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<br />lit. p~tsu l'ur>"t'~~ :\r.l:n, <~ul.utt•tno
<br />that' Lr nrrded lu insu l'e ~un'ita 1. 9'roes that :u'0 br.<t
<br />ruilrJ :nal hate 4!und sureieal ;nr 1lucky \lou nL;lin •ju-
<br />nip,•r. o;e.lrrn mdrrd: u', punderl ~s;r pine, :uvl tiitteri:w ehn.
<br />;<hruh. that :ur host suitrJ :u'I• skunhbush sumac awl
<br />I i I:II'.
<br />'I'h0se soils nro puurle suitrll lu \rildlil'e habit;k. They
<br />;u'e typia•.dl}' us0d as ha hil:0. fur I:utl;e Luul \\ih4lifc, wrh
<br />as sr:d011 quail nod :Int0lupo. 1•irrst nck !; ratios; nnut ho
<br />cr~r}' r:url'ull\' nl:maprd il' u'iLllifO is to salisl\' nursl ul' its
<br />hahil:rt ter pl irenu•N s.
<br />'I'L,• main limit atiun lur rnnsl tart ion un Lhe St•lt:nnher
<br />roil i. strrp slopes. Kec:nlx• ul' rapid pa•rule•abilit}', Lhura
<br />i~ :I har:vd of poltutinu il' this wlil is us0d for wyaic tank
<br />nhsurpliun 1'ield~. Th0 high content ul' cu: u'sr 1'ra{tm0nts
<br />mad' coast pruhlvuts tcith e[cae~ltinns, mainly h0causc cal
<br />hands cat'e in. Flu•cial desi~nx I'ur builrlht!;s :uvl roads :u•e
<br />nrress;n•) to ul'1>et thr IimiL•diun ul' slope. The Kuzur sail
<br />i~ limited hr depth lu shale, slmc pcrnu•ability, limited
<br />;Ihility to support a luau, shrink-s\rell pulenti:d.:md slope.
<br />Ruth soils :nx• limited h}• Il'ust-aa•Liou potential. 5pec•ial
<br />drsia<ns fnr LuiL lin)<s :uul ru:uls :nr n~l0d In ot'eraunc
<br />IhOx• linilt:rt ions. C:glabilil ~' subclass \'110.
<br />~;-tilapla•lon sandy lu:un, :{ lu 1 pa•rrcnl slopes. This
<br />der~p, noncala•:u'onus, tcell rh'ainoJ sail formed in sandy :d-
<br />lut'iunt drriccd Irunl :u'knsic her h~nck nn uplande. L:Ice:r
<br />lion l'a n!;rs tram d: ion W ?,:,nn fret. The at•eral;c annual
<br />lnrripitation is about ]:~ inches, the arrra!'c :atonal air
<br />trntprrature is about ~17 dey;rees P, :uul the at~cral;e• Il'ust-
<br />Il're period is about la3 rL•t~•s.
<br />9;t•picnllc, thr surface la~rr i. grayish hrntcn c;unl~•
<br />loam shoal 11 inehos thick. 'I'hc subsoil i. ); rtq•ish brutrn
<br />cratelly s:uuly lu;un about G iuchrx thick. 9'hc wbsU•auun
<br />rV rods to , depth of fin inches nr nunr. It ix p:de bruu'n
<br />era crllr .:I nrlr In:un in the upper pa rl :nut }; radrs lu
<br />Irra yell)' In:mtc sand iu lho InmOr part.
<br />lurluded tcilll Ibis soil iu m:glpinp arr• small :u'eas of
<br />LuuriOrs sill ~' rla\' to:un„^, W l.~ percent xlnprs: Itlakel;uul
<br />lo;uuy .,.:uul, 1 to P porcont stapes; l'ohunhine };raecll}'
<br />s:uul~' lu, nt, n to :: percent >lupes; :nvl I'luvaquentic
<br />H:gdaquu.l.a, ue:uiy lo\'el. Also included are :u•exs tchere
<br />:u'Luxv ha•Ils u!' ~:uu lsunte and shade' :u•e nt :I depth oC 11 to
<br />.lu inches. Included :u•oas make up about Ya p0 rcenl ul' the
<br />mapped nrir;l!;o.
