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Soils, Infiltration, and On-site Testing

Soils, Infiltration, and On-site Testing

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Soils, Infiltration, and On-site Testing

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  1. Soils, Infiltration, and On-site Testing Presented by: Mr. Brian Oram, PG, PASEOWilkes UniversityGeoEnvironmental Sciences and Environmental Engineering DepartmentWilkes - Barre, PA 18766570-408-4619

  2. Soils Defined • Natural Body that Occurs on the Land Surface that are Characterized by One or More of the Following: • Consists of Distinct Horizons or Layers • The ability to support rooted plants in a naturalenvironment • Upper Limit is Air or Shallow Water • Lower Limit is Bedrock or Limit of Biological Activity • Classification based on a typical depth of 2 m or approximately 6.0 feet

  3. Another Definition of Soils • A Natural 3 - Dimensional Body at the Earth Surface • Capable of Supporting Plants • Properties are the Result of Parent Material, Climate, Living Matter, Landscape Positionand Time. • Soil Composed of 4 Components (mineral matter, organic matter, air, and water)

  4. Five Soil Formation Factors • Organisms • Climate • Time • Topography and Landscape Setting • Parent Material R

  5. Soil Food Web - Organisms • Micro & Macroscopic • Decomposition of Organic Matter • Animals Living in Soil • Vegetation Types • Human Activity • Redoximorphic Feature Formation Image Source: The University of Minnesota, 2003

  6. Climatic Elements(Energy & Precipitation) • Annual and Seasonal Rainfall • Temperature Range • Biologic Production and Activity • Weathering (Wind, Water, and Ice) • Translocation of Material

  7. Climate and Soil Development Image Source: University of Wisconsin, 2002

  8. Geologic Time Time

  9. Landscape and Relief(Soil Texture) A- Sandy Texture andLoamy SandB- Sandy Textures C- Clay Loam, Loam, Silt Loam Image Source: University of Wisconsin, 2002

  10. Landscape and Relief (Drainage) Water MovementSoil DrainageLandscape Configuration (Convex, Concave)ElevationWater Movement Image Source: NJ NRCS, 2002

  11. Parent Material • Geological Materials • Minerals and Rocks • Glacial Materials • Loess (wind blown) • Alluvial Deposits • Marine Deposits • Organic Deposits • Influences • Minerals Present • Colors • Chemical Reactions • Water Movement • Soil Development Glacial Material Bedrock

  12. Describing Soils • Soil Texture • Structure • Consistency • Soil Color • Coarse Fragment Content • Redoximorphic Features • other Diagnostic Properties

  13. Soil Texture The way a soil "feels" is called the soil texture. Soil texture depends on the amount of each size of particle in the soil. The three soil separates are sand, silt, and clay Sand are the largest particles and they feel "gritty." Silt are medium sized, and they feel soft, silky or "floury." Clay are the smallest sized particles, and they feel "sticky" and they are hard to squeeze.

  14. Soil Textural Triangle

  15. Soil Structures

  16. Water Movement and Structure

  17. Soil Consistency Soil Consistency the feel of the soil, reflecting relative resistance to pressure: eg friable, firm, hard, loose, plastic. The term soil consistency is used to describe the resistance of a soil at various moisture contents to mechanical stresses or manipulations. It is commonly measured by feeling and manipulating the soil by hand.

  18. Consistency Terms

  19. Soil Color Munsell Notations In the Munsell system of notation, color characteristics are designated by three axes:Hue (the name of the color) Value (the darkness or lightness of the color) Chroma (the intensity, or strength of the color) For example, 10YR4/3 Hue (10YR), Value (4), Chroma (3) Color: brown In PA - The primary hues are typically 10YR and 7.5YR.

  20. SoilColor-Munsell Notation Red- indicates the presence of Fe-oxides (iron oxides). Grey- indicates the presence of elevated water tables and reduced Fe (iron).Black-indicates the presence of organic matter, Mn-oxides (manganese), or FeS (iron sulfides). Organic matter suggest the soil is nutrient rich and fertile. Iron sulfides occur in wetlands and associated with rotten egg odor. White- indicates the presence of carbonate or soluble salts.

