Soils of the - Agriculture and Agri-Food Canada
Soils of the - Agriculture and Agri-Food Canada Soils of the - Agriculture and Agri-Food Canada
DEFEHR SOILS (DR) Location and Extent : Defehr soils mainly occur in the vicinities of Haney, Port Hammond, Peardonville and Abbotsford Airport although small, scattered areas are also present elsewhere on the uplands . There are abou t 360 ha of pure map units and 380 ha of soil complexes dominated by Defehr soils . The complexes are mainl y with Lehman, Heron and Sunshine soils . Topography and Elevation : The topography of Defehr soils is very gently to gently sloping and undulating . Slope gradients range between 1 and 5 percent and elevations lie between 40 and 80 m above sea level . Parent Material and Texture : Defehr soils have developed from coarse-textured (mainly sandy ) glaciofluvial and marine lag deposits, at least 2 m deep and usually underlain by glacial till or glaciomarine sediments . A shallow veneer of medium-textured, eolian or slopewash material sometimes caps or is mixed into the surface . Surface textures are sandy loam or loam while subsurface and subsoil textures vary from sand t o gravelly sand . Occasional stones are sometimes present . Soil Moisture Characteristics : Defehr soils are imperfectly drained . They are rapidly pervious and have slow surface runoff and low water holding capacity. During periods of heavy rain, fluctuating, perche d watertables develop above the less permeable geologic materials present at depth . General Soil Description : Defehr soils have a friable, dark brown or dark yellowish brown, loamy, cultivate d surface that is about 15 cm thick . The surface is underlain by about 40 cm of friable, weakly structured or loose , yellowish-brown or pale brown sand or loamy sand containing few to common, strong brown or reddish-brow n mottles . This grades, below about 80 cm, to variably coloured, loose, gravelly sand or sand containing many reddish or brownish mottles. Surface soil reaction is strongly acid, changing to medium acid in the subsurfac e and subsoil. Soil classification is Gleyed Humo-Ferric Podzol. Commonly Associated Soils : Lehman, Sunshine, Heron, Columbia and Abbotsford soils often occur i n close association with Defehr soils, either in soil complexes or in adjacent map polygons . Sunshine soils are generally similar to Defehr soils, except that they are well-drained and contain no mottles in the subsurface an d subsoil . Heron soils, although also sandy, are poorly drained . Lehman, Columbia and Abbotsford soils are gravelly rather than sandy in the subsoil . Additionally, Lehman soils are poorly drained while Columbia an d Abbotsford soils are well to rapidly drained . Abbotsford soils also have a silty surface capping from 20 to 50 c m thick . Vegetation : Substantial areas of Defehr soils are cleared for agricultural or urban uses . Uncleared area s support a variable forest of coast Douglas-fir, western hemlock, western red cedar, red alder, black cottonwoo d and willow. Rooting is generally unrestricted to at least 60 cm depth, then becomes variably restricted by the fluctuating watertables . General Land Use Comments : (1) Most cultivated areas of Defehr soils are used for forage and pastur e although most other crops are possible also . Low water holding capacity leads to droughty conditions in th e summer and irrigation is required for good crop production . The fluctuating watertables which may damag e some perennial crops during the winter can be controlled by artificial drainage . (2) Defehr soils are moderatel y suited for urban and related uses . The fluctuating watertables may cause problems with basements and othe r excavations . The operation of septic tank disposal fields is also impaired during the periods of high watertables . (3) Data from a few plots indicate that Defehr soils produce good forest growth . Douglas-fir produces about 1 2 to 15 m 3 of wood/ha/yr. The low soil water holding capacity appears to be effectively offset by the fluctuatin g watertables . 64
