eference <strong>and</strong> also Publication No . 89-2 <strong>of</strong> theOntario Institute <strong>of</strong> Pedology (19). Additionalassistance in determining subclasses W, M, <strong>and</strong> Dwas obtained by using a computer modeldeveloped by McBride <strong>and</strong> Mackintosh (20,21) .<strong>The</strong> subclasses applied <strong>and</strong> brief descriptions<strong>of</strong> the limitations they represent follow:Subclass D - Undesirable soil structure <strong>and</strong>/orpermeability .Subclass E - Erosion damage, or potential damagefrom erosion, results in lower productivity .Subclass F - Low natural fertility which may ormaynot be possible to correct by additions <strong>of</strong>fertilizers or manure.Subclass 1- Inundation by flooding <strong>of</strong> streams orlakes causing crop damage or restrictingagricultural use .Subclass M - Droughtiness affecting crop growth<strong>and</strong> mainly caused by low moisture holdingcapacity.Subclass S - Adverse soil characteristics. Usedwhen two <strong>of</strong> the limitations represented bysubclasses D, F or M are present <strong>and</strong> someadditional limitation occurs, for example T.Subclass T - Adverse topography due to steepnessor complexity <strong>of</strong> slopes which: a) increases thecost <strong>of</strong> farming over that <strong>of</strong> level l<strong>and</strong>; b)decreases the uniformity <strong>of</strong> growth <strong>and</strong> maturity<strong>of</strong> crops; <strong>and</strong> c) increases the hazard <strong>of</strong> erosiondamage by water.Subclass W - Excess water, other than fromflooding, limits use for agriculture. <strong>The</strong> excesswater may be due to poor drainage, a high watertable, seepage, or run<strong>of</strong>f from surrounding areas .Assumptions<strong>The</strong> classification system, <strong>and</strong> the ratings givenin Table 4, are based upon the followingassumptions :a) <strong>The</strong> soils will be well managed <strong>and</strong> croppedunder a largely mechanized system.b) L<strong>and</strong> requiring improvements, for examplestone removal or artificial drainage, that can becarried out by the fanner himself, is classifiedaccording to its limitations or hazards for useafter the improvements have been made . <strong>The</strong>resulting class, therefore, reflects the potentialcapability <strong>of</strong> the l<strong>and</strong> in its improved state .Since it is not always feasible to install tiledrainage, alternate classes for poorly drainedsoils are also given in Table 4.c) <strong>The</strong> following are not considered: distances tomarket, kind <strong>of</strong> roads, location or size <strong>of</strong>farms, type <strong>of</strong> ownership, cultural patterns,skills or resources <strong>of</strong> individual operators, <strong>and</strong>hazard <strong>of</strong> crop damage by storm.d) <strong>The</strong> classification includes capabilities <strong>of</strong> soilsfor common field crops such as forage crops,small grains <strong>and</strong> corn. It does not includecapabilities for special crops such as soybeansor tobacco, or for horticultural crops .e) Capability classes are subject to change as newinformation on the properties, behaviour, <strong>and</strong>responses <strong>of</strong> soils becomes available. In somecases technological advances may alsonecessitate changes.(2) Capability Classification forOrganic <strong>Soils</strong>Several agricultural capability classificationsystems have been devised for organic soils whichclassifies them into seven capability classes (22,23,24) . Those systems, however, were not used toclassify the organic soils which occur in the<strong>County</strong> for the following reasons: a) the limitedoccurrence <strong>of</strong> organic soils in the <strong>County</strong>, b) thelimited use <strong>of</strong> organic soils for agriculture; <strong>and</strong> c)the increasing importance <strong>of</strong> wetl<strong>and</strong>s ashydrologic recharge areas.(3) How to Determine CapabilityRatings for Areas on the Soil Maps<strong>The</strong> soils or l<strong>and</strong> units which occur withinareas shownon the soil maps are identified in themap symbols for those areas . Explanations <strong>of</strong> themap symbols <strong>and</strong> their components are providedon each map in the section titled "Key to the MapSymbols". Similar explanations are also given inthe Glossary at the back <strong>of</strong> this volume <strong>of</strong> thereport. Symbols shown on the maps mayrepresent one <strong>of</strong> the following: 1) a l<strong>and</strong> unit,2) a single soil type which occurs on a singleslope, 3) a single soil type which occurs on twodifferent slopes ; <strong>and</strong> 4) two different soil types .When two slopes or two soil types areidentified in the map symbol, dominant <strong>and</strong>significant soils occur for which capability ratingsmust be determined . Dominant means that 40 to80% <strong>of</strong> the area represented by the map symbolconsists <strong>of</strong> that soil type <strong>and</strong> associated slopeclass . Significant means that 20 to less than 40%<strong>of</strong> the area represented by the map symbolconsists <strong>of</strong> that soil type <strong>and</strong> associated slopeclass .
