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Published byArron Blair Modified over 9 years ago
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Weathering / Soils http://youtu.be/Xdg1lpQfLbo
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Weathering The process by which natural forces break down rocks Erosion: The break up and transport of earth materials
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Mechanical Weathering The breaking up of rocks by physical forces Ice Wedging: water freezing, expanding and splitting rock Pressure release: (exfoliation) Inside pressure causes rock to expand when overlying burdens are removed Plant root growth: plant roots expand cracks Abrasion: wearing down by friction (moving water rubbing rocks against each other)
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Ice Wedging Root growth ExfoliationAbrasion
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Chemical Weathering Breakdown of rock by chemical reactions Dissolving: minerals dissolving in water or weak acids Rusting: Iron in rocks combining with oxygen to produce rust (iron oxide)
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Soil A mixture of weathered rock particles, organic matter, water and air Humus: decayed plant and animal material
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Soil Horizons A horizon: upper most layer (topsoil) containing the most humus. Darkest layer B horizon: little humus, brown to reddish brown, contains clay that washes down from A horizon C horizon: deepest layer, largest least- weathered rock particles, light yellowish brown
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Soil Properties Texture: size of particles in soil Sand: largest, visible, feels gritty Silt: smaller – microscopic, feels silky Clay: smallest – microscopic, feels sticky when wet
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Properties continued Color: comes from iron compounds and humus humus – black, iron – reddish original rock- yellows or tans bright colored soils drain well Pore space: the spaces between particles Chemistry: pH (acidity) determines how well nutrients dissolve
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