DELTA SOILS (DT) Location and Extent : Delta soils are common in central and western Delta Municipality and centra l Richmond Municipality. There are a total of 1130 ha of pure map units and 1720 ha of soil complexes dominate d by Delta soils . The complexes are mainly with Spetifore, Blundell and Ladner soils . Topography and Elevation : Delta soils are very gently undulating with slope gradients less than 3 percent . Some areas have been partially levelled . Elevations lie between 1 and 3 m above sea level . Parent Material and Texture : The parent material of Delta soils is medium to moderately fine texture d Fraser River deltaic deposits, usually 100 cm or more deep and overlying medium or fine sand . Surface texture s are mostly silt loam, varying sometimes to silty clay loam . The subsurface is usually silty clay loam while th e upper subsoil is again silt loam . The lower subsoil textures change to sand, loamy sand or interbedded san d and silt . Below 75 cm depth, the soils are generally saline and contain substantial amounts of compounds hig h in sulphur. Soil Moisture Characteristics : Delta soils are poorly drained . They are moderately pervious and have slo w surface runoff and high water holding capacity . The watertable is near the soil surface during most of the winte r but recedes somewhat during the summer. Temporary surface ponding during heavy rainfall is common in th e slight depressions . General Soil Description : Delta soils have a very dark gray or black, friable to firm, cultivated surface that i s about 20 cm thick and usually contains between 10 and 20 percent organic matter . The surface is underlain b y a grayish-brown, firm to very firm, silty to clayey zone, about 30 cm thick, which breaks to prismatic or block y clods and contains some reddish-brown mottles . Underlying this is about 30 cm of dark gray or grayish-brown , massive, silty material containing common, reddish-brown mottles as well as light yellowish brown to yello w mottles in the lower part . The lower part is also often saline and high in sulphur compounds . This silty zon e gradually grades to massive olive-gray, saline, sandy or silty material below about 100 cm . Soil reaction i s extremely to very strongly acid throughout . Soil classification is Orthic Humic Gleysol:saline phase . Commonly Associated Soils : Ladner, Spetifore, Blundell, Westham, Guichon and Crescent soils usuall y occur in close association with Delta soils . Ladner soils differ from Delta soils by having well developed cla y accumulation layers in the subsurface as well as being finer textured . Spetifore soils are similar to Delta soil s except that they are saline at or near the surface . Blundell soils vary by having an organic surface . Guichon soil s are sandy below 50 cm as well as being saline at or near the surface . Westham and Crescent soils contain lowe r amounts of organic matter in the surface ; Crescent soils are also somewhat better drained than Delta soils . Vegetation : All areas of Delta soils are cleared and cultivated . Rooting is partially restricted in the upper 50 c m by dense soil strata and is severely restricted at lower depths by high watertables . General Land Use Comments : (1) Delta soils are good agricultural soils and are utilized for a variety o f crops, including forages, cereal grain, potatoes, vegetables and some small fruits . Watertable control throug h artificial drainage, however, is required for optimum utilization . The saline subsoil conditions are usuall y sufficiently deep to not hinder most crops except possibly, near the boundaries with the more strongly salin e Spetifore or Guichon soils . (2) Delta soils are poorly suited for urban and related uses . Soil bearing capacitie s are variable (usually low), high watertables preclude basements and similar excavations while undergroun d utility installations are highly susceptible to corrosion if not adequately protected . High watertables an d relatively slow permeability limit efficient operation of septic tank effluent disposal fields. (3) Delta soils are moderately to poorly suited for most forest crops . Sitka spruce is estimated to produce from 5 to 6 m3 of wood/ ha/yr. 65
