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CELE Geotechnical EngineeringConsolidation and SettlementCheat Sheet

One-page cheat sheet for CELE Geotechnical Engineering — Consolidation and Settlement. Every formula, definition, and key fact you need for this chapter, condensed to a single printable page. Designed for the final review session before the CELE 2026.

Exam context

On the CELE 2026, the Geotechnical Engineering subtest carries a "Core" weight in Professional Regulation Commission (PRC) — Board of Civil Engineering's pattern. Consolidation and Settlement lands at position 6th out of 11 in the standard review order. Target score is 70% weighted average, no sub-test below 50%, and roughly a meaningful share of items come from Geotechnical Engineering on a typical CELE paper.

Consolidation and Settlement - Cheat Sheet

Your last-minute revision companion for Consolidation and Settlement. This sheet condenses all formulas, definitions, and board-exam essentials into rapid-fire reference points. Master the compression indices, time-factor calculations, and settlement predictions.

Sections

Formulas

Formula

S_c = (C_c / (1 + e_0)) × H × log₁₀((σ'_0 + Δσ) / σ'_0)

Meaning

S_c = primary settlement (mm); C_c = compression index (slope of virgin e–log σ' line); e_0 = initial void ratio; H = layer thickness (mm); σ'_0 = initial effective stress (kPa); Δσ = stress increase (kPa)

Watch Out

Use log₁₀ (base 10), NOT natural log. Use C_c ONLY if final stress > preconsolidation stress σ'_c

When To Use

Calculate settlement for normally consolidated (NC) clay under load increase

Formula

S_c = (C_r / (1 + e_0)) × H × log₁₀((σ'_0 + Δσ) / σ'_0)

Meaning

S_c = recompression settlement (mm); C_r = recompression index (much smaller than C_c, typically 0.1–0.2 × C_c)

Watch Out

C_r is much smaller than C_c — using C_c for OC clay OVERESTIMATES settlement significantly

When To Use

Calculate settlement for overconsolidated (OC) clay while final stress ≤ preconsolidation stress σ'_c

Formula

S_c(total) = S_c(recompression, OC range) + S_c(virgin, NC range)

Meaning

For OC clay loaded beyond σ'_c: split into two stages — recompression (C_r) up to σ'_c, then virgin compression (C_c) beyond

Watch Out

Easy to forget the two-stage calculation — check if loading crosses σ'_c

When To Use

OC clay with stress path crossing the preconsolidation pressure

Common Values

Value

0.20–0.50

Symbol

C_c

Quantity

Compression Index for clay (typical range)

Value

0.01–0.10

Symbol

C_r

Quantity

Recompression Index (typical range)

Value

0.6–1.2

Symbol

e

Quantity

Void ratio for clays (typical range)

Section Title

Primary Consolidation Settlement

Important Facts

  • Settlement is caused by expulsion of pore water from saturated clay under load — a time-dependent process.
  • NC clays settle more than OC clays under the same stress increase because C_c >> C_r.
  • The settlement magnitude depends ONLY on C_c (or C_r), e_0, H, and the stress ratio — NOT on c_v or drainage.
  • Use H in consistent units with S_c result (mm → use H in mm; m → use H in m).
  • The stress ratio log₁₀((σ'_0 + Δσ) / σ'_0) = log₁₀(1 + Δσ/σ'_0) captures the nonlinear compression behavior.
  • For clay with c_c ≈ 0.009 × (LL − 10) (empirical correlation), where LL is liquid limit.
  • Secondary consolidation (creep) occurs after primary consolidation ceases; usually much smaller than primary settlement.
  • Total settlement = primary consolidation + secondary consolidation + immediate (elastic) settlement.

Key Definitions

Term

Compression Index (C_c)

Example

C_c = 0.30 means void ratio drops by 0.30 for every 10× increase in effective stress

Definition

Slope of the virgin consolidation curve (e vs. log σ') in the e–log σ' diagram for normally consolidated clay.

Term

Recompression Index (C_r)

Example

If C_c = 0.30, then C_r ≈ 0.03–0.06

Definition

Slope of the unload–reload curve (flatter than virgin) for overconsolidated clay; typically 0.1–0.2 × C_c.

