Cone Penetration Test (CPT)

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The Cone Penetration Test (CPT) is an advanced in-situ geotechnical test that provides continuous soil profiling and direct measurement of soil strength parameters. In Australia, CPT testing is widely used for major infrastructure, mining, and coastal developments.

What Is the CPT?

The CPT involves pushing a cone-tipped probe (typically 15 cm² base area, 60° apex angle) into the ground at a constant rate of 20 mm/s while continuously measuring:

  • Cone resistance (q_c) — end bearing resistance
  • Sleeve friction (f_s) — side friction on the 150 cm² friction sleeve
  • Pore pressure (u₂) — (for CPTu) measured at the cone shoulder

The resulting data is recorded at 10–20 mm intervals, providing a continuous profile of soil behaviour.

Measured Parameters

Parameter Symbol Unit What It Indicates
Cone resistance q_c MPa Soil strength, density
Sleeve friction f_s kPa Soil type, grain size
Friction ratio R_f % f_s / q_c × 100 — soil type classification
Pore pressure u₂ kPa Groundwater, drainage characteristics
Pore pressure ratio B_q (u₂ — u₀) / (q_t — σ_v₀)

CPT vs SPT

Aspect CPT SPT
Continuity Continuous profile Discrete points (every 1–1.5 m)
Speed Faster (20–30 m/h) Slower (requires rod handling)
Sample No physical sample Disturbed sample collected
Accuracy Highly repeatable Operator-dependent
Cost Higher mobilisation Lower mobilisation
Soil types Limited in gravels All soil types
Penetration Typically to 30–40 m Typically to 30–50 m

CPT Equipment in Australia

Onshore

  • 15–20 tonne rigs — standard for most projects
  • Track-mounted CPT rigs — for soft or uneven terrain
  • Lightweight CPT rigs — limited access, environmental sites

Offshore / Marine

  • Seabed CPT systems — lowered to seafloor
  • Downhole CPT — deployed through drill string
  • Free-fall CPT — for very soft seabed sediments

Soil Behaviour Type (SBT) Charts

The standard Robertson (1990, 2010) SBT chart classifies soil into 9 zones using q_c and R_f:

Zone Soil Behaviour Type Typical q_c (MPa) Typical R_f (%)
1 Sensitive fine-grained < 0.5 < 0.5
2 Organic soils / clay 0.5–1.0 1–3
3 Clays — silty clay 1.0–2.5 2–4
4 Silt mixtures 2.5–5.0 1–3
5 Sand mixtures 5.0–10.0 0.5–2.0
6 Sands — clean sand 10.0–20.0 0.2–1.0
7 Dense sand — gravelly > 20.0 < 0.5
8 Very stiff sand / clay N/A N/A
9 Very stiff fine-grained N/A N/A

Correlations

Undrained Shear Strength (Clays)

$$ s_u = \frac{q_t - \sigma_{v0}}{N_{kt}} $$

Where N_kt = 14–16 typically (site-specific calibration recommended).

Friction Angle (Sands)

$$ \phi' = 17.6 + 11.0 \times \log_{10}\left(\frac{q_c}{\sqrt{\sigma_{v0}}}\right) $$

Relative Density (Sands)

$$ D_r = \frac{1}{2.96} \times \ln\left(\frac{q_c}{0.064 \times \sigma_{v0}^{0.5}}\right) $$

Constrained Modulus (Settlement)

Soil Type M (MPa)
Clays M = 2–8 × q_c
Silts M = 3–6 × q_c
Sands M = 3–12 × q_c

Applications

Application CPT Use
Foundation design Stratigraphy, bearing capacity, settlement parameters
Pile design End bearing, skin friction, continuity of bearing stratum
Liquefaction assessment Cyclic resistance ratio (CRR) from CPT data
Ground improvement verification Pre- and post-treatment CPT profiling
Land reclamation Consolidation assessment, fill performance
Offshore investigations Seabed strength, pipeline trenching
Contaminated sites Stratigraphy for contaminant transport modelling

CPTu (Piezocone)

The CPTu adds pore pressure measurement for enhanced capabilities:

Measurement Indication
u₂ at cone shoulder Most reliable pore pressure reading
High u₂ Compressible clay, silt
Low or negative u₂ Dense sand, overconsolidated clay
Dissipation test In-situ permeability, consolidation coefficient (c_h)

Pore Pressure Dissipation Test

The penetration is stopped at a target depth and the pore pressure decay is recorded:

  • Sands — dissipation in seconds
  • Silts — dissipation in minutes
  • Clays — dissipation in hours

The dissipation test gives:

  • Equilibrium pore pressure (u₀)
  • Coefficient of consolidation (c_h)
  • Hydraulic conductivity (k)

Advantages and Limitations

Advantages

  • Continuous, repeatable data
  • Fast (20–30 m per hour)
  • Direct measurement — no operator bias
  • Detailed stratigraphy identification
  • Pore pressure and dissipation data (CPTu)
  • Correlated to many design parameters
  • Good for soft soils

Limitations

  • Cannot penetrate gravel, boulders, or hard rock
  • No soil sample for visual classification or lab testing
  • Higher mobilisation cost than SPT (typically)
  • Requires reaction weight (20-tonne rig)
  • Limited depth near bedrock or very dense layers

Australian Standards

Standard Title
AS 1726-2017 Geotechnical site investigations
AS 1289.6.5.1 Determination of the cone resistance of a soil — Static cone penetrometer test
ISSMGE TC16 International reference test procedure for CPT

Frequently Asked Questions

Can CPT replace SPT?

CPT provides more detailed data for most applications but does not collect a soil sample. For projects where physical samples are critical (classification, lab testing), CPT is best combined with limited boreholes for sample collection.

What is the maximum depth of CPT?

Onshore CPT typically reaches 30–40 m in ideal conditions. Greater depths (40–60 m) are possible with heavier rigs. Offshore CPT can reach 50–80 m depending on the system.

Can CPT detect gravels?

CPT can identify gravel layers through tip resistance fluctuations, but cannot penetrate through thick gravel beds. SPT or rotary drilling is needed where gravels are anticipated.

How is CPT used for liquefaction assessment?

CPT is the preferred method for liquefaction assessment. The cone resistance is used to calculate the Cyclic Resistance Ratio (CRR) and is less ambiguous than SPT-based methods for silty soils.