- Page 29 and 30: CHAPTER TWO SOIL CLASSIFICATION AND
- Page 31 and 32: CHAPTER THREE DESCRIPTION OF THE SO
- Page 33 and 34: UPLANDS STREA M Figure 6. A schemat
- Page 35 and 36: Description of the Soils
- Page 37 and 38: n Plate 5 Abbotsford soil profile (
- Page 39 and 40: - _ I Plate 6 Landscape typical of
- Page 41 and 42: General Soil Description : Albion s
- Page 43 and 44: ANNACIS SOILS (AS) Location and Ext
- Page 45 and 46: ARNOLD SOILS . (AR) Location and Ex
- Page 47 and 48: BATES SOILS (BT) Location and Exten
- Page 49 and 50: BEHARREL SOILS . (BL) Location and
- Page 51 and 52: BERRY SOILS (BR) Location and Exten
- Page 53 and 54: BLANEY SOILS . (BE) Location and Ex
- Page 55 and 56: BONSON SOILS (BN) Location and Exte
- Page 57 and 58: ' - -_) - r or - ' _ ti _ L , -~ s,
- Page 59 and 60: BUCKERFIELD SOILS (BK) Location and
- Page 61 and 62: Plate 13 Buntzen soil profiie -. -H
- Page 63 and 64: CALKINS SOILS (CN) Location and Ext
- Page 65 and 66: CAPILANO SOILS . (CP) Location and
- Page 67 and 68: CASCADE SOILS . (CC) Location and E
- Page 69 and 70: CHEHALIS SOILS (CS) Location and Ex
- Page 71 and 72: Plate 14 Cloverdale soil pro/0e fHu
- Page 73 and 74: COLUMBIA SOILS Location and Extent
- Page 75 and 76: COQUITLAM SOILS . (CO) Location and
- Page 77 and 78: subsurface layers to extremely acid
- Page 79: DEAS SOILS (DS) Location and Extent
- Page 83 and 84: Plate 20 Dennett soil profile (Typi
- Page 85 and 86: DEWDNEY SOILS (DW) Location and Ext
- Page 87 and 88: DURIEU SOILS (DU) Location and Exte
- Page 89 and 90: ELK SOILS (EK) Location and Extent
- Page 91 and 92: EMBREE SOILS : (EM) Location and Ex
- Page 93 and 94: ERROCK SOILS (ER) Location and Exte
- Page 95 and 96: FADDEN SOILS (FD) Location and Exte
- Page 97 and 98: FELLOWS SOILS . (FS) Location and E
- Page 99 and 100: GLEN VALLEY SOIL S Location and Ext
- Page 101 and 102: GOLDEN EARS SOILS . (GE) t . Locati
- Page 103 and 104: GOODY SOILS (GY) Location and Exten
- Page 105 and 106: GRIGG SOILS (GG ) Location and Exte
- Page 107 and 108: GUICHON SOILS (GU) Location and Ext
- Page 109 and 110: HAMMOND SOILS . (HA) Location and E
- Page 111 and 112: HARRISON SOILS . (HR) Location and
- Page 113 and 114: HAZELWOOD SOILS (HD) Location and E
- Page 115 and 116: HERON SOILS (HN ) Location and Exte
- Page 117 and 118: HOLLYBURN SOILS (HB) Location and E
- Page 119 and 120: HOPEDALE SOILS (HP) Location and Ex
- Page 121 and 122: JUDSON SOILS (JN) Location and Exte
- Page 123 and 124: KENNEDY SOILS , -n Plate 26 A t ypi
- Page 125 and 126: KENWORTHY SOILS (KW) Location and E
- Page 127 and 128: KITTER SOILS (K) Location and Exten
- Page 129 and 130: (L) Commonly Associated Soils : Del
DELTA SOILS (DT)<br />
Location <strong>and</strong> Extent : Delta soils are common in central <strong>and</strong> western Delta Municipality <strong>and</strong> centra l<br />
Richmond Municipality. There are a total <strong>of</strong> 1130 ha <strong>of</strong> pure map units <strong>and</strong> 1720 ha <strong>of</strong> soil complexes dominate d<br />
by Delta soils . The complexes are mainly with Spetifore, Blundell <strong>and</strong> Ladner soils .<br />
Topography <strong>and</strong> Elevation : Delta soils are very gently undulating with slope gradients less than 3 percent .<br />
Some areas have been partially levelled . Elevations lie between 1 <strong>and</strong> 3 m above sea level .<br />
Parent Material <strong>and</strong> Texture : The parent material <strong>of</strong> Delta soils is medium to moderately fine texture d<br />
Fraser River deltaic deposits, usually 100 cm or more deep <strong>and</strong> overlying medium or fine s<strong>and</strong> . Surface texture s<br />
are mostly silt loam, varying sometimes to silty clay loam . The subsurface is usually silty clay loam while th e<br />
upper subsoil is again silt loam . The lower subsoil textures change to s<strong>and</strong>, loamy s<strong>and</strong> or interbedded san d<br />