Term

Normally Consolidated (NC) Clay

Example

Young clay deposits in river deltas; no glacial or tectonic unloading

Definition

Clay that has never been subjected to effective stress greater than the current overburden; current stress = maximum historical stress.

Term

Overconsolidated (OC) Clay

Example

Glacially overridden clays; heavily weathered deposits; desiccated surface clay

Definition

Clay that has experienced higher effective stress in the past; current stress < preconsolidation stress σ'_c due to erosion or unloading.

Term

Preconsolidation Pressure (σ'_c)

Example

Determined by Casagrande's graphical method or oedometer testing

Definition

The maximum effective stress to which clay has ever been subjected; stress at which e–log σ' curve changes from steep (recompression) to gentler (virgin).

Term

Void Ratio (e)

Example

e = 0.80 means 1 m³ of solids corresponds to 0.80 m³ of voids

Definition

Ratio of volume of voids to volume of solids; e = V_v / V_s.

Diagrams To Know

  • e–log σ' (consolidation) curve: virgin line (steep), recompression line (flat), kink at σ'_c
  • Oedometer test load increments: typical 50 kPa steps; plot e vs. log(stress); determine C_c and C_r graphically

Formulas

Formula

T_v = (c_v × t) / H_dr²

Meaning

T_v = dimensionless time factor (–); c_v = coefficient of consolidation (m²/yr or m²/s); t = elapsed time (yr or s); H_dr = longest drainage path (m)

Watch Out

Units must be consistent: if c_v in m²/yr, then t in yr; if c_v in m²/s, then t in s. Do NOT mix.

When To Use

Convert real time to time factor for use with U–T_v relationships

Formula

H_dr = H / 2 (double drainage, both top and bottom); H_dr = H (single drainage, one end only)

Meaning

H_dr = effective drainage path; double drainage halves the path, speeding consolidation 4×; H = total layer thickness

Watch Out

Double drainage (sand layer both top and bottom) ⟹ H_dr = H/2. Single drainage (impermeable base) ⟹ H_dr = H. Confusing these is a common exam error.

When To Use

Determine drainage path before calculating time factor

Formula

U ≤ 60%: T_v = (π/4) × U² (for fast consolidation approx.)

Meaning

U = degree of consolidation (%) = 0–60%; simplified relation valid in early stages

Watch Out

This is an APPROXIMATION. Use only if U ≤ 60%. Beyond 60%, use the exact table or iterative form.

When To Use

Quick calculation of T_v from U when U ≤ 60%

Formula

U > 60%: T_v = 1.781 − 0.933 × log₁₀(100 − U)

Meaning

U = degree of consolidation (%) = 60–99%; exact empirical relation for later stages

Watch Out

Use log₁₀ (base 10). Easy to confuse with the U ≤ 60% formula. Check which range U falls into.

When To Use

Calculate T_v when U > 60% or vice versa

Formula

t = (T_v × H_dr²) / c_v

Meaning

Solve for real time (yr or s) given T_v, c_v, and H_dr

Watch Out

Rearranged form of T_v equation; units must be consistent throughout

When To Use

Find elapsed time to reach a target degree of consolidation

Formula

U = S / S_∞ (or S_c / S_c∞, if referring to settlement)

Meaning

U = ratio of settlement (or excess pore pressure reduction) at time t to final (100%) settlement; always expressed as decimal or %

Watch Out

Ensure numerator and denominator use same units and time reference (e.g., don't mix settlement at different depths)

When To Use

Define degree of consolidation; sometimes settlement-based (S/S_c), sometimes pore-pressure based (Δu/Δu_0)

Common Values

Value

0.197

Symbol

T_v (U=50%)

Quantity

Time factor at 50% consolidation

Value

0.848

Symbol

T_v (U=90%)

Quantity

Time factor at 90% consolidation

Value

1–5 m²/yr

Symbol

c_v

Quantity

Coefficient of consolidation (typical clay)

Value

5–20 m²/yr

Symbol

c_v

Quantity

Coefficient of consolidation (typical silt)

