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Lower Welland River Characterization Report - Niagara Peninsula ...

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<strong>Lower</strong> <strong>Welland</strong> <strong>River</strong> Study Area<br />

<strong>Characterization</strong> <strong>Report</strong><br />

Table 1: Soils of the <strong>Lower</strong> <strong>Welland</strong> <strong>River</strong> Study Area<br />

Soil<br />

Series<br />

Mineral Soils<br />

Toledo<br />

Soils<br />

(TLD)<br />

Beverly<br />

Soils<br />

(BVY)<br />

<strong>Welland</strong><br />

Soils<br />

(WLL)<br />

<strong>Niagara</strong><br />

Soils<br />

(NGR)<br />

Ontario<br />

Soils (OTI)<br />

Alluvial<br />

Soils<br />

(ALU)<br />

Chinguaco<br />

usy Soils<br />

(CGU)<br />

Peel Soils<br />

(PEL)<br />

Lincoln<br />

Soils (LIC)<br />

Geologic<br />

Deposits<br />

Mainly lacustrine<br />

silty clay<br />

Mainly lacustrine<br />

silty clay<br />

Mainly reddishhued<br />

deep water<br />

lacustrine heavy<br />

clay<br />

Mainly reddishhued<br />

deep water<br />

lacustrine heavy<br />

clay<br />

Mainly reddishhued<br />

deep water<br />

lacustrine heavy<br />

clay<br />

Variable alluvial<br />

deposits on<br />

floodplain<br />

Natural<br />

Drainage<br />

Poor<br />

Imperfect<br />

Poor<br />

Imperfect<br />

Moderately<br />

welldrained<br />

Various<br />

but most<br />

are<br />

imperfect or<br />

poor<br />

Water<br />

Holding<br />

Capacity<br />

Relatively<br />

High<br />

Medium to<br />

High<br />

Relatively<br />

High<br />

Moderate<br />

to High<br />

Moderate<br />

to High<br />

Vary,<br />

depending<br />

on soil<br />

textures<br />

and<br />

horizons<br />

thickness<br />

Clay loam till Imperfect Relatively<br />

High<br />

40-100cm<br />

lacustrine silty<br />

clay over clay<br />

loam till<br />

Mainly lacustrine<br />

heavy clay<br />

Imperfect<br />

Medium to<br />

High<br />

Permeability<br />

Slow<br />

Moderate to<br />

Slow<br />

Slow<br />

Moderate to<br />

Slow<br />

Moderate to<br />

Slow<br />

Vary,<br />

depending on<br />

soil textures<br />

and horizons<br />

thickness<br />

Moderate to<br />

Slow<br />

Moderate to<br />

Slow<br />

Surface<br />

Runoff<br />

Moderate<br />

to High<br />

Moderate<br />

to High<br />

Slow to<br />

Moderate<br />

Slow to<br />

Rapid<br />

Fairly<br />

Rapid<br />

Vary,<br />

dependin<br />

g on soil<br />

textures<br />

and<br />

horizons<br />

thickness<br />

Moderate<br />

to Rapid<br />

Moderate<br />

to High<br />

Poor High Slow Slow to<br />

Rapid<br />

Class<br />

3W<br />

2D<br />

3WD,<br />

4W, 5W<br />

3D<br />

Land use<br />

Comments<br />

Require artificial<br />

drainage to be useful for<br />

agriculture<br />

Used mainly for corn,<br />

small grains and forage<br />

crops.<br />

Range from unsuitable<br />

to poorly suitable for<br />

most fruit & vegetable<br />

crops<br />

Their suitability is poor<br />

for most horticultural<br />

crops; artificial drainage<br />

usually necessary.<br />

3 Main limitation is high<br />

clay content. Fair to<br />

good suitability for<br />

canola, soybeans and<br />

white beans.<br />

Vary<br />

2D<br />

2D<br />

3WD<br />

Flooding is the greatest<br />

limitation for agricultural<br />

uses<br />

Widely used for growing<br />

common field crops<br />

With artificial drainage<br />

they have fair to good<br />

suitability for select fruit<br />

and vegetable crops.<br />

Susceptible to soil<br />

compaction and erosion<br />

should<br />

Used for common field<br />

crops such as forages,<br />

small grains and corn.<br />

Usually considered<br />

problem soils because<br />

of poor drainage and<br />

high clay content.<br />

12

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