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Web Soil Survey <br />Page 1 of 2 <br />�'•- � . -e a I*a� - <br />Contact Us Subscribe Archived Soil Surveys Soil Survey Status Glossary Preferences Link Logout Help n A A <br />Area of Interest (AOI) Soil Map Soil Data Explorer Download Soils Data Shopping Cart (Free) <br />View Soil Information By Use: All Uses Printable Version I Add to Shopping Cartl <br />Intro to Soils Suitabilities and Limitations for Use Soil Properties and Qualities Ecological Site Assessment Soil Reports <br />Search <br />Map— Hydrologic Group <br />Soil <br />Q � J <br />J� 21 M —0 A <br />Properties and Qualities Ratings <br />- <br />r. <br />Open All Close All <br />Soil Chemical Properties <br />Soil Erosion Factors <br />Soil Physical Properties <br />Available Water Capacity <br />- <br />Available Water Storage <br />Available Water Supply, 0 to 100 cm <br />*' <br />Available Water Supply, 0 to 150 cm <br />w' <br />,3 <br />°`%.,� <, <br />5008 ! _ <br />8 <br />Available Water Supply, 0 to 25 cm <br />Available Water Supply, 0 to 50 cm <br />Bulk Density, 15 Barxs <br />Bulk Density, One -Tenth Bar <br />Bulk Density, One -Third Bar <br />Warning: Soil Ratings Map may not be valid at this scale. <br />You have zoomed in beyond the scale at which the soil map for this area is intended to be used. Ma r <br />Linear Extensibility <br />soils is done at a particular scale. The soil surveys that comprise your AOI were mapped at 1:24,00 . <br />design of map units and the level of detail shown in the resulting soil map are dependent on that m <br />Liquid Limit <br />Enlargement of maps beyond the scale of mapping can cause misunderstanding of the detail of mar p <br />accuracy of soil line placement. The maps do not show the small areas of contrasting soils that coul J I <br />been shown at a more detailed scale. <br />Organic Matter <br />Percent Clay <br />Tables — Hydrologic Soil Group — Summary By Map Unit <br />Summary by Map Unit — Mesa County Area, Colorado (C0680) <br />Percent Sand <br />Map unit Map unit name Rating Acres in Percent of <br />Percent Silt <br />symbol AOI AOI <br />66 Bodot -Sill -Rock outcrop complex, 5 to 25 percent slopes, C 30.0 56.8% <br />Plasticity Index <br />very bouldery <br />904 Rock outcrop, 50 to 99 percent slopes D 22.8 43.2 <br />Saturated Hydraulic Conductivity (Ksat) <br />Totals for Area of Interest 52.8 100.0 <br />Saturated Hydraulic Conductivity (Ksat), Standard <br />Classes <br />Description — Hydrologic Soil Group <br />Hydrologic soil groups are based on estimates of runoff potential. Soils are assigned to one of four <br />Surface Texture <br />groups according to the rate of water infiltration when the soils are not protected by vegetation, are <br />thoroughly wet, and receive precipitation from long- duration storms. <br />Water Content, 15 Bar <br />The soils in the United States are assigned to four groups (A, B, C, and D) and three dual classes (A /D, <br />8 /D, and C /D). The groups are defined as follows: <br />Water Content, One -Third Bar <br />Group A. Soils having a high infiltration rate (low runoff potential) when thoroughly wet. These consist <br />Soil Qualities and Features <br />mainly of deep, well drained to excessively drained sands or gravelly sands. These soils have a high rate <br />of water transmission. <br />AASHTO Group Classification (Surface) <br />Group B. Soils having a moderate infiltration rate when thoroughly wet. These consist chiefly of <br />moderately deep or deep, moderately well drained or well drained soils that have moderately fine texture <br />Depth to a Selected Soil Restrictive Layer <br />to moderately coarse texture. These soils have a moderate rate of water transmission. <br />Group C. Soils having a slow infiltration rate when thoroughly wet. These consist chiefly of soils having a <br />Depth to Any Soil Restrictive Layer <br />layer that impedes the downward movement of water or soils of moderately fine texture or fine texture. <br />These soils have a slow rate of water transmission. <br />Drainage Class <br />Group D. Soils having a very slow infiltration rate (high runoff potential) when thoroughly wet. These <br />Frost Action <br />consist chiefly of clays that have a high shrink -swell potential, soils that have a high water table, soils <br />that have a claypan or clay layer at or near the surface, and soils that are shallow over nearly <br />impervious material. These soils have a very slow rate of water transmission. <br />Frost-Free Days <br />http : / /websoiIsurvey.nres.usda.gov /app /WebSoiISurvey.aspx 2/27/2014 <br />