|
Br;ter cou~~
<br />r shnRotc Tr;n-c•ssilla coils, n~Lrrr tLe. Baca soil borders
<br />r s:unl-tune hrclka.
<br />Phis Boil tnl:es iu \cnler nuxlrralelc nett and has a high
<br />Ater-h,rlllln_ capacitc. Runnll is nuxlerute. 1'he erosion
<br />azard is nnnlcrnlr.
<br />UI ul Ihr arrraer is used as t:•In~c. RnJntin~ and drfrr-
<br />tn~ ~ruzin~ :Ind hrnridin~- fur food dish'ihul ion of lice-
<br />ocl, br luvpr•r plun'mcut of n'ater and salt ore~ood
<br />•arrirrs Jn rank ntano~rntcnt. (Capn6ilily unit `-Ie-I,
<br />mirrig;,tcd:Li,alu~~l'lainsruli_csile)
<br />iAll{<fl l'(~ SCPIC$
<br />The ]i:nll:;u'tl series rnnsirts of nearlc level. calcareous,
<br />tninlc s:uul}~ suite that, formed iu stratified, lim}', smuh•
<br />lluciuut. '1Tr<(• =oils are adjacent to the main channel of
<br />Ir .i glut nsa> ] ; i ct•r.
<br />In a tvpiral profile. tLr -nrfare lacer i. ~ra~'isL-bro\cn
<br />nnnl :ILout -{ inrltes tLick.'1'Le. next lacer is ~racish-bruo'n.
<br />imc fine sand about 8 inr•Lrs thi,9:. Lt spots it is mottled
<br />u tlu•. lomrr hart Lecause of a tlnchlnt.in~ runlet table Tho
<br />uulrrlrin;< mntrrial is s;nulc alluvium that is dnminantl)~
<br />~raci;lt Invnen. Gram) is at. n tlclttlt of whom 3i inrltes.
<br />13anl:nrrl >nils arc excessively (lrainefl. Internal drainaje
<br />s crrc ral+id. and the \rttrr-L~~Idiu_ caparirc is lo\c. P.nn-
<br />IIl' is•crl.c slotc,'The \vnler tal?Ic is Lich when tLc trnter is
<br />li_h in the riser, and tlnndin~ is a hnznrd. \alural fcr-
<br />ilil ~~ is lun~. 'l~ltc. erosion Lnrv'd is nnnlrratr.
<br />lirrau:r• tllece =nil.a arc samh and subject to frrrpu'nt
<br />1oodin~~, the}' arc not. suiLlblr for cult.ic:diuu. Then arc
<br />r.'rd as lr;latn~c, and Ihcy vtpply ;:Doll ~•rnrin~ thrnn~hout
<br />hr. tear. ('ultnntcnods :std tanun'ISI: protect rattle ringing
<br />mrirnh n1" I~ad tyratLcr.
<br />'I)'Iriral prntili• of a li:nlharrl lnnw (].col) fret unrlh and
<br />;:.n Prot to=r ref ~1:. earner ~\\-l, j srr.:I. '1'. _:1 ~_ . 1.. 5°_
<br />\1-.l
<br />\I-rr t.. a inrhr=. ;; ra ci-h~bretcn 11111'R :.%]) Ina m. 4a rl:
<br />;; r: n'ish Lronn IIUI'It J%!1 tchrn amid: st goer nrr
<br />1, r,.:r6x from tcr;l L. mrrli urn. i4a U' L, n'ra h, liar.
<br />;: ra rnUar: h:u~d open Ilre. lriold~• ohen urni,t;
<br />>t r~~ucly c;rlrn rrnnx: clca r, smooth hnuuda ry.
<br />.11'--1 In 77 inrhr~. pen ci.lrhrn tru (tul~li ..-.%_) tiny se all, do rl:
<br />p en ci-h hrotcn Ihrl'R -1/H) tchrn mniat; sinFlr train;
<br />.IiFhtl)' lirm a'hon Qrc, louse; a'hrn IDoi.l; st rouFl}'
<br />ra lrn rcou<: clear, rmonth hntuula rr.
