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<br />air-o to o inches, grayisL-hrow R o PHILLIPS COp~*Tp COL O
<br />grayish br n OR
<br />ve own (lOYR 3 (16Y /2) loa ~
<br />g'ranula~' Platy etructure t amt moisC • m ^k thinark Alm
<br />731--u to ll lcareous habrupt5 dry, fiinb7orwhs to weak, fine b'roU oat all the acreAp-
<br />ate, ~~ rseshrDrurynt~ OYR 3/210YR ~/2)mloam, ve n kt d of irrat~tr0ld yfarmeclnTliPtcheatd, bTrl~3soiorvn tl
<br />to moderate, medium ar block ) tvhep moist; modes of follow' la° ed crops. Ill dr ~' also'tre sUrted shunt
<br />dry, Rrm when
<br />moist; snbnnglnr~siit~tj that breaks helps in m ° small grain or sot faivled fields ih tO man
<br />RYl t--, fine gravel ~ clear, nonealcareous; , y hard when mUlchino. alntaining Soil ghnm with Si ~ e Practi G to 1# inches amoath boundary. 'b0nt 2 Percent tires ° and worki „ moistttre and inlmer
<br />brmm ' t~ d tq~'arg o~'shz$browtt n tl RR 4ry2) clay III irrige,~t dr COntlolling erosion e into thetsoil aretubbl~
<br />tbi'n, s to modemwh 1 nr soeangpla~Y 3/_) utnun I$zer q reads lu farrn'je soils can be level Prac
<br />E ~?tl>`jvero ?g m hest darkens uclema°r sinoo nalcareoousre eery ~,° conttolaerosion ~lorkil ~ ~olp yesipclueeSpond cell liftfere
<br />fine i darDrtsmatic gran t2% }when slty say loath, (~ e1atlleSSter 1S <~ ~ ~graSS~ancl similar t ~ the soil 1tRe1Pe
<br />~' t Gr Y and tilth.
<br />moist; 6 L1Se p rff,$g
<br />subnoncaiea hlaeky ethn~dth hen omazct0 stroa°' srte~ `nd} and TIe- d as rano-e, Ca ~, es grow n'ell
<br />E3oab-- 31m~; gradllai, Smooth thick, nearly Cbn[~i n1Tn ryhen' , wlndl7reak Stiitd {irT'hateq) i L4 ~Ihty t711its 1]"C~l
<br />~ inches, boundary, ohs cla bilitY. b oup 7, Y Plains range
<br />OIIID Pale.b.
<br />dmark hratvn tlorg ~ n) llse R s/a) silt ~ Richfield
<br />media Prism /3 tvL Y clay ~eP1Cg
<br />medium, subangttc Structure that a moza[; moderate,
<br />aloegl cleayaom0u~~ blockt~; slightly Iznsrd uhenera te, to rr~~soils~eld aeries consist- .
<br />strong y caseate drg of El a o
<br />a is ver vnayk sand h~Lrowut (r yR enCUOt ~ ~bteli~o nortera ely slo al'G Linla~Id5. Z~ht,Be so 1B deep, lnainl ra
<br />clear ule(1
<br />the ho• mod P oft occur ,
<br />Ole - G to ¢3 finer b ary, n 10 3/-} n h , n COitllt
<br />brown tees, c-cry pale bro,,,n moist; Iu a y Ica Pm°. 3 acid are Ile Yin the
<br />(lOPR 6/g {10YR s/3 loam ~ t P 7 pro$Ie arty level to
<br />Prismatic struetnre ryhen most; m ) ~ mectin m, r Ub p j SUrs a. ~r`t 151
<br />subruzgnlar blocky; that breaks to moderate, m~llPaie The S o inches thickilt i ~ layer is
<br />Porto eous; der- alcareo
<br />z PPer t stir x°ePtut ?r f horiian coat 2henedryime prom. Bard, sh blog ~V shd clay loam nC j est~ of wed, Y us. It is
<br />C~ boundary, ,abo Porcent ins less lien ' nd sli brow .peer
<br />--~s~to so i she gray e than ghtly hat n clay l0 1 art, slims
<br />vet aches, rery ale el~ clear, sac Part, d, light browns a7n to the middl~ahtly
<br />9 Pale erstvn (i0Y brou3r (wOYR g ) silt I < y Iinderly g the s sh gra:Y loath iu the Paer,
<br />(structuret : /3 gam, fine sand ul ubsoil is cer ~ loft
<br />vet9 strongly role reo h u cIr hen matsE; massive Y loam that 5 pale bTOtt7
<br />The d horizon r ns. y friable ryhen moi tvorkeC
<br />teas d po
<br />° anges'fro xt; l locals
<br />r vet
<br />E-t Lorizo riot is ver Y by Hind an steed b oath o
<br />n rnna~ from IO ° to s; ~,fl ,p wind and then rey
<br />moi,St the E'2tb hariz aches in thickness coritai str
<br />to lime ran on i to =o inches in ~ and the ns In tell ~ Cely calcareous or st'ontrlnderly~ing mate-
<br />anderlf ges flnm 22 to ~ melt S tluvery dark rckueds. When hi1ROlI' 1S itmnlafed little. a Y Calcareous, It
<br />~tim whe
<br />bo sails are Ptfi of ¢p . some areas- a teeth ~;~ i
<br />Rao es the loess ak a de rvf Inch motet gravel pr tvh n12 1P ~ SIO I nears
<br />In contrast t associated th the es or d d ere they , e en re 1 es are y ley
<br />brown layer ~ Rich&eld suits, R Rama ~ le fly a tl
<br />stmt go sons su a areails and ~c keid so' are ~ liable water holdmagse~ann~tor moderately 101> lt~s
<br />um. Ra bsoll and have a b rls. hi h.
