® Ontario ontario institute of pedology - Agriculture and Agri-Food ...
® Ontario ontario institute of pedology - Agriculture and Agri-Food ... ® Ontario ontario institute of pedology - Agriculture and Agri-Food ...
INGRAM SOILParent Material:Drainage:Usual Classification:Relatively undecomposed organic materials greater than 160 cm thickVery poorly drainedTypic FibrisolDescription : Om - 0-40 cm moderately decomposed organic material, derived chiefly frommosses ; strongly acidic in reactionOf,OftKANIMIWISKIA SOILParent Material:Drainage :Usual Classification :Description:Of,Bgcg40-120 cm slightly decomposed organic material, derived from mosses,wood, etc. ; strongly acidic in reaction120 cm+ slightly decomposed organic material, derived from mosses,sedges, wood; strongly acidic in reactionSlightly decomposed organic material, greater than 160 cm thickVery poorly drainedOf,OftKENABEEK SOILParent MaterialDrainage:Typic Fibrisol0-40 cm slightly decomposed sphagnum moss ; very strongly acidic.40-120 cm slightly decomposed organic material derived from sphagnum,cedar chips, etc . ; very strongly acidic.120 cm+ slightly decomposed organic material, dominantly of cedarorigin ; very strongly acidic.Noncalcareous, stratified outwash sandPoorly drainedUsual Classification:Orthic Humic GleysolDescription: Ah 0-13 cm sandy loam ; very dark brown (10 YR 2/2) ; highly organic; finecrumb structure ; friable consistency; stonefree ; pH - 5 .2KERNS SOILParent MaterialDrainage:Usual Classification :13-46 cm sznd ; gray (10 YR 6/1) ; very mottled ; single grain ; loos,stonefree ; pf . - 5.5sand ; very pale brown (10 YR 7/3) ; very mottled ; single grain; loose;stonefree ; noncalcareous ; pH - 5 .6Moderately decomposed organic material 40 to 160 cm thick over sandy claymineral subsoilVery poorly drainedTerric Mesisol
Description:Om l - 0-40 cm moderately decomposed organic material, derived from mosses,grasses and sedgesOm2 - 40-130 cm moderately decomposed organic materialIIC - 130 cm + sandy clay mineral subsoilMALLARD SOILParent Material:Drainage:Usual Classification:Outwash sand, sandy loam and gravelly sandImperfectly drainedGleyed Humo-Ferric PodzolDescription : LFH - 3-0 cm raw humus and roots, very dark gray (10 YR 3/1) ; pH - 5.0Ae - 0-8 cm sand ; light gray (10 YR 7/1) ; single grain structure ; looseconsistency ; stonefree ; pH - 4.5Bhfg - 8-46 cm sand ; brown (10 YR 5/3) ; mottled ; single grain ; occasionallycemented ; stonefree; pH - 5.3Cg - 46 cm+ sand; very pale brown (10 YR 7/3) ; mottled ; single grain ; pH -5.5MAYBROOK SOILParent Material:Drainage :Usual Classification :Slightly to moderately decomposed organic materials ranging between 40 and160 cm thick over clayey mineral subsoilVery poorly drainedTerric Fibric MesisolDescription : Of - 0-40 cm slightly decomposed organic materials derived mainly fromsphagnum mossOm - 40-130 cm moderately decomposed organic materialsHC - 130 cm+ clayey mineral subsoilMILBERTA SOILParent Material:Drainage:Usual Classification ;Varved, calcareous lacustrine clayVery poorly drainedOrthic Humic GleysolDescription: OH - 0-30 cm well-decomposed organic material ; very dark brown (10YR 2/2) ;pH - 6.530-53 cm clay ; gray (10 YR 6/1) ; mottled; mottles are yellow (2 .5 Y7/6) ;massive structure ; very hard consistencywhen dry ; very plastic when wet;stonefree ; pH - 7.0Ckg - 53 cm+ clay; white (10 YR 8/2) and yellowish brown (10 YR 5/4);varved ; very hard when dry ; very plastic when wet; stonefree ; calcareous ;pH - 7.859
