Backed by Peer-Reviewed Agronomic Science

Precision Soil Math.
Zero Black Boxes.

Stop guessing with generic lookup charts. Use our 8 free, university-backed soil calculators to find the exact lime, sulfur, gypsum, or fertilizer blend your crops and soil require.

Lime Requirement Engine Output
Silt Loam Soil | Target pH 6.5
Current pH5.4
SMP Buffer pH6.8
CEC Capacity14.2 meq
Lime Needed1.8 tons/ac
4.5 5.5 6.5 7.5
SMP Buffer Method USDA Handbook 60 Sodic Model Kohlrausch Ionic Conductance
Free Precision Suite

8 Precision Calculators for Every Grower

Select an agronomic tool below to get instant, scientifically accurate amendment recommendations tailored to your specific soil, crop, and water conditions.

Raises Soil pH

Lime Requirement

Calculate exact pure CaCO3 tons/acre or bags needed based on SMP buffer pH, Adams-Evans, or CEC shift, adjusted for ECCE product fineness.

  • SMP & Adams-Evans buffer models
  • ECCE fineness & depth adjustment
Calculate lime
Lowers Soil pH

Precision pH Down

Determine safe elemental sulfur (S0) or aluminum sulfate rates with bio-oxidation kinetics and built-in single-dose plant safety caps.

  • Thiobacillus Q10 temp kinetics model
  • Automatic root burn split-dosing
Lower soil pH
N-P-K-S Blending

Fertilizer Blend

Formulate multi-nutrient dry or liquid blends. Solves sequential P → K → S → N matrix, liquid specific gravity, and inert filler volume.

  • Dry bulk & liquid fertigation support
  • Spray nozzle flow calibration & filler mass
Build custom blend
Cation Chemistry

CEC Calculator

Convert lab ppm concentration to charge equivalents (meq/100g). Includes empirical organic matter and clay mineralogy estimation models.

  • Faraday atomic valence divisors
  • Clay & organic humus CEC estimates
Calculate CEC
Albrecht Balance

Base Saturation

Balance cation ratios (Ca, Mg, K, Na, H) and Ca:Mg ratios on the exchange complex using William Albrecht targets to improve soil tilth and aeration.

  • Ca:Mg soil compaction diagnostic
  • Calcitic vs Dolomitic amendment selection
Balance base saturation
Sodic Reclamation

Gypsum Requirement

Reclaim sodic soils (ESP > 15%). Computes pure CaSO4·2H2O tonnage using the USDA Handbook 60 sodium displacement model.

  • USDA 0.86 displaced sodium formula
  • Soil depth & leaching fraction guidelines
Calculate gypsum
Water Permeability

SAR & CROSS Diagnostic

Evaluate irrigation water sodicity hazards. Calculates standard SAR, Rengasamy CROSS, Suarez calcite-adjusted SARadj, and water gypsum dosing.

  • CROSS structural stability index
  • Water gypsum injection rate (lbs/ac-ft)
Diagnose water SAR
Hydroponic Dosing

PPM to EC Fertigation

Convert elemental PPM targets to raw salt weights. Predicts solution EC (mS/cm) via Kohlrausch ionic molar conductances and Tank A/B segregation.

  • Kohlrausch molar conductivity engine
  • Tank A/B precipitation segregation
Calculate fertigation
Simple Workflow

Calculate. Amend. Grow.

Three simple steps to scientifically optimized soil and peak crop performance.

1

Test Your Soil or Water

Get baseline water pH, buffer pH, CEC, or cation PPM using a home test kit or professional lab analysis.

2

Run the SoilTune Engine

Input your metrics. Our calculation engine applies SMP buffer equations, USDA reclamation stoichiometry, or Kohlrausch molar conductances.

3

Apply & Thrive

Get precise, cost-effective shopping lists in lbs, tons, or bags with built-in plant safety caps and apply with confidence.

Why SoilTune Is Different

Not Just Guesswork.
Peer-Reviewed Science.

Most online calculators use oversimplified, linear formulas that ignore soil buffering capacity, Cation Exchange Capacity, and osmotic salt limits. SoilTune utilizes peer-reviewed agronomic models to reflect physical soil chemistry accurately.

SMP Buffer & Adams-Evans Equations Quantifies exchangeable reserve acidity to prevent severe under-liming in clay or over-liming in sand.
USDA Handbook 60 Reclamation Model Applies the 0.86 displaced sodium factor per acre-furrow-slice to safely reclaim sodic soil structure.
Kohlrausch Ionic Conductivity & CROSS Predicts true fertigation EC and water structural stability indices beyond standard SAR assumptions.
Why Buffer pH & CEC Matter

“Two soils can have the same active water pH of 5.5, but a heavy clay soil will require up to 3× more lime than a sandy loam to reach pH 6.5. Our calculators account for buffer pH, texture, and CEC to prevent costly under- or over-application.”

ST
SoilTune Agronomy Team Based on USDA-NRCS & Extension Guidelines

Same pH. Different Lime Demand.

Illustrative relative lime requirement to move soil from pH 5.5 to pH 6.5.

Coarse Sand
Heavy Clay

Buffer pH and CEC measure reserve acidity held on exchange sites that must be neutralized.

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Frequently Asked Questions

Agronomic & Technical Questions

Clear answers regarding soil testing protocols, buffer models, and calculator accuracy.

How is active soil pH different from buffer pH?

Active soil pH measures hydrogen ion concentration in the soil water solution (<1% of total soil acidity). Buffer pH (e.g., SMP or Adams-Evans) measures reserve acidity electrostatically bound to clay and organic matter particles. Calculating lime without buffer pH often under-estimates lime needs in clay soils by up to 300%.

Which lab extraction methods are compatible with SoilTune calculators?

Our engines support standard Mehlich-3, Ammonium Acetate (pH 7.0), Bray-1, Morgan, and 1:1 soil-water slurry extractions. Cation Exchange Capacity (CEC) is calculated using charge summation (meq/100g) normalized across all major laboratory standards.

Why do your pH lowering calculators split sulfur doses?

Applying more than 20 lbs of elemental sulfur or 50 lbs of aluminum sulfate per 1,000 sq ft in a single dose risks severe osmotic root burn and aluminum phytotoxicity. SoilTune automatically partitions large requirements into safe, split applications spaced 60 days apart.

What is the difference between SAR and CROSS water tests?

Sodium Adsorption Ratio (SAR) measures sodium hazard relative to calcium and magnesium. CROSS (Cation Ratio of Structural Stability) provides a superior measurement by factoring in potassium dispersion and the lower flocculating power of magnesium compared to calcium.

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