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' <br /> ' The A horizon has hue of 10 value of 2 3 <br /> YR, or ,and chroma of 1 or 2. The A horizon is clay loam,loam,silt loaui, <br /> or silty clay loam.It has 20 to 30 perccut clay.It is mod�ately acid to neutral.An E horizon as much as 3 inches <br /> ' thick is in some pedons. <br /> The AB horizon has characteristics similaz to the A and the Bt. <br /> ' The upp�part of the Bt horizon has hue of lOYR or 2.SY,value of 3 to 5,and chroma of 2 ar 3. The lower pazt of <br /> the Bt horizon has a hue of 2.SY,value of 4 or 5,and chroma of 2 to 4. The Bt horizon is mostly clay loam or loam. <br /> � The argillic horizon ave�rages be�.wweeu 24 and 35 perce.nt clay and from 15 to 40 pprc�t fine sand or coars�rr. The Bt <br /> horizon is strongly acid to slighfly acid in the upper part and strongly acid to neatral in the lower part. The bulk <br /> deasity ranges from 1.30 to 1.45 gm/cc. <br /> ' Some pedons have a BC or Bk horizon. <br /> The C horizon has hue of 2.SY or SY,value of 4 to 6,and chroma of 2 to 4.It is loaw or clay loam.It is sli�tly <br /> ' alkaline or modeaately alkaline.The balk density ranges from 1.45 to 1.60 gm/cc. <br /> COMPETII�iG SERIE5:These are the Andres.Aurand(T),Aztaian.C�an •Darroch•��,Houst�ader(T),I,� <br /> � H M���N--S��4,T���.�oti�,Tiderishi,ViFar,and ilm�sc�ries.The <br /> Aurand(T)and Tiderishi series are prese�atiy not in the OSD file. The Andres,Aztalan,and Mokena soils have silty <br /> clay loam low�B and C horizons.Aztalan soils also have hue of 7.SYR in the B and C horizons. Crane soils have <br /> more than 8 percent rock fragments in the lower patt of the argillic horizon.Dan�och soils have C horizons of <br /> 1 stratified silty and sandy seidiments within the series control section.Gilboa soils have silt loam and silty clay loam <br /> in the upper part ofthe series control section.Honstenadex soils have 30 to 40 percent gravel in the lowea third ofthe <br /> series control sectian.I,a Hogue soils have less than 20 percent clay in the low�part of the series control section. <br /> ' Marcella�soils have less than 24 percent clay in the argillic horizon.Nachnsa soils do not have rock fragments in <br /> the upper part of the series control section.Neuno soils have more than 8 p�cent rcek fra�ents in the lower part of <br /> the series control sectian.Newhaven soils do not have frce carbonates in the saies control section.Odell soils have <br /> hue of lOYR in the lower B and C horizons and higha chroma in the nppea B horizon. Protivin soils have balk <br /> ' de,nsity geater than 1.60 gm/cc in the lowea part ofthe series control section. Vigar soils have a mollic�ipedon <br /> great�than 24 inches thick.Wilmer soils have more than 40 percent Sne sand or coars�in the azgillic horizon. <br /> � GEOGRApHIC SET'17NG:The Le Suear soils have slighdy concave,plane,or slightly convex slopes on <br /> moraines within the Dcs Moines lobe and Grantsburg sablobe of the Late Wisconsin glaciation. They formed in a <br /> calcareous,loaruy till. Slopes range from 1 to 3 perceut.Mean annual air temperature ranges from 45 to 52 degrees <br /> F.Mean annual precipitation ranges from 25 to 32 inches.Frost-free days range from 125 to 165. Elevation above <br /> ' sea level ranges&om 700 to 1600 f�eet. <br /> GEOGRAPHICALI.Y ASSOCTATED SOIIS:The main ones are the Cordova.Lest�,and Fi el soils. These <br /> � soils f�med in mataials similaz to the I.e Suair soils and are memb�s of a hydrosequence with the I.e Sueur soils. <br /> The poorly drained Cordova and Hamel soils are oommon associates on adjaceut nearly level slopes. The well <br /> drained Lester soils are the most common associate on the undulating to ge.nfly undnlating slopes. The well drained <br /> ' H �soils and the poorly drained I�soils are associates in some places. <br /> DRAINAGE AND PERMEABII,ITY:Somewhat poorly dramed. Surface runoff is low.Pcrmeability is modeaate. <br /> An apparent watea table is at 1.5 to 2.5 fcet dnring Nov�be,r to June in most years. <br /> ' USE AND VEGETATION:Mostly under cultivation with corn,soybeans,grain,and hay the ' ci al cro . <br /> Native vegetation was decidnons forest,dominanfly elm, � p � <br /> basswood,and maple in some areas,and oak with prairie <br /> ' and brush understory in the timbea ontliers within the prairie. <br /> DISTRiBUTION AND EXTENT: South-central Minnesota and north-central Iowa. This soil is ext�sive. <br /> � Swboda Ecolo 'cal Resources <br /> � 2180 Abingdon Way <br /> Project No.2007-056-03 Orono,Minnesota <br /> ' <br />