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Published byRandell Douglas Modified over 8 years ago
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Weathering It is surface processes that break down rock Breaks rocks into smaller and smaller pieces Ex.) Sand, silt, clay The formation of soil depends on the amount of weathering that occurs
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Weathering: 2 types 1.) Mechanical: when rocks are broken apart by physical means Chemical make-up stays the same Different factors can be mechanical weathering 1.) Plants and animals: plants grow, roots wedge rocks apart Animals push rocks and soil to the surface 2.) Ice Wedging: ice forms in cracks and then expands 3.) Surface Area: increases the amount of chemical weathering
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Continued… 2.) Chemical Weathering: chemicals dissolve the minerals in the rocks and alter them Different factors affect chemical weathering Chemical composition is changed 1.) Natural acids: H 2 O and CO 2 mix, make weak acid Ex.) Dissolve calcite, destroys the rock marble 2.) Plant acids: acids made from decaying plants 3.) Oxygen: causes oxidation Oxidation is the same as rusting Ex.) magnetite rusting to limonite
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10-2: Rates of Weathering Takes a long time Different factors can increase weathering rates though Differential Weathering: softer, less weather resistant rocks wear away and leave harder more resistant rocks behind Natural selection of the rock cycle
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Different Factors: 1.Size and Surface Area: Larger the surface area the more weathering will occur Think of your face in the cold winter wind 2.Weather & Climate: Chemical weathering increases in warm, humid climates Water and temperatures also increases mechanical weathering Ex.) Frost Wedging, heat buckling 3.Elevation: Greater the slope the greater the mechanical weathering Higher the peaks are the more weathering occurs
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Ch. 10-3: Soil: Soil: weathered rock, decayed organic matter, mineral fragments, water, and air Can take thousands of years to form Can be 60m or a few cm thick There are 5 factors that affect soil formation: 1.) Climate 2.) Slope of land 3.) Types of rock 4.) Types of vegetation 5.) Amount of time rock has been weathered
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Soil Composition: We know what makes up soil Most organic matter comes from plants though, not dead animals When the plant and animal remains do decay by fungus and bacteria it becomes humus Serves as a great nutrient supply for plants Good surface soil has a ~50/50 mix of humus and rocky soil
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Soil Profile: Different layers of soil are called horizons All horizons together form a soil profile Horizon A: top layer Covered with litter (leafs, plant remain etc.) Known as topsoil Horizon B: middle layer Lighter then topsoil Nutrients are leached to this level Horizon C: bottom layer Lowest layer Not much organic material (light in color) Under C or in C is rock
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10-4: Soil Conservation What is it? Method to maintain soil fertility Soil provides: Minerals Housing Water Storage Soil Damage and Loss: Soil Erosion: movement of soil Water, wind, gravity How? 1.) vegetation is removed 2.) slopes are steepened
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Soil Conservation techniques 1.) Contour plowing 2.) Terracing 3.) No-till farming 4.) Cover crop
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