Garden Soil pH Amendment Calculator

Calculate lime or sulfur needed to adjust soil pH to target

Enter your current soil pH, target pH, soil texture (sandy, loam, or clay), and area in square feet to compute pounds of agricultural lime to raise pH or elemental sulfur to lower it. For home gardeners and growers. It runs free in your browser on Gera Tools, with nothing uploaded.

Last updated Source: Gera Tools

How much lime raises soil pH by one point?

Roughly 5 pounds of agricultural lime per 100 square feet raises pH by about one point in loam. Sandy soil needs less (about 3.5 lb) and clay needs more (about 7 lb) because clay buffers pH more strongly. This tool scales to your area and pH gap.

Most plants take up nutrients best within a specific pH band, so correcting soil pH is a common garden task. This calculator tells you whether to add lime or sulfur, and how much, based on your pH gap, soil texture, and bed area.

How it works

The direction depends on whether you are raising or lowering pH, and the rate depends on soil texture (its buffering capacity). Standard per-100-square-foot, per-pH-point rates are:

RAISE pH with agricultural lime (lb / 100 sqft / pH point):
  sandy 3.5   loam 5.0   clay 7.0

LOWER pH with elemental sulfur (lb / 100 sqft / pH point):
  sandy 1.0   loam 1.5   clay 2.0

amount = rate × |target − current| × (area / 100)

If the target is above current pH the tool recommends lime; if below, sulfur; if equal, no amendment is needed.

What target pH to aim for

Different plants thrive in different pH ranges. Here are practical targets for common garden plants:

Plant typeTarget pH range
Most vegetables and annual flowers6.0–7.0
Lawn grasses (cool-season)6.0–7.0
Roses6.0–6.5
Blueberries4.5–5.5
Rhododendrons and azaleas4.5–6.0
Potatoes4.8–5.5 (suppresses scab)
Asparagus6.5–7.5
Brassicas (cabbage, broccoli, kale)6.5–7.0

Most vegetable gardens aim for 6.5 — slightly acidic, but close to neutral — which keeps the widest range of nutrients soluble. The acidic end of the scale (below 5.5) locks out phosphorus and calcium; the alkaline end (above 7.5) locks out iron and manganese.

Why soil texture changes the rate

Clay particles and organic matter carry a net negative charge that holds positively charged hydrogen ions (which create acidity) tightly. Sandy soil has few such sites and responds quickly to amendments; clay has many and buffers pH change strongly, requiring more lime or sulfur for the same pH shift.

This “buffering capacity” is why the same soil test pH reading in clay and sandy soil does not mean the same total acidity reserve. A laboratory buffer-pH (also called the SMP buffer or lime requirement test) measures this reserve directly and is the most accurate guide for heavy or high-organic soils. The rates in this calculator are standard field approximations; for high-clay beds or large-scale work, a lab lime requirement test is worth the small cost.

Worked example

You have a 200 square foot loam vegetable bed currently at pH 5.8 and you want to reach pH 6.5 for a tomato crop:

  • pH gap: 6.5 − 5.8 = 0.7 points
  • Lime rate for loam: 5.0 lb per 100 sqft per point
  • Amount: 5.0 × 0.7 × (200 / 100) = 7 lb of agricultural lime

Apply that lime, till it into the top 6 inches, water in, and wait 6–8 weeks before re-testing. Do not add another round without re-testing — lime reacts slowly and it is easy to overshoot.

Tips and notes

Incorporate amendments into the top several inches rather than leaving them on the surface; pH changes happen where the amendment contacts the soil. Change pH gradually, no more than about one point per application, to avoid overshooting and locking out micronutrients. Both lime and sulfur act slowly — lime several weeks to months, elemental sulfur even slower in cold or dry soil because it depends on bacterial activity.