Available Water Capacity Calculator
Calculate available water capacity from field capacity, wilting point, root depth, and bulk density. Plan irrigation amounts and frequency.
Calculate gypsum tons per acre to reduce sodium percentage in soil based on soil Na%, target Na%, CEC, and treatment depth.
| Depth (in) | Product (tons/ac) | Product (lbs/ac) | Cost/Acre |
|---|---|---|---|
| 6 | 0.32 | 645 | $15.00 |
| 8 | 0.43 | 860 | $19.00 |
| 12 * | 0.65 | 1,290 | $29.00 |
| 18 | 0.97 | 1,935 | $44.00 |
| 24 | 1.29 | 2,580 | $58.00 |
| ESP Range | Classification | Management |
|---|---|---|
| < 5% | Non-sodic | Normal management |
| 5 - 15% | Slightly sodic | Monitor and light amendment |
| 15 - 25% | Moderately sodic | Gypsum amendment required |
| > 25% | Severely sodic | Heavy amendment + drainage |
The Gypsum Rate Calculator determines how many tons of gypsum (calcium sulfate) to apply per acre to reduce the exchangeable sodium percentage (ESP) in sodic soils. Sodic soils โ those with ESP above 15% โ suffer from poor structure, reduced infiltration, and crusting that severely limits crop growth.
Gypsum works by supplying calcium ions that replace sodium on the soil exchange complex. The displaced sodium is then leached below the root zone with irrigation or rainfall. The amount of gypsum needed depends on the current ESP, target ESP, soil CEC, and the depth of soil to be treated.
This page converts ESP, CEC, and treatment depth into a starting gypsum tonnage that can then be checked against field response and follow-up tests.
Sodic-soil reclamation usually fails when the rate is guessed or when leaching needs are ignored. This page gives a defensible starting rate.
Gypsum tons/ac = (Current ESP% โ Target ESP%) / 100 ร CEC ร Depth factor ร 0.0086
Where:
ESP = Exchangeable Sodium Percentage
CEC = Cation Exchange Capacity (meq/100g)
Depth factor = inches of soil ร soil weight per inch (โ 300,000 lbs per acre-inch)
0.0086 = Conversion factor (tons gypsum per meq Na)Result: 7.7 tons gypsum/ac
Na to replace = (20% โ 5%) / 100 ร 20 meq/100g = 3.0 meq Na/100g. For 12 inches: 3.0 ร 12 ร 300,000 / 100 / 2000 ร 0.086 = approximately 7.7 tons gypsum per acre.
Sodic soils are identified by ESP greater than 15%, poor water infiltration, surface crusting when dry, and a slick or greasy feel when wet. Lab analysis of a saturated paste extract provides ESP, EC, and SAR (Sodium Adsorption Ratio) values. Soils with SAR above 13 are generally classified as sodic.
Mined gypsum is quarried from natural deposits and typically has 85โ98% purity. FGD gypsum is a byproduct of coal-fired power plant scrubbers and is equally effective with purity often above 90%. Both sources are approved for agricultural use. Phosphogypsum from fertilizer manufacturing is restricted in some areas due to radioactivity concerns.
Gypsum application alone doesnโt solve the problem โ water is needed to move displaced sodium out of the root zone. The leaching requirement depends on the amount of sodium to remove and the soilโs infiltration rate. Plan to apply 6โ12 inches of water per treatment cycle. In arid regions, coordinate gypsum application with irrigation scheduling.
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Exchangeable Sodium Percentage is the fraction of the CEC occupied by sodium. ESP above 15% causes soil dispersion, poor water infiltration, and surface crusting. Reducing ESP restores soil structure.
Gypsum dissolves to release calcium ions, which replace sodium on soil exchange sites. The freed sodium moves into the soil solution and is leached downward by water. Calcium is preferred by clays, so the exchange is thermodynamically favorable.
Lime (CaCOโ) supplies calcium but raises pH. For sodic soils that are already alkaline (pH >8.5), lime is less effective because it has low solubility at high pH. Gypsum is more soluble and does not change pH.
Time depends on water availability for leaching. With adequate irrigation, measurable improvement occurs in one season. Full reclamation of deeply sodic soils may take 2โ4 years with repeated applications and leaching.
Yes. Gypsum is a neutral salt (pH 6.5โ7.0) and supplies calcium and sulfur, both essential nutrients. It will not harm crops at recommended rates.
Sulfuric acid is effective for calcareous sodic soils because it dissolves native calcium carbonate, releasing calcium to replace sodium. It is faster-acting but requires specialized application equipment and is hazardous to handle.
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