PE Civil (NCEES Principles and Practice of Engineering) — All Questions
409 questions
Which soil type generally has the highest hydraulic conductivity (permeability)?
- a.Clay
- b.Gravel✓
- c.Silt
- d.Silty clay
Gravel has the highest hydraulic conductivity because its large, well-connected pore spaces let water flow freely. Clay has the lowest permeability (often 10^-9 m/s or less) owing to its tiny pores, which is why clays act as aquitards and consolidate slowly.
According to Terzaghi's principle, the shear strength and volume change of a saturated soil are governed by which stress?
- a.Pore water pressure alone
- b.Total unit weight
- c.Total stress
- d.Effective stress✓
Terzaghi's principle states that effective stress (sigma' = sigma - u) controls the strength and deformation of soil, because only the grain-to-grain contact stress mobilizes friction. This is why raising pore pressure (lowering sigma') can trigger failure.
Using the Mohr-Coulomb criterion, what is the shear strength of a soil with c = 10 kPa and phi = 30 degrees on a plane where the effective normal stress is 100 kPa?
- a.100 kPa
- b.77 kPa
- c.57.7 kPa
- d.67.7 kPa✓
Mohr-Coulomb: tau_f = c + sigma'·tan(phi) = 10 + 100 x tan(30) = 10 + 100 x 0.577 = 67.7 kPa. Shear strength combines a cohesion intercept with a frictional component that grows with effective normal stress.
A cohesionless sand (c = 0) has phi = 32 degrees. What is its shear strength on a plane where the effective normal stress is 150 kPa?
- a.93.7 kPa✓
- b.150 kPa
- c.75 kPa
- d.120 kPa
With c = 0, tau_f = sigma'·tan(phi) = 150 x tan(32) = 150 x 0.625 = 93.7 kPa. In cohesionless soil the shear strength is purely frictional and rises linearly with effective normal stress, passing through the origin.
In a total-stress (phi = 0) analysis of saturated clay under undrained loading, the shear strength is taken as which quantity?
- a.c + sigma·tan(phi) with phi = 30 degrees
- b.Always zero
- c.The undrained cohesion cu (constant)✓
- d.sigma·tan(phi)
Under undrained conditions saturated clay is analyzed with phi = 0, so its shear strength equals the constant undrained cohesion cu (half the unconfined compressive strength). Because no drainage occurs, strength does not increase with applied total stress in the short term.
In one-dimensional consolidation theory, what time factor Tv corresponds to 50% average degree of consolidation?
- a.0.848
- b.0.5
- c.0.197✓
- d.1.0
For 50% consolidation the dimensionless time factor is Tv = 0.197. (90% corresponds to Tv = 0.848.) These standard values from Terzaghi's consolidation solution let you convert between degree of consolidation and elapsed time.
If the drainage path length of a consolidating clay layer is doubled, the time required to reach a given degree of consolidation changes by what factor?
- a.4 times✓
- b.Unchanged
- c.2 times
- d.Half
From Tv = cv·t/H_dr^2, for a fixed Tv the time is proportional to the square of the drainage path: t is proportional to H_dr^2. Doubling H_dr multiplies the time by 4. This is why sand drains (shortening the drainage path) dramatically speed consolidation.
The Standard Penetration Test (SPT) N-value in sand correlates most directly with which soil property?
- a.Plasticity index
- b.Hydraulic conductivity
- c.Relative density and friction angle✓
- d.Organic content
The SPT blow count N reflects the relative density of granular soil, which in turn correlates with the friction angle and bearing capacity of sands. Correlations (with energy and overburden corrections to N60 and (N1)60) are widely used for foundation design in sand.
In bearing capacity theory, what is the value of the factor Nc for a soil with a friction angle of zero (saturated clay, undrained)?
- a.5.14✓
- b.1.0
- c.9.0
- d.0
For phi = 0 the bearing capacity factor Nc = 5.14 (equal to 2 + pi) for a strip footing, from Prandtl's plasticity solution. This underlies the undrained bearing capacity q_ult = 5.14·cu (plus surcharge) for saturated clay.
A deep (pile) foundation is generally selected instead of a shallow footing when:
- a.It is always cheaper than a footing
- b.The structure carries only light loads
- c.It is never structurally justified
- d.Near-surface soils are weak and load must be transferred to deeper competent strata✓
Deep foundations are used when the shallow soils are too weak or compressible to support the loads at acceptable settlement, so piles or drilled shafts carry the load down to firmer strata through end bearing and skin friction. They cost more, so they are chosen when shallow foundations are inadequate.
