Standard Casagrande Mechanical Liquid Limit Device
Brass cup dropping 10.0 ± 0.2 mm onto a calibrated hard ebonite rubber base via hand crank.
Determine the Liquid Limit (LL), Plastic Limit (PL), and Plasticity Index (PI) of cohesive soil using the Casagrande mechanical liquid limit cup according to ASTM D4318 / BS 1377-2. Explore interactive structural mechanics, materials simulation, and civil engineering telemetry.
Ready to sample with Blow Count N = 25.0 blows.
Adjust Blow Count N, 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 (15.0 to 40.0 blows). High-plasticity alluvial clay (CH under USCS). Linearized flow curve relates moisture content w directly to log10(N) with flow index slope -14.5000 %/log(blow) and 0-blow intercept 62.00%. Liquid limit LL at N = 25 blows evaluates as w(25) = -14.50 · log10(25) + 62.00 = -14.50(1.39794) + 62.00 = 41.73%.
Brass cup dropping 10.0 ± 0.2 mm onto a calibrated hard ebonite rubber base via hand crank.
Precision brass/plastic grooving tool cutting clean 2.0 mm wide, 8.0 mm deep central channel.
Smooth frosted glass plate (450 x 450 mm) and flexible steel spatulas for paste blending.
Electric oven maintaining 110 ± 5 °C and airtight aluminum containers weighing moisture portions.
10.0 mm machined step gauge verifying exact cup drop height prior to testing.
Weighs soil moisture portions to 0.01 g resolution (capacity 200 g).
Determine the Liquid Limit (LL), Plastic Limit (PL), and Plasticity Index (PI) of cohesive soil using the Casagrande mechanical liquid limit cup according to ASTM D4318 / BS 1377-2. Standardized parameter settings: 15.0, 20.0, 25.0, 30.0, 35.0, 40.0 blows.
Pass air-dried soil through the 425 μm (No. 40) sieve; take 250 g; calibrate Casagrande cup drop height to exactly 10.0 mm using the thickness gauge on the grooving tool.
Place soil on glass plate; add distilled water gradually, working thoroughly with spatulas for 10 minutes to produce a uniform, smooth plastic paste.
Place a portion of paste into the brass cup above the hinge; spread with spatula to maximum depth of 10 mm; level surface parallel to rubber base.
Draw grooving tool firmly along the cup centerline from hinge toward front in a single continuous stroke, dividing soil pat into two symmetrical halves.
Turn crank at steady rate of 2 blows per second; count blows until soil halves flow together and close across a continuous bottom length of 12.7 mm; record blow count N.
Extract a 15 g sample across the closed groove; weigh immediately; dry in oven at 110 °C to determine w; repeat at varying moisture contents between 15 and 40 blows to establish the Flow Curve.
Points are your recorded observations. The solid regression line validates Casagrande Liquid Limit mathematical scaling.
| # | Casagrande Cup Blow Count N (blows) | Moisture Content w (%) | Common logarithm of blow count log10(N) | Moisture content w (%) | Remove |
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No readings yet. Execute a civil engineering trial and record it.
The consistency and physical behavior of cohesive fine-grained soils depend profoundly on moisture content rather than particle size alone. In 1911, Swedish chemist Albert Atterberg defined four fundamental physical states of soil consistency: solid, semi-solid, plastic, and liquid. In 1932, Arthur Casagrande standardized the mechanical boundary between the plastic and liquid states—the Liquid Limit (LL)—using the mechanical cup apparatus (ASTM D4318). The Liquid Limit is defined as that gravimetric moisture content at which a trapezoidal groove cut through a pat of soil in a brass cup closes over a length of exactly 12.7 mm (0.5 inches) upon receiving exactly 25 standard mechanical blows dropped from a height of 10.0 mm at 2 blows per second onto a hard rubber base. At the liquid limit, all fine-grained soils possess an identical, tiny undrained shear strength of approximately 1.7 to 2.4 kPa. Because achieving exactly 25 blows in a single trial is virtually impossible, tests are performed across four to six trials with blow counts spanning 15 to 40 blows. Plotting moisture content w against log10(N) yields a straight line termed the Flow Curve, whose slope defines the Flow Index I_f = -dw / d(log10 N). The moisture content at N = 25 blows interpolated from the flow curve provides the Liquid Limit LL. Combined with the Plastic Limit (PL, moisture where 3.2 mm soil threads crumble), the Plasticity Index PI = LL - PL classifies soils on Casagrande's Plasticity Chart under the Unified Soil Classification System (USCS). In this laboratory, Casagrande tests are performed to evaluate the Flow Index I_f and establish LL.
High-plasticity alluvial clay (CH under USCS). Linearized flow curve relates moisture content w directly to log10(N) with flow index slope -14.5000 %/log(blow) and 0-blow intercept 62.00%. Liquid limit LL at N = 25 blows evaluates as w(25) = -14.50 · log10(25) + 62.00 = -14.50(1.39794) + 62.00 = 41.73%.