Soil Report - Agriculture et Agroalimentaire Canada

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Soil Key GENERAL DESCRIPTIONS OF THE SOILS A . Soils Developed on Glacial Till Deposits I . Silty clay loam till parent materials (a) Moderately well-drained 1 . Muriel (MUI) 2. Muriel coarse phase (MUI.C) 3. Muriel loamy phase (MULL) (b) Imperfectly drained 1 . Gobles (GOB) 2. Gobles coarse phase (GOB.C) 3. Gobles loamy phase (GOB .L) (c) Poorly drained 1 . Kelvin (KVN) 2. Kelvin coarse phase (KVN.C) 3. Kelvin loamy phase (KVN.L) (d) Very poorly drained l . Kelvin peaty phase (KVN.P) II . Reddish clay loam to clay till parent materials (a) Moderately well-drained 1 . Ontario (OTI) 2 . Ontario coarse phase (OTI.C) (b) Imperfectly drained 1 . Niagara (NGR) 2 . Niagara coarse phase (NGR.C) 3 . Niagara loamy phase (NGR.L) (c) Poorly drained 1 . Welland (WLL) 2 . Welland coarse phase (WLL.C) 3 . Welland loamy phase (WLL .L) 111 . Loam till parent materials (a) Well-drained 1 . Seneca (SNA) 2 . Seneca coarse phase (SNA.C) 3 . Seneca shallow phase (SNA .S) 4 . Seneca very shallow phase (SNA.V) IV . Gravelly sandy till parent materials (a) Rapidly to well-drained 1 . Wilsonville (WIL) 2. Wilsonville coarse phase (WIL.C) 3. Wilsonville loamy phase (WIL.L) 4. Wilsonville shallow phase (WIL .S) B . Soils Developed on 40 to 100 cm of Lacustrine Materials over Glacial Till Deposits I. Sandy lacustrine over silty clay loam till parent materials (a) Well-drained 1 . Bookton till phase (BOO.T) (b) Imperfectly drained 1 . Berrien till phase (BRR.T) (c) Poorly drained 1 . Wauseon till phase (WUS.T) II. Sandy lacustrine over gravelly sandy till parent materials (a) Rapidly to well-drained 1 . Scotland (STD) (b) Imperfectly drained 1 . Oakland (OKL) (c) Poorly drained 1 . Vanessa (VSS) 29 C . Soils Developed on Lacustrine Deposits I . Loamy sand and sand lacustrine parent materials (a) Rapidly to well-drained 1 . Fox (FOX) 2 . Fox shallow phase (FOX .S) 3 . Fox very shallow phase (FOX.V) (b) Imperfectly drained 1 . Brady (BAY) 2 . Brady loamy phase (BAY .L) (c) Poorly drained 1 . Granby (GNY) 2 . Granby loamy phase (GNY .L) 3 . Granby very shallow phase (GNY.V) (d) Very poorly drained 1 . Granby peaty phase (GNY .P) 11 . Mostly loamy fine sand and fine sandy loam lacustrine parent materials (a) Well-drained 1 . Wattford (WAT) (b) Imperfectly drained 1 . Normandale (NDE) 2 . Normandale coarse phase (NDE .C) (c) Poorly drained 1 . St. Williams (SLI) 111 . Loamy fine sand and fine sand lacustrine parent materials (a) Very poorly drained 1 . Lowbanks (LOW) IV . Mostly silt loam lacustrine parent materials (a) Well-drained 1 . Brant (BRT) 2. Brant coarse phase (BRT .C) 3. Brant very shallow phase (BRT.V) (b) Imperfectly drained 1 . Tuscola (TUC) 2 . Tuscola coarse phase (TUC.C) 3 . Tuscola shallow phase (TUC .S) 4 . Tuscola very shallow phase (TUC.V) (c) Poorly drained 1 . Colwood (CWO) 2. Colwood coarse phase (CWO .P) V . Silty clay loam and silty clay lacustrine parent materials (a) Moderately well-drained 1 . Brantford (BFO) 2. Brantford coarse phase (BFO.C) 3. Brantford loamy phase (BFO.L) 4. Brantford shallow phase (BFO.S) 5 . Brantford very shallow phase (BFO.V) (b) Imperfectly drained 1 . Beverly (BVY) 2. Beverly coarse phase (BVY.C) 3. Beverly loamy phase (BVY .L) 4. Beverly shallow phase (BVY .S) 5 . Beverly very shallow phase (BVY.V) (c) Poorly drained 1 . Toledo (TLD) 2 . Toledo coarse phase (TLD.C) 3 . Toledo shallow phase (TLD .S) 4 . Toledo very shallow phase (TLD.V)