<br />Cl-]- n~ a7 inrht•t. In:nny fine sa ud; color duwina led Lc
<br />rnlm~e uF indicitlnnl QI'a lll), FCIICra I1C gra dth Drotcn
<br />i Inl-[f :~%'/ tchrn mni~[; =inFle firaiu: louse n~hrn drp
<br />anal mr,ia: st rota of ton my .;tad anQ can4 ranpr in
<br />Ilii~ I:nc~s fr~nn :I fraction of au inch to sccv rnl innc~s.
<br />f Il'_ }:. to r,U inrhr•.~, ri rc•r Fr;rrel.
<br />'I"hr .ll h~n~izun ra nF••x (rv•m ^ [o $ inrhr= in Ihid: m•<s and
<br />front hsnu to In:nuy t^u4 in u•xturr. The Cl horizon rnnFrs
<br />from !n In ru ittrhr. in thin: uc•s=. It. ix light Fra yidt I~roten or
<br />Fra yi~h I~r~non iu rolrn• curl in Irlarw+ is mottlcQ in the lotgrr
<br />part. II i~ limy In err}~ ~Irmlplc lien c.
<br />l::nll::u'd =~~il: are uu, rr sn nd>' than ~Irnhr•rF soil.. TIu•v are
<br />nl~o mnn~ ~a udy Ih:ni Lila .\niulss .oils, and thee Jnrl: nalL
<br />;old Ih~• nllirr ocidr^r.•. of p~~ur dra ina pR Ihat ago Iol•i~~;il of
<br />thu"..nil..
<br />Bankartl soils 10 In 1 prrcrut slopes) IBdI.-'1'hr-e soils
<br />urrnr ns irrrnlarlc shalu•d nrra=. 10 fn 100 ogres in size.
<br />on the flood plain adjarrnt ter the stain rhanncl of the
<br />:>,rl:ansas 1(iyer. 'I'lu• vurfar e laver is loam to ln;lmc s:nnl
<br />lu S inchrc tllir•L-, '1'Lr ursl Inyr•r i; luuul\~ ~:nul ter sand
<br />about ]:. inrLr> ihiok.'I'hi~ material is highly ctratiGrd. Lt
<br />]Ilnrr: ricer ~~r,nrl nrrnrs ut a drlrlh o[ Dole about °_0
<br />inrhr=. TurlnJrd fu uulppin;; \rrre=pots of Glruhcr~ saute
<br />III IIIIIIIIIIIIIIII • I1
<br />loan], ,,, 999 „the sli;;hlly raised harts of ills L•uul-
<br />scapc, ;;eucroll~' farther array farm the riser rLnnncl tLau
<br />the 73nnl:ard -oils arc; and nrcas of I,ns .\nimas soils, 1
<br />or ? acres in sire, lehieL occur as sli;tht del?ressions.
<br />1'hesr soils a re not suited to enltic;ttrd reaps because lhr\'
<br />are sonde and subject to Ituudiu~. '1•hc~' talc in realer
<br />rapidlc but hncu a lo\c \cu.ter-Loldin;; cap;lcin'. 'l hrv me
<br />subjeci to deposition of sand and silt during 11uoJs, and
<br />to bans; caving durin~r tloods:uul during period; tvhcu the
<br />cLanuel cL;ul~rs location. Ruuoll' is eery' slu\c.'Che rrusiuu
<br />Larar(1 is uuxlcrntc.
<br />All of these soils arc used as p;G<lm'c.'1'he~• ~uly~l~' ~ub-
<br />sLUtt.ial nnumnl~ of usable. forage duriln_ l,crirrd: of loth
<br />\eatcr. (Capa6ilitc unit I\-s-°, irri,dted; c•apubilitl' unit
<br />L'I\c-~%, uouirrigaterl; Sande L'uttunt Land rank =de)
<br />~aSC p SCrSC3
<br />The (,'a=eajo =cries consists of st ruu~l~~ sloping to vu~~•
<br />~h•on~lc _lopin soils that arc shallo\c acre lion', vet}'
<br />sandy amt rracell~' out\cash. The..<.o soils arc wainlp in the
<br />north-central part. of the county, just north of the John
<br />.llat•tin Rcsrrcuir.
