SOIL222 - Lecture 6 - Sulfur & Cations
Sulfur in Plants
Essential for plant functions, required similarly to phosphorus (P).
Deficiency leads to reduced photosynthesis and chlorosis.
Critical S concentration: 0.15-0.30% in whole tops or index leaves.
Deficiency Symptoms
S deficiency appears as chlorosis throughout the plant, unlike nitrogen (N) deficiency (older leaves only).
Similar symptoms in wheat and sunflowers.
Sulfur in Soil
In well-drained soils, >90% S is organic; exceptions include saline and acid sulfate soils.
Four types of organic S: reducible by HI acid (e.g., ester sulphates) and non-reducible (C-S bonded organics).
Plants uptake S as sulfate ions (SO₄²⁻); mineralization is key for availability.
Sulfur Cycle
Analogous to the nitrogen cycle; involves biological and biochemical mineralization.
Leaching is a significant loss mechanism.
Agricultural Cycles for Sulfur
Crop removal rates (kg/ha): Corn (9-11), Wheat (10-13), Cotton (13-17), Alfalfa hay (22-27).
Replacement of S requires fertilizers or organic matter mineralization.
Sources of Sulfur
S input from rainfall decreases with distance from the coast.
Common S fertilizers and their sulfur contents:
Ammonium sulfate - 24%
Potassium sulfate - 16%
Calcium sulfate - 18%
Typical fertilization rates: Pastures (5-30 kg/ha), Wheat (10-15 kg/ha).
Cations in Soil: Ca, K, Mg
Typical optimal nutrient concentrations (%) for crops:
K: 1.5-3.0, Ca: 0.2-0.5, Mg: 0.15-0.5.
Plant deficiencies are rare due to high soil reserves.
Importance of Potassium (K)
Essential for enzyme function, photosynthesis, disease resistance, and turgor.
K deficiency manifests in older leaves, leading to necrosis.
Importance of Calcium (Ca)
Involved in many plant functions: ion absorption, growth, and protection against toxic ions.
Deficiency affects younger leaves and fruit development.
Importance of Magnesium (Mg)
Vital for chlorophyll synthesis and enzyme activation.
Deficiency symptoms include interveinal chlorosis, primarily in older leaves.
Soil Content and Distribution
Soil K, Ca, Mg concentrations: 1-3% or higher, variable due to weathering and leaching.
Forms: Readily available (inorganic), non-exchangeable (primary/secondary minerals), and exchangeable (soil solution).
Availability to Plants
Uptake as K⁺, Ca²⁺, and Mg²⁺; affected by soil concentration and cation saturation.
Soil Testing
Assessed through exchangeable concentrations or % cation saturation; comparisons can help yield response.