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<br />l:l
<br />
<br />solr. sur«(>s
<br />7noluded ~ ntalrping \vcre afcas u ULa•o sanly faun
<br />aml 7'ivul s:uul.
<br />1.'hcso till bare moderately sl runoii ;aid nurilorntc
<br />:[cailal :water c;tpacity. Soil h wiur° i ;~ severe Jtazttrc
<br />\c 'ly ;III of the na'cago ~s eultivaterl., or ha:; b; n
<br />col ralcd. lirnuutcurn ;url n•gLwn arc r.hc uuun r, lts,
<br />b in wnnc. yonas they uu~r nut l+rovulyd al' pour
<br />.aver n.ud rho soil hash .n crode~a.:\ vegcf,aYise .over is
<br />ncrc=s:u'v at :[ll tiracs .'Ito cultivated acreage . weld be
<br />rc5cedcrl to gross, b this is diflirulr.. On r: rie, prupet•
<br />manaccmrnt (u•act' r-; :ur. Jlecrssary to ran o] ;nil Lloty-
<br />ing. ~i',;t(,abiht}• nit VIc :3, nonu't'tgata Sandy Yhtius
<br />rali~c site; Sn 1 y tt'indbrcalt suit;lbili group]
<br />'~S7:lI,rES
<br />'L'lic ales ~crics consists o,`' ecp, nearly level, rlark-
<br />r;ulorr ln:uns that uccnL~y s earn torrucus ihrou^,'hout
<br />hhc nutty.
<br />n a I~.yltirnl prufilr, the. u•1';ICC layer is hr•uwnislt-gr;ty
<br />:un shoal, ~1 inches f.h~ :. The subsoil, shnil6 S inch .
<br />Lhirl:, is a. Crn.yish-hen n clay loam that is stron~l;; ai-
<br />c:n•eons in the ]one • fcty ine.hrs. It is h:u•d tt'hc d1.y
<br />anti first whmt mn ..:Cite unucrivirl[( material is town,
<br />sUvm;~ly calcarco .', wealdy strnt.ificd clay loom.
<br />1Fa;;es soils 'c wrll drained and have him available
<br />wntcr capnoir -
<br />.}(nst ni' t r, ncrgn.ne is in natit-o ;grass, ainly bulialn-
<br />• gr;iss nor clot gr:una. Lt cuiLivafed rns, wheat and
<br />sor~lau arc the main crops.
<br />'I'v ':al hrofdc of 11'n~•es ln:un ( iiG fret notch :ut[1
<br />•]0 f .1, wesh of S[;. corner, ec,. I,' L9 $., It. •13 11'.)
<br />Al-0 Ln •t inrbcs, Fra,9iail-Imot t ISO)'1[ :~/'-') lu:nu, vm'y
<br />tin rl: Fl;~,r ish bra++'u ( 'li '/::) tchcu moist: wrn k,
<br />find, Fro uuler xti'uC re; sli;:ht15 h:u'ri tchen dt_v,
<br />very Crinblr whir moist; nuncalcarcuus, Pli S.(~
<br />uhnpd, ctnnnlh ,nntl:u•y.
<br />1121-1 In 5 in.-hes, Fr•, iah.h town (111]'7L fl?) clay Ir ut,
<br />very d;u'1: ;; r;, ish 6rotvn (]UY It a!'LI when ,i,vC;
<br />teen k, nuvli n. Prisutn [ic .fracture Chat I~' 'IS to
<br />uexlera tc•, tedium to tint, subnu;;nlnr Ll nr ~; herd
<br />tchrn dr lirm o'hc^ umi.al,; Ihht, Pn tch t' ny chins;
<br />nnuaul cross, pfd ..U; den r, amnulh ands ry.
<br />P3-S to 1'? 'tchrs, ;:rn}'ish-Crown (3l1\1[ 51' chq• lo;nn,
<br />d:u' Frn,Y i.vh brown (1G}'It 4/_) 09; moil l.; o'ce 1:,
<br />u ilium, pri.anm tic struahrrc thn parts to e'ra k,
<br />trdimn, subnnathtr hlnrl:p ; hu when firy, lirm
<br />tehen ^InisC: sfrmlgll• calcnrr I., pIi ".A; cirnr
<br />snmoth hrrundn ry.
