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<br />1.E. CEF;? "E'.f SE AG9IC;LiURE PAGE 2 OE 2
<br />!1~-';=:=_ ._~:U.°,C ES CO~VSERVAifOV SEnY1C~ 02/7197
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<br />;N;IHEEPi'I, I'7DE( Pr.GPEH1fES
<br />..r:.z -- ='~;IYEE'-+G I;'DE;( p~OPESifES
<br />~.. _.,. ; 7:'re5 3S. W3C2; Of the 2nG:nE?ring C!3;i1f1C3 C!C:'. 20d Of the ra r.ge J* lnde% prD D2i a2$ fJr tn2
<br />'3;Jr i3; ['` ;.` ?3C11 s l in Che S'!i Vey 2re3. ~'1oSC ;C11; h3':2 ]3'/°ii Gf COn tr?S C!GJ~ Gr7;?rC1e5 W1 Ci1in ChE UD^er
<br />, .. ] -eI,
<br />;E% Y :,, ..? U,Cer 3n,'. 17Aef DCUOd IfleS ]f each L=:'2' is :ndi^3:2d, ih2 r3nG2 1G :2DCh 3nv 1!liJf ni i!J~l un G:Oef
<br />r:;y :'3; ,` each later ]re given in the Jublish? Soi! Surv?y fcr zach sail s?rigs un13r °Seil S?rie; and ihzir
<br />. .. : ,~^ :^ the Sianlard Cefi9i US2d D}' tree S.j. .?C31:Y_a: Ji hg: ;: J!tC: 2. .i.3:? :2r 1; 3f2 ':?fl•i 2'1
<br />3:]:r ~:'3 :7 ;. ,;; ?;3;2; 0' S.1Od, S!l:, and C!3y f'3L t::l Jf ih2 ;C1. :n3 `. :i 12;i thdn ? mll!i-e t_'i3 10
<br />T,o re :? .Jo 1, fJ~ ?t37pie, !3 ;C!1 C`li !> i :C ?7 J2fC3'.I Cld'+, 2"J CJ SG :2rC2nC SL t, 3i,J 1?;; than 7?
<br />_ >z'.?'~ :: '. .` zhz cz n:2ni Cf Car tlCl2S C73'S2r :har 53rd 3S 3; much d; 3b0Ut !] De rCedt, 3n 3pDrODrl3 Ce .nGdl P:ef li
<br />i::: 1, '. e(3',p!3, gr 3'+elly. i2n tU'3l term 3fe d2 °I f.;1 I1 Ch2 SC:i .Uf'!2V G'.:5;2f'/.
<br />-. i:;: f,; 3:.]' ? SO!lS l; ~e~Cfa]nE~ iC Lu'f~l''7 CC Ch2 jn;fl?•~ iJt. C13ii1C!C3Cl,in ;yF a.- ]q~1 C-•? ;YiCEm
<br />a::C::: :, ? ?]_ :73J ?iCCi3t b:1 Uf ']Cold Ylg`n3+ 3f] ?'3"iCJ::ii::.. 1r `1C131;.
<br />. ._. '~;:e". Ci 3SS1 fi23 SJ:iS dCCJrd:nd C7 G'7]e: fl'_; :h3C 3ffzL: Chelr US2 a'i CJnitr.C tlOn m3 Cer131. ~C'. is 3r3
<br />:.;li:":-: 1::; ".:: -.g W ~J raIO-i1:E dt;tr:CUt1 C.9 Cf : 3 fr3C t:cn 1255 thad J lnC'i'_' In is 3:13:2! 3i,C dCCOrd ing t~i
<br />.._,.._... .•~'?~, lia'.id knit, and uganic latter calLnt. Sardy and gravelly sails ]re idzntified as G:a, GP, r,.9, GC.
<br />:~' `.:. -,. 31a EC; ;llty and clayey sails as `~, CL. ;L, pi, ~:H, and CH; and nigl:+ Jrganic soils 3s Pi. Sails
<br />z,l:aiti-g 3 ]:resit:g prc7ertl?s Of tae gams can havE 3 $;31 classification, r„r exanole. CL-el.
<br />. ~?:. h.°S ;y3C°_n C!3;s1•12i iClls 3000r11ry t7 t`J;2 D. ;,per;i?; th3C 3ifeC: rJ3'?a 3'/ CGnS:r UC :ion 3rd Gain [e n3nCe.
<br />:n t..; - -.-,. _ 'ractiai cf a linzrll ;Cil t'.lt is less thla 3 inc5es in dizr.etzr i; c!]s;ifizd in one of seven
<br />yr: 3]i ' +-1 tprC'Jg5 A-7 On the Jai:; Cf yf31 '.-:: 2? d:StritUC!C 1, lloa!a 1171f, and ,7131 t;C!ty index. `:Dili In
<br />gr:.c 1-: 1•' :]3:SZ g-3ined ard law i~ cDntz^; .` finei (si:t ar.d •:1ayl. At the Jthe^ extreae. sails in groin A-7
<br />3r2 ~,• :"a:P°. d. Plg`1}' Grg;n:: ;oils arz classifizd in g-ecb A-S cn the oasis of visual inspection. if labcratpry
<br />d3;a are a+3i ab!z, the -1, A-2, and A-7 groups are 'other cia;sified as A-l-a, A-t-b, A-?-J, A4-5, A-2-6, A-'-1, A-7-
<br />`-~, Ji A-7-5. F; an addi;;onal refinemsnt, tte suitability of a sJll as subgrade la[erial can be indicated by a group
<br />index nlltr . Grcuo index numbers range frog 0 far the best subarade material to 20 or higher for [he poorest.
<br />..~ '--i'cY ? ili g?' th30 ~ l:1L h2; !G d13D2 Cer are Ild IC 3;ed 75 3 Jerren:3ge L. :he t]t31 i01i C. 7 dry-~elghC
<br />~+S:i. r'e Ce'C2rt 1,g2S dre e;tl la Cei d2 Cer71 n2d n3191 y' by C]rl3rCing 901L're DerCe ];3ne In the field t0 8elgh:
<br />]o !7'1;;;3 ~'.r 50:a :3f [:•: i'_i pl;e:'.y' 1?i!Gl3 tea i:2Y J; l~ ?l E.'I L;' 'tE~!f{: EICYE ', I,'+j[-_~!; t.`.' ,°rC2n :7C2 0: C`.2
<br />_... f-;c::_n Itss ;han S irch2; it dig,=_'.er Jaszd n 3n CL2ridfv aeici:. ih2 sieve;, nuabers t~ !0, :0, amt ?00 (';S.a
<br />S,z_,,, ....`.2;1, na,e 7peliCgi Jf 4.76, :.CO, v.=.0, apd ;.C"> ]illimeters, respzc;ive!y. Estiaa:es ,ire based cn
<br />:3dJ'3:C'} :e;t5 of saili sanaled in [ha Surrey 3rza and in nearby areas and on z;tiaates .Wade in [he field.
<br />L:;d:D !'7ii and ?LASiiifiY iNDFX (Aiterberg limits) indicate the plasticity ch3rac[zristics of a soil. the
<br />zstin3:es are based cn test data frcm the sun'ey area or frcm nearby areas and on field examipatien. the estimates
<br />of grain-size distribution, liGUid lion, and Dlasticity index are generally rounded to the nearest S percent. thus,
<br />if the ranges of gradation and Atterberg Baits extend a marginal amount (1 or 2 percentage points) across
<br />classification boundaries, the classification in the marginal zone is oaitted in this report.
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