Capability ratings for the soils <strong>and</strong> l<strong>and</strong> unitsidentified in the symbols shown on the soil mapsare given in Table 4 . <strong>The</strong> following examples <strong>of</strong>typical map symbols' will demonstrate theprocedures that should be followed when usingTable 4 to determine the appropriate soilcapability rating or ratings for symbols shown onthe soil maps .Example 1. BV .LCIn this example, 80% or more <strong>of</strong> the arearepresented by the symbol consists <strong>of</strong> Beverlyloamy phase (BV.L) soils which occur on simple Cslopes <strong>of</strong> 2 to 5%.Procedure:1) Locate the symbol'BV.L" in the first column <strong>of</strong>Table 4 titled "Map Symbol" .2) Determine the appropriate slope class columnby locating the slope class "C" which appearsunder the heading tided "Capabilityclassification by slope classes".3) Now move horizontally across the line forBV.L soils to the C slope class column, wherethe capability rating is given. <strong>The</strong> soilcapability rating for BV .L soils which occur onC slopes is 2DE.Example 2BV.LC>bIn this example, 40% to 80% <strong>of</strong> the arearepresented by the symbol consists <strong>of</strong> Beverlyloamy phase (BV.L) soils which occur on simple Cslopes <strong>of</strong> 2 to 5% (dominant slope), <strong>and</strong> 20% toless than 40% <strong>of</strong> the area consists <strong>of</strong> Beverly loamyphase (BV.L) soils which occur on complex bslopes <strong>of</strong> 0.5 to 2% (significant slope) . Twocapability ratings must therefore be determined.Procedure:1) Locate the symbol'BV.L" in the first column <strong>of</strong>Table 4 titled "Map Symbol".2) Determine the appropriate slope class columnsby locating slope class "C" <strong>and</strong> slope class "b"which appear under the heading tided"Capability classification by slope classes".3) Nowmove horizontally across the BV .L line tothe C slope class column, where the capabilityrating <strong>of</strong> 2DE is shown . This is the rating forBV.L soils which occur on C slopes. On thesame line, now move to the b slope classcolumn where the capability rating <strong>of</strong> 2D isshown. This is the rating forBV .L soils whichoccur on b slopes.4) <strong>The</strong> soil capability rating for the map symbolis 2DE>2D .Example 3.BV>TO.CbIn this example, 40% -to 80% <strong>of</strong> the areaprepresented by the symbol consists <strong>of</strong> Beverly(BV) soils which occur on complex b slopes <strong>of</strong> 0.5to 2%, <strong>and</strong> 20% to less than 40% <strong>of</strong> the areaconsists <strong>of</strong>Toledo coarse phase (TO.C) soils whichalso occur on complex b slopes .Procedure:1) Locate the symbols "BV" <strong>and</strong> 'TO.C' in thefirst column <strong>of</strong> Table 4 titled "Map Symbol".2) Determine the appropriate slope class columnby locating slope class "b" which appearsunder the heading titled "Capabilityclassification by slope classes" .3) Now go to the BV line <strong>and</strong> move horizontallyacross the line to the b slope class column,where the capability rating <strong>of</strong> 2D is shown .This is the rating for BV soils which occur onb slopes .4) Now go to the TO.C line <strong>and</strong> movehorizontally across the line to theb slope classcolumn . <strong>The</strong> capability rating <strong>of</strong> 3W is shownin the b slope class column, which is theappropriate rating if tile drainage is feasible orin place. If tile drainage is not feasible for theTO.C soils, the capability rating is 5W, whichis the rating shown in brackets . In Table 4,where tile drainage is not feasible for poorly<strong>and</strong> very poorly drained soils, the non-drainedcapability rating is given in brackets .5) <strong>The</strong> soil capability rating for the map symbol,therefore, is 2D>3W if tile drainage is feasibleor in place for the TO.C soils. However, if tiledrainage is not feasible for the TO.C soils, thecapability rating would then be 2D>5W.Example 4.BV>TAb>cIn this example, 40% to 80% <strong>of</strong> the arearepresented by the symbol consists <strong>of</strong> Beverly (BV)soils which occur on complex b slopes <strong>of</strong> 0.5 to 2%(dominant slope), <strong>and</strong> 20% to less than 40% <strong>of</strong> thearea consists <strong>of</strong> Tavistock soils (TA) which occuron complex c slopes <strong>of</strong> 2 to 5% (significant slope) .57