Section Title

Time Rate of Consolidation

Important Facts

  • Settlement MAGNITUDE (S_c) is independent of c_v and time — it depends only on compression index and stress.
  • Settlement RATE (how fast S_c is reached) depends on c_v, drainage path, and layer thickness.
  • Doubling layer thickness (without changing c_v) increases time to reach same U by 4× (because H_dr² in denominator).
  • Double drainage cuts consolidation time to 1/4 compared to single drainage (H_dr halves, but H_dr² quarters the time).
  • T_v = 0.197 at U = 50%; T_v = 0.848 at U = 90% — these are anchor points for most board problems.
  • Coefficient of consolidation c_v is typically 0.5–10 m²/yr for clays; sandy silts are faster; pure clays are slower.
  • In very thick clay, consolidation may take decades; in thin clay (< 1 m), a few years to a decade.
  • High permeability ⟹ high c_v ⟹ fast consolidation; high compressibility ⟹ low c_v ⟹ slow consolidation.
  • Pore pressure dissipation and settlement are coupled; 50% pore pressure drop ≠ 50% settlement (nonlinear).

Key Definitions

Term

Degree of Consolidation (U)

Example

U = 50% means half the total settlement has occurred; U = 90% means 90% complete, only 10% remaining

Definition

Ratio of consolidation (settlement or excess pore pressure dissipation) achieved at time t to final consolidation; ranges 0–100%.

Term

Time Factor (T_v)

Example

T_v = 0.197 corresponds to U = 50%; T_v = 0.848 corresponds to U = 90%

Definition

Dimensionless group T_v = c_v t / H_dr² relating real time, soil properties, and drainage path; used to find U from charts/tables.

Term

Coefficient of Consolidation (c_v)

Example

High c_v (e.g., 10 m²/yr) ⟹ fast consolidation; low c_v (e.g., 0.5 m²/yr) ⟹ slow consolidation

Definition

Measure of soil's ability to drain and consolidate under load; c_v = k / (γ_w × m_v), where k = permeability, m_v = volume compressibility.

Term

Drainage Path (H_dr)

Example

2 m clay layer with sand above and below: H_dr = 1 m. Same layer with rock below: H_dr = 2 m

Definition

Longest distance water must travel to escape the clay layer; H/2 for double drainage (two permeable boundaries), H for single drainage (one permeable boundary).

Term

Primary Consolidation

Example

Takes months to years; 90% completion typically defines end of primary consolidation

Definition

Time-dependent settlement caused by gradual dissipation of excess pore water pressure and volume change of soil skeleton.

Diagrams To Know

  • U vs. T_v curve: S-shaped, slow start, rapid middle, asymptotic tail approaching 100%
  • T_v vs. time graphs for different H, c_v, and drainage configurations; importance of H_dr²

Formulas

Formula

σ'_c > σ'_0 + Δσ ⟹ ENTIRE loading range is OC; use C_r only

Meaning

If final stress stays below preconsolidation, clay behaves as OC throughout; only recompression occurs

Watch Out

Forgetting to check OCR (overconsolidation ratio) = σ'_c / σ'_0 before choosing index

When To Use

Check if clay is overconsolidated and whether loading stays in OC range

Formula

σ'_0 < σ'_c < σ'_0 + Δσ ⟹ TWO-STAGE: recompression (C_r) to σ'_c, then virgin (C_c) beyond

Meaning

Loading path crosses preconsolidation; split settlement into OC stage (C_r) and NC stage (C_c)

Watch Out

Must calculate TWO logarithmic terms, not one; easily confused with single-stage NC

When To Use

Most realistic OC clay scenario in practice

Formula

σ'_c ≤ σ'_0 ⟹ ENTIRE loading is NC (virgin compression); use C_c only

Meaning

Preconsolidation stress is already exceeded; all loading is on virgin curve

Watch Out

Easy to assume OC, but if σ'_c ≤ σ'_0, then it's effectively NC for this loading event

When To Use

NC clay or highly loaded OC clay; stress path entirely on steep portion of e–log σ' curve

Common Values

Value

1–2

Symbol

OCR

Quantity

OCR for lightly OC clay

Value

2–10

Symbol

OCR

Quantity

OCR for heavily OC clay (glaciated)

Section Title

NC vs. OC Clay — Settlement Calculation Strategy

Important Facts

  • NC clay: C_c ~ 0.30, settles ~150–300 mm per 100 kPa load over ~1 m layer.
  • OC clay: C_r ~ 0.03–0.06, settles ~15–30 mm per 100 kPa load over same layer (10× less).
  • Two-stage OC settlements are often split: ~5–10% from recompression, ~90–95% from virgin compression.
  • OCR decreases with depth (deeper clays are often more NC due to higher overburden history).
  • Determining C_c and C_r requires lab oedometer test or empirical correlations (C_c ≈ 0.009(LL − 10)).
  • OCR can be estimated from cone penetration or torvane tests; lab is most accurate.

