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The Soils of Brant County - Agriculture and Agri-Food Canada

The Soils of Brant County - Agriculture and Agri-Food Canada

The Soils of Brant County - Agriculture and Agri-Food Canada

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that in <strong>Brant</strong> <strong>County</strong>, the series is a category <strong>of</strong> paramountimportance because it is used for defining <strong>and</strong> classifying soilswhich are the components <strong>of</strong> soil map units displayed onthe soil map.Soil Phases<strong>The</strong> soil phase is used to differentiate certain characteristics<strong>of</strong> soil series which are significant to plantgrowth, or use<strong>of</strong>the soil or l<strong>and</strong> . Only one kind <strong>of</strong> soil phase has been recognized in <strong>Brant</strong> <strong>County</strong> which is the coarse texture phase. It iscommonly associated with soils <strong>of</strong> the Burford, Guelph <strong>and</strong>Fox soil series. A coarse phase <strong>of</strong> the Burford soil is designatedas BUF.C .Miscellaneous L<strong>and</strong>Units<strong>The</strong>reare some l<strong>and</strong> areas too variable or complex in terms<strong>of</strong> soil or slope conditions to classify <strong>and</strong> map in the conventionalway as soil map units . <strong>The</strong>se are recognized as Miscellaneous L<strong>and</strong> Units <strong>and</strong> include recent floodplains adjacent tomajor rivers <strong>and</strong> streams, e .g . ALU <strong>and</strong> steep escarpments<strong>of</strong>ten associated with entrenched or eroded stream valleys, e .g.ESC . Marsh (MAR) <strong>and</strong> Urban L<strong>and</strong> (ULD) MiscellaneousL<strong>and</strong> Units are also recognized .Soil Map Units<strong>The</strong> natural l<strong>and</strong>scape is comprised <strong>of</strong> soils which are portrayedon soil maps by means <strong>of</strong> soil map units . Usually soilsoccur in a repetitive pattern within a l<strong>and</strong>scape <strong>and</strong> the soilmap unit describes this pattern in terms <strong>of</strong> dominant <strong>and</strong> subdominantsoil components . In some soil l<strong>and</strong>scapes where thesoils are relatively homogeneous, the soil map unit will consist<strong>of</strong>only one soil component, e.g . the BRT 1 map unit comprised<strong>of</strong> only <strong>Brant</strong> soils . <strong>The</strong> usual case is one in which soil mapunits consist <strong>of</strong>a dominant soil component, which is estimatedto occupy approximately 70% <strong>of</strong> the areal extent <strong>of</strong> the soildelineation, <strong>and</strong> a subdominant component occupying theremaining 30% <strong>of</strong> the area . For example, the BRT 4 soil mapunit consists <strong>of</strong> dominantly <strong>Brant</strong> soils <strong>and</strong> subdominant Tuscolasoils, in approximately 70 :30 proportions . Although mapunits are defined with rather precise limits, it should be recognizedthat within anyl<strong>and</strong>scape there is <strong>of</strong>ten variability in soilconditions which cannot be described <strong>and</strong> mapped at the mapscale employed . <strong>The</strong>se seemingly aberrant soils are referred toas soil inclusions, <strong>and</strong> are generally considered to occupy lessthan 20% <strong>of</strong> the area <strong>of</strong> a map delineation .

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