<strong>and</strong> silt . Below 75 cm depth, <strong>the</strong> soils are generally saline <strong>and</strong> contain substantial amounts <strong>of</strong> compounds hig h<br />
in sulphur.<br />
Soil Moisture Characteristics : Delta soils are poorly drained . They are moderately pervious <strong>and</strong> have slo w<br />
surface run<strong>of</strong>f <strong>and</strong> high water holding capacity . The watertable is near <strong>the</strong> soil surface during most <strong>of</strong> <strong>the</strong> winte r<br />
but recedes somewhat during <strong>the</strong> summer. Temporary surface ponding during heavy rainfall is common in th e<br />
slight depressions .<br />
General Soil Description : Delta soils have a very dark gray or black, friable to firm, cultivated surface that i s<br />
about 20 cm thick <strong>and</strong> usually contains between 10 <strong>and</strong> 20 percent organic matter . The surface is underlain b y<br />
a grayish-brown, firm to very firm, silty to clayey zone, about 30 cm thick, which breaks to prismatic or block y<br />
clods <strong>and</strong> contains some reddish-brown mottles . Underlying this is about 30 cm <strong>of</strong> dark gray or grayish-brown ,<br />
massive, silty material containing common, reddish-brown mottles as well as light yellowish brown to yello w<br />
mottles in <strong>the</strong> lower part . The lower part is also <strong>of</strong>ten saline <strong>and</strong> high in sulphur compounds . This silty zon e<br />
gradually grades to massive olive-gray, saline, s<strong>and</strong>y or silty material below about 100 cm . Soil reaction i s<br />
extremely to very strongly acid throughout . Soil classification is Orthic Humic Gleysol:saline phase .<br />
Commonly Associated <strong>Soils</strong> : Ladner, Spetifore, Blundell, Westham, Guichon <strong>and</strong> Crescent soils usuall y<br />
occur in close association with Delta soils . Ladner soils differ from Delta soils by having well developed cla y<br />
accumulation layers in <strong>the</strong> subsurface as well as being finer textured . Spetifore soils are similar to Delta soil s<br />
except that <strong>the</strong>y are saline at or near <strong>the</strong> surface . Blundell soils vary by having an organic surface . Guichon soil s<br />
are s<strong>and</strong>y below 50 cm as well as being saline at or near <strong>the</strong> surface . Westham <strong>and</strong> Crescent soils contain lowe r<br />
amounts <strong>of</strong> organic matter in <strong>the</strong> surface ; Crescent soils are also somewhat better drained than Delta soils .<br />
Vegetation : All areas <strong>of</strong> Delta soils are cleared <strong>and</strong> cultivated . Rooting is partially restricted in <strong>the</strong> upper 50 c m<br />
by dense soil strata <strong>and</strong> is severely restricted at lower depths by high watertables .<br />
General L<strong>and</strong> Use Comments : (1) Delta soils are good agricultural soils <strong>and</strong> are utilized for a variety o f<br />
crops, including forages, cereal grain, potatoes, vegetables <strong>and</strong> some small fruits . Watertable control throug h<br />
artificial drainage, however, is required for optimum utilization . The saline subsoil conditions are usuall y<br />
sufficiently deep to not hinder most crops except possibly, near <strong>the</strong> boundaries with <strong>the</strong> more strongly salin e<br />
Spetifore or Guichon soils . (2) Delta soils are poorly suited for urban <strong>and</strong> related uses . Soil bearing capacitie s<br />
are variable (usually low), high watertables preclude basements <strong>and</strong> similar excavations while undergroun d<br />
utility installations are highly susceptible to corrosion if not adequately protected . High watertables an d<br />
relatively slow permeability limit efficient operation <strong>of</strong> septic tank effluent disposal fields. (3) Delta soils are<br />
moderately to poorly suited for most forest crops . Sitka spruce is estimated to produce from 5 to 6 m3 <strong>of</strong> wood/<br />
ha/yr.<br />
65