GenetixBayEST. 2009
Glossary · pH, EC and water

pH

pH measures how acidic or alkaline a solution is on a 0–14 scale; in growing it controls nutrient uptake, with soil best near 6.0–7.0 and hydro 5.5–6.5.

Also written ph levelpotential of hydrogenaciditypH value

EstablishedDraft: awaiting expert reviewUpdated

pH is the negative base-10 logarithm of the hydrogen ion activity in a solution. Low pH is acidic, high pH is alkaline, and 7 is neutral at 25 °C. In the root zone, pH controls nutrient solubility and uptake: iron, manganese and zinc become less available as pH rises, while calcium, magnesium and molybdenum are less available when pH falls too low.

In practice

Accepted ranges, which GenetixBay treats as settled practice:

Medium pH
Soil about 6.0–7.0
Coco, rockwool and hydro about 5.5–6.5

Drift within the range is normal and even helpful: a solution that wanders from 5.6 to 6.2 over a few days exposes roots to the best uptake window for different elements. Correct only when it leaves the range. Established.

Measure pH of your input solution after adding nutrients, because fertilisers shift it. In soil, the medium buffers pH strongly, so the input matters less than in hydro. Check runoff occasionally to see what the root zone is doing.

Units and formula

pH = −log₁₀[H⁺]. A change of 1 unit means a 10-fold change in hydrogen ion concentration.

Don't confuse with

  • Alkalinity: the water's capacity to resist pH change, not the pH itself.
  • EC: total dissolved salts; unrelated to acidity.

Myth check

"pH must be held at exactly 5.8" is a Myth. A range is the target; see pH and nutrient availability.

Related terms

Sources

  1. Marschner P (ed.). 2012. Marschner's Mineral Nutrition of Higher Plants, 3rd ed. doi.org/10.1016/C2009-0-63043-9
  2. Bugbee B. 2004. Nutrient management in recirculating hydroponic culture. Acta Horticulturae 648:99-112. ishs.org/ishs-article/648_12
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