Soil and Rock Testing

Specific Gravity Test of Soil and Aggregate

Determining particle density for soil classification, mix design, and void ratio analysis

IS 2720 Part 3 Sec 1 IS 2720 Part 3 Sec 2 IS 2386 Part 3
The specific gravity of a soil or aggregate is the ratio of the mass of a given volume of the material to the mass of an equal volume of distilled water at a reference temperature. It is a fundamental index property used in nearly every geotechnical calculation, from void ratio to degree of saturation.

What Is the Specific Gravity Test?

Specific gravity (G) quantifies how dense the solid particles of a soil or aggregate are compared to water. For most natural soils, G falls in the range of 2.60 to 2.80, with organic soils sometimes dropping below 2.50 and iron-rich laterites exceeding 3.00. In aggregate testing, specific gravity values determine the mass-volume relationships essential for concrete and bituminous mix design. The test method varies depending on the material. For fine-grained soils, the pycnometer method per IS 2720 Part 3 Section 1 is used. For fine aggregates and soil fractions passing 4.75 mm, the density bottle method per IS 2720 Part 3 Section 2 is standard. For coarse aggregates retained on 10 mm sieves, the wire basket method per IS 2386 Part 3 is employed. When testing expansive or highly reactive soils, kerosene is used instead of water to prevent hydration and swelling during the test. NKMPV performs specific gravity testing as part of comprehensive grain size analysis and aggregate quality assessment packages. The results feed directly into void ratio calculations, settlement analysis, compaction control, and concrete mix proportioning. Our laboratory serves contractors, geotechnical consultants, and government agencies across 10 states including Punjab, Haryana, Himachal Pradesh, Delhi, and more.

Test Parameters & Acceptance Criteria

The following parameters are measured or derived during specific gravity testing. Acceptance criteria depend on the material type and the design application — soil classification, mix design, or earthwork quality control.

Parameter Value / Range Unit Standard
Specific Gravity of Soil (Fine-Grained) 2.60-2.80 (typical) IS 2720 Part 3 Sec 1
Specific Gravity of Soil (Organic/Peaty) 1.80-2.50 (typical) IS 2720 Part 3 Sec 1
Specific Gravity — Density Bottle (Fine Aggregate) 2.50-2.70 (typical) IS 2720 Part 3 Sec 2
Specific Gravity of Coarse Aggregate (Oven-Dry Basis) 2.50-3.00 (typical) IS 2386 Part 3
Water Absorption of Coarse Aggregate < 2% (most specifications) % IS 2386 Part 3
Apparent Specific Gravity Higher than oven-dry Gs IS 2386 Part 3
Temperature Correction Factor (Ct) Applied for tests not at 27 °C IS 2720 Part 3 Sec 1 Table 1

Applicable Indian Standards

IS 2720 Part 3 Sec 1

Methods of Test for Soils — Determination of Specific Gravity (Fine-Grained Soils) — Fine, Medium and Coarse Grained Soils

IS 2720 Part 3 Sec 2

Methods of Test for Soils — Determination of Specific Gravity — Fine, Medium and Coarse Grained Soils (Density Bottle Method)

IS 2386 Part 3

Methods of Test for Aggregates for Concrete — Specific Gravity, Density, Voids, Absorption and Bulking

IS 1498

Classification and Identification of Soils for General Engineering Purposes

IS 2720 Part 2

Methods of Test for Soils — Determination of Water Content

Equipment Used

Pycnometer (1000 ml)

Standard IS pycnometer with brass conical cap

1000 ml capacity, fits fine-grained soil samples up to 400 g

Calibrated

Density Bottle (50 ml)

Borosilicate glass with ground-glass stopper

50 ml capacity, suitable for fine aggregate and soil passing 2 mm sieve

Calibrated

Wire Basket Apparatus

Stainless steel mesh basket with suspension frame

Accommodates coarse aggregate samples up to 3 kg, mesh aperture 6.3 mm

Calibrated

Vacuum Desiccator with Pump

Glass desiccator with mechanical vacuum pump

Removes entrapped air from soil-water slurry in pycnometer

Calibrated

Constant Temperature Water Bath

Thermostatically controlled stainless steel bath

Maintains temperature at 27 ± 0.2 °C as required by IS 2720 Part 3

Calibrated

Digital Weighing Balance

Shimadzu / Mettler Toledo

Least count 0.01 g (for density bottle) and 0.1 g (for pycnometer), NABL-calibrated

Calibrated

Testing Process

1

Sample Collection & Preparation

Day 1

A representative soil or aggregate sample is collected from the project site or received at the laboratory. For fine-grained soil, approximately 200-400 g of oven-dried material passing the 4.75 mm IS sieve is prepared. For coarse aggregates, a sample of approximately 2 kg is washed, dried, and graded. The appropriate test method — pycnometer, density bottle, or wire basket — is selected based on particle size.

