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Series • <br />The ZPcld series rnnsists of well-dninrd. nearly level <br />soils on uplands. Tltrse soils farmed in wind-worl:ed <br />loamy materials. <br />In a reprnsentativr, nrofilr, the sttrfue la~•er is brown <br />loam abort 6 inches thick. It is noncalcaremts. The npner <br />part of the s»bsoil is dart;-beater[ clac about 6 incites <br />thiclc It is noncalcareotts. The lower part of tltr. soh=nil <br />is pale-brown and very fate sandy loam al>nttt ~fl incltrs <br />thirl;. It is highly calcareous, and mach of the limn is <br />visible as splotches. The underlyin_ material is highly <br />calcareous, pale-brown silt loam and li;ht yellowislt- <br />brown fine sandy loam. <br />~Peld soils absorb water at a moderate rte, and the <br />available water canacity is high. Prrmeahility is slow, <br />and the entire soil is snitahlr for plant roots. <br />Representative profile of ZYrld loam. 1 to 3 percent <br />slopes, in an area of rrr_ss, 0."5 mile east and 75 feet <br />north of the southwest corner of section 86, T. 3 S.. R. <br />59 ti1T.: <br />Al--0 to 8 inehn, brown (lOYR 5!3) loam, dark brovia <br />(lOYR 3/3) whet[ moist; weak to modente. doe. <br />grandar structure; soft, Lriable; nancalcareous; <br />mildly alkaline: abrupt, smooth boundary. <br />H~t~ m L^ inches, dark-brown (lOYR 4/3) clay, dark <br />brown (10YR 313) when moist; strong, doe, pris- <br />made structure part(ag to strong, medium gad floe, <br />aagnlar and svbnagalar blatdcy saactttre; hard, Hem; <br />matiaaous clay Hlma; graTng is cracks la upper <br />part; aoacalcareons; mildly a1L-aline; clear, smooth <br />bomdary. <br />B31ca-L" co ^_1 inches. pale-brown (lOYR 8/3) loam, brown <br />(lOYR 5/3) when moisc; weak to modente, me• <br />dlnm. prismatic srmccnre Parting to moderate, me- <br />dium to coarse, subnngnlar blocYy sanccare; slightly <br />hard, Iriahle; thin patchy clay dims; calcareous and <br />rnacaias lime disseminated and is splotches: moder- <br />ately alkaline: clear, smooth boundary. <br />B3:ca-^1 to 3~ inches. pale-brown (lOYR 8/3) very Hoe <br />sandy loam, brown (lOYR 5/3) When moisc: weak, <br />croane, Drisma[ic s[mctnre Parting to weal:, coarse, <br />snbaagular Ulocky structure: salt. very fnaUle; thin <br />patchy clay dims on vertical Cates; calcareous gad <br />contains lime disseminated and is splotches; strongly <br />alkaline; clear, smooth bomdary. <br />Clca;,^ to 58 inches. pale-bmwn (10YI2 8/3) silt loam, <br />brawn (lOYR i/3) when moisc: massive; soft, very <br />friable; calcareous and contains lime cllssemiaaced <br />gad in flaely divided particles; moderately alkaline; <br />clear, wavy bomdary. <br />C:ca;,3 [0 88 inches, light yellowish-brown (lOYR 8/i) doe <br />sandy loam, yellowish brown (lOTR 5/i) when <br />moist: massive; soft, verT friable: calcareous and <br />contains lime disseminated and in flaely divided <br />Particles; saoagly alkaline. <br />The ~ horizon Wages from i to 9 inches in Chicl.-aess, from <br />brown [o dark grayish brown is color, gad Crnm loam [o <br />silt Ivan[ is teSCUre. The B horizon rases Lrnm 10 co ^_9 <br />inches is thickness. Depth Co lime ranges from 30 to .0 <br />inches. <br />Weld loam, l to 3 percent slopes Iwm61.-This soil llas <br />the pmfilc drsrrihrd as' representatit'c for the series. It <br />is on uplands. The areas arr. irtr_ntlar in shape and <br />ran_c from 3Q to TOQ acres in size. jurf;u•c nmoff is <br />medium. and the hazard of water erosion is mo~lrratr to <br />severe. The hazard of soil binwin_ is srrere in ~lrefarmcd <br />areas if rainfall is below ltol•mal. - <br />Inclttded in mappin_ arc some small areas where. <br />slopes are less than 1 percent..11sn included ;tee some <br />small cress of Adena loam that arc in most slopitii; <br />areas. <br />1lmost ail of this ~Peld soil is rnltivatrd.:\ few areas <br />are irrigated. Scattered arras thmn_hrntt Clie ~~nnnty arc <br />in native brass. Capability unit IIc-l, irri_ tted, and <br />IIId-1. nnnirrirlted; Loamy Plains ran_~e site; tree plant- <br />in_ suitability ;ronp 1. <br />