Soils of the - Agriculture and Agri-Food Canada
Soils of the - Agriculture and Agri-Food Canada Soils of the - Agriculture and Agri-Food Canada
STURGEON SOILS (SG) Location and Extent : Sturgeon soils occur mainly in the Pitt Polder area and in the northern part of Pit t Meadows Municipality. Lesser areas are found along the western edge of the lower Pitt River and near the mout h of Widgeon Creek . About 320 ha of pure map units and 1550 ha of soil complexes dominated by Sturgeon soil s are mapped . Most complexes are with Addington, Alouette and Widgeon soils . Topography and Elevation : The topography of Sturgeon soils varies from slightly depressional or nearl y level to gently undulating with slopes of less than 2 percent . All areas lie less than 5 m above sea level . Parent Material and Texture : Sturgeon soils have developed from medium-textured, mixed floodplai n deposits of the Alouette, Pitt and Fraser Rivers, capped by 20 to 40 cm of mostly well-decomposed organi c material . Surface texture is humic, usually containing from 20 to 50 percent silt . The subsurface is silt loam , occasionally varying to silty clay loam or silt . The upper subsoil is similar but below depths of 100 cm or more , the texture gradually changes to fine loamy sand or fine sandy loam . Soil Moisture Characteristics : Sturgeon soils are very poorly to poorly drained . They are moderatel y pervious and have high water holding capacity and slow surface runoff . The watertable is at or near the surfac e for most of the winter and recedes only slightly during the summer . Undyked areas are susceptible to flooding . General Soil Description : Sturgeon soils usually have about 10 cm of black, well-decomposed, friable , granular, organic material at the soil surface . This grades to a further 30 cm of very dark brown to dark yellowis h brown, friable, organic material that contains variable amounts of silt (usually 20 to 50 percent) and crack s vertically on drying . This is underlain by about 50 cm of silty material that is massive, dark grayish brown i n colour, friable and contains few to common, dark brown to reddish-brown mottles . Occasional vertical crack s are present which contain organic material from above . Under this is massive, very dark gray to olive-gray, silty or fine sandy material that contains common, prominent, brownish mottles along old root channels . Soil reactio n grades from extremely acid in the upper soil to medium or very strongly acid below 100 cm depth . Soi l classification is Rego Gleysol:peaty phase. Commonly Associated Soils : Alouette, Widgeon and Addington soils often are closely associated with Sturgeon soils . Alouette soils are generally similar to Sturgeon soils except that the upper part of the minera l subsurface layer is well structured . Alouette soils are also usually slightly better drained than are Sturgeon soils . Addington soils are usually more poorly drained and have water on the soil surface for large parts of the year . The mineral subsurface and subsoil of Addington soils is also more sandy than are those in Sturgeon soils . Widgeon soils differ by being organic in the upper 40 to 160 cm . Vegetation : Cultivated (and drained) areas are used mostly for forage production and some blueberries . The majority of Sturgeon soils are undeveloped and support a variety of moisture tolerant species including sedge s and reeds, willow, some black cottonwood, hardhack, sweet gale and others . Rooting is confined mainly to th e upper 60 cm by the high groundwater tables . General Land Use Comments : (1) Where unreclaimed, Sturgeon soils are agriculturally limited to mainl y permanent pasture uses. With adequate watertable control (both subsurface and flooding), these soils ar e potentially suited for most crops, except perhaps, those that are especially susceptible to periodic we t conditions . (2) Urban and related uses are generally unsuited for Sturgeon soils . Bearing strengths are variabl e (usually low), a flooding hazard is present in most locations and high watertables preclude basements an d severely inhibit operation of septic tank effluent disposal fields . (3) High watertables and periodic floodin g preclude most commercial tree species . 180