<br />L' ' lu Go inehrn, brntvn (7oSII .;/.'.) clay loam, d;trl:
<br />brntvn (1GYI[ 4/3j tehcu moiet; very woa lr, mc-
<br />• 4imn, sub^IiFnlnr binel:y ynu'tu rn; ba ivl when dry,
<br />frinhle whrn moist; s tingly ,tales reous, LI[ S.L.
<br />Iu said pia cos. rlrptli In li c ra u~cs from 1.. 'l2 ~incl s,
<br />Lnl soon. rnllir;J wi nrrnc c lint;- to ii;c cn rfa ec. The ec-
<br />nu'c of Ibr ]rLt Lorirnn ,m des Cram loom in dnc Ir ,m.
<br />11'ages loam (0 tn:; p crut. slopes) (Woi•-This oil lies
<br />alnn« sta'cant terrace: ' nearly all parts of t.he -caurt.y.
<br />Jnclndcd in map air trcrc srrmll arras \IcCoolc
<br />]n:nn, Rara. r,lny 1 nt, and Nunn cloy lout
<br />'l•hcsc soils nh n•h nntor rcarlily. Thep •e mnrlcratcly
<br />perutcablr. oat rave high av;[ilnhlo \ra .r capacity.
<br />\(ost. of t. acrca~c is in native v ~rtnt.ion. IiulF: o..
<br />grass soil ue ~t;rona a4•c t.hr. main gasses. 1Vhca soil
<br />sor~hnm aro thr. main rultivatc crops. In it gated
<br />areas, ertilization, land levclil , use of trop residue,
<br />and titer management are ne scary for Prot ing good
<br />crol,r viclds ;tall
<br />ing :aril striper
<br />faraled areas, ;
<br />and chiselinr i
<br />areas. On an,
<br />~Ftrollin~ soil iilmvin~- .ubblc nntlch-
<br />put~ art nrudcd iu it rated. and +iry-
<br />duriu;; lrm'iods of dr nght, dcclr lisfin
<br />t control suit Llo mg m3 dryfartard
<br />dcfe.rred ;uul cation ^ratimr hrll;
<br />nwinLaiu .I~lequare grass corer
<br />irri~atr , :md alluLhilitY 1.
<br />Loan Plains [:urge site; I.
<br />~1Viley Series
<br />;apaLiliL}' unit llc.-1.,
<br />]llc-1, nuuirriga.CO;i;
<br />tciJlrlbrcah suit;IbilLLy
<br />The 1Viley series consist; u1` dce,p, m::u'Ip level to
<br />strongly slultutg, ]i~hC-colored roams on km~s-rnoaltled np-
<br />];utds in ncnrly all p:u'ts of Lhc rosary
<br />Ll a t.ylrica,l prolilc l.he surface ]sync is ]igLl. Lrnwni:.h-
<br />~;rn.y io;uu abouC 5 incites thir,l.. 'L'ho snilsnil is ahrSac ill
<br />Inr,itc:; chir.i:. 'L'hr ultln+r parC is ~ruvislt-Lrorvn, s1i~Pdlc
<br />calcareoas si1Ly clay ]oars, and t.hc ]mvm• halt is palc-
<br />bruwn, strongly calcareous silt. ]oast. 7'he subsoil is hnt-d
<br />u'hcn dry, hut. frinblc •,t'hrn moist. 'L'ha nndu'lyin;; Jial-
<br />Ceria] is lxl.lc-hrotvn silt Lrun fluff is frinblr,, cnntaius
<br />lino.. ;uul is e;lsily penehraterl Ly pi;utf, roots. .
<br />1Vilc,y sriils are nnCnritlly wcll•draincd.'I•hcsc soils arc
<br />moderately pa•tncu.hle and hove lii~h ucailable watrr ca-
<br />pacity. 7'hoy are high in naLurnl fr;rtility, Ina are sus-
<br />crptiLlc to Loch soil hlon'in; ;aril traicr erosion.
