DrainageCalculators

Rock/Sediment Gradation Calculator

Analyze Wolman, riprap, or calibrated-photo particle measurements to calculate D-percentiles, a percent-finer curve, sediment class, and compliance with project gradation envelopes.

Analyze a Wolman pebble count, manual riprap count, or calibrated photograph measurements. The calculator returns D16, D30, D50, D84, D90, a cumulative percent-finer curve, material classification, and transparent checks against FHWA Classes I-X or custom project gradation limits.

Particle-size units

Existing physical-size entries are converted when units change.

Input Parameters

Measurement Method

Choose a field count or explicit measurements from a scaled photograph.

Particle Measurements

Enter individual intermediate-axis (b-axis) sizes in in. Commas, spaces and new lines are accepted.

Use one value per sampled particle. Do not enter class counts or percentages here.

0 valid particles

Gradation Specification (Optional)

Compare the measured sample with an agency/project class or a point-by-point percent-finer envelope.

What this analysis reports

Characteristic sizes

D16, D30, D50, D84 and D90, plus D5/D10/D15/D60/D85/D95/D100 for specification work.

Transparent comparisons

Every entered class limit or percent-finer envelope point is shown as an individual pass/fail check.

For educational purposes only. Not a substitute for professional engineering judgment.

How gradation analysis works

1. Measure consistently

For a field Wolman count, measure the intermediate or b-axis of each selected particle. Each observation has equal count weight.

2. Order and interpolate

Values are sorted from smallest to largest. Characteristic D-percentiles use inclusive linear interpolation between adjacent ordered measurements.

3. Compare limits

Select an FHWA HEC-23 Table 4.1 D50/D100 class screen, or supply controlling agency D15/D50/D85/D100 limits or a percent-finer curve envelope for point-by-point checks.

Count gradation versus sieve gradation

This tool reports an equal-count particle distribution. A laboratory sieve analysis usually reports percent passing by mass. Those distributions answer related but different questions and should not be substituted for one another unless the governing method explicitly allows it.

Method Weighting Typical use
Wolman / riprap count One vote per particle Surface substrate and placed-rock screening
Laboratory sieve Mass retained or passing Aggregate and soil material specifications

Frequently asked questions

What do D16, D50, and D84 mean?

Dx is the particle size for which x percent of the measured sample is finer. D50 is the median size. D16 and D84 describe the spread around that median and are commonly used in streambed and sediment analyses.

How many particles should a Wolman pebble count include?

A traditional field count commonly uses about 100 spatially distributed particles. The calculator can analyze smaller samples, but it flags them because a small or selectively collected sample can give unstable percentiles.

Can the calculator automatically measure stones in a photograph?

No. Automatic segmentation can be unreliable when particles overlap, shadows vary, or scale and perspective are not controlled. The scaled-photo workflow instead asks for a known pixel scale and explicitly measured particle axes, making every conversion reviewable.

Which FHWA standard riprap classes are included?

FHWA Classes I through X are preloaded from HEC-23 Volume 2, Table 4.1. The built-in screen uses each class's nominal D50, allowable D50 range, and D100 maximum. Because Table 4.1 is not a complete D15/D85 or percent-finer acceptance envelope, agency and project-specific limits can still be entered separately.

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Last verified: August 2026