doodlefine

Fact sheet · updated

GRAIN SIZE, IN PLAIN ENGLISH

How fine is
your soil?

Rub a pinch of damp soil between your fingers.

Test a pinch
Two hands letting crumbly brown garden soil fall through the fingers above a freshly dug vegetable bed
AI-generated image, not a photograph of a real person or place.

GRITTY, SMOOTHor sticky?

Gritty, smooth or sticky: that feeling is grain size at work. Sand, silt and clay are defined by how big their particles are, and the finest of them, clay, shapes how a soil drains, warms and works.

At a glance

≈ 20%

Clay needed to act clayey

Colorado State University Extension notes that a soil with as little as 20% clay behaves as a clayey soil, even with 80% sand. RHS classes clay soils as those with over 25 percent clay.

CLAY · CSU EXTENSION

2× wider

Each size class versus the one below

On the Udden-Wentworth scale used by geologists, the diameter limits of each subcategory are twice as large as the one beneath it, from clay up to boulders.

SIZE STEPS · WENTWORTH

TWO NUMBERS WORTH KNOWING

A little clay
goes a long way.

One figure on how clay dominates a soil,
one on how geologists step through sizes.

Where clay starts depends on the scale: soil guides such as RHS use 0.002 mm, while the USGS, following Wentworth (1922), puts the clay boundary at 4 µm (0.004 mm).

THE RIBBON TEST

Squeeze it,
then ribbon it.

Knead a little moist soil into a putty-like ball, then push it out between thumb and finger into a flat ribbon until it breaks under its own weight. Pick what happened. The bar shows how clay-like the soil behaves.

A quick field guide, not a lab test. Texture names follow the USDA texture triangle used by the source.

Ribbon check

What did your soil do?
It would not stay in a ballSand

A moist ball that falls apart is sand. RHS notes sandy soil feels gritty and cannot be rolled into a sausage shape.

A ball, but no ribbonLoamy sand

It holds together when squeezed but will not push out into a ribbon: a loamy sand, still light and quick-draining.

A ribbon under 1 inch (about 2.5 cm)Loam family

Very gritty means sandy loam, equally gritty and smooth means loam, very smooth means silt loam.

A ribbon of 1 to 2 inchesClay loam family

Rub a pinch: very gritty is sandy clay loam, gritty and smooth is clay loam, very smooth is silty clay loam.

A ribbon of 2 inches or moreClay

A long ribbon means a clay soil. RHS adds that clay can be rolled into a long thin sausage and rubbed to a shiny finish.

Source: Colorado State University Extension, GardenNotes #214, Estimating Soil Texture; RHS, Soil types explained.

THE SHORT ANSWER

It all comes down
to grain size.

Sand, silt and clay are size classes, not materials.
The finest grains have the biggest say.

BY FEEL

Gritty, smooth, sticky

Moisten a pinch and rub it. Colorado State University Extension sums it up: sand feels gritty, silt feels smooth and clay feels sticky.

Try the ribbon test

IN A JAR

Let the grains settle

Shake soil with water and the grains sort themselves: sand drops in about a minute, silt within about two hours, and clay can take days.

How to do it

BY SIZE

Two scales, one idea

Gardeners call clay anything under 0.002 mm. Geologists use the Wentworth scale, where each size class is twice the one below.

See the numbers
A riverbank where small pebbles and coarse sand give way to smooth, fine grey mud at the water's edge
AI-generated image, not a photograph of a real person or place.

THE JAR TEST

Let water
do the sorting.

This is the settling test described by Colorado State University Extension. You need a tall, slender jar with a lid, some dry soil and a ruler.

  1. Dry and crush the soil

    Spread it out to dry, pick out stones and roots, and crush the lumps finely.

  2. Fill and shake

    Fill the jar a quarter with soil, add water to three-quarters, add a teaspoon of powdered non-foaming dishwasher detergent and shake hard for 10 to 15 minutes.

  3. Mark the layers

    Mark the sand depth after 1 minute and the silt after 2 hours. Mark the clay once the water clears, typically 1 to 3 days.

  4. Work out the shares

    Divide each layer's thickness by the total to get the percentage of sand, silt and clay, then look the mix up on a soil texture triangle.

WHY FINE GRAINS MATTER

Small grains,
big surface.

RHS explains that tiny clay particles have a huge surface area for their volume, so they dominate a soil. Clay soils hold nutrients and water, drain slowly, warm up late in spring and bake hard in summer.

Sandy soils are the opposite: light, quick-draining and easy to dig, but they dry out fast and lose nutrients to rain. Silt sits between, fertile but easily compacted. Loams mix all three and avoid the extremes.

A glass jar of soil and water on a windowsill, settled into a pale sand layer at the bottom, finer brown layers above and cloudy water on top
AI-generated image, not a photograph of a real person or place.

Questions

Questions people ask

How small is a clay particle?

In soil guides such as RHS, clay particles are less than 0.002 mm across, silt is 0.002 to 0.05 mm and sand is 0.05 to 2 mm. Anything bigger than 2 mm counts as stones.

Why do geologists give different sizes?

Geologists use the Udden-Wentworth scale, where sand runs from 2 mm down to about 0.063 mm. The USGS puts the clay boundary at 4 µm, so the classes overlap but do not match soil science exactly.

How can I tell silt from clay by touch?

Silt feels smooth or floury and, RHS says, slightly soapy, and does not clump easily. Clay is sticky when wet, smears, and can be rolled into a long thin sausage.

What is loam?

Loam is a mixture of clay, sand and silt. RHS says loams avoid the extremes of clay or sandy soils and are fertile, well drained and easily worked.

How do I know if my soil is chalky?

RHS suggests dropping a little soil into a jar of vinegar. If it froths, it contains free calcium carbonate (chalk) or limestone and is lime rich.

Sources

Where the facts come from

  1. RHS: Soil types explained
  2. Colorado State University Extension: Estimating soil texture, sandy, loamy or clayey (GardenNotes #214)
  3. Earle, Physical Geology (BCcampus): 6.1 Clastic sedimentary rocks, the Udden-Wentworth scale
  4. USGS Open-File Report 2006-1195: Sediment nomenclature and the Wentworth grade scale

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