raises water table & lowers crop productivity Fig.13–23 © Brooks/Cole Publishing Company / ITP Soil Conservation reduces soil erosion & restores fertility some methods: • conservation–tillage • terracing, contour farming, strip cropping, alley cropping • organic fertilizers • crop rotation © Brooks/Cole Publishing Company / ITP Conservation-Tillage Farming • minimizes soil disturbance • uses special tillers or no–till methods that inject seeds, fertilizers, & herbicides in unplowed soil • poses new problems of heavy herbicide use © Brooks/Cole Publishing Company / ITP Some Means to Prevent Erosion • terracing protects steep slopes • contour farming follows natural land contours • strip cropping maintains strips of different vegetation between crops • alley cropping grows crops between rows of trees © Brooks/Cole Publishing Company / ITP Some Means to Prevent Soil Degradation • organic fertilizers: manure, "green manure" = plant matter, & compost • decreased use of inorganic fertilizers • crop rotation: alternating between different crops & fallow times; planting crops that restore nutrients © Brooks/Cole Publishing Company / ITP Pesticides – “To use or not to use?” What you already know about pesticides . . . . The case FOR pesticides The case AGAINST pesticides A spectrum of choices Conventional Agriculture Least sustainable Integrated Pest management Organic farming Biodynamic agriculture most sustainable Integrated pest management Overarching philosophy: Eradication of pests is not possible, so the goal must be pest suppression. General practice: Monitor pest populations. When damage of crops will cost more than the cost of action, IPM managers take steps to control pests. Pesticides will be used only as a last resort. Cultivation/physical approaches Crop rotation – non-legume, legume, fallow field/cover crop Cultivation/physical approaches Hedge rows provide shelter for beneficial insects, birds and other pest predators Cultivation Approaches Delayed planting If the pest can’t find the crop at the right part of it’s life cycle, the pest can’t use the crop. Cultivation Approaches Polyculture, intercropping and agroforestry – increasing diversity of crops! Biological pest control Release beneficial insects (pest predators), encourage insectivorous birds Other predators Biological Pest control Release of sterile males: mate with females, no offspring produced. Chemical Pest control Pheromones: used in bait traps to lure insects away from crops Chemical control Hormone disruptors prevent molting or development to next stage. Chemical control As a last resort, IPM farmers will use pesticides (herbicides, insecticides, rodenticides, fungicides) IPM approaches Advantages Disadvantages