GUELPH, ONTARIO - Agriculture and Agri-Food Canada

GUELPH, ONTARIO - Agriculture and Agri-Food Canada GUELPH, ONTARIO - Agriculture and Agri-Food Canada

sis.agr.gc.ca
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Agriculture General farming and dairying are the main endeavours practised on the Teeswater silt loam. The type is well suited for the growing of nearly all crops commonly grown in the County and good yields are obtained from fall wheat, oats, barley, alfalfa, corn, turnips, tree fruits, hay and pasture. The soil is also adapted to certain cash crops such as raspberries, strawberries, corn, peas, beans and tomatoes. Fertilit)y and organic matter maintenance are the main requisites for successful crop production. The soil has a medium cont,ent of potassium and organic matter but is low in phosphorus. Fertilizer additions will benefit most crops, particularly the cash crops where high yields are required. Additions of appropriate amounts of organic matter are ensured when the farm livestock population is kept at an adequate level. The rapid internal drainage permits early spring cultivation. Occasionally stones and cobbles occur on the surface and to some extent interfere with cultivation. This condition only happens when the stonefree silty overburden has been eroded. Sargent Loam (5,300 acres) Sargent loam is developed on well sorted gravelly materials and is a Brown Forest - Grey-Brown Podzolic soil. The type is characterized by its shallow profile and the high lime content of the parent material. The profile described below is typical of the Sargent loam situated in a cut-over forested area where hard maple and beech form the tree cover: Ao - Thin layer etc. of partially decomposed leaves, twigs, A1 - O-3 inches loam; very dark brown (10 YR 2/2) ; fine granular structure; friable consistency; gravelly; pH - 7.2. BI - 3-6 inches loam; yellow-brown (10 YR 5/4); coarse granular structure; friable consistency; gravelly; calcareous; pH - 7.4. B2 - 6-l 1 inches clay loam; dark brown (10 YR 4/3) ; fine nucif orm structure ; friable consistency ; gravelly; calcareous; pH - 7.5. C - Sand and gravel; brown (10 YR 5/3) ; single grain structure; loose consistency; many stones; calcareous; pH - 8.0. Profiles exhibiting Grey-Brown Podzolic characteristics have a loam textured A2 horizon which has a weak platy structure and is pale brown in colour. The B horizon, of these profiles, is usually of slightly heavier texture and is somewhat better defined than that of the Brown Forest, soil. Sargent loam is well drained with rapid internal drainage and medium external drainage. The topography is generally smooth gently sloping but in a few areas, particularly on t!he Bruce Peninsula, some steeper slopes occur. 64

Agriculture Sargent loam is used chiefly for general farming since it occurs in a part of the County where the cool climate prevents the growth of certain cash crops for which it is well adapted. The type is fairly well suited to the growing of oats, wheat, alfalfa, hay and pasture. The production of agricultural crops is limited by low fertility levels. However, the use of fertilizers high in nitrogen, phosphorus and potassium will help to increase crop yields. The Sargent soils are shal low and care should be taken valuable surface soil in areas where erosion might occur. (b) Grey in Colour (i) Good Drainage Burford Loam (10,500 acres) to prevent loss of The Burford series is developed on well sorted gravelly materials derived largely from limestone containing smaller proportions of siliceous and argillaceous materials. The Burford is the well drained member of the cat,ena bearing the same name, and exhibits the characteristics of the Grey-Brown Podzolic soils. The following is a description of a Burford loam developed under a cover of deciduous trees consisting chiefly of hard maple and beech: , Ao - Thin etc. layer of partially decomposed leaves, t*wigs, A1 - O-4 inches loam; very dark greyish brown (10 YR 3/2) ; fine granular structure; friable consistency; few stones; pH - 6.5. Az I- 4-17 inches loam; yellowish brown (10 YR 5/4) ; weak platy struct’ure; friable consistency; few stones; pH - G.3. Az2-17-20 inches loam; light yellowish brown (10 YR G/4); weak platy structure; very friable consistency; pH - 6.2. B2 - 20-33 inches clay loam; dark brown (10 YR 4/3) ; medium nucif orm structure ; hard consistency ; gravelly; frequent stones; pH - 6.8. C - Gravel and sand; light grey (10 YR 7/2); single grain structure; loose consistency; calcareous; pH - 7.8. The Burford loam is a gravelly well drained soil that has developed on smooth gently sloping topography. Although most of the area mapped has been cleared, it would appear that the Burford loam developed under a tree cover of hard maple and beech. The surface soil when cultivated is a greyish brown loam, low in organic matter. The type is comparatively low in phosphorus and potassium. Agriculture Burford loam is well suited to hay and pasture crops and fairly well adapted to fall wheat, oats, barley, alfalfa and sweet clover. Potatoes and other vege- 65