<br />1'ernx•ahilit~' u1' this titaplelrrn sail is rapid. F.ffedivc
<br />r. ~,d int' drlil li I~ I{n in'llr\ nr Innl'•~. :\c:u la Llr trot of
<br />r.il ~arll t' Irn ..L~r:d r. :~lu'!: u'r rnllnl~f h >luo, :uul Ihr
<br />L: rr u'J. ul'en~~lun .uul soil Lluttuq: are rnu, 1, ~ral o.
<br />'Plus su,l i,. u~wl :IS ra nt;l ~hwd. lur oiLllil~•~ hahil;rl, :old
<br />.i> hulW~>IIr~.
<br />X:nive ropelatinu is maiul\' tcesl0rn teheat.Gr:rss, sidr-
<br />".d: Cr:una. needle:uvlthr0ad, :uul little Iduosu•nt. 'I'h0
<br />prednwiu:un <In~ub nu this soil is uvc uunuri:unmahup:m ~•.
<br />1'lura ucrt n's ul .urnr ;ut as.
<br />Ih•frrrrJ t: razin:; Lao in :•u nurser :uul in 1':dl imprures
<br />lire rundil inn of the r:uty;c. I'rv.pcrly locating livestock
<br />,t :n rl'Inp I:Ir'lhllo~ helps to fUlll rut !; 1':I%Illr;.
<br />11'imlLrrak>: and rnvirnnnlerrtal phuuiu~s ar0 !;enerally
<br />suitrd to this sail. tinil hluo'inr; ix the pri~ripal limitation
<br />I'ur the o.<lahli<lunrnt ut' tror•~ :uul au~ul~<. 'hhi~ linul:u it ill
<br />c:ut br nrrrc•nnta• br rultitatiuC .ndc in rho u'el~ rett~ :un!
<br />loAC111,L' a %t 1'll, Of \e¢olat lnn In-tNern Iho t'nU .. `uI+I.Ir
<br />tnrutal irrit-nlian mad' ho nrrJ••J \\~hr•n I~I:I nlinc :u IJ Jar.
<br />inF.. dry pel'iull.<. 'll~rr•~ Ih:rt :n'r LI~:.I .uilr••I ., n,l ha\o c~•r ~~l
<br />surcic;d are Kuck}' phnnrt;lm iuuil u~r, ra-torn rl •rlrr~, I:u~.
<br />pnnd0rma pine. tiihr rims clot, I:u~<i:ucoli\~r •, :unl hart, L,~r
<br />I.c, tilu•u h. that :u'0 hr>t ~uil ~~d are :.hlnll,l,l l-I, .unc,~
<br />lilac, :nut tiiUe ri;ut peashruh.
<br />'I'bis writ is suiL0r1 Lu hnI,IUIL fur nprul:ucl :aul r:u~y;~~la n•i
<br />v ilJlil'e. I(:uttirl:uul tciL llil'o. .w'h :r.. pruuc horn :~ntrL,l.~
<br />c:m be cntcnutaKcd by drr0lnpin~ liccst url. t. alrnnC larlh-.
<br />ti0s, prapcrl)• muna!;iu4' lir0st url. ,L'1 :IZIIIL', all~l r'~•~ee~lulp
<br />r:ml;c tehc•ro needed.