SU MAS SOILS so_ Location and Extent : Sumas soils occur only in the eastern part of the map area . west of the Vedder Can a and occupy mainly the basin of former Sumas Lake (the lake was drained in the 1920`s) . About 2400 ha e' r map units and 270 ha of Sumas-Dixon :shallow variant soil complex are mapped . topography and Elevation : The topography of Sumas soils is nearly level with some variation to gent'' , undulating Slope gradients are less than 2 percent and elevations are below 5 m above sea level . r Parent Material and Texture : The parent material of Sumas soils is coarse-textured lacustrine deposit s rface textures are usually loamy sand with some variation to sandy loam . Subss, aCe and subsoil ire s dium or coarse sand . occasionally containing bands of loamy sand Soil Moisture Characteristics : Sumas soils are poorly to very poorly drained . They are rapidly perv c _ have low water holding capacity and slow surface runoff . Most of the Sumas soil areas have controlled war s s achieved through a system of ditches . floodgates and pumping . Sub-irrigation of most of the are a mplished by manipulation of water levels in drainage ditches During the winter especially, temporar y ing may occur during heavy rains which rapidly raise the already high groundwater table . i F General Soil Description : Sumas soils have a sandy, cultivated surface about 15 to 20 cm thick, which is , dark grayish brown, friable and contains sometimes, faint reddish or brownish mottles . The surface is unde r by about 30 cm of very friable to loose . grayish-brown to olive-gray, medium sand containing few to comma ' usually faint mottles along old root channels . This zone, in turn, grades to loose, olive-gray, medium or coars e sand . usually water saturated and containing occasional, variably coloured mottles . Soil reaction gere n a . 1 i grades from strongly or eery strongly acid irl the surface to slightly acid or neutral in the subsoil (1 1 H-n) S classification is Rego Gleysol . i Commonly Associated Soils : Dixon soils are often found near the margin of Sumas soils They are poorl y drained as are Sumas soils but have s i lty to o ayes __ : rface and subsurface textures which sandy textures of Sumas soil s east with +h F 1 I Vegetation : Essentially all areas of Sumas soils are cleared and cultivated . A few, isolated uncleared area s support grasses, sedges, reeds, willow and black cottonwood Hooting is generally restricted to the upper 5 0 cm by the high groundwater level s to 38 Landscape across the nearly level, poorly drained sandy Sumas soils . These soils are used for a variety of annua l cash crops . Note the level of the water in the ditch. Subirrigatlon during the growing sea - son is provided by controlling the water levels in the ditches . 181
- Page 145 and 146: MATHEWS SOILS (MW) Location and Ext
- Page 147 and 148: =-'~ squi soil profile (Eluviated E
- Page 149 and 150: McELVEE SOILS (ME) Location and Ext
- Page 151 and 152: MILNER SOILS (ML) Location and Exte
- Page 153 and 154: (M) General Land Use Comments : (1)
- Page 155 and 156: General Land Use Comments : (1) Mur
- Page 157 and 158: NEPTUNE SOILS (NP) Location and Ext
- Page 159 and 160: (N) General Land Use Comments : (1)
- Page 161 and 162: NIVEN SOILS (NN) Location and Exten
- Page 163 and 164: PALISADE SOILS (PA) Location and Ex
- Page 165 and 166: equired to ensure soil instability
- Page 167 and 168: PELLY SOILS (Pl ) Location and Exte
- Page 169 and 170: POIGNANT SOILS (PT) Location and Ex
- Page 171 and 172: PREST SOILS (PR) Location and Exten
- Page 173 and 174: ROACH SOILS (RH) Location and Exten
- Page 175 and 176: ROSS SOILS (RS) Location and Extent
- Page 177 and 178: (RD ) Plate 37 Ryder soil profile (
- Page 179 and 180: BARDIS SOILS (SD) Location and Exte
- Page 181 and 182: SCAT SOILS Location and Extent : Sc
- Page 183 and 184: SEABIRD SOILS (SB) Location and Ext
- Page 185 and 186: SECRECY SOILS (SL) Location and Ext
- Page 187 and 188: SHALISH SOILS Location and Extent :
- Page 189 and 190: SIM SOILS (SI) Location and Extent
- Page 191 and 192: STAVE SOILS Location and Extent : S
- Page 193 and 194: STEELHEAD SOILS Location and Extent
- Page 195: STRACHAN SOILS (SN) Location and Ex
- Page 199 and 200: SUMMER SOILS (SR) Location and Exte
- Page 201 and 202: SURREY SOILS (SU ) Location and Ext
- Page 203 and 204: TSAWWASSEN SOILS (TS) Location and
- Page 205 and 206: VEDDER SOILS (VD) Location and Exte
- Page 207 and 208: Plate 39 Vinod soil profile (Rego G
- Page 209 and 210: (VY) Plate 4 1 Vye soil profile (Gl
- Page 211 and 212: General Land Use Comments : (1) Wes
- Page 213 and 214: WHATCOM SOIL S Plate 42 A typical u
- Page 215 and 216: W) Commonly Associated Soils : Scat
- Page 217 and 218: WIDGEON SOILS (WG ) Location and Ex
- Page 219 and 220: MISCELLANEOUS LAND TYPE S Miscellan
- Page 221 and 222: SELECTED BIBLIOGRAPHY Armstrong, J.
