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Textures: Subsoil{ndicator{s)of Saturation: Consiste�ce: <br /> c-clay S1. pistinct gray or red redox features Loose• Intact specin�en not availabte <br /> siasitty cEay 52. bepleted matrix{vatue>/=4 and chroma =/=2) Friable- Stight force between fingers <br /> sc•sandy clay 53. 5Y chroi��a</= 3 Firm- Moderate lorce between fingers <br /> S4. 7.5 YR or redd�r faint redox concentrations or redox depietio Extremely_ Moderate force between hands or slir,ht <br /> ct-clay loam firm: foot pressure <br /> sicl-silty clay loam If yes to one of the above indicators then: Rigid- Foat pressure <br /> scl�sandy day Ioam Topsoit Indicator(s)of Saturation: Stop�Shap�: <br /> si•silt T1. Wetland Vegetation Slope shape is described in two directions:up and down slape <br /> sil-silt Eoana 'Sand Modifters T2.Depressianai Laildscape (perpendicular to tfie contour), and across slope {along the <br /> !•Eoam co•caarse 73.Organic texture or ors;anic modifiers horizontat contour};c.p. Linear, Canvex ar LV'. <br /> sl-sandy loam' m•medium T�. N 2.5/0 calor <br /> Es•loamy sand' f-fine T5.Redox features m tapsoil <br /> s-sand' vf-very fine T6. Nydraulic indicators <br /> Soil StrucEure � <br /> Grade: • • .. � • ` <br /> Massive• No observable aggregates,or no orderly arran�ement of natural lin�s of weakness � <br /> Weak�, Poorly formed, indistinct peds, bat'eIy observable in plate • � - " <br /> Mode�ate- Well formed,drstinct peds, moderately durable and evident, bUt ttOt diStlrlCt in UIKfiStu�bcad • ` _ � <br /> �urable peds ti�at are quite evident in un•displaced soit, adhere weakty to one another, _ ,. � - � <br /> Strong: w�khstand disptacement,and becon�separated when soil is disturtsed <br /> , . <br /> . . • . . <br /> loase- t�o peds sancly soiE `"�,�.`„•"�'°,•,••`"°": .. . , . <br /> + �...:,::;�� • ��- � <br /> �.__ ,._ �>>..�<<,��•� - . .. . . . . . <br /> __ [„�-s_•.��i.. 1 ! . , . _ , <br /> $03�$Lrt7G�Ui'@ ��,:�r ���.,�,. <br /> Shape: � ��•.�.,.,..,..- <br /> Granutar: The peds are approximately spherical or poiyhedral and are commonEy found in topsoil. These are the small, rounded peds that hang onto roois <br /> Pl.aty;- The peds are ftat and ptate like.They are oriented horizontally and are usually overlapping. PEaty s[ructure is commonly found in for�sted areas <br /> Bla{�y- The peds are btock-iike or polyhedrat,and are bounded by flat or s{ightly ro�mded surface that are casting of the faces of wrrounding peds. <br /> Prismatic�,., Flat or sltghtly rounded vertical faces bound the individuat�eds. Pecis are distincity longer verticalEy, and fac�s are typically cast or motds of <br /> Sin te Grain•Tlie structure found +ii a sandy soil.The individual particles are not I�etd together. <br />