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What does soil pH actually do to my plants?

pH does not feed a plant — it decides whether the food already in the soil can be reached. Which is why the fix for yellow leaves on chalk is not more fertiliser.

Difficulty
intermediate
Time
15 min
Read
3 min

Short answer

pH controls solubility. Below about 6.0 phosphorus locks up and aluminium becomes available enough to damage roots. Above about 7.0 iron, manganese and zinc lock up, which is why acid-lovers turn yellow between the veins on chalk. Almost every nutrient is simultaneously available between 6.0 and 7.0, and that is why that range is the general recommendation.

The single most common feeding mistake in a garden is treating a pH problem as a nutrient problem. A rhododendron with bright yellow leaves on chalky soil is not short of iron — the soil around it contains plenty. It is unable to dissolve that iron into a form its roots can take up, and adding more iron to the soil changes nothing at all.

How soil pH changes which nutrients a plant can take up

Step by step

  1. Understand what the number is.pH measures how acidic or alkaline the soil water is, on a logarithmic scale from 0 to 14 with 7 as neutral. Logarithmic matters: pH 5 is ten times more acidic than pH 6, and a hundred times more than pH 7. Small numbers describe large changes.
  2. Understand the mechanism: solubility, not quantity.Nutrients are only useful to a plant when dissolved in soil water. pH governs which compounds stay dissolved and which precipitate out as solids the roots cannot touch. The nutrient is still there; it is simply out of reach.
  3. Learn what goes wrong at the alkaline end.Above roughly pH 7.0, iron, manganese, zinc, copper and boron become progressively insoluble. Iron chlorosis — yellow leaves with sharply green veins, on the newest growth first — is the signature, and it is what kills acid-lovers on chalk.
  4. Learn what goes wrong at the acid end.Below roughly pH 5.5, phosphorus locks up with iron and aluminium, calcium and magnesium leach away, and free aluminium starts to damage root tips directly. Growth stunts, roots stay short and stubby, and nothing responds to feeding.
  5. Note that phosphorus is squeezed from both ends.It is locked by aluminium and iron in acid soil and by calcium in alkaline soil. It is only genuinely free in a narrow window around 6.5, which is a large part of why that figure keeps appearing.
  6. Note the effect on soil life.Most bacteria, including the nitrogen-fixing bacteria in pea and bean roots and the ones that convert organic nitrogen into a usable form, work best near neutral. Below pH 5.5 the whole nitrogen cycle slows down. Fungi tolerate acidity better, which is part of why woodland soils are fungal and acidic.
  7. Match your plants to the range you have.Blueberries, rhododendrons and heathers want 4.5 to 5.5. Most vegetables and border plants want 6.0 to 7.0. Brassicas prefer 6.5 to 7.5, partly because higher pH suppresses club root. Lawn grasses are happy at 5.5 to 6.5.
  8. Stop reaching for fertiliser when the pattern says pH.Yellowing between green veins on new growth, on several unrelated plants, in a garden with chalky stones, is a pH diagnosis. Feeding harder makes no difference and eventually causes salt damage.

Tips

  • Chelated iron sprays relieve iron chlorosis for a few weeks by supplying iron in a form that stays soluble at high pH. They are a symptom treatment and they need repeating; they are not a soil correction.
  • Ericaceous fertiliser works partly by being acidifying, not just by containing iron. That is why using it in a pot of ordinary compost gives poorer results than using it in ericaceous compost.
  • Rainwater is slightly acidic; hard tap water is alkaline and carries dissolved calcium. Watering an ericaceous pot with hard tap water raises its pH steadily over a season.
  • Peat-free composts are not automatically acidic. Check the pH stated on the bag if you are growing anything fussy.

Questions people ask

Can I just change my soil's pH to whatever I want?

Raising pH with lime works and is routine. Lowering it in open ground is close to futile where the subsoil is chalk or limestone, because the rock keeps buffering it back up. Growing acid-lovers in containers of ericaceous compost is the reliable answer.

How much does pH move naturally?

Downward, slowly, almost everywhere in the UK, because rain is mildly acidic and leaches calcium out. Cultivated ground drifts a little more acid each decade unless something is added. Chalk subsoil prevents this entirely.

Does adding compost change pH?

Only slightly, and it moves soil towards neutral from either direction rather than in one direction. Its more useful effect is buffering — high-organic soil resists pH swings, so nutrients stay available across a wider range.

What to do next

Written and maintained by the GuideHQ editorial team. More in Garden.