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Soil pH

Quick definition

The measure of acidity or alkalinity (on a 0-14 scale) affecting nutrient availability; most plants prefer slightly acidic soil (pH 6.0-7.0).

In plain terms

pH is acidity (low pH, 0-7) or alkalinity (high pH, 7-14), with 7.0 being neutral. Most nutrients are most available at pH 6.0-7.0 (slightly acidic). Too acidic (below 6.0) or too alkaline (above 7.5) locks up nutrients. Limestone raises pH; sulfur lowers pH. Soil pH determines which plants grow well; acidic soils suit blueberries, azaleas; neutral soils suit most crops.

Why this matters

pH affects nutrient availability. A nutrient-rich soil at wrong pH won't feed plants because nutrients are locked up. Understanding and testing pH prevents frustration.

In practice

Examples

  • Acidic soil (pH 5.0): blueberries thrive; tomatoes struggle; limestone raises pH.
  • Alkaline soil (pH 7.8): tomatoes thrive; blueberries struggle; sulfur lowers pH.
  • Optimal pH (6.5): most plants thrive; nutrients available.
  • Nutrient-deficient plant in rich soil at wrong pH; nutrient lockup; pH adjustment fixes it.

Practical applications

  • Test soil pH (cheap kit or lab); know your starting point.
  • Limestone raises pH (apply fall, takes months to act).
  • Sulfur lowers pH (apply fall, takes months to act).
  • Choose plants suited to your pH rather than constantly adjusting.
  • Retest every 2-3 years; pH changes slowly but does shift over time.

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