Soil Compaction Calculator
Calculate soil compaction percentage from wet density, dry density, and optimum moisture. Enter values for instant results with step-by-step formulas.
Reviewed for accuracy by Daniel Agrici, Founder & Lead Developer
Soil Compaction Calculator
Calculator
Adjust values & calculateEnter your values below. Every result is computed in your browser โ no data is sent to any server.
Formula: ฮณd = Ws / V | w = (Ww - Wd) / Wd ร 100 | RC = ฮณd / ฮณd_max ร 100
Worked example โ 94.5% (Fail โ needs more compaction)
Formula
ฮณd = Ws / V | w = (Ww - Wd) / Wd ร 100 | RC = ฮณd / ฮณd_max ร 100
Dry density = dry weight / volume. Moisture content = (wet-dry)/dry ร 100%. Relative compaction = field density / max Proctor density ร 100%. RC โฅ 95% typically required.
Worked Examples
Example 1: Field test
Problem:Wet=1850g, Dry=1650g, V=943.3cmยณ, Max=1.85 g/cmยณ
Solution:ฮณd=1.749, w=12.1%, RC=94.5%
Result:94.5% (Fail โ needs more compaction)
Frequently Asked Questions
Why is 95% compaction required?
Most building codes require โฅ95% relative compaction for foundations and roads. Under-compacted soil settles unevenly, causing structural damage.
What is the Proctor compaction test and why is it used?
The Standard Proctor test (ASTM D698) compacts soil in a mold using a specified rammer and number of blows to determine the maximum dry density and optimum moisture content. The Modified Proctor (ASTM D1557) uses higher compaction energy for heavily loaded projects like highways and airfields. Field density is then expressed as a percentage of this lab-determined maximum.
How does moisture content affect soil compaction?
Soil compacts most efficiently at its optimum moisture content (OMC). Too dry and soil particles resist rearrangement; too wet and water fills pore spaces, preventing further densification. The Proctor curve shows a bell-shaped relationship between moisture and dry density. Field compaction should target moisture within 2% of the OMC for best results.
What is soil composition and how is it measured?
Soil is composed of minerals (45%), organic matter (5%), water (25%), and air (25%). Texture is classified by percentages of sand (0.05-2mm), silt (0.002-0.05mm), and clay (less than 0.002mm) using the USDA soil texture triangle. Loam, an ideal garden soil, has roughly equal parts of each.
Background & Theory
History
Reviewed for accuracy by Daniel Agrici, Founder & Lead Developer ยท Editorial policy
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