  21. Soil Horizons • Layer of Soil Parallel to Surface • Properties a function of climate, landscape setting, parent material, biological activity, and other soil forming processes. • Horizons (A, E, B, C, R, etc) Image Source: University of Texas, 2002

  22. Soil HorizonsO- Organic Horizons • Organic Layers of Decaying Plant and Animal Tissue • Aids Soil Structural Development • Helps to Retain Moisture • Enriches Soil with Nutrients • Infiltration Capacity function of Organic Decomposition O Horizon Dark in Color Because of Humus Material - 1,000,000 bacteria per cm3

  23. Soil HorizonsA Horizons: “ Topsoil” • Mineral Horizon NearSurface • Accumulation of OrganicMaterial • Eluviation Process Moves Humic and Minerals form O Horizon into A horizon • Ap - Plowed A Horizon • Ab - Buried Horizon • Soil dark in color, coarser in texture, and high porosity A Horizon

  24. Soil Horizons: E HorizonsAlbic Horizon (Latin - White) • Mineral Horizon NearSurface • Movement of Silicate Clay, Iron, and Aluminum from the A Horizon through Eluviation • Horizon does not mean a water table is present, but the horizon can be associated with high water table , use Symbol Eg (gleyed modifier) • Underlain by a B (illuvial) horizon E Horizon

  25. Soil Horizons: B HorizonsZone of Maximum Accumulation • Mineral Horizon • Illuviation is Occurring - Movement into the Horizon • B Horizon Receives Organic and Inorganic Materials from Upper Horizons. • Color Influence by Organic, Iron, Aluminum, and Carbonates • Bw - Weakly Colored or Structured • Bhs- Accumulation of illuvial organic material and sesquioxides • Bs- Accumulation of sesquioxides • Bt- Translocation of silicate clay • Bx- Fragipan Horizon, brittle Bhs Horizon Bs Horizon Bw Horizon

  26. Soil Horizons: Bx and Bt Horizons Horizons Indicate Reduced Infiltration Capacity and Permeability Bx: B horizon with fragipan, a compact, slowly permeable subsurface horizon that is brittle when moist and hard when dry.Prismatic soil structure, mineral coatings and high bulk density Area of Highest Permeability along Prism Contact Bt: Clay accumulation is indicated by finer soil textures and by clay coating peds and lining pores

  27. C- HorizonsDistinguished by Color, Structure, and Deposition • Mineral Horizon or Layer, excluding Rock • Little or No Soil-Forming • May be Similar to Overlying Formation • May be Called Parent Material • Layer can be Gleyed • Developed in Place or Deposited

  28. R- Horizons • Hard, Consolidated Bedrock • Typically Underlies a C Horizon, but could be directly below an A or B Horizon. R Horizon

  29. Soil Structure and Horizon

  30. Source of Soils Data Soil Surveys in GIS Format Soil Survey Maps

  31. Soil Hydrologic Cycle Source: Vepraskas, M.J, et. Al. “ Wetland Soils”, 2001.

  32. Soil Drainage Class and Soil Group Soil Drainage Class - Refers to Frequency and Duration of Periods of Saturation or Partial Saturation During Soil Formation. There are 7 Natural Soil Drainage Classes. Hydrologic Soil Group-Refers to Soils Runoff Producing Characteristics as used in the NRCS Curve Number Method. There area 4 Hydrologic Soil Groups (A, B, C, D).

  33. Group A and B • Group A is sand, loamy sand or sandy loam types of soils. It has low runoff potential and high infiltration rates even when thoroughly wetted. Deep, well to excessively drained sands or gravels and have a high rate of water transmission. Root Limiting / Impermeable layers over 100 cm or 40 inches ***************** • Group B is silt loam or loam. It has a moderate infiltration rate when thoroughly wetted. Moderately deep to deep, moderately well to well drained soils with moderately fine to moderately coarse textures. Root Limiting / Impermeable e layers over 50 to 100 cm or 20 to 40 inches Group A- Well Drained