Key Definitions

Term

Overconsolidation Ratio (OCR)

Example

OCR = 2 ⟹ clay was historically subjected to 2× current stress; settling slowly

Definition

Ratio OCR = σ'_c / σ'_0; OCR > 1 means clay is OC; OCR ≈ 1 means NC.

Diagrams To Know

  • Overlay of OC and NC curves on e–log σ' plot: showing kink at σ'_c and two-stage loading path

Formulas

Formula

Settlement equation summary: S_c = (C_* / (1 + e_0)) × H × log₁₀(σ'_f / σ'_0)

Meaning

C_* = C_c for NC or OC loading beyond σ'_c; C_* = C_r for OC loading below σ'_c; σ'_f = σ'_0 + Δσ

Watch Out

Numerator is C_*, NOT (C_c or C_r) — be clear on which applies

When To Use

Universal form; always start here and substitute appropriate C

Formula

Time to consolidation: t (yr) = (T_v × H_dr²) / c_v, where H_dr in m, c_v in m²/yr

Meaning

Key for all time-rate problems; T_v from U–T_v table or formulas

Watch Out

H_dr² is critical; single vs. double drainage changes answer by 4×

When To Use

Any problem asking 'how long until settlement reaches X% or how much settlement after Y years'

Formula

U lookup table: (50%, T_v=0.197), (60%, T_v≈0.286), (70%, T_v≈0.403), (80%, T_v≈0.567), (90%, T_v=0.848)

Meaning

Standard values from Terzaghi consolidation theory; memorize 50% and 90%

Watch Out

T_v is NOT linear with U; nonlinear curve; small errors at boundary (60%) can compound

When To Use

Exam problems often use these standard U values; saves time vs. solving formula

Common Values

Value

40–100 %

Symbol

LL

Quantity

Liquid limit (LL) for clay (typical)

Value

15–40 %

Symbol

PL

Quantity

Plastic limit (PL) for clay (typical)

Section Title

Quick Reference: Key Equations & Lookup Tables

Important Facts

  • All formulas use log₁₀ (base 10 logarithm) unless explicitly stated otherwise.
  • Settlement is typically expressed in mm; thickness H should be in mm for consistency.
  • Stress always in kPa in board problems (SI standard); watch for kN/m² (same as kPa).
  • Water unit weight γ_w = 9.81 kN/m³ ≈ 10 kN/m³ (if problem gives 'unit weight', check if total or effective).
  • Coefficient of consolidation c_v can be estimated from c_v = k / (γ_w × m_v) where m_v = compression modulus inverse.
  • Practical settlement limit: typical allowable = 50–100 mm; differential settlement = 25–50 mm (depends on structure type and RA 544 / NSCP 2015).

Formulas

Formula

S_secondary = C_α × H × log₁₀(t_2 / t_1)

Meaning

S_secondary = secondary (creep) settlement (mm); C_α = secondary compression index; H = layer thickness (mm); t_1, t_2 = times before and after interval

Watch Out

C_α is MUCH smaller than C_c (typically 0.01–0.05 × C_c); often overlooked in exams but can be significant over decades

When To Use

Estimate long-term creep settlement after primary consolidation (t > t_100% primary)

Formula

S_total = S_immediate + S_primary + S_secondary

Meaning

Total settlement = elastic (immediate) + consolidation (primary) + creep (secondary)

Watch Out

Secondary consolidation often neglected but can reach 20–30% of primary in organic clays; critical for long-term projects

When To Use

Final settlement prediction for design; not all three always significant

Formula

S_immediate ≈ (Δσ / E_s) × H (rough elastic estimate)

Meaning

Immediate settlement using modulus E_s or E_0; order-of-magnitude only

Watch Out

This is VERY approximate for saturated clays; more relevant for sands. Do not use without noting 'order-of-magnitude only'

When To Use

Quick check; not rigorous; more accurate methods exist (Schmertmann, Boussinesq)