(d) Very poorly drained 1 . Toledo peaty phase (TLD .P) VI . Heavy clay lacustrine parent materials (a) Moderately welldrained 1 . Smithville (SHV) 2. Smithville coarse phase (SHV.C) 3 . Smithville loamy phase (SHV .L) 4. Smithville shallow phase (SHV .S) 5 . Smithville very shallow phase (SHV.V) (b) Imperfecxtly drained 1 . Haldimand (HIM) 2 . Haldimand coarse phase (HIM.C) 3 . Haldimand loamy phase (HIM.L) 4 . Haldimand shallow phase (HIM .S) (c) Poorly drained 1 . Lincoln (LIC) 2 . Lincoln coarse phase (LIC .C) 3 . Lincoln loamy phase (LIC .L) 4 . Lincoln shallow phase (LIC .S) 5 . Lincoln very shallow phase (LICK) (d) Very poorly drained 1 . Lincoln peaty phase (LICY) D . Soils Developed on 40 to 100 cm of Lacustrine and Eolian Materials over Contrasting Lacustrine Deposits 1 . Sandy sediments over silt loam lacustrine parent materials (a) Well-drained 1 . Walsher (WSH) (b) Imperfectly drained 1 . Vittoria (VIT) (c) Poorly drained 1 . Silver Hill (SIH) 11 . Silty sediments over silty clay loam and silty clay lacustrine parent materials (a) Imperfectly drained 1 . Tavistock (TVK) (b) Poorly drained 1 . Maplewood (MPW) III . Sandy sediments over silty clay loam and silty clay lacustrine parent materials (a) Well-drained 1 . Bookton (BOO) (b) Imperfectly drained 1 . Berrien (BRR) (c) Poorly drained 1 . Wauseon (WUS) (d) Very poorly drained 1 . Wauseon peaty phase (WUS .P) IV . Sandy sediments over heavy clay lacustrine parent materials (a) Imperfectly drained 1 . Berrien heavy clay phase (BRR.H) E . Soils Developed on Glaciofluvial Deposits I. Gravelly loamy sand on gravelly glaciofluvial parent materials (a) Rapidly to well-drained 1 . Burford (BUF) F . Soils Developed on Eolian Deposits 1 . Fine sand eolian parent materials (a) Rapidly to well-drained 1 . Plainfield (PFD) 2. Plainfield dune phase (PFD.D) (b) Imperfectly drained 1 . Walsingham (WAM) (c) Poorly drained 1 . Waterin (WRN) (d) Very poorly drained 1 . Waterin peaty phase (WRN .P) G . Shallow Soils Over Bedrock I . Various parent materials less than 20 cm thick over bedrock (a) Rapidly drained 1 . Farmington (FRM) (b) Poorly drained 1 . Brooke (BOK) H . Soils Developed on Organic Deposits 1 . Organic soils 40 to 160 cm thick over coarsetextured mineral soil (a) Very poorly drained 1 . Hampden (HMP) II . Organic soils 40 to 160 cm thick over mediumtextured mineral soil (a) Very'poorly drained 1 . Oakview (OVW) III . Organic soils 40 to 160 cm thick over fine-textured mineral soil (a) Very poorly drained 1 . Lonsdale (LDL) IV. Deep organic soils greater than 160 cm thick (a) Very poorly drained 1 . Styx (SYX) 1. Miscellaneous Land Units 1. Soils developed on recent alluvial deposits (a) Undifferentiated drainage 1 . Undifferentiated textures i) Alluvium 1 (1-ALU) 2 . Mainly sand and gravel i) Alluvium 2 (2-ALU) 3 . Mainly silt loam and loam i) Alluvium 3 (3-ALU) 4. Mainly clay i) Alluvium 4 (4-ALU) 11 . Landscape complexes 1 . Beach - scarp complex (CPX 1) 2 . Marsh - beach complex (CPX 2) 3 . Marsh - dune complex (CPX 3) 4 . Marsh - ridge complex (CPX 4) 5 . Beach - dune complex (CPX 5) 6 . Beach - ridge complex (CPX 6) III . Miscellaneous units 1 . Marsh (MAR) 2 . Ridge (RID) 3 . Gravel pit (G.P.) 4 . Quarry (Q) 5 . Urban Land (U.L.)