- Page 13 and 14: EARLY PRECAMBRIANMafic Metavolcanic
- Page 15 and 16: DExposed bedrock andground moraineG
- Page 17 and 18: SOIL CLASSIFICATIONThe soils descri
- Page 19 and 20: Diagrammatic horizon patterns for f
- Page 21 and 22: Table 5 .Soils mapped in the Ville-
- Page 23 and 24: 3 . Calcareous silt loam(a) Good dr
- Page 25 and 26: Coutts soilsCoutts soils are imperf
- Page 27 and 28: Kanimiwiskia soilsThe Kanimiwiskia
- Page 29 and 30: Thwaites soilsThwaites soils are we
- Page 31 and 32: Frost ProbabilitiesFor 1951-1980 11
- Page 33 and 34: CropsAdapted field crops andassocia
- Page 35 and 36: Soil Physical Properties and Tillag
- Page 37 and 38: SOIL INTERPRETATIONS FOR AGRICULTUR
- Page 39 and 40: (c) The following are not considere
- Page 41 and 42: Subclass T (Topography) RatingsIn T
- Page 43 and 44: Table 10.Universal Soil Loss Equati
- Page 45 and 46: Table 11 .Slope class descriptions
- Page 47 and 48: In Table 13, soil erosion potential
- Page 49 and 50: REFERENCES1 . Hoffman, D.W., R.E. W
- Page 51 and 52: APPENDIXChemical and Physical Analy
- Page 53 and 54: Table 16 .Chemical and physical ana
- Page 55 and 56: B .Detailed Descriptions of Typical
- Page 57 and 58: CANE SOILParent MaterialDrainage :L
- Page 59 and 60: DAWSON SOILParent MaterialDrainage:
- Page 61 and 62: Bt - 33-51 cm silty clay loam; yell
- Page 63: Btg, - 23-33 cm clay; light yellowi
- Page 67 and 68: MUD LAKE SOILParent Material :Drain
- Page 69 and 70: THWAITES SOILParent Material:Draina
INGRAM SOILParent Material:Drainage:Usual Classification:Relatively undecomposed organic materials greater than 160 cm thickVery poorly drainedTypic FibrisolDescription : Om - 0-40 cm moderately decomposed organic material, derived chiefly frommosses ; strongly acidic in reactionOf,OftKANIMIWISKIA SOILParent Material:Drainage :Usual Classification :Description:Of,Bgcg40-120 cm slightly decomposed organic material, derived from mosses,wood, etc. ; strongly acidic in reaction120 cm+ slightly decomposed organic material, derived from mosses,sedges, wood; strongly acidic in reactionSlightly decomposed organic material, greater than 160 cm thickVery poorly drainedOf,OftKENABEEK SOILParent MaterialDrainage:Typic Fibrisol0-40 cm slightly decomposed sphagnum moss ; very strongly acidic.40-120 cm slightly decomposed organic material derived from sphagnum,cedar chips, etc . ; very strongly acidic.120 cm+ slightly decomposed organic material, dominantly <strong>of</strong> cedarorigin ; very strongly acidic.Noncalcareous, stratified outwash s<strong>and</strong>Poorly drainedUsual Classification:Orthic Humic GleysolDescription: Ah 0-13 cm s<strong>and</strong>y loam ; very dark brown (10 YR 2/2) ; highly organic; finecrumb structure ; friable consistency; stonefree ; pH - 5 .2KERNS SOILParent MaterialDrainage:Usual Classification :13-46 cm sznd ; gray (10 YR 6/1) ; very mottled ; single grain ; loos,stonefree ; pf . - 5.5s<strong>and</strong> ; very pale brown (10 YR 7/3) ; very mottled ; single grain; loose;stonefree ; noncalcareous ; pH - 5 .6Moderately decomposed organic material 40 to 160 cm thick over s<strong>and</strong>y claymineral subsoilVery poorly drainedTerric Mesisol
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