Soil Amendment Calculator
Pounds and bags of compost, manure, peat or biochar to amend a given area.
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Enter sand, silt and clay percentages to classify your soil into one of the twelve USDA texture classes, with drainage, plant-available water and a handling verdict.
Chlorova · updated for 2026
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Classification follows the published USDA Soil Survey Manual decision rules, but a texture class describes mineral particle size only — it does not measure organic matter, structure, pH or compaction, all of which change how the same class behaves from yard to yard. The three percentages must add to about 100; a total far off, a blank field or a non-numeric entry returns dashes rather than a forced class, so treat any dash as missing data. Borderline samples that sit within a point or two of a boundary genuinely belong to both neighboring classes, so read the guidance for each and let a ribbon or feel test confirm the lab number.
Soil texture sorting is guesswork until you put numbers on it. Measure the sand, silt and clay percentages from a jar test or a lab report, enter the three figures, and this calculator places your sample on the USDA soil texture triangle, names one of the twelve texture classes, and translates that class into the practical facts gardeners actually need: drainage speed, plant-available water, and how the soil behaves under a spade. It removes the eye-balling from loam claims and gives a defensible answer for watering, amending and bed-building decisions before you buy anything.
The USDA triangle plots percent clay on the left axis and percent sand on the base, so once two fractions are set the third is the remainder, and three numbers that should sum to one hundred fix a single point inside the diagram. That point falls in one of twelve regions, and this calculator finds the region with the standard ordered decision rules: clay-dominant classes first, then the silt classes, then the sandy corner, testing the published boundary lines such as the silt-plus-1.5-clay cutoff between sand and loamy sand.
Each passing test returns a class number, and the bands turn that number back into the name, the drainage class, the plant-available water range and a handling note, every one keyed to the same texture result. Because the evaluator only sees finite numbers, a missing or non-numeric percentage yields dashes instead of a wrong class, and a total far from one hundred flags itself so a bad jar reading never becomes a confident answer.
A quick read of what each USDA class means before you commit to a bed, a watering plan or a load of amendment.
| Texture class | Quick field meaning |
|---|---|
| Sand | drains instantly, feed lightly and often |
| Loamy Sand | loose and warm early, leaks fast |
| Sandy Loam | easy to dig, great for root crops |
| Loam | balanced, best all-around garden soil |
| Silt Loam | fertile, compacts badly when wet |
| Silt | rich but fragile, crusts and erodes |
| Sandy Clay Loam | workable moist, crusts after rain |
| Clay Loam | fertile, till only when crumbly |
| Silty Clay Loam | nutrient-rich but compaction-prone |
| Sandy Clay | heavy, add organic matter |
| Silty Clay | sticky and slow, raised beds help |
| Clay | hard when dry, sticky when wet |
Classify texture before you build beds, plan an irrigation schedule, price amendments, or decide between in-row planting and raised beds, since those choices hinge on drainage and water-holding more than on fertility. It answers particle size only, so for nutrient questions send a sample to the extension lab and use the pH, lime and fertilizer calculators beside this result rather than expecting a texture class to explain poor growth on its own.
A careful jar test typically lands within about ten percent of a lab hydrometer reading, which is close enough to place most garden soils in the right class. Borderline samples can straddle a boundary, so confirm any result that feels off with the ribbon and gritty feel test before you buy amendment in bulk.
Usually silt, because it is measured by subtraction and every sand or clay error lands on it. Recheck the sand estimate by how gritty it feels and the clay by how long the ribbon holds, then nudge silt so the three total near 100 before trusting the class.
Loam is the most forgiving because it balances drainage, water-holding and workability, which is why it supports the widest range of crops. Yet a well-managed sandy loam or a compost-rich clay often out-yields a neglected loam, so texture sets the difficulty level and management still decides the harvest.
Not meaningfully across a bed, since moving a sandy soil into the loam region would require hauling in clay at a depth that is impractical and often counterproductive. What you can change fast is structure and water-holding through organic matter, which improves behavior without changing the mineral class.
A dash means a field was blank or not a clean number, so the evaluator refuses to invent a class from incomplete data. Fill sand, silt and clay with numeric percentages that total near one hundred and the twelve-way classification returns normally.
Use it to set irrigation frequency and to choose crops that suit the drainage, then send a sample for pH and nutrients because texture never measures fertility. Pair the class with the amendment, lime and watering calculators to turn the label into a concrete bed plan.
Chlorova Gardening Team
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Checked against extension-service publications
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