<br />Rama soils. hate a more eta deeper to m° dark- Jlost of the P Y and natural fertil' y
<br />yey $~ horizo I y sob- soils ar acreaa
<br />Ra8'u and $qm n than the e suited to ae ofRichfieId soils is cnlticated. ~`hese
<br />in broad areas a lows (0 to 3 vegetation consis n7nter wheat <
<br />ghat is is lent of hhe Uplands. Percent s1o es a ~ mostl 'L1d sorghums.
<br />1 cal
<br />}ino P ~Zrti These soils P ) (Ro) alo aroma, but so uffalov of western wheatgr~ eltie7d blue
<br />~lretisU;.rit is the Most ~teantthem separately, Thishnilar ~ here more clay has aceulnulgrotrs in depressional areas
<br />fro genOral]y extend in o- s e one in Philli map_ eed is a common ated in the .
<br />Rno-l 40 to 400 acres in size t southeast PS County, have b Perennial we subsoil. Snake_
<br />~o soil, and 30 about ip direction and ran e T een overb~zed. ~ where the native gt.
<br />x111;abo soil percent is Iw Percent of the uni g 3Pica1 profile of Rieh6el asses
<br />Included inand others are all ma soil, but some fields tis in a cultir<ated m d loam, 0 to 3
<br />field maPPina ,were Iimna soil, zre the southcest cornertoflse~ L~o~ ~ Z, Percent slopes,
<br />' and Dames soils~The small areas of ~~~ 2,~¢p feet ltolfh of
<br />Part of the count - Pln6ler soil }s Plntner, Rich- `tn-0 to s inches, ., , . 9 w., R. 43 IV,)
<br />and the 3> the Richfiel in the tvestarrt g~yish draytsh0~otvn
<br />Dawes soil is in b d soil is in tl
<br />) 'Len 2} loam, very Bark
<br />=~Iso urohide ofh the central an re eastern part, granulartyt~•ut ur ,R ~ isiOY~
<br />is•eak, &ne
<br />d were areas of a soil that i
<br />, eSCe it d tt'estern moist; non
<br />'hen dry, qe
<br />gam CaIClreana ~
<br />o I that rvrav s sir parts, B1 -G to 1o inches c7e L
<br />TY friable w
<br />attar f dark e , grayt'ait-bro ar' sm 5th b
<br />rya (IOYR o onndary,
<br />4 inches. Jlany s n elty material is at ° Raao °rayish bra en
<br />6 ~bol slapped areas and are lhowt Inkesaorepoltlo ies~ttt ve bang, lair blockyt bn a`a liar breakseto eak,'nc7 ~ SQ'~
<br />n Oil the 9011 ma fire Y thin, Patchy when dry, firm
<br />Rego and Il tllp< faces of Peds; nonenle films on vertical and horizooist;
<br />P b2
<br />These smisana runo$' calase berob o stet at a moderate to t--lo~~tme Merv edar& grab h~b,•~~wa, smootL ~/z) dci yt
<br />have high available n durino- moderate ilorR
<br />moisture ° some Storms, breaks to niedinm, prismatic YR 3/2) when
<br />capacity, tbhleky; slight~jy hard media Grand fine subnngular
<br />Cantlnnona Cla R112II y, drm
<br />faces of Peds; y films on verticat and Lorizontnl
<br />nonealcareous; clear, smooth boundary,
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