<br />The main limiLUiun of thi. soil (nr urh:ul ate i< fro~l~
<br />action potential. lp0cial desiFln nl' roads :uu ~u'oet• I,
<br />ncc•ess:u'e La minimir0 fns<t hca \~e rl:uu:rec. til,r ~r i.ll I~rm~
<br />tires Hurst be prodded to minimrz,• \vatvr orunion :uul :on
<br />hlutein); un construcliun siu•s tt hrrr• c0{;rtatint h:,< hreu
<br />rnmoced. Access ruarls moot bare :p ley u;ue cut--iup,
<br />>_a':ulc :ntd be Itroeid0d tcith drain.. ur control surl'aro ru
<br />noff. ('apabilit}• subclass R'c.
<br />7+1-54tplclon sandy loam. ~ lu 13 percent stapes
<br />This deep, noncalcareuux. toll drained .oil G~rnu•rl ire
<br />sooty allueimn deriv0d from acku.ir hcd rock un upl:uul>
<br />1•;Iecatiun ra n{;es from Ii,Lun t.. 7, ;nu Cent 'f L,~ act ra c.
<br />:uuwnl preripilalimt is shunt 1:. inches. the ac~~ra ~,~ :ur
<br />oust air temperature is :Juno .17 drl;rec> 1', :nl~i Ih,
<br />^v0ra>~c Crost-free perin<I is ,haul I"", does.
<br />Typically, the .w•I:rcr la\'cr ix t;r: n•i..h hrntrn .anJ~
<br />l u:un ;Ibnut 11 inc•hrs thick. Tho subsoil i.~ t;ra ci:.h hro,tl
<br />:; r;lrclly candy lucent shoal n innc~s ihicb:. 'I'h.• wb. uanw.
<br />o~trouls to a depth a( fin inrh0~ or morn. It is p:dr l,run 1.
<br />y; ra rrlly s:uuly lu:un iu for ulyu~r Ira n't :onl padr- I,i
<br />); ra coll~' lo:nny s:uul iu the In\cer p: u't.
<br />lut•huled tritlt this soil iu m:gglint! arc .mall :ur;u a!
<br />IS rrssrr s:uuly loam. •i W !r pr•rrr•nt slnprs: Luu\'ier, silt
<br />clay lea nt, J to Iti percent stogy.. 'I'rurktuu .:md~' lo:un.
<br />to A percent slopes; Yoder >•ra colt)' sonde In:u lt, 1 in r
<br />percent slopes; and sutall outcre!ts u!' :u'kuce bed= ..f vut,l
<br />stony and shale.
<br />1'w'ux•abilit}• of this Slaldelnn ..ail is ra pit 1. F: II'rcticr
<br />runliny; depth is lie inches or aloe. •. acaila hlr t\at cl
<br />rapacity i. mud0ratr. Ju rlaco ru nnll i> ulr~llunl. .~lui ti..
<br />I~:I Z:IrJ of erusilm i. IonJe ral,•
<br />'I'lu. .volt 1~ used .Ih I:IUCr', I~~i ,~. Ililh 1, L.J.a ..:. •~I~,I .
<br />huluonitr..
<br />Ihali\~e ce!; 0latiun i> nlai air ,tra,~ru t. L,,it rr.~~ :.IJ,
<br />naL !;r:una, nOrdlo:uuhhrrad, and liltl.. Llu,~-I,~ui 'I'li•
<br />dominant shrub un this .ail I~ uw• annul!:~ulul.~hur:,n•.
<br />1Lcra is presort in sunu• phtcr<
<br />I)rl'et•red {; raring late w sunuurr and torte w I'..11 un
<br />p rotes the cunditinu ul' thl• range. I'nq„a'I ~. 1..r .Itiu:
<br />lirosUlck tcuterin}; fnc'ihtirs holp> t.. rnntnd fir: u.ulr
<br />R'indbrcaks and oncirntnucntal pl..nt ntc- l~enrt:dh :u
<br />suited Lu this soil. tioil blot, mp i~ III,' maln linlil:~lnai I•~~
<br />thr rst;ddish ntent ul' ores ;nut sh ru L.. 'I'hi~ linm:n i~~n oat
<br />be ncercouu• by cuhit•atiult only in th~• Urr tort. :nu
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