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Published byBenjamin Gregory Modified over 8 years ago
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From Bedrock to Soil
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Bellringer In your notebook answer the following questions: Has there always been soil on Earth? What makes soil valuable to humans?
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Describe the source of soil. Explain how the different properties of soil affect plant growth. Describe how various climates affect soil. Objectives
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Soil is a loose mixture of small mineral fragments, organic material, water, and air that can support the growth of vegetation. Where do plants live? Where do some insects live? Defining Soil
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Soil Formation Soil is an important natural resource It is found almost everywhere on Earth Exactly what is it?
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Soil Formation Soil forms in layers during the process of its development. The parent rock is the solid bedrock from which weathered pieces of rock first break off. The smallest pieces of weathered rock, along with living and dead organisms, remain in the very top layer. Rainwater seeps through this top layer of materials, dissolves soluble minerals, and carries them into the lower layers of the soil.
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Residual Soil Soil that remains above its Parent rock. Transported Soil Soil that is blown or washed away fomr its parent rock. Types of Soil
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Soil Layers Topsoil Animals, bacteria, fungi. Humus Subsoil Smaller particles than parent material but not much life Parent Material Slightly weathered bedrock Bedrock Solid layer of rock
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Soil Layers
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Soil Profiles What is a soil profile? A vertical sequence of soil layers A soil horizon is a distinct layer, or zone, within a soil profile. There are three major soil horizons: A, B, A, B, and C. Horizon A contains high concentrations of organic matter and humus. Horizon B contains subsoil that are enriched with clay minerals. Horizon C, below horizon B and directly above solid bedrock, contains weathered parent material. The O horizon is organic material, that may or may not be present.
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Humus The organic material formed in soil from the decayed remains of plants and animals. Acidity Soils can be acidic or basic. The pH scale is used to measure how acidic or basic a soil is. Colors of plants flowers may be due to pH of soil Leaching The removal of substance that can be dissolved from rock and soil due to water passing through. Horizon Information
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Why does soil feel different? Many different particles give soil its texture Soil contains: Sand Silt Clay
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Soil Texture
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Soil Textures Particles of soil are classified according to size as being clay, silt, or sand, with clay being the smallest and sand being the largest. The relative proportions of these particle sizes determine a soil’s texture. The texture of a soil affects its capacity to retain moisture and therefore its ability to support plant growth.
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Soil Textures To determine the texture of a soil sample, find its percent for sand, silt, and clay. The texture of the soil will be where all three lines intersect.
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Infiltration How well can water move through the soil. Leaching Soil Texture and Water
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Soil Fertility A measure of how well a soil can support plant growth Factors involved include: Availability of nutrients/minerals Precipitation Topography Acidity Number of microorganisms present
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The topography of a region affects the thickness of developing soil. Soils on slopes tend to be thin, coarse, and infertile. Soils formed in lower areas, such as in valleys, are thick and fertile. Topography of Soil
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Soil Color Factors that determine soil color include: Climate Soil’s composition Topsoil-usually dark (rich in humus) Red/yellow soils-caused by iron minerals oxidizing Yellow soils are often poorly drained, associated with environmental problems Gray/bluish soils-poorly drained, constantly wet, lacking in oxygen
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Soil Types Polar Soils Form at high latitudes and high elevations. Located in Greenland, Canada, Antarctica. No distinct horizons, very shallow soil. Just below the soil the ground is permanently frozen-known as permafrost. Permafrost in Denali
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Soil Types Temperate Soils Lots of variation Support forests, grasslands, prairies Amount of rainfall determines what grows in this type of soil Grasslands-lots of humus-soil is rich and fertile Forests-soil is less deep/less fertile, containing clays and iron oxides (Eastern US) Prairies-dry soil-lots of grasses and bushes
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Soil Types Desert Soils Very little precipitation High levels of salts Limited vegetation Little or no organic matter Very thin topsoil (A horizon) Light colored and coarse soil
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Soil Types Tropical Soils High temperatures, heavy rainfall Soil is intensely weathered, infertile Source of ores (iron), but not great for growing plants
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In your notebook answer the following questions; 1.What is the difference between transported soil and residual soil? 2.What does each of the following mean: 1.Soil texture 2.Soil fertility 3.Soil structure Recap
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