  34. Group C and D • Group C soils are sandy clay loam. They have low infiltration rates when thoroughly wetted and consist chiefly of soils with a layer that impedes downward movement of water and soils with moderately fine to fine structure. Perched water table 100 to 150 cm or 40 to 60 inches; root limiting 20 to 40 inches. ***************** • Group D soils are clay loam, silty clay loam, sandy clay, silty clay or clay. They have very low infiltration rates when thoroughly wetted and consist chiefly of clay soils with a high swelling potential, soils with a permanent high water table, soils with a claypan or clay layer at or near the surface and shallow soils over nearly impervious material ( < 20 inches). Group D - Poorly DrainedHighest Runoff Potential

  35. Definitions Infiltration - The downward entry of water into the immediate surface of soil or other materials. Infiltration Capacity- The maximum rate at which water can infiltrate into a soil under a given set of conditions. Infiltration Rate- The rate at which water penetrates the surface of the soil and expressed in cm/hr, mm/hr, or inches/hr. The rate of infiltration is limited by the capacity of the soil and rate at which water is applied to the surface. This is a volume flux of water flowing into the profile per unit of soil surface area (expressed as velocity). Percolation -Vertical and Lateral Movement of water through the soil by gravity.

  36. Infiltration Rate and Capacity Soil Factors that Control Infiltration Rate: - Vegetative Cover, Root Development and Organic Content - Moisture Content - Soil Texture and Structure - Porosity and Permeability - Soil Bulk Density and Compaction - Slope, Landscape Position, Topography

  37. Infiltration Rate (Time Dependent) Decreasing Infiltration Steady Gravity Induced Rate Infiltration with Time Rate is Initially High Because of a Combination of Capillary and Gravity Forces Final Infiltration Capacity(Equilibrium)- InfiltrationApproaches Saturated Permeability

  38. Infiltration Rate (Moisture) Infiltration Decreases with Time1) Changes in Surface and Subsurface Conditions2) Change in Matrix Potential3) Overtime - Matrix Potential Decreases and Gravity ForcesDominate - Causing a Reduction in the Infiltration Rate

  39. Measuring Infiltration Rate • Flooding (ring) Infiltrometers • Single ring • Double ring • Flooded Infiltrometers • Tension Infiltrometers • Rainfall-Runoff Plot Infiltrometers

  40. Measuring Infiltration Rate

  41. Single Rings Infiltrometers Cylinder - 30 cm in DiameterDrive 5 cm or more into Soil Surface or HorizonWater is Ponded Above the Surface Record Volume of Water Added with Time to Maintain a Constant Head Measures a Combination of Horizontal and Vertical Flow

  42. Double Rings Infiltrometers Outer Rings are 6 to 24 inches in Diameter (ASTM - 12 to 24 inches)Mariotte Bottles Can be Used to Maintain Constant HeadRings Driven - 5 cm to 6 inches in the Soil and if necessary sealed

  43. Other Infiltrometers Ponded Infiltrometers Tension InfiltrometerUnsaturated Flow Of Water

  44. Infiltration Rate by Soil Group/ Texture Source: Texas Council of Governments, 2003.

  45. Infiltration Rate Function of Slope & Texture Source: Rainbird Corporation, derived from USDA Data

  46. Infiltration Rate Function of Vegetation Source: Gray, D., “Principles of Hydrology”, 1973.

  47. Comparison Infiltration to Percolation Testing Percolation Testing Over Estimated Infiltration Rate by 40 to over 400%

  48. Infiltration (Compaction/ Moisture Level)

  49. Case 1 :Myers Proposed Development Worcester Township, Pennsylvania • Abbottstown Silt Loam, Deep to Moderately Deep, Somewhat Poorly Drained • Some Areas Shallow Depth to Firm Bedrock • Signs of Erosion • Low Surface and Near Surface Infiltration Rates Associated with Surface Smearing, Btx, Bx Horizons • BC/ C /R Horizons Higher Infiltration Rate. • Readington Silt Loam • Deep Moderately Well Drained • Low Infiltration Surface, Bd, and Btx • High Infiltration in C and R Horizons