<strong><strong>Agri</strong>culture</strong><br />

Sargent loam is used chiefly for general farming since it occurs in a part of<br />

the County where the cool climate prevents the growth of certain cash crops<br />

for which it is well adapted. The type is fairly well suited to the growing of<br />

oats, wheat, alfalfa, hay <strong>and</strong> pasture. The production of agricultural crops is<br />

limited by low fertility levels. However, the use of fertilizers high in nitrogen,<br />

phosphorus <strong>and</strong> potassium will help to increase crop yields.<br />

The Sargent soils are shal low <strong>and</strong> care should be taken<br />

valuable surface soil in areas where erosion might occur.<br />

(b) Grey in Colour<br />

(i) Good<br />

Drainage<br />

Burford Loam (10,500 acres)<br />

to prevent<br />

loss of<br />

The Burford series is developed on well sorted gravelly materials derived<br />

largely from limestone containing smaller proportions of siliceous <strong>and</strong> argillaceous<br />

materials. The Burford is the well drained member of the cat,ena<br />

bearing the same name, <strong>and</strong> exhibits the characteristics of the Grey-Brown<br />

Podzolic soils. The following is a description of a Burford loam developed<br />

under a cover of deciduous trees consisting chiefly of hard maple <strong>and</strong> beech:<br />

,<br />

Ao -<br />

Thin<br />

etc.<br />

layer of partially<br />

decomposed leaves, t*wigs,<br />

A1 - O-4 inches loam; very dark greyish brown (10 YR<br />

3/2) ; fine granular structure; friable consistency;<br />

few stones; pH - 6.5.<br />

Az I- 4-17 inches loam; yellowish brown (10 YR 5/4) ;<br />

weak platy struct’ure; friable consistency; few<br />

stones; pH - G.3.<br />

Az2-17-20 inches loam; light yellowish brown (10 YR<br />

G/4); weak platy structure; very friable consistency;<br />

pH - 6.2.<br />

B2 - 20-33 inches clay loam; dark brown (10 YR 4/3) ;<br />

medium nucif orm structure ; hard consistency ;<br />

gravelly; frequent stones; pH - 6.8.<br />

C - Gravel <strong>and</strong> s<strong>and</strong>; light grey (10 YR 7/2); single<br />

grain structure; loose consistency; calcareous;<br />

pH - 7.8.<br />

The Burford loam is a gravelly well drained soil that has developed on<br />

smooth gently sloping topography. Although most of the area mapped has<br />

been cleared, it would appear that the Burford loam developed under a tree<br />

cover of hard maple <strong>and</strong> beech. The surface soil when cultivated is a greyish<br />

brown loam, low in organic matter. The type is comparatively low in phosphorus<br />

<strong>and</strong> potassium.<br />

<strong><strong>Agri</strong>culture</strong><br />

Burford loam is well suited to hay <strong>and</strong> pasture crops <strong>and</strong> fairly well adapted<br />

to fall wheat, oats, barley, alfalfa <strong>and</strong> sweet clover. Potatoes <strong>and</strong> other vege-<br />

65

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