CEE42 Exam 1 Review: Soil Mechanics and Geotechnical Engineering

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Vocabulary practice cards covering fundamental soil mechanics concepts, phase relationships, weight-volume properties, soil classifications, compaction tests, and stress equations for CEE42 Exam 1.

Last updated 7:20 PM on 10/13/26
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33 Terms

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Liquid Limit (LLLL)

The boundary moisture content representing the transition of soil behavior from a plastic state to a liquid state.

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Plastic Limit (PLPL)

The boundary moisture content representing the transition of soil behavior between a semi-solid state and a plastic state.

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Plasticity Index (PIPI)

A measure of the plasticity of a soil, calculated as the numerical difference between the liquid limit and plastic limit.

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Water Content (ww)

The ratio of the weight or mass of water to the weight or mass of soil solids: w=WwWsw = \frac{W_w}{W_s} or w=MwMsw = \frac{M_w}{M_s}.

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Void Ratio (ee)

The ratio of the volume of voids to the volume of solids: e=VvVs=n1−ne = \frac{V_v}{V_s} = \frac{n}{1 - n}.

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Porosity (nn)

The ratio of the volume of voids to the total soil volume: n=VvVt=e1+en = \frac{V_v}{V_t} = \frac{e}{1 + e}.

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Specific Gravity (GsG_s)

The ratio of unit weight of solid particles to the unit weight of water at 4∘C4^\circ\text{C}: Gs=γsγ0G_s = \frac{\gamma_s}{\gamma_0} (where γ0=γw\gamma_0 = \gamma_w at 4∘C4^\circ\text{C}).

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Degree of Saturation (SS)

The ratio of the volume of water to the volume of voids: S=VwVvS = \frac{V_w}{V_v}.

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Phase Relationship: Gs⋅wG_s \cdot w

A fundamental soil mechanics relationship establishing that specific gravity multiplied by water content equals degree of saturation multiplied by void ratio: Gs⋅w=S⋅eG_s \cdot w = S \cdot e.

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Total Unit Weight (γt\gamma_t)

The total weight of a soil mass divided by its total volume: γt=WtVt\gamma_t = \frac{W_t}{V_t}.

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Saturated Unit Weight (γsat\gamma_{\text{sat}})

The total unit weight of a soil mass when its voids are fully filled with water: γsat=WtVt\gamma_{\text{sat}} = \frac{W_t}{V_t} when S=100%S = 100\%.

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Dry Unit Weight (γd\gamma_d)

The weight of soil solids divided by the total volume of the soil mass: γd=WsVt\gamma_d = \frac{W_s}{V_t}.

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Unit Weight of Solid (γs\gamma_s)

The weight of soil solids divided by the volume of solid particles: γs=WsVs\gamma_s = \frac{W_s}{V_s}.

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Unit Weight of Water (γw\gamma_w)

The weight of water per unit volume: γw=WwVw=62.4 pcf\gamma_w = \frac{W_w}{V_w} = 62.4\,\text{pcf}.

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Buoyant Unit Weight (γb\gamma_b or γ′\gamma')

The submerged unit weight of soil, defined as saturated unit weight minus the unit weight of water: γb=γ′=γsat−γw\gamma_b = \gamma' = \gamma_{\text{sat}} - \gamma_w.

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Total Density (‘‘pt’’ / ρt\rho_t)

The total mass of soil divided by its total volume: ρt=MtVt\rho_t = \frac{M_t}{V_t}.

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Saturated Density (‘‘psat’’ / ρsat\rho_{\text{sat}})

The density of soil when degree of saturation is complete: ρsat=MtVt\rho_{\text{sat}} = \frac{M_t}{V_t} when S=100%S = 100\%.

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Dry Density (‘‘pd’’ / ρd\rho_d)

The mass of soil solids divided by the total soil volume: ρd=MsVt\rho_d = \frac{M_s}{V_t}.

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Density of Solid (‘‘ps’’ / ρs\rho_s)

The mass of soil solids divided by the volume of solid particles: ρs=MsVs\rho_s = \frac{M_s}{V_s}.

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Density of Water (‘‘pw’’ / ρw\rho_w)

The mass of water divided by its volume: ρw=MwVw=1000 kg/m3\rho_w = \frac{M_w}{V_w} = 1000\,\text{kg/m}^3.

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G Soil Classification

Gravel classifications consisting of GW (well graded gravel), GP (poorly graded gravel), GM (silty gravel), and GC (clayey gravel).

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S Soil Classification

Sand classifications consisting of SW (well-graded sand), SP (poorly graded sand), SM (silty sand), and SC (clayey sand).

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C Soil Classification

Clay classifications consisting of CL (lean clay) and CH (fat clay).

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M Soil Classification

Silt classifications consisting of ML (silt) and MH (elastic silt).

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O Soil Classification

Organic soil classifications consisting of OL (organic silt/clay) and OH (organic clay/silt).

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P Soil Classification

Peat soil classification designated as PT (peat).

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Standard Penetration Test (SPT)

An in-situ geotechnical test that determines soil bearing capacity and evaluates soil density and consistency.

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Darcy's Equation

The hydraulic flow law expressed as Q=k⋅i⋅A=k(ΔhtL)AQ = k \cdot i \cdot A = k \left(\frac{\Delta h_t}{L}\right) A and q=QA=k(ΔhtL)q = \frac{Q}{A} = k \left(\frac{\Delta h_t}{L}\right).

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Standard Proctor Test (ASTM D698)

A laboratory soil compaction test performed using a 5.5 lb5.5\,\text{lb} rammer compacted in 33 layers.

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Modified Proctor Test (ASTM D1557)

A laboratory soil compaction test performed using a 10 lb10\,\text{lb} rammer compacted in 55 layers.

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Proctor Test Purpose

A laboratory compaction method used to determine a soil's maximum dry density and optimum moisture content.

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Specific Surface

The geometric ratio of soil particle surface area to its unit volume (surface area/unit volume\text{surface area} / \text{unit volume}).

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Total Stress

The overall stress within a soil mass, calculated as the sum of effective stress and pore water pressure: σ=σ′+u\sigma = \sigma' + u.