Common Values

Value

0.001–0.010

Symbol

C_α

Quantity

Secondary compression index (inorganic clay)

Value

0.010–0.050

Symbol

C_α

Quantity

Secondary compression index (organic clay, peat)

Section Title

Secondary Consolidation & Total Settlement

Important Facts

  • Primary consolidation: excess pore pressure reduces to ~zero; typically 90–95% complete in 1–5 years for typical clay.
  • Secondary consolidation: excess pore pressure zero; soil continues to compress very slowly, rate proportional to log(time).
  • Secondary settlement often negligible in inorganic clays but significant (30–50% of primary) in organic clays and peats.
  • Total settlement includes immediate (elastic) + primary (consolidation) + secondary (creep); rarely all three are large.
  • Settlement rate slows dramatically after primary consolidation; most damage occurs during primary phase.

Key Definitions

Term

Secondary Compression Index (C_α)

Example

C_α ≈ 0.005 for typical clay; very small but cumulative over years

Definition

Slope of e vs. log t curve during secondary consolidation; measure of creep rate in clay after excess pore pressure dissipates.

Term

Secondary Consolidation (Creep)

Example

Organic clays and peats exhibit significant creep; inorganic clays show minor creep

Definition

Time-dependent volume change at constant effective stress; occurs after primary consolidation (excess pore pressure = 0).

Diagrams To Know

  • Settlement vs. log(time) curve: showing immediate jump, primary consolidation (curve), then secondary creep (linear on semi-log plot)

Must Remember

  • Settlement formula is S_c = (C_* / (1 + e_0)) × H × log₁₀(σ'_f / σ'_0); use C_c for NC/virgin, C_r for OC recompression.
  • Drainage path H_dr = H/2 (double) or H (single); halving H_dr cuts consolidation time by 4×; confusing these is a common exam error.
  • Time factor T_v = c_v × t / H_dr²; key pairs: T_v = 0.197 at U = 50%, T_v = 0.848 at U = 90%.
  • For U ≤ 60% use T_v = (π/4)U²; for U > 60% use T_v = 1.781 − 0.933 log₁₀(100 − U); pick the right branch.
  • NC clay has C_c ~ 0.20–0.50 (large); OC clay has C_r ~ 0.01–0.10 (small, ~0.1–0.2 × C_c); using wrong index gives 10× error.
  • Settlement MAGNITUDE depends ONLY on compression index, e_0, H, and stress ratio — NOT on c_v or time.
  • Settlement RATE depends on c_v, H_dr, and thickness; magnitude is independent of rate.
  • Two-stage OC settlement: recompression (C_r) from σ'_0 to σ'_c, then virgin (C_c) from σ'_c to σ'_f; do not forget either stage.
  • All logarithms in consolidation equations are log₁₀ (base 10), not natural log; easy mistake.
  • Effective stress σ' = total stress σ − pore pressure u; always use effective stress in settlement and time calculations, NOT total.

Last Minute Tips

  • In double-drainage problems, time reduces by 4×, not 2×. The drainage path is H/2, so (H/2)² = H²/4. Many students forget the square.
  • When loading an OC clay and the final stress exceeds σ'_c, split the calculation: first leg uses C_r, second leg uses C_c. Forgetting this is an instant 50% error.
  • T_v ≈ 0.197 at U = 50% and T_v ≈ 0.848 at U = 90%. If your problem uses different values, you chose the wrong formula or made a calculation error.
  • Always check units: c_v in m²/yr matches t in yr; c_v in m²/s matches t in s. Mixing units is a silent killer in time calculations.
  • If a problem does not explicitly state 'double drainage', assume SINGLE drainage (H_dr = H). Double drainage is special and usually mentioned.

