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1�he A or Ap horiaans have hue �f 1�JYR, tialue aF?or 3, an� chroma oF 1 ar 2_ 'I'he �
<br /> horiz�n wherc pr�:sent, has vaiue of 3 ta 5,an�! cllrom�c�F l t� 3. The A And E horiz�ns
<br /> are loam c�r clay loam. (�ut sand}' Ioarrl, fine sandy loam, a� silt kc�am is within the ran�e.
<br /> (liey range frcarn rnocle�a�ely aciJ to neutral.
<br /> 1'I1e Ht horizan has izue c�f l{)YK ar 2.SY, ��alue aP�or 5. an� chroma ot 3 or 4. lt is clav
<br /> loam or (uam and has 2�4 to 35 peccent elay anci 30 to 45 percent Sand. The B/.A clay
<br /> ratios ranae fr�m 1.2 to 1.�. It is stron};ly acid tu sii�htly acia in the upper part and
<br /> rnoderately acicl t� ncutral in the IoN�er part. A Brv hc�riaon iy somctimes present belc�w
<br /> the Bt.
<br /> The Bk horizon h�s hue of lOYR or?.S�r'R, value of� or�, und chroma of� tt� 6. The Bk
<br /> harizon is loain or clay Ic�nm. lt is sliglttl�� alkaline or �tiacierately alkaline, Relict
<br /> redc�timorphie teatures ac•e pcesent in some pe�ons.
<br /> The � horizan has hue oF2.5Y or IQYE�, value aF4 to 6,anci cl7roma oF3 t� 6. [t is foam
<br /> or clay loam. (t is slightlti• alkaline or moderately afkaline. Relict red�ximorphic features
<br /> arc present in s�me pecions.
<br /> CC�IIPET[�1C SG�I�S: The�e ��'� Che 1<<��,�u<, _1r��,,���. (3 il�i��i,����,�, ►�a.,�t„ [sl���;ir�in,�.
<br /> ._ _ _ __�
<br /> � :f�:P', �1� t, �I.i4. �)llll��l 14{"C'� { �:t1�41. �'1>51ti`=I`Ii`� �.i1411'ililll�� �.i)Il��1"�[1t � �i.111"�� �4�lk�1c11\,��
<br /> . __. _ _ __... � + . ._, ...., _._..._.
<br /> �+tii� I � •_��.CnI1�C1� k)li�1u 1 )Ititiir _�, �41e1t1�:, E� 2�."�1"I, �l�flti {cl��11. 11 :t�It.�1'1,1, �I1C�
<br /> _- - -.__.__---__ ,___.. _ �._.w� __
<br /> _ -_
<br /> ��_i�:�;c�.i�i�; soils in the same familr�. An�,us and 5ebbo soi) have saturation in the lotivcr
<br /> third of the series cc�ncrol secti�n. Ar�;yle, Baltirnu��e, ancl t�neco soils have B horizc�ns
<br /> with 7.5`r'R ur recider hue. Bassett soils ar�vcry stronely acid to mc�der�tely acid in che
<br /> upper p�rt uf ti�e Bt I�arizon. Blooming and Racine soils hav� !5 to 35 perc�nt sand in the
<br /> tipper part af tlie pal�icle-size cnntrol sectian. C�(eb soils have some subharizons that
<br /> hav� more than =1� percent in the lower part of th�c�ntrc�l section. Uu�v�giac and Koronis
<br /> soils have tess than 2� percent cfay in the fow�r onc; third ot the �articl�-sixe contrc�l
<br /> section. Qunbrid��, bb`aucorna, l�e���umer and �Vinnesiiiek soils liave sola terminated bp•
<br /> bedrack at depths aaove 6U inche�. G�ra scrils average les5 than 2 percent rock fra�ments
<br /> in the contrnl section. I.,onglc�is, t.ydic, and Necis soils have more than 8 p�rcent rock
<br /> Fr��ments ir, sc�me subhorizon c�f the control section. (_auramie soil, have more than �5
<br /> per�ent �and in s�m� subhorir��n in the middle part of the cantrc�l section. titoha4vk soils
<br /> have a tiigher content of silt and hav�darlc cnlors in thc: B hc.tirizon which apparentl}' arr
<br /> inhericed from dark shale. Ur��o��d soils have na rac� fra�ments in the particle-size
<br /> cantrol sectic�n. (ta�art soils have less than 3� percent sand in the control sectian.
<br /> GEUGR�PHIC SGTT[NG. These soils have com�ex slupc:s on moraines and till plains.
<br /> 51a�e gradients range t'rom 5 to 70 percent. They forrned in caleareous, Ic�amv glac:ial till
<br /> c�f late Wis�onsinan A�;e. i�tean annual Eernperature ranges frvm �� de�rees to �? de�rees
<br /> P. h•1�an anr,uaC pr��cipitation ranges fram 2S to 33 inehes, Frc�st free day�s r�nge frcam [?a
<br /> to I 65. Elevations r�nge frc�m 7(�f to !6U0 feet.
<br /> GE()t:R�PfllCALLY AS50CIAT�D SOILS: These inciud� the +. .���I�,�,�, f>��r.�.�,,
<br /> _
<br /> ( �I��Fa,.,:, f 1.�;�z�l, I I��ti,�l��t�����, i��.l �; �,,�r, l �: `�u��G��. �I�E�� �����, and �;��� soiis. Pu�r(y
<br /> �
<br /> .. _ __. _ _ _� _-
<br /> drained C�r�lova and someyvhat pc�r(y ttnd poUrly dcained l7undas s�ils ar�on flats anci
<br /> uppzr draina�etivays 4vith � high seasona) water table. Vcry pac�rly drnined Gl�ncoe,
<br />
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