09-20-2004 Planning Packet - Laserfiche WebLink

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RANCE IN CHARACTERISTICS: SoUim ihi„Wnc.> and depth to free carbonaicv ianj:c fiom 24 to 54 inchoN. Ciut-e fi.ijiments of nii\ed lithology eompiisc 2 to S percent ot the volume of the control vcctioii The A horizon h.i> hue of lOYR. value of 2 or 3. and chroma ol I or 2 The Ap horizon hav value of 4 or 5 and chroma of I oi 2 and value of 6 when dry The E horizon ha> hue of lOYR. value of 4 or 5. and chroma of I or 2. The A and E hcrizon.s lypieally are ioam. silt loam, sandy loam, or fir.' ' mdy loam, but include clay loam, if erected. They are neutral to medium aeid The B: horizon h.rs hue of lOYR in the upper part ar.il lOYR or 2 5V in the lower part, value of 4 or 5. .ind chioma ol 3 thiough 5 Mottles arc present in the lower s 'izon.s m some pedons It typically i> clay loam or loam, but sandy cl.iy loam is in parts in some pedens. The argillic horizon has IS to 35 percent clay and 30 to 45 percent sand It is slightly acid to strongly .acid Some pedons have a BC horizon. The C horizon has a hue of lOYR or 2 5Y. value of 4 or 5. and chroma of 3 through 6. It is loam or clay loam. It lacks mottles in son.e pedons it ha.s 15 to 25 percent calcium carbonate equivalent and is mddly or moderately alkalikrc COMPETING SERIES: These aic the Amanda. Be!mom. Delmoie. Qigtuull. Chili. Coggon . Conevtoga. El Data. Cull nan. Grcllton. Hebron, iiiikijiy. HiSh-GiiC* Hollingcr . Katjm.>zoo. Kanawha. Kerda.lvillc. K dJer. KoNcu.>ko. LcRoy. I.etorr. Lindlcv. McHeniv. Mandeville. Martinsville. Miam;. Mifflin. Mjlitary. Nccline. Not deg, (Mley. OwossQ. Pecatonica. Princeton. Rawispn. g.?iay. RenQva. Rictlanij. Riddle^. Rockbridge. Roseville. Sisson. Strawn. Suirimuville. Teanawav. Theresa. Wawascc. WeMville. Whalan. and Woodbine soils in the same family Amanda horizon sods have more dine in the B and C horizon, Belmont sods have redder hue ;n the B horizon. Bclmorc. Chdi. Kalamazoo, and Ockley sods formed in glacial outwash and have sandy or s.indy-skcletal 2C horizons Chenault sods have chert fr.agments m the solum and are underlaid by limestone bedrock. Coggon. Gallman. Hickory’. Pccaionica. Renova. Riddles. Summitvillc. and Wests die sods have thicker sola In addition. Coggon soils have low chroma mottles in p.irt of ihc B2 horizon Conestoga. Kendaliville. Lciort. Richland, and Rockbridge soils have more coarse fragmc.iis Drmds. El Dara. Kidder. Sisson, and Wawascc sods have less clay and more sand or sill in the lower part of the B horizon and in the C horizon. High Gap. Hollingcr. Mandeville. .Mifflin. Military. Norden. Roscvdlc. Whalan. and Woodbine sods have bedrock beginning between depths of 20 and 60 inches. GrcUton. Hebron. Lindlcy. and Raw son sods have more silt or clay or both in cither the lower part of the B horizon or C horizon or both Kanawha sods .are formed in alluvium from ac.d sfulc and are in an area of higher rainfall. LcRoy and Straw n sods have thinner sola. McHenry and Miami sods have more sill or clay, or both in the upper pan of the solum .Maninsvillc soils have redder hue in the B horizon and formed in stratified outwash or lacustrine sediments Nodine soils have thicker sola which is more stratified and leached of free carbonates to greater depths. Owosso soils have more sand and less silt or clay in the upper part of their sola Princeton soils formed in aeolian sedim.cnts and have stratified C horizons Relay soils have hue of 2.5Y or 5Y in all parts of the B horizon Teanawav .soils have fitm sandy clay loam C horizons with