- Page 223 and 224: Luttmerding, H .A. and P.N . Sprout
- Page 225 and 226: oulders : Rock fragments over 60 cm
- Page 227 and 228: eluviation : The transportation of
- Page 229 and 230: lithic layer : Bedrock under the co
- Page 231 and 232: unoff : The portion of the total pr
- Page 233 and 234: Appendices
- Page 235 and 236: APPENDIX C Average Minimum and Maxi
- Page 237 and 238: Soil Name (Map Symbol) Simple Map U
- Page 239 and 240: APPENDIX F SOIL DRAINAGE CLASSES *
- Page 241 and 242: APPENDIX I SOIL REACTION CLASSES *
SU MAS SOILS<br />
so_<br />
Location <strong>and</strong> Extent :<br />
Sumas soils occur only in <strong>the</strong> eastern part <strong>of</strong> <strong>the</strong> map area . west <strong>of</strong> <strong>the</strong> Vedder Can a<br />
<strong>and</strong> occupy mainly <strong>the</strong> basin <strong>of</strong> former Sumas Lake (<strong>the</strong> lake was drained in <strong>the</strong> 1920`s) . About 2400 ha e' r<br />
map units <strong>and</strong> 270 ha <strong>of</strong> Sumas-Dixon :shallow variant soil complex are mapped .<br />
topography <strong>and</strong> Elevation : The topography <strong>of</strong> Sumas soils is nearly level with some variation to gent'' ,<br />
undulating Slope gradients are less than 2 percent <strong>and</strong> elevations are below 5 m above sea level .<br />
r<br />
Parent Material <strong>and</strong> Texture :<br />
The parent material <strong>of</strong> Sumas soils is coarse-textured lacustrine deposit s<br />
rface textures are usually loamy s<strong>and</strong> with some variation to s<strong>and</strong>y loam . Subss, aCe <strong>and</strong> subsoil ire s<br />
dium or coarse s<strong>and</strong> . occasionally containing b<strong>and</strong>s <strong>of</strong> loamy s<strong>and</strong><br />
Soil Moisture Characteristics :<br />
Sumas soils are poorly to very poorly drained . They are rapidly perv c _<br />
have low water holding capacity <strong>and</strong> slow surface run<strong>of</strong>f . Most <strong>of</strong> <strong>the</strong> Sumas soil areas have controlled war s<br />
s achieved through a system <strong>of</strong> ditches . floodgates <strong>and</strong> pumping . Sub-irrigation <strong>of</strong> most <strong>of</strong> <strong>the</strong> are a<br />
mplished by manipulation <strong>of</strong> water levels in drainage ditches During <strong>the</strong> winter especially, temporar y<br />
ing may occur during heavy rains which rapidly raise <strong>the</strong> already high groundwater table .<br />
i<br />
F<br />
General Soil Description : Sumas soils have a s<strong>and</strong>y, cultivated surface about 15 to 20 cm thick, which is ,<br />
dark grayish brown, friable <strong>and</strong> contains sometimes, faint reddish or brownish mottles . The surface is unde r<br />
by about 30 cm <strong>of</strong> very friable to loose . grayish-brown to olive-gray, medium s<strong>and</strong> containing few to comma '<br />
usually faint mottles along old root channels . This zone, in turn, grades to loose, olive-gray, medium or coars e<br />
s<strong>and</strong> . usually water saturated <strong>and</strong> containing occasional, variably coloured mottles . Soil reaction gere n a . 1 i<br />
grades from strongly or eery strongly acid irl <strong>the</strong> surface to slightly acid or neutral in <strong>the</strong> subsoil (1 1 H-n) S<br />
classification is Rego Gleysol .<br />
i<br />
Commonly Associated <strong>Soils</strong> : Dixon soils are <strong>of</strong>ten found near <strong>the</strong> margin <strong>of</strong> Sumas soils They are poorl y<br />
drained as are Sumas soils but have s i lty to o ayes __ : rface <strong>and</strong> subsurface textures which<br />
s<strong>and</strong>y textures <strong>of</strong> Sumas soil s<br />
east with +h F<br />
1 I Vegetation : Essentially all areas <strong>of</strong> Sumas soils are cleared <strong>and</strong> cultivated . A few, isolated uncleared area s<br />
support grasses, sedges, reeds, willow <strong>and</strong> black cottonwood Hooting is generally restricted to <strong>the</strong> upper 5 0<br />
cm by <strong>the</strong> high groundwater level s<br />
to 38 L<strong>and</strong>scape across <strong>the</strong> nearly<br />
level, poorly drained s<strong>and</strong>y Sumas soils .<br />
These soils are used for a variety <strong>of</strong> annua l<br />
cash crops . Note <strong>the</strong> level <strong>of</strong> <strong>the</strong> water in <strong>the</strong><br />
ditch. Subirrigatlon during <strong>the</strong> growing sea -<br />
son is provided by controlling <strong>the</strong> water levels<br />
in <strong>the</strong> ditches .<br />
181