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The Nature of Soil Chapter 7, Section 2 The Formation of Soil  What is Soil?  Mixture of weathered rock, decayed organic matter, mineral fragments, water, and air. Formation of Soil  How does soil form?   Weathering breaks down rocks and minerals into fragments. Plants and animals add organic material to the soil.   May take thousands of years to form. May range in thickness from a few centimeters to 60 meters thick. Composition of Soil  Rock and Mineral Fragments   Mostly small particles of sediment such as clay, silt, and sand. Some larger rocks can be present. Composition of Soil  Organic Material  Dead and Decaying Plants    Make up the majority of organic material. Leaves, stems, roots, etc. Dead and decaying animals and microorganisms Composition of Soil  Organic Material  Humus  Dark colored material formed from decayed plants and animals.    Decay process is due to bacteria and fungi in the soil. Serves as a nutrient source for plants. Mixed with other components of soil by burrowing rodents, worms, and insects.  Good-quality surface soil has about 50% humus. Composition of Soil  Water and Air  Fill the spaces between the particles of soil. Soil Profile  Horizons  Different layers of soil.   Typical soils have an A, B, and C horizon. All the horizons form a soil profile. Soil Profile  A Horizon      Top layer of soil. Also known as topsoil. Contains a higher percentage of humus. Generally dark and fertile. May be covered with litter.  Litter consists of leaves, twigs, and other organic material.  Helps prevent erosion and holds water. Soil Profile  B Horizon  Contains material moved down from the A horizon through leaching.  Leaching is the removal of minerals that have been dissolved in water. Soil Profile  C Horizon     Consists of partially weathered rock. Coarser than other horizons. Contains less humus. Similar to the parent rock found beneath the horizon. Soil Types  What affects formation of soil and soil type?       Glaciation Climate Type of parent rock Type of vegetation Slope Time Soil Types  Glacial Deposits   Unsorted mass of clay, silt, sand, and boulders. Creates very fertile soil. Soil Types  Climate  Desert soils    Prairie soils   Contain little organic material. Thinner than soils in wet climates Thick, dark A horizons due to the large number of grasses. Temperate Forest soils  Thinner A and B horizons enriched in minerals due to leaching. Soil Types  Parent rock   Affects the type of soil that develops. Can also affect the vegetation that grows in the area. Soil Types  Slope  Steep slopes   Soil horizons are often poorly developed. Bottomland  Soils are often thick, dark, and full of organic material. Soil Types  Time   At first, soil characteristics are determined by the characteristics of the parent rock. Over time, soil resembles the parent rock less and less.