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Published byJulian Pearson Modified over 9 years ago
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Food and Agriculture How to feed the ever expanding population Currently 5.8 billion 30 years 12 billion
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Modern methods in Agriculture Green Revolution Blue Revolution
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What’s needed to grow food? soil - the outer weathered layer of the earth's crust. Water Light nutrients
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Soil contains both Biotic and Abiotic Components Topsoil is the upper 1 ft of land that is usable for plant growth Composition is clay:sand:silt defines the character of the soil Topsoil varies in different Biomes –Grasslands are the riches –Tropical Rainforest are some the poorest
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BIOTICABIOTIC HUMUSSILT (0.02-0.05mm) Insect, Worms Nematodes Sand (0.05-2 mm) Bacteria Protista Symbiotes Clay (<0.02 mm) Charged
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organic matter - typically about 1% in nature litter - partially decayed organic matter on the soil surface. humus - highly decomposed, fine, amorphous organic matter in the soil.
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Functions of Organic Matter: 1) stabilizes soil structure 2) increases water retention and availability 3) increases drainage and aeration 4) increases cation exchange capacity 5) supplies nutrients upon decay (only if low C:N ratio) 6) stabilizes pH 7) food source for microorganisms
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Bacteria and Fungi Decompose Organic Matter Micorrhizal Symbiotes (tree and fungi) enhance mineral uptake into plants Worms, Nematode and Insects decompose organic matter and aerate the soil
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Soil Horizon
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A Horizon or topsoil - highly weathered - abundant life, therefore, high in organic matter - dark colored plow pan - a compacted impermeable layer in the A horizon due to repeated plowing or tilling (approx. 6" deep) B Horizon or subsoil - less weathered; higher in clay - less life, therefore, low in organic matter - lighter colored clay pan - impermeable layer high in clay. hard pan - impermeable layer high in iron. C Horizon or parent material - little weathered - little life, except deep rooted plants and little to no organic matter D Horizon or bedrock - rock base
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TYPICAL AGRICULTURAL SOIL Agriculturally productive soil is a balanced mixture of sand, silt, and clay. Riches farming soils: grasslands (Mollisols) deciduous forest (Alfisols)
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Land Degradation Overgrazing Deforestation Agricultural activities Overexploitation Industrialization
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water and wind are the main agents of erosion Trees and Ground Cover Prevent erosion.
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Why has 100 years of farming in the U.S. resulted in a loss of ½ of all cropland? Row crops Deep plowing Heavy herbicide use (no ground cover) Machine made gullies Chemical fertilizer No rotation of crops monoculture
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72% of all fresh water (rivers, lakes and ground water) is used for irrigation Over-watering leads to –Loss of Oxygen –Salinization
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Fertilizers Provide Inorganic Nutrients Major: N, K, P, C, Mg,S Applied Fertilizer –1950: 20 kg/ha –1990:91kg/ha Phosphates and nitrates from farm field and cattle feed lots are aquatic pollutant.
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Alternative Ways to Fertilize Manure Crop residues Ashes Composted refuse Green manure –*nitrogen fixing crops
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Climate: The greenhouse effect Increasing CO 2 increases productivity
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