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Detailed Soil Survey of the Mount Revelstoke Summit Area.

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42TABLE 7.GUIDES FOR ASSESSING SOIL LIMITATIONS FOR ROADS AND PARKING LOTSThis guide applies to soils evaluated for construction and maintenance <strong>of</strong> roads and parking lots havingsome kind <strong>of</strong> surfacing, commonly gravel . They consist <strong>of</strong> : (1) underlying local soil material (ei<strong>the</strong>r cutor fill) called <strong>the</strong> subgrade ; and (2) gravel surface . They also are graded to shed water and have ordinaryprovisions for drainage . The roads are built mainly from <strong>the</strong> soil at hand, and cuts and fills are limited,usually less than 6 feet . Excluded from consideration in this guide are highways designed for fast-movingheavy trucks .Properties that affect design and construction <strong>of</strong> roads are : (1) those that affect <strong>the</strong> load supporting capacityand stability <strong>of</strong> <strong>the</strong> subgrade ; and (2) those that affect <strong>the</strong> workability and amount <strong>of</strong> cut and fill .The AASHO and Unified Classification, and <strong>the</strong> shrink-swell potential give an indication <strong>of</strong> <strong>the</strong> trafficsupporting capacity . Wetness and flooding affect stability . Slope, depth <strong>of</strong> bedrock, stoniness, rockiness,and wetness affect <strong>the</strong> ease <strong>of</strong> excavation and <strong>the</strong> amount <strong>of</strong> cut and fill to reach an even grade .<strong>Soil</strong> limitation ratings do not substitute for basic soil data or for onsite investigations .ItemsAffectingUseone to SlightDegree <strong>of</strong> <strong>Soil</strong> LimitationModerateevere<strong>Soil</strong> drainage Rapidlyl, well and mod- Imperfectly drained. Poorly and very poorlyclassl erately well drained . drained .Flooding None . Once in 5 years . More than once in 5 years .Slope 0 to 9% (AD) . 9 to 15% (E) . More than 15% (> E) .Depth to bedrock More than 40 inches . 20 to 40 inches . Less than 20 inches .Subgrade2 (Str .)a. AASHOGroup index30 to 4 . 5 to 8 . more than 8 .b . Unified GW, GP SW, GM, SM, C1 (with PI5 less than CL (with PI5 15 or more),soil classes and GC~+ and SC4. 15), ML, SP . CH, MH, OH, CL, Pt .Shrink-swell Low (PI5 less than 15) . Moderate (PI5 10 to 35) . High (PI5 greater than 20) .potential6Susceptibility Low (Fl, F2)6 . Moderate (F3)6 . High (F4)6 .to frost heave7Stoniness8 Stones greater than 5' Stones 2 to 5' apart . Stones less than 2' apart .apart .Rockiness8 Rock exposures greater Rock exposures 300 to Rock exposures less than 100'than 300' apart and 100' apart and cover 2 apart and cover greater thancover less than 2% <strong>of</strong> to 10% <strong>of</strong> <strong>the</strong> surface. 10% <strong>of</strong> <strong>the</strong> surface .<strong>the</strong> surface .1 . For an explanation <strong>of</strong> soil drainage classes see <strong>the</strong> System <strong>of</strong> <strong>Soil</strong> Classification for Canada (C .S .S .C .,1970), pp . 215-216 .2 . This item estimates <strong>the</strong> strength <strong>of</strong> a soil as it applies to roadbeds . When available, AASHO GroupIndex values from laboratory tests were used ; o<strong>the</strong>rwise <strong>the</strong> estimated Unified classes were used . Onunsurfaced roads, rapidly drained, very sandy poorly graded soils may cause washboard or rough roads .3 . Group Index values were estimated from information published by <strong>the</strong>1962), pp . 23-25 .4 . Downgrade to moderate if content <strong>of</strong> fines (lessthan 200 mesh) is greater than about 30% .5 . PI means plasticity index.6 .Inherent swelling capacity is estimated as low when <strong>the</strong> plasticity index is less than 15, medium when<strong>the</strong> plasticity index is 10 to 15 and high when <strong>the</strong> plasticity index is greater than 20 (Tarzaghi andPeck, 1967) . Gravelly and stony soils may not exhibit shrink-swell as estimated by <strong>the</strong> plasticityindex because <strong>of</strong> dilution <strong>of</strong> <strong>the</strong> fines with coarse fragments . In <strong>the</strong>se situations decrease a severelimitation to moderate and a moderate limitation to slight .7 .Frost heave is important where frost penetratesportable by capillary movement is sufficient tobility classes are taken from <strong>the</strong> United Statesreproduced from <strong>the</strong> above article.below <strong>the</strong> hardened surface layer and moisture transformice lenses at <strong>the</strong> freezing front . The suscepti-Army Corps <strong>of</strong> Engineers (1962), pp . 5-8 . Table 11 is8 . See also definitions for rockiness and stoniness in <strong>the</strong> System <strong>of</strong> <strong>Soil</strong> Classification for Canada (C .S .S .C .,1970), pp . 213-214 .

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