<br />A{ost of LLe aarea~c in fire c;tstcru hart of the rount,Y
<br />is rultiraterl; most of khe a.crea:ge. in Cho wastorn hart is
<br />in nat.ivo rang. 1Vhctt and soi•~~Lrnn art, Lhc. cnlnraon
<br />crnls in Ludt rlryl:u•nted and irri~atr:l :nits. ~Rhlc hr;tma
<br />and LuiTalo~rass ;ll'r, cnlnnton on raurc.
<br />1'}picai ln•rnilc of 1Vilry ]n:nn (lr:. fi•.i:t srnd.h a.nd ;Q
<br />fret nest oi' NI?- corucr, ecs•. G, 'P. 29 S., IZ. <In 1V.)
<br />.\"l-U to i. inehcs, ]iclit 6rn+cni.;h~Frny (JVlli n/~) Ian m,
<br />do rl: ;; rapi8li Lrn+cn (lol'li 4/:1 whrtl nmisl.; weal:,
<br />' liar, Frnnalar slrucl arc; c;i Fld 1}' h:; rd mhru 4t;c.
<br />very Iriahlu whru nnri5t; small lisle ~~rtcrclions:
<br />strongly en lcarnuns; c•ICm', sntnal li bnnndn rc.
<br />I','Lt-G to 30 inches, grayish-brawn 1)UT1[ ~d21 silty clay
<br />]nma, ~inri: zrn yish broo•n (h)}'1[ 4/21 tchrn uvri ,t:
<br />weal: U. mmlera tr. ntrrlinut, Pricnlnl it slrnc[nn+ Iltat
<br />parts co n•cak to umderal e, medium, rnbangular
<br />hlin•I:y; hard tvbrn rlrp, iris6le •atron moi ,t; tLir.,
<br />Ualch.y flal' sl:ins; wcal<ly calcarrous; ciea r, smooth
<br />bmaularg.
<br />.li&rt---]0 tr. .1. inches, palo-hrotrn (C)PR it/.".i silt Irr:nn,
<br />d:n9: brown (lOY It 4/a) tvilrn tnnist; very n'rn lc to
<br />wca 1:, mi•diunt, nobs n¢nl:n' blocky st nuance; bnr6
<br />t+'hen dry, friable ¢•hen mniaC: sl:roagll' calca reJUV;
<br />CI L`a 1', vmnnth bnnlldnt't-.
<br />X13 Lo ria inches, Pale-Urnn'n (lUPi[ f/aj silt ]soar, 6run'n
<br />(inPJt :./'1 when tnnist; m;i 6Nir.~; Im r4 tvho^ dr}',
<br />I riabir ++brn mviSt; shoal: ;i p.!rr;r'111. slot sPuls;
<br />s; rnnFly ra lea trans.
<br />1•hc a inn'i:um r:u c;e:; ,rmn :; lu '. inrbcr: in ILiclu;r:aa :roil
<br />:rant Silt lo:un i~r loam [n li;:ht silty rla}- loom in Irstmr.
<br />9'br lr3t. lwrirnn ran;-mp from .; In 7a incbr•v in Ildr•hnrv~.v.
<br />'Cba ;Wore :aa pinF t1'iL ;Y •~nilti Cr•u r•rully lnirr Ir:-: slay iu
<br />Lbeir 1: I/n~iznn„t 111 ;~ h, n'ianu of on[+.':c;L nr ulhieinl Innmc
<br />malaria la nrcwts brt trrrn 4rp; au oC 4U nnrl fo lu¢hrn In
<br />Wiley loam, Il to 1 percent slopes (WIAL. 'I'h i.ti ~r:il
<br />nrr'tnx n.; rrlatlruiy l:n~;_e, nrcas LLrnlt~hnul. I hr. rr,ilnl.c.
<br />lllchtdcd in mapltin~r tcmr. many small :urns n( Pnc:,
<br />clay lo;uu, and in tLr, nurthcastrrn p;u•t n{ r.hc r;ouuty,
<br />some ;u'eas of Colby silt loam tint] IL'u•horil lu;lln.
<br />This soil ub=orbs nearly all of the moisture that falls
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