Detailed Soil Survey of the Mount Revelstoke Summit Area.
Detailed Soil Survey of the Mount Revelstoke Summit Area. Detailed Soil Survey of the Mount Revelstoke Summit Area.
orizonPyrophosphate96ANALYTICAL DATA 8BHorizonDepthcmCaC12pHN(I)Org .C(7)C/N NH4Ac Ext . Cations (me/100g)Na K Ca Mg T .E .C .L 4-0 3 .6 - - - 0 .09 0 .66 0 .16 0 .38 65 .5Ah 0-15 4 .3 .44 10 .41 23 .7 0 .08 0 .09 0 .21 0 .17 39 .9Bf 15-35 4 .5 .11 2 .89 26 .3 0 .02 0 .02 0 .31 0 .41 19 .3C 35+ 4 .7 - - - 0 .01 0 .01 0 .06 0 .05 4 .40Fe A1 Fe+A1 (I) Text.Class>2mm(/°)SandMSiltMClayMBulkDens .g/cm3Ah 0 .68 0 .57 1 .25 SiL 5 22 69 9 0 .4Bf - - - SL 15 66 28 6 -C - - - LS 15 84 15 1 -
Soil Map Unit 9The soils of Map Unit 9 occur mostly at the lower elevationsin the southern half of the study area,under fairly continuous treecover .These are well developed Podzolic soils with eluviated surfacehorizons and cemented B horizons .Classification :These soils are classified as Ortstein Ferro-Humic Podzols,although the Bhf horizon may not always satisfy the 10 cm minimum depthrequirement for such horizons . The lower B horizons are firmly cemented(ortstein layer) .Associated Map Units :Map Unit 9soils are often associated with bedrock outcrops(R) and lithic soil phases (Map Unit 10) . Map Unit 9 soils grade toMap Unit 8 soils as Ah horizons become thicker and Ae horizons disappear .Vegetation :Vegetation commonly consists of Abies lasiocarpa - Rhododendronalbiflorum dominated communities with Vaccinium membranaceum ,Luetkeapectinata and Phyllodoce emQetriformis often abundant .Pedon Description :Described by : L . KnapikDate : August 27, 1973Location : S-9Parent Material :tillLandform :moraine covered bedrock ridge
- Page 52 and 53: TABLE 10 . DEGREE AND NATURE OF SOI
- Page 54 and 55: 49The soils of map units 1, 8 and 9
- Page 56 and 57: 51compounds thus inhibiting percola
- Page 58 and 59: 53PRODUCTIVITYProductivity ratings
- Page 60 and 61: S4 XTABLE 11 . DISTRIBUTION OF SOIL
- Page 62 and 63: 57BIBLIOGRAPHYAlberta Department of
- Page 64 and 65: 59Terzaghi, K . and R .B . Peck . 1
- Page 66 and 67: 61ecosystem .While the activities i
- Page 68 and 69: TABLE A. CLASSES OF FRAGILITY FOR P
- Page 70 and 71: TABLE B. CLASSES OF FRAGILITY FOR S
- Page 72 and 73: 67than to channel use to a rarer ty
- Page 74 and 75: 69approximately 10 cm thickness and
- Page 76 and 77: 71ANALYTICAL DATA 1HorizonDepthcmCa
- Page 78 and 79: 73several species of common occurre
- Page 80 and 81: 75Soil Map Unit 3The imperfectly to
- Page 82 and 83: 77Soil Classification :Orthic Regos
- Page 84 and 85: 79ANALYTICAL DATA 3BHorizonDepthcmC
- Page 86 and 87: 81Elevation : 6,000 ft . ASL (1,830
- Page 88 and 89: 82ANALYTICAL DATA 4HorizonDepthcmCa
- Page 90 and 91: Aspect :southeastElevation : 6,200
- Page 92 and 93: Soil Map Unit 6Hummocky microrelief
- Page 94 and 95: ANALYTICAL DATA 6HorizonDepthcmCaC1
- Page 96 and 97: Location : S-7Parent Material :glac
- Page 98 and 99: Soil Map Unit 8These soils have med
- Page 100 and 101: Elevation : 6,250 ft . ASL (1,910 m
- Page 104 and 105: Slope : 5%Aspect :northElevation :
- Page 106 and 107: Soil Map Unit 10Map Unit 10 soils h
- Page 108 and 109: Vegetation : Abies lasiocarpa (shru
- Page 110 and 111: 104ANALYTTCAL DATAlOBHorizonDepthcm
- Page 112 and 113: A further separation of sands is ma
- Page 114 and 115: (D1) Rapidly drained - soil moistur
- Page 116 and 117: 110TABLE 13 . UNIFIED SOIL CLASSIFI
- Page 118 and 119: GLOSSARYThis is included to define
- Page 120 and 121: illuviation -the process of deposit
- Page 122 and 123: pH - a notation used to designate t
- Page 124: LATIN AND COMMON NAMES OF PLANTS ME
orizonPyrophosphate96ANALYTICAL DATA 8BHorizonDepthcmCaC12pHN(I)Org .C(7)C/N NH4Ac Ext . Cations (me/100g)Na K Ca Mg T .E .C .L 4-0 3 .6 - - - 0 .09 0 .66 0 .16 0 .38 65 .5Ah 0-15 4 .3 .44 10 .41 23 .7 0 .08 0 .09 0 .21 0 .17 39 .9Bf 15-35 4 .5 .11 2 .89 26 .3 0 .02 0 .02 0 .31 0 .41 19 .3C 35+ 4 .7 - - - 0 .01 0 .01 0 .06 0 .05 4 .40Fe A1 Fe+A1 (I) Text.Class>2mm(/°)SandMSiltMClayMBulkDens .g/cm3Ah 0 .68 0 .57 1 .25 SiL 5 22 69 9 0 .4Bf - - - SL 15 66 28 6 -C - - - LS 15 84 15 1 -
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