<br />Ina typical profile tho surface layer is pule-Lronn
<br />~r:Jrcllr lo:un about i. inches thick.'1'hc next layer i light
<br />Lruu~ni=h-_•t•ac ~~r;n'elly loam that. ~t:ules to _rracrl :nut
<br />sand nt a •dcpth of about 10 inches.'1'6c _rncvl and sand
<br />aru eery liulc. Gcneralh• the unda'side of the ~r;nal (lid.
<br />5) is liutc cu;ttcd.
<br />'1'hr•=e =nil. ore too ~racelly and Ion sLullmc In Ile soiled
<br />!u colligated crops. 'Chcy arc nat.lually tcell dro in(•d. 'CLo\'
<br />Lon; ral,id intcruul drauutec, spill pcrnleaLilily, :unl a
<br />lute nolid'-Lnllliu_ rtpnrit e. Xahual fertility i; Int.. "hIn•ro
<br />is uo >i_nilicnu hazard of soil blotyiu~ ar of tenter rrn.iun,
<br />Lccausc of the gcrc ~rdvclly surfncc laym'.
<br />The cutire acren~c i= u~cd ^s r;ut~r.
<br />'l,rpical prnlile of a Casrtju }ragcll}' loam (('al feel >nulh
<br />and 7.:, nulr~ cost of rand juurtion, scr 1 "I' '':; ~., L'.
<br />:ell ~~~.)
<br />.\1-U W :. iuchr~, pa lrhrntrn (lOS It f/al ;: ra tolls Iu:un, da rF.
<br />;; rnyixh Lmtcu (1/11'It a/7r o~hral nmi~f: nm.:icc:
<br />loosu o'hru dn', ern' trio hlc tc tern uwisL: nrnu~a lea err
<br />ous: clra r, swouth Iwnuda re; untvh lino Feu ml.
<br />.\('-~ 1n lU iucltes, light hrownieh-Fray (htl~lt n%'1 Fen crllc
<br />l unnt, hrotcn IIOLIt 6/3) tc tern moist; um ssicr; w~Ct
<br />tchett Qty, re rg [ria ale tc hc•u muiat; ccr)' at ruuFlc rnl-
<br />nv'rnus: dra r, smooth hou nda r?~; ninny rrvrl.; :r little
<br />lima-coated Fra crl.
<br />Clia-]U to 17 inrhr>, ee n' pale Lrmcn f lal'It 7/37 lime pea vet
<br />and sa ud, pale 6rrnrn (]OSll n/.3) trhru umi>I; m:re.
<br />~icr: ahnlpt, smnmh bomula n'; mncli r,,;n~>~•. linm-
<br />ruetc•(1 Fra ccl, t•o:rtwl sin lute on the undnr~id~~: cog}'
<br />st ran Flc ca lea renal
<br />l"-17 lu fu iuchcs, reL•n icelg clean grarrl an4 s;nul; sl rnnglp
<br />cu Ica rcouc.
<br />The :1l horizon ranges from a In i; iuchcs to Ihichn~•.; :unl
<br />frni^ Fi:r tolls 6.~m In Fra vollc p:u1d)' In:nn in Ir~l nro. 'I'hr .\C
<br />hnrinm rnue•s front .-~ b, I_ totters in thigh u•... and ern des into
<br />crrc limp Fra rel. Thr>r toils Irmuu u• xhnllno'rr n'ilh iurrra •iu~
<br />alupc.
<br />Caeca in coils am room gravelly th:ut either ]Ia eery ur
<br />$L~urhaw Soils.
<br />Cascajos~ils and gracell}' land (;. to `_'0 pt•rrrnf slopes)
<br />ICaI.-1'lli;nnfl i~aLuut falprrrrnl ('^aoajr.>r~ilxalld;drnnf
<br />:Itt prrrr•ul crrc are.p, googly In'nl:rtt :Irr•:I: r+l' _r~r:nrl. It
<br />rn~~~nt> a; rlnug:urd, irrr~nlar•Ic ..6nprr bra ~~+r t
<br />the north-rruh~al p:u•I, lust uortL of 1 I~.~(h~~[il~
<br />
<br />MINrn Lt•r~p h rl ~. ',tTlr'•! "':~ISIO"1
<br />
|