Comparison Tables

Rows

Values

  • C_c (larger, ~0.20–0.50)
  • C_r (smaller, ~0.01–0.10) — until σ'_c is exceeded

Property

Compression Index Used

Values

  • Large (~100–300 mm per m)
  • Small (~10–30 mm per m) in OC range; increases sharply if σ'_c exceeded

Property

Settlement per 100 kPa Load

Values

  • Steep (virgin line); C_c is slope
  • Flat (recompression line); C_r is slope until kink at σ'_c

Property

e–log σ' Curve Slope

Values

  • Time factor same for given c_v and H_dr; no difference from OC in TIME RATE
  • Same TIME RATE (T_v) as NC; settlement MAGNITUDE is difference

Property

Consolidation Time

Values

  • σ'_c ≈ σ'_0 (current stress is max historical stress)
  • σ'_c > σ'_0 (clay experienced higher stress; now unloaded/eroded)

Property

History

Values

  • Young river deltas; marine clays; recent deposits
  • Glaciated regions; heavily weathered profiles; desiccated clays

Property

Typical Examples

Columns

  • Property
  • Normally Consolidated (NC)
  • Overconsolidated (OC)

Table Title

NC vs. OC Clay Settlement Behavior

Rows

Values

  • ~0.031
  • T_v ≈ (π/4)U² = 0.785 × 0.04 ≈ 0.031
  • Very early, rapid consolidation rate

Property

20%

Values

  • 0.197
  • T_v = (π/4) × 0.25 = 0.196 ≈ 0.197 ✓
  • HALF settlement reached; exam staple

Property

50%

Values

  • ~0.286
  • T_v ≈ 0.286 (transition; both formulas valid)
  • Boundary between approximation regimes

Property

60%

Values

  • ~0.403
  • T_v = 1.781 − 0.933 log(30) ≈ 0.404 ✓
  • 70% done; 30% remaining

Property

70%

Values

  • 0.848
  • T_v = 1.781 − 0.933 log(10) ≈ 0.849 ✓
  • PRACTICAL completion; exam staple

Property

90%

Values

  • ~1.781
  • T_v = 1.781 − 0.933 log(1) = 1.781 ✓
  • Near complete; takes very long time

Property

99%

Columns

  • Degree of Consolidation (U, %)
  • Time Factor (T_v)
  • Quick Approximation Formula
  • Settlement Progress

Table Title

Time Factor (T_v) vs. Degree of Consolidation (U) — Key Pairs

Rows

Values

  • H/2
  • Consolidation 4× faster (H_dr² in denominator)
  • 2 m clay layer → H_dr = 1 m; t(50%) halves vs. single

Property

Double drainage (sand above & below)

Values

  • H
  • Reference; baseline time
  • 2 m clay layer → H_dr = 2 m; baseline

Property

Single drainage (impermeable base)

Values

  • H/3 (or H/4 depending on layer configuration)
  • Consolidation 9× faster (for H/3)
  • Rarely considered; mostly academic

Property

Triple drainage (sand both sides + internal sand layer)

Columns

  • Drainage Configuration
  • H_dr
  • Time Factor Change
  • Example

Table Title

Drainage Path (H_dr) & Consolidation Time Scaling

Rows

Values

  • S_c = (C_c / (1 + e_0)) H log(σ'_f / σ'_0)
  • Is final stress > σ'_c? If yes, NC applies.
  • S_c in mm, H in mm, stresses in kPa

Property

Find settlement amount for NC clay

Values

  • S_c = (C_r / (1 + e_0)) H log(σ'_f / σ'_0)
  • Final stress ≤ σ'_c? Use C_r only.
  • S_c in mm, H in mm, stresses in kPa

Property

Find settlement for OC clay staying below σ'_c

Values

  • Split: S = S_c(recomp) + S_c(virgin); calculate each separately
  • σ'_0 < σ'_c < σ'_f? Calculate two log terms.
  • Two settlement calculations combined

Property

OC clay loading crosses σ'_c

Values

  • t = (T_v × H²) / c_v
  • Is it double drainage? If no, use H full thickness.
  • t in yr (if c_v in m²/yr); H in m

Property

Find time for degree U at single drainage

Values

  • t = (T_v × (H/2)²) / c_v = (T_v × H²) / (4 c_v)
  • Is it double drainage? If yes, use H/2.
  • Consolidation 4× faster; t in yr

Property

Find time for degree U at double drainage

Values

  • Calculate T_v = c_v t / H_dr²; look up U from T_v–U table or formula
  • Which U formula applies? Check T_v vs. 0.286
  • T_v dimensionless; then find U from table

Property

Find U given time and c_v

Columns

  • Scenario
  • Use This Formula
  • Key Check
  • Typical Units

Table Title

Common Board-Exam Formulas: When to Use

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