Motorized Unconfined Compression Testing Machine
Applies constant vertical strain rate (0.5 to 2.0 mm/min) with electronic load cell monitoring force P.
Determine the unconfined compressive strength (q_u), undrained shear strength (c_u), and stress-strain deformation modulus (E_u) of undisturbed and remolded cohesive soil according to ASTM D2166 / AASHTO T208. Explore interactive structural mechanics, materials simulation, and civil engineering telemetry.
Ready to sample with Axial Strain = 3.0 %.
Adjust Axial Strain, then execute civil engineering measurement.
Civil engineering telemetry is evaluated rigorously using 64-bit IEEE 754 precision. Residuals reflect ordinary least-squares regression across successive observations. Continuous data structures support high-fidelity structural mechanics and geotechnical continuum modeling.
The civil engineering physical models apply within the specified calibrated operational window (1.0 to 6.0 %). Undisturbed silty clay specimen (diameter D_0 = 38.0 mm, length L_0 = 76.0 mm). Peak UCS q_u = 171.0 kPa, undrained shear strength c_u = q_u / 2 = 85.5 kPa. Linearized initial elastic response relates deviator stress σ_d to strain ε with slope 28.5000 kPa/% (E_u = 2.850 MPa).
Applies constant vertical strain rate (0.5 to 2.0 mm/min) with electronic load cell monitoring force P.
Measures compressive force up to 5.0 kN with 0.5 N resolution and digital display.
Measures vertical axial specimen deformation ΔL to 0.001 mm precision.
Trims cylindrical specimens to exact 38.0 mm diameter and 76.0 mm height.
Measures specimen diameter, length, and wet weight to 0.01 mm and 0.01 g.
Maintains 110 ± 5 °C for post-test moisture content determination.
Determine the unconfined compressive strength (q_u), undrained shear strength (c_u), and stress-strain deformation modulus (E_u) of undisturbed and remolded cohesive soil according to ASTM D2166 / AASHTO T208. Standardized parameter settings: 1.0, 2.0, 3.0, 4.0, 5.0, 6.0 %.
Trim an undisturbed cohesive soil core to 38.0 mm diameter and 76.0 mm height (L/D = 2.0) on the soil lathe; measure diameter at ends and middle; record initial length L_0 and mass M_0.
Place specimen centrally on lower platen of the UCS machine; raise platen until upper spherical bearing platen just makes contact; zero load cell and LVDT channels.
Engage motorized drive at a constant deformation rate of 1.0 mm/min (~1.3% strain/min); record compressive load P and axial deformation ΔL at 15-second intervals.
Calculate axial strain ε = ΔL / L_0; compute corrected cross-sectional area A = A_0 / (1 - ε) at each interval assuming constant specimen volume.
Continue loading until compressive load P peaks and begins dropping, or until axial strain reaches 15%; record peak load P_max and unconfined compressive strength q_u.
Sketch failure mode (single diagonal shear plane vs bulging barrel); measure shear failure angle θ; dry specimen in oven at 110 °C to determine moisture content w.
Points are your recorded observations. The solid regression line validates Unconfined Compression Test mathematical scaling.
| # | Axial Compressive Strain ε (%) | Axial Deviator Stress σ_d (kPa) | Axial strain ε (%) | Axial compressive stress σ_d (kPa) | Remove |
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The Unconfined Compressive Strength (UCS) test provides the most rapid, economical, and widely used laboratory method for determining the undrained shear strength (c_u) of cohesive fine-grained soils. Standardized under ASTM D2166, the test is a special limiting case of the unconsolidated-undrained (UU) triaxial compression test where confining cell pressure is zero (σ_3 = 0). A cylindrical undisturbed cohesive soil specimen (typically 38 mm or 50 mm diameter, with standard length-to-diameter aspect ratio L/D = 2.0 to 2.5) is mounted between flat end platens and loaded axially in compression without lateral lateral restraint. Loading is applied at a rapid strain rate of 0.5% to 2.0% per minute so that testing is completed within 10 to 15 minutes, ensuring that zero water can drain from low-permeability clay pores (undrained condition). As axial compressive force P increases, axial strain ε = ΔL / L_0 increases, and cross-sectional area expands from initial area A_0 to corrected area A = A_0 / (1 - ε). Deviator stress σ_d = P / A rises to a peak unconfined compressive strength q_u. According to the Mohr–Coulomb failure criterion for total stress with friction angle ϕ_u = 0, the Mohr circle passes through the origin (σ_3 = 0) and has diameter q_u. Consequently, the undrained shear strength is exactly half the unconfined compressive strength: c_u = q_u / 2. In this laboratory, cohesive soil specimens are tested across axial strains from 1% to 6% to calibrate the undrained modulus E_u and evaluate undrained shear strength c_u.
Undisturbed silty clay specimen (diameter D_0 = 38.0 mm, length L_0 = 76.0 mm). Peak UCS q_u = 171.0 kPa, undrained shear strength c_u = q_u / 2 = 85.5 kPa. Linearized initial elastic response relates deviator stress σ_d to strain ε with slope 28.5000 kPa/% (E_u = 2.850 MPa).