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Origins of agriculture

o. Soils Utube videoclips Soil Horizons http://www.youtube.com/watch?v=YQhyMsisRD8 Soil Stories http://www.youtube.com/watch?v=Ego6LI-IjbY. Origins of agriculture. Agriculture originated independently in several regions. Soil as a system.

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Origins of agriculture

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  1. o

  2. SoilsUtube videoclipsSoil Horizons http://www.youtube.com/watch?v=YQhyMsisRD8Soil Storieshttp://www.youtube.com/watch?v=Ego6LI-IjbY

  3. Origins of agriculture Agriculture originated independently in several regions.

  4. Soil as a system Soil is a complex mixture of organic and inorganic components.

  5. Soil formation • Parent material: starting material affects composition of the resulting soil. • It can include bedrock, the solid rock that makes up the Earth’s crust. • Weathering: the processes that break down rocks and minerals, and the first step in soil formation. • Erosion: the movement of soil from one area to another.

  6. Three kinds of weathering • Physical or mechanical • Chemical • Biological

  7. Soil profile • Consists of layers called horizons • Simplest: A = topsoil B = subsoil C = parent material • But most have O, A, E, B, C, and R

  8. Soil profile • O Horizon: Organic or litter layer • A Horizon: Topsoil; mostly inorganic minerals with some organic material and humus mixed in; crucial for plant growth • E Horizon: Eluviation horizon; loss of minerals by leaching, a process whereby solid materials are dissolved and transported away • B Horizon: Subsoil; zone of accumulation or deposition of leached minerals and organic acids from above • C Horizon: Slightly altered parent material • R Horizon: Bedrock

  9. Soil characterization • Soil can be characterized by color and several other traits: • Texture • Structure • pH

  10. Soil texture • Determined by size of particles • Three main categories: Clay = particles < 0.002 mm diameter Silt = particles 0.002–0.05 mm diameter Sand = particles 0.05–2.0 mm diameter • Best for plant growth is loam, an even mix of these three types.

  11. Soil texture

  12. Soil structure • Soil structure: a measure of the “clumpiness” of the soil • Soil pH: the degree of acidity or alkalinity, which influences a soil’s ability to support plant growth

  13. World soil conditions Soils are becoming degraded in many regions.

  14. Regional soil differences and agriculture • Soil and soil profiles vary from place to place, with implications for agriculture. • Amazonian rainforest soil = lots of rain; leaches nutrients from topsoil out of reach of plant roots. Other nutrients taken up by lush vegetation, leaving little in soil. • Thus when farmed, soil gives out after a few years. • Kansas prairie soil = low rainfall keeps nutrients in topsoil, where plants take them up and recycle them back into soil when they die. Topsoil rich and productive.

  15. Swidden agriculture In swidden agriculture, tropical forest is cut, the plot is farmed for 1-2 years, and the farmer moves on to clear another plot, leaving the first to regrow into forest.

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