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Soil Types and Textures
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Definitions Soil Texture The way a soil feels A name given a textural group based on the relative proportions of each size of soil particle
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Definitions Aggregate Mass or cluster of soil particles such as a clod, crumb or granule Soil Structure The combination or arrangement of soil particles into aggregates
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Objectives Define aggregate, soil structure, and soil texture Identify and describe the three basic soil particles Identify the major textural classes
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SOIL - Fundamental Concepts Prepared by Earl D. Lockridge National Soil Survey Center Lincoln, NE http://soils.usda.gov/education/resources/k_12/tools.html
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What is Soil? Geologic definition: Loose surface of the earth as distinguished from solid bedrock (support of plant life not required). Traditional definition: Material which nourishes and supports growing plants (includes rocks, water, snow, air).
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Air 25% Mineral Matter 45% Water 25% Organic Matter 5% SOIL o Component definition: Mixture of mineral matter, organic matter, water, and air.
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SOIL Soil Taxonomy definition: Collection of natural bodies of the earth’s surface, in places modified or even made by man or earthy materials, containing living matter and supporting or capable of supporting plants out of doors. (Its upper limit is air or shallow water and its lower limit is the depth to which soil weathering has been effective.)
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Soil Taxonomy At the highest level, soils can be recognized in one of 12 categories known as orders. For more information: http://soils.ag.uidaho.edu/soilorders
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SOIL As a portion of the landscape: Collection of natural bodies occupying portions of the earth’s surface that support plants and that have properties due to the integrated effect of climate and living matter, acting upon parent material, as conditioned by relief, over periods of time.
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Soil Pedon – A unit of soil Smallest unit than can be called a soil. A three-dimensional sample that extends from the soil surface to the deepest roots Area covered by a pedon varies from 10 - 100 square feet, depending on changes in soil properties.
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Polypedons – units of soil Groups of pedons with very similar characteristics that are closely associated in the landscape are called polypedons. Polypedons that have a common set of characteristics that fall within a particular range are referred to as a soil series Soil series are the basic units used to map soils The Cooperative Soil Survey (http://soils.missouri.edu/tutorial/page1.asp)
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Physical Properties of Soil Soil texture Soil structure Soil color Bulk density
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Three Fractions of Mineral Matter Sand Silt Clay
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Soil Particles Sand Largest of the soil particles Feel “gritty” Silt Medium sized Feel soft, silky, or “floury” Clay Smallest particles Feel “sticky”
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USDA Texture Triangle
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12 Soil Texture Classes Sand (S) Loamy Sand (LS) Sandy Loam (SL) Loam (L) Silt Loam (SIL) Silt (SI) Sandy Clay Loam (SCL) Silty Clay Loam (SICL) Clay Loam (CL) Sandy Clay (SC) Silty Clay (SIC) Clay (C) Compositions of each of the 12 texture classes is defined by the USDA Soil Triangle
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Examples of Soil Structure
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Aspects of Soil Structure The arrangement into aggregates of desirable shape and size The stability of the aggregate The configuration of the pores
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Factors that Affect Soil Structure Kind of clay Amount of organic matter Freezing and thawing Wetting and drying Action of burrowing organisms Growth of root systems of plants
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Effects of Bulk Density Engineering properties Water movement Rooting depth of plants
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Soil Color Indicator of different soil types Indicator of certain physical and chemical characteristics Due to humus content and chemical nature of the iron compounds present in the soil
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Major Forms of Iron and Effect on Soil Color FormChemical FormulaColor Ferrous oxideFeOGray Ferric oxide (Hematite)Fe 2 O 3 Red Hydrated ferric oxide (Limonite)2Fe 2 O 3 3H 2 OYellow
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Soils are maps Soil Series or Soil Map Units: Soil Series a group of soils that are similar in texture and profile. This is the finest level of soil classification. Soil Map Units are groupings of soils that occur together and it is difficult to draw lines between where the individual series occur. Therefore, a group of series are often grouped for mapping reasons. Soil maps – applied to ecological sites
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Ecological Sites are based on different topographic settings
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