2

Calibration of Apparatus

Day 1

The pycnometer or density bottle is cleaned, dried, and weighed empty (W1). It is then filled with distilled water (or kerosene for expansive soils), brought to the reference temperature of 27 °C in a constant-temperature water bath, and weighed again (W2). This calibration establishes the mass of water the apparatus holds at the standard temperature, which is essential for all subsequent calculations.

3

Soil/Aggregate Introduction & De-airing

Day 1

The oven-dried soil sample is placed into the pycnometer (W3 recorded), and distilled water is added until the pycnometer is approximately half full. The slurry is gently heated or subjected to vacuum in a desiccator for at least 30 minutes to remove all entrapped air — a critical step, as even small air bubbles cause significant error. For the wire basket method, the saturated surface-dry aggregate is weighed in air (Wa) and then submerged in water (Ww).

4

Temperature Equilibration & Final Weighing

Day 1

After complete de-airing, the pycnometer is topped up with distilled water to the calibration mark, the cap is secured, and the assembly is placed in the constant-temperature water bath at 27 °C for at least 1 hour. Once equilibrated, the pycnometer is removed, dried externally, and weighed (W4). The difference between W2 and W4, corrected for the soil mass, gives the volume of soil solids displaced.

5

Repeat Determination

Day 1-2

To ensure reliability, a minimum of two parallel determinations are performed on separate sub-samples as required by IS 2720 Part 3. If the two values differ by more than 0.03, a third determination is carried out. For aggregate testing per IS 2386 Part 3, duplicate tests are standard practice. This repetition is a core requirement of our NABL quality system.

6

Calculation & Reporting

Day 2-3

Specific gravity is calculated using the formula G = (W3 - W1) / [(W2 - W1) - (W4 - W3)], with a temperature correction factor applied if the test was not conducted exactly at 27 °C. For aggregates, oven-dry, saturated surface-dry, and apparent specific gravities are computed along with water absorption percentage. The NABL-accredited report includes all raw weights, temperature readings, individual and average Gs values, and the applicable IS code reference.

Where This Test Is Used

Specific gravity is one of the most fundamental material properties in geotechnical and construction engineering. In soil mechanics, it is used to compute void ratio, porosity, and degree of saturation — parameters that underpin soil classification per IS 1498 and settlement analysis for foundations. For concrete technology, the specific gravity of coarse and fine aggregates is an essential input for volumetric mix design per IS 10262. In highway construction, the bulk specific gravity of aggregate determines theoretical maximum density for bituminous mix design. Specific gravity also helps verify soil mineralogy — unusual values may indicate organic content, mineral contamination, or the presence of heavy minerals. NKMPV often performs this test alongside moisture content determination as part of a standard soil characterisation package.
Void ratio and porosity calculation for settlement analysis Soil classification per IS 1498 using grain size and Gs data Concrete mix design per IS 10262 — volumetric batching Bituminous mix design — theoretical maximum density calculation Earthwork compaction control — phase relationship verification Identification of organic or contaminated soils with anomalous Gs values Quality control of imported fill material and borrow-area soils

Detailed Information

The specific gravity test of soil and aggregate is a fundamental laboratory test used to determine the relative density of soil particles and aggregates compared to water. NKMPV conducts specific gravity tests of soil and aggregate in accordance with applicable IS standards to support mix design, soil classification, and quality assessment for construction and infrastructure projects.


What Is the Specific Gravity Test

The soil and aggregate gravity test measures the ratio of the weight of soil or aggregate particles to the weight of an equal volume of water. This property helps engineers understand the composition, density, and quality of materials used in geotechnical and construction applications.


Importance of Specific Gravity in Construction

Specific gravity plays a critical role in:

• Soil classification and identification
• Concrete and bituminous mix design
• Determination of void ratio and porosity
• Assessment of material quality and consistency
• Geotechnical analysis and design calculations


Specific Gravity Test for Soil

For soils, the specific gravity test is used to evaluate mineral composition and particle characteristics. Typical values vary depending on soil type:

• Sands and silts generally range between 2.65 to 2.70
• Clays may have higher values depending on mineral content

The results are essential for compaction analysis, permeability studies, and stability assessment.


