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S. DEPARTMENT OP AGRICULTURE <br />TURAL RESOURCES CONSERVATION SERVICE <br />CONSTRUCTION MATERIALS <br /> <br />Endnote -- CONSTRUCTION MATERIALS <br />PAGE 2 OF 3 <br />O2/18J97 <br />RECEft~/ED <br />APR`s 10 2002 <br />Oiv(siaa afMimewls end Geofopy <br />This report gives information about the soils as a source of roadfill, sand, gravel, and topsail. The soils are rated <br />'Good', 'Fair', or 'Poor' as a source of roadfill and topsoil. That' are rated as a 'Probable' or 'Improbable' <br />source of sand and gravel. The ratings are based on soil properties and site features that affect the removal of the <br />soil and its use as construction material. Normal comvaction, minor processing, and other standard construction <br />practices are assumed. Each soil is evaluated to a depth of 5 or 6 feet. <br />Roadfill is soil material that is excavated in one place and used in road embankments in another place. In this report, <br />the soils are rated as a source of roadfill for low embankments, generally less khan 6 feet high end less <br />exacting in design than higher embankments. the ratings are for the soil material below the surface layer to a <br />depth of 5 or 6 teat. It is assumed that soil layers will be mixed during excavating and spreading., Many soils have <br />layers of contrasting suitability within th¢ir profile. The report entitled Engineering Index Properties is also available <br />and iY provides detailed information about each soil layer. This information can help determine the suitability of each <br />later for use as roadfill. the performance of soil after it is stabilized with lime or cement is not considered in <br />the ratings. <br />the ratings are based on soil Properties, site features, and observed performance of the soils. The thickness of <br />suitable material is a major consideration. The ease of excavation is affected by large stones, a high water table, <br />and slope. How well the soil performs in place after it has been compacted and drained is determined by its strength (as <br />inferred from the engineering classification of the soil) and shrink-swell potential. <br />Soils rated 'Good' contain significant amounts of sand or gravel or both. They have at least 5 feet of suitable <br />material, a low shrink-swell potential, few cobbles and stones, and slopes of IS Percent or less. Depth to the <br />water table is more than 3 feet <br />Soils rated 'Fair' have more than 35 percent silt- and clay-sized particles and have a plasticity of less than I0. <br />They have a moderate shrink-swell potential, slopes of 15 to 25 Percent, or many stones. Depth to the water table is 1 <br />to 3 feet. <br />Soils rated 'Poor' have a vlasticitr index of more than 10, a high shrink-swell potential, many stones, or slopes of <br />more than 25 percent. They are wet, and the depth to the water table is less than 1 foot. These soils may have <br />layers of suitable material, but the material is less than 3 feet thick. <br />Sand and gravel are natural aggregates suitable for Commercial use with a minimum of processing. Sand and <br />gravel are used in many kinds of construction. Specifications for each use vary widely. In this report only <br />the probability of finding material in suitable quantity is evaluated, the suitability of the material for specific <br />purvoses is not evaluated, nor are factors that aftect excavation of the material, The properties used to evatuate <br />the soil as a source of sand or gravel are gradation of grain sizes (as indicated by the engineering classification <br />of the soil), the thickness of suitable material, and the content of rock fragments. Kinds of rack, acidity, and <br />stratification are given in the soil series descriptions. Gradation of grain sizes is given in the fngineerin9 Index <br />Properties report. <br />A soil rated as a 'Probable' source has a layer of clean sand and gravel or a layer of sand or gravel that contains <br />up to 12 percent silty fines. This material must be et least 3 feet thick and less than 50 percent, by weight, large <br />stones. All other soils are rated as an 'Improbable' source. Coarse fragments of soft bedrock, such as shale and <br />silt st one, are not considered to be sand and gravel. <br />