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Sulphur Fertilizer Application in Crop Production

Introduction:

Sulphur (S) is an essential plant nutrient for all crop production. This situation is especially true for canola, which has a higher requirement for S than other annual crops such as wheat (Table 1).

Sulphur is essential for protein synthesis and the formation of chlorophyll. Sulphur is required in the development of fertile canola flowers and must be present for good nodule development on alfalfa roots.

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Sulphur deficiency in alfalfa
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Sulphur deficiency in alfalfa: deficient plant on left
is short in stature with yellowing most severe on young leaves.
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Table 1. Nutrients removed by average yields of canola, wheat and alfalfa in Alberta
Crop
Yield
Crop Part
Nutrients Removed (lbs/acre)
N
P
K
S
Canola
35 bu/ac
Seed/straw
105
22
69
21
Wheat
50 bu/ac
Straw/straw
106
17
67
13
Alfalfa
5tons/ac
Total
290
32
250
20
Adapted from Alberta Agriculture, Food and Rural Development, Soil and Crop Diagnostic Centre Laboratory Yield Increase tables (N = nitrogen, P = phosphorus, K = potassium, S = sulphur)
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Fall applied Tiger 90 (left) vs spring banded 20-0-0-24 (right).
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In Alberta, 7 million acres are considered S deficient for optimum canola production, and the acreage is increasing. Plants use S in the sulphate (SO4-S) form, which like nitrate (NO3-N), is very mobile in the soil and leachable. Soil organic matter is the primary source of plant available SO4-S. Soils that are sandy, low in organic matter and found in upper to mid-slope positions are especially prone to S deficiency since the small amount of SO4-S released from organic matter is susceptible to leaching loss.

GERO LUX LUCIS MMVIII

In Alberta, 7 million acres are considered S deficient for optimum canola production, and the acreage is increasing. Plants use S in the sulphate (SO4-S) form, which like nitrate (NO3-N), is very mobile in the soil and leachable. Soil organic matter is the primary source of plant available SO4-S. Soils that are sandy, low in organic matter and found in upper to mid-slope positions are especially prone to S deficiency since the small amount of SO4-S released from organic matter is susceptible to leaching loss.

Soils most prone to S deficiency are the Grey Wooded, Thin Black and Black soils (Figure 1) because they were formed in areas of relatively high rainfall (>leaching) and have greater yield potential (high S demand). Brown and Dark Brown soils are usually not considered S deficient because they often have gypsum (CaSO4) laden subsoils. However, within all soil zones, various combinations of high rainfall, high yield potential, low organic matter, topography and coarse texture predispose fields to S deficiency...

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