Specific Gravity Test for Aggregate

For aggregates, the test determines density characteristics that influence:

• Concrete strength and durability
• Bituminous mix performance
• Water absorption behavior
• Mix proportioning and quality control

Accurate specific gravity values help ensure consistency in construction materials.


Testing Methodology and Standards

Specific gravity test of soil carried out in geotechnical laboratory using standard apparatus as per IS 2720
Specific gravity test of soil conducted in NKMPV geotechnical laboratory for soil classification and engineering analysis.

The specific gravity test of soil and aggregate is conducted as per relevant Indian Standards (IS). The testing methodology involves controlled measurement of mass and volume using standardized equipment and procedures to ensure accuracy and repeatability.


Applications of this Test

This test is commonly used in:

Soil and rock testing programs
• Concrete and bituminous mix design
• Quality control of construction materials
• Geotechnical investigations
• Research and laboratory analysis

References Code: IS 2720 (Part 3)


Why Choose NKMPV for Specific Gravity Testing

• NABL-accredited laboratory facilities
• Standardized testing as per IS guidelines
• Experienced technical professionals
• Accurate and reliable test results
• Support for design and quality decisions

Why Choose NKMPV for Specific Gravity Testing?

NABL Accredited Results

Our specific gravity test reports carry NABL accreditation (ISO/IEC 17025:2017), making them accepted by NHAI, state PWDs, courts, and arbitration tribunals without additional verification.

All Three Standard Methods

We perform the pycnometer method (fine-grained soil), density bottle method (fine aggregates and sand), and wire basket method (coarse aggregates) — covering the full range of materials you may encounter on a project.

Vacuum De-airing for Accuracy

Entrapped air is the primary source of error in specific gravity testing. Our vacuum desiccator setup removes air bubbles far more effectively than manual boiling, yielding reproducible results within ± 0.02 of the true value.

Same-Day Express Option

For urgent projects, we offer same-day specific gravity testing with results delivered within 24 hours. Standard turnaround is 2-3 days including full NABL-accredited reporting.

Comprehensive Soil Package

We combine specific gravity with grain size analysis, Atterberg limits, moisture content, and compaction tests — giving your geotechnical consultant a complete dataset in a single engagement.

Frequently Asked Questions

Most natural inorganic soils have a specific gravity between 2.60 and 2.80. Sandy soils with predominantly quartz particles typically show G around 2.65. Clayey soils range from 2.67 to 2.80 depending on mineral composition. Organic and peaty soils can have values as low as 1.80-2.20, while lateritic and iron-rich soils may exceed 3.00.
The standard methods are covered under IS 2720 Part 3. Section 1 covers the pycnometer method for fine, medium, and coarse-grained soils. Section 2 covers the density bottle method for fine-grained soil and fine aggregate. For coarse aggregates used in concrete, IS 2386 Part 3 is the applicable standard. NKMPV tests as per both standards depending on the material type.
Kerosene is used when testing expansive or highly plastic soils such as black cotton soil. These soils swell and absorb water on contact, which would alter the measured volume of soil solids and produce incorrect results. Kerosene, being a non-polar liquid, does not cause swelling or hydration, ensuring accurate measurement of true particle density.
For the pycnometer method (fine-grained soil), approximately 200-400 g of oven-dried soil passing a 4.75 mm sieve is required. For the density bottle method, about 50-100 g of material passing a 2 mm sieve is sufficient. For coarse aggregate testing by the wire basket method, a sample of approximately 2 kg is needed. We recommend sending extra material to allow for repeat determinations.
A standard specific gravity test takes 2-3 days from sample receipt to report delivery. The actual laboratory procedure — including oven-drying, de-airing, temperature equilibration, and duplicate determinations — typically takes 1-2 days. Report preparation and NABL-accredited documentation adds an additional day. Express same-day testing is available for urgent requirements.
Specific gravity alone does not indicate soil strength or quality, but it reveals important information about soil composition. A value significantly below 2.60 suggests the presence of organic matter or lightweight minerals. A value above 2.80 may indicate heavy minerals or metallic inclusions. In geotechnical design, specific gravity is essential for calculating void ratio (e), degree of saturation (S), and dry density — all of which directly influence foundation design, settlement predictions, and compaction specifications.

Need Specific Gravity Testing? Get a Quote Today.

+91-XXXXX-XXXXX