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SoIL IUIVll ll'l'lRl~lTA?IOl5 / for m~y ~p~l.o. lnfo~tt~ about ~b properties iud .elected u~, for ~cb LnterP~etOt fv~ ibet. · t. co . of Tb ,.. : S~O~ C~SS DISCII~S~ ~.Kik ~Ibo~ ! or L Slope Dq,crlptton ~tkr~ [ tall ~r l~ feet St~t~. C~l~ : ' [ 0 to 2 HOlily level Neirty l~e~ C ~ 6 to 12 Sloptnl Iolllnl lO to 25 St.~ Stee~ I :F [ ~r 2~ Ve~ 0reap Ve~ steep iI ~ ~l) i1~ dO ~.Ot Ilill~ltt tbl lled for oim~llni end teotJfll et t~ .~te of I~ciftc enit~ur~nj uockl tb ktn~s of [problw t~t my ~ ox~ctod. The .'t[mt.~ phy.tc.I .nd cMlcaJ pro. rtL., of tbs .o11 lT. Itv.n for t..utf.ce Layer..ubloi~. iud ~F~Y~nt Mterlot of · t~cil soil profile. Depths for otbr profiles of n particular 60 t~bb, ~0~, .of] ocient/0to Mmlly insect tb soil to t~t ~ptb or to bdr~k ~Jc~ver C~ass~lfhcac m tKlWs th ~M textural ilion, q~ Unified Ctoostft~tt~/: aM tb Amri~u Aoo~tatton ~E~of Id, slit, M cby tu th soil. h Unified ChsstfLutL. ti koe6 ~ irate I~e a~ phs* sO~i~ a~ f mt~fiod nct~dt~ to S~tu otse n~ ph0tictty. ~ ~s ~f~t tb ~rto~e of ~t h~7 ~lu~o. La.tut o~ t~ Soil hss~ Sb~e Wa. ~ (~.7 m.), Io. IO (2.0 m), Bo. ~0 (0.~ m.) ~rC~nt: I~ Il. mad. nM ~ut fires (sLit i~ thy) cie k eot~tod ft~ tbil bra. iud th~ liq, Id tisit, fro i pbottc to i liquid otnte. T~ phsticity i~x ia tb erotical difference ~t~e~ tk liquid limit and t~ pbotic iimit. It indicates tb ~ule of diet C~teUt within Wich ~i~li, ~br rites are: olNly= 0.~ to 0.20; ~toly sl~ - 0.20 to 0.6; ~rate - 0.6 to 2.0; ~Fo~oly ~lptd - 2.0 to 6.0; ~ptd -6. O to 20.0; iud ve~ rapid - ~re t~n 20.0. ¼bd leboutce testate lsd NiJor Lind laeoirct kress of the United Steres. AlrlevJtura Hildboo~ 296. ~e lxpertsint SCatlon, Corps of I.Itnlers, 19~3. Tho Unified Soil ,K,. 3-357, 2 v., iud Ap~ndlx I, VJcklbur8, Hiss. i Aeooctatioo of StiLe #tlbvay OfficLell, 1961. Standard SpoctficitLO~l for #18briny Kiterlels ~ods of Sampltug end Testifll.