Page 1 and 2: REGIONAL MUNICIPALITY OF HALDIMAND=
Page 3 and 4: INTRODUCTION The soil survey conduc
Page 5 and 6: 1 . Condition of farmland in the Re
Page 7 and 8: MANITOBA Figure 1. General location
Page 9 and 10: TOWNSHIP OF NORFOLK K,bmel,es 5 0 5
Page 11 and 12: Ô rt-v., s o s ro Waterford Port D
Page 13 and 14: Table 3. Number and size of farms i
Page 15 and 16: mainly bedrock-controlled. Most of
Page 17 and 18: Figure 10 . Schematic landscape cro
Page 19 and 20: i Wattford soils I Figure 15 . Sche
Page 21 and 22: Figure 17. Location of regional wea
Page 23 and 24: Table 8. First field seeding or pla
Page 25 and 26: Mh Well-to moderately well-drained
Page 27 and 28: A vertical section through the expo
Page 29: Table 9 . Soils mapped in the Haldi
Page 33 and 34: Landformand Topography Most Berrien
Page 35 and 36: anges from nearly level on the lacu
Page 37 and 38: Parent Materials and Textures Colwo
Page 39 and 40: Figure 30. These Gobles coarse phas
Page 41 and 42: Parent Materials and Textures Kelvi
Page 43 and 44: Soil Moisture Characteristics Maple
Page 45 and 46: Landform and Topography Oakview soi
Page 47 and 48: Figure 37 . Vegetable crops, such a
Page 49 and 50: Styx Soils (SYX) Location and Exten
Page 51 and 52: Parent Materials and Textures Vanes
Page 53 and 54: strong brown to brownishyellow mott
Page 55 and 56: Parent Materials and Textures Wilso
Page 57 and 58: SOIL INTERPRETATIONS FOR AGRICULTUR
Page 59 and 60: Table 10. Agricultural land capabil
Page 61 and 62: (Footnotes for Table 10) tOrganic s
Page 63 and 64: (5) Table 12 . Agricultural land su
Page 65 and 66: Table 12. Agricultural land suitabi
Page 67 and 68: Table 14 . The relative effectivene
Page 69 and 70: Table 15. K-values, K-ranges and er
Page 71 and 72: Continuedfrom page 66 (c) Slope Gra
Page 73 and 74: Table 18. C-values for continuous a
Page 75 and 76: Table 20. C-values for horticultura
Page 77 and 78: (4) Soil Erosion Assessment Regiona
Page 79 and 80: (b) Site Specific Soil Loss Potenti
Page 81 and 82:
Table 24. Estimated susceptibility
Page 83 and 84:
v c a> ç C U a PROCEDURE : With ap
Page 85 and 86:
Table 27. Description of wind erodi
Page 87 and 88:
Table 28. Drainage characteristics
Page 89 and 90:
(cm) 0- 20 . 40- 60 80- 100- . 0- 2
Page 91 and 92:
Table 31 . Drainage code slope clas
Page 93 and 94:
N Table 32. Soil interpretations fo
Page 95 and 96:
Table 32 . Soil interpretations for
Page 97 and 98:
Table 35. Explanation of terms and
Page 99 and 100:
1 . Ontario Soil Survey. 1928 . Soi
Page 101:
O %LLSONBUR6.WV¬COMBE,__ 1 7OWNSHI
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