Compressibility and Consolidation

Consolidation is the time-dependent settlement of saturated fine-grained soils (clays/silts) resulting from the expulsion of water from the soil pores. It is a critical consideration for the design of structures on soft ground.

Types of Settlement

Settlement Components

  • Immediate (Elastic) Settlement (SeS_e): Occurs rapidly in all soils upon load application. Dominated by elastic deformation.
  • Primary Consolidation Settlement (ScS_c): Occurs over time as excess pore water pressure dissipates. Only significant in saturated clays.
  • Secondary Compression (Creep) (SsS_s): Occurs after primary consolidation is complete (after excess pore pressure has fully dissipated). Caused by the slow, viscous plastic readjustment of clay particles.

One-Dimensional Consolidation Theory

Terzaghi's theory assumes flow occurs only in the vertical direction.

Preconsolidation Pressure (σc\sigma'_c)

The maximum effective vertical stress that a soil element has ever sustained in the past.
  • Normally Consolidated (NC): Present effective stress equals the past maximum pressure (σo=σc\sigma'_o = \sigma'_c).
  • Overconsolidated (OC): Present effective stress is less than the past maximum pressure (σo<σc\sigma'_o < \sigma'_c).

Overconsolidation Ratio

Settlement Formulas (Primary Consolidation)

Normally Consolidated Clay:

Primary Consolidation (NC Clay)

Overconsolidated Clay:
  • Case 1: σo+Δσσc\sigma'_o + \Delta \sigma \le \sigma'_c (Remains OC)

Primary Consolidation (OC Clay, Case 1)

  • Case 2: σo+Δσ>σc\sigma'_o + \Delta \sigma > \sigma'_c (becomes NC)

Primary Consolidation (OC Clay, Case 2)

Secondary Compression (Creep) Settlement

Secondary compression continues indefinitely at a logarithmic rate after primary consolidation ends at time tpt_p. It is highly significant in highly organic soils and peats.

Secondary Compression Settlement

Interactive Consolidation Simulation

Explore how soil properties (CvC_v) and layer thickness (HH) affect the rate of consolidation settlement over time.

Interactive Consolidation Lab

Time to 90% Consolidation (U=90U=90\\%)

0.00 years

Excellent! Construction can proceed quickly.

Sand / Fill (Drainage)
SOFT CLAY
Sand (Drainage)

Time Rate of Consolidation

The time required for a certain percentage of consolidation to occur depends on the permeability and compressibility of the soil.

Time Factor (TvT_v)

Time Factor

Degree of Consolidation (UU): The percentage of primary consolidation that has occurred at time tt.

Time Factor vs. Degree of Consolidation

Determining Cv from Lab Data

Because CvC_v dictates how fast a building will settle, determining it accurately from an Oedometer lab test is critical. There are two standard graphical methods:
  • Casagrande's Logarithm-of-Time Method: Uses the settlement vs. log(time)\log(time) curve. It identifies the t50t_{50} point (time for 50% consolidation) graphically. CvC_v is calculated using T50=0.197T_{50} = 0.197.
  • Taylor's Square-Root-of-Time Method: Uses the settlement vs. time\sqrt{time} curve. It identifies the t90t_{90} point (time for 90% consolidation) by drawing a secant line with 1.15 times the initial slope. CvC_v is calculated using T90=0.848T_{90} = 0.848.
Key Takeaways
  • Consolidation is the expulsion of water from saturated clay pores under load, leading to settlement over time.
  • Normally Consolidated (NC) soils settle significantly more than Overconsolidated (OC) soils for the same load increase.
  • Preconsolidation Pressure (σc\sigma'_c) is the memory of the maximum past stress.
  • The Coefficient of Consolidation (CvC_v) governs the time rate of settlement, evaluated using the Casagrande (t50t_{50}) or Taylor (t90t_{90}) graphical methods.
  • Double drainage speeds up consolidation by a factor of 4 compared to single drainage.
  • Secondary Compression (Creep) is the continuous, plastic readjustment of clay particles that occurs after pore pressures have fully dissipated.