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An open channel is rectangular, 3 m wide, flowing at a depth of 1.0 m, with Manning n = 0.013 and a bed slope of 0.0016. Using Manning's equation (SI), what is the mean flow velocity?
- a.3.08 m/s
- b.0.088 m/s
- c.1.10 m/s
- d.2.19 m/s✓
Manning (SI): V = (1/n)·R^(2/3)·S^(1/2). Area A = 3(1) = 3 m^2, wetted perimeter P = 3 + 2(1) = 5 m, so hydraulic radius R = A/P = 0.6 m. V = (1/0.013)(0.6^0.667)(0.0016^0.5) = 2.19 m/s. Using R = depth (1 m) gives the wrong 3.08; using S instead of sqrt(S) gives 0.088.
For the same rectangular channel (3 m wide, depth 1.0 m) flowing at a mean velocity of 2.19 m/s, what is the discharge?
- a.3.29 m^3/s
- b.2.19 m^3/s
- c.6.57 m^3/s✓
- d.10.95 m^3/s
Continuity: Q = V·A. The flow area is A = b·y = 3 x 1.0 = 3 m^2, so Q = 2.19 x 3 = 6.57 m^3/s. Discharge is velocity times cross-sectional area, not velocity alone.
A circular pipe of diameter 0.6 m flows completely full. What is its hydraulic radius?
- a.0.3 m
- b.0.075 m
- c.0.15 m✓
- d.0.6 m
For a full circular pipe, R = A/P = (piD^2/4)/(piD) = D/4 = 0.6/4 = 0.15 m. A common error is to use the diameter (0.6) or radius (0.3) directly; the hydraulic radius of a full circle is one-quarter of the diameter.
A rectangular open channel is 4 m wide and flows at a depth of 1.5 m. What is the hydraulic radius?
- a.0.857 m✓
- b.0.667 m
- c.4 m
- d.1.5 m
R = A/P. Area A = 4 x 1.5 = 6 m^2; wetted perimeter (bed plus two sides) P = 4 + 2(1.5) = 7 m; R = 6/7 = 0.857 m. The hydraulic radius uses the wetted perimeter, not the flow depth or width alone.
Using the Rational Method, what is the peak runoff from a 12-acre watershed with runoff coefficient C = 0.7 and a design rainfall intensity of 2.5 in/hr?
- a.30 cfs
- b.14.7 cfs
- c.21 cfs✓
- d.4.29 cfs
Rational Method: Q = C·i·A, with i in in/hr and A in acres yielding Q in cfs (conversion factor ~1). Q = 0.7 x 2.5 x 12 = 21 cfs. The method applies to small drainage areas where the storm can cover the whole basin.
A watershed has 5 acres of pavement (C = 0.9) and 15 acres of lawn (C = 0.3). What is the area-weighted composite runoff coefficient?
- a.0.90
- b.0.60
- c.0.45✓
- d.0.30
The composite coefficient is area-weighted: C = (5(0.9) + 15(0.3))/(5 + 15) = (4.5 + 4.5)/20 = 0.45. Averaging the two C values without weighting by area (0.60) is the common mistake.
Water flows in a channel at 3.0 m/s with a depth of 0.5 m. What is the Froude number?
- a.1.35✓
- b.0.61
- c.0.45
- d.2.72
Froude number Fr = V/sqrt(g·y) = 3.0/sqrt(9.81 x 0.5) = 3.0/2.215 = 1.35. The Froude number is the ratio of inertial to gravitational forces and classifies open-channel flow regime.
For flow with a Froude number of 1.35, the flow regime is best described as:
- a.critical
- b.subcritical
- c.tranquil
- d.supercritical✓
When Fr > 1 the flow is supercritical (rapid, shallow, high velocity); Fr < 1 is subcritical (tranquil); Fr = 1 is critical. A Froude number of 1.35 exceeds 1, so the flow is supercritical.
A rectangular channel 3 m wide carries 6 m^3/s. What is the critical depth?
- a.0.204 m
- b.1.13 m
- c.0.408 m
- d.0.742 m✓
Critical depth for a rectangular channel: yc = (q^2/g)^(1/3), where unit discharge q = Q/b = 6/3 = 2 m^2/s. yc = (2^2/9.81)^(1/3) = (0.408)^(1/3) = 0.742 m. At critical depth the specific energy is minimum.
Open-channel flow has a depth of 1.2 m and a velocity of 2.0 m/s. What is the specific energy?
- a.0.204 m
- b.1.20 m
- c.2.24 m
- d.1.40 m✓
Specific energy E = y + V^2/(2g) = 1.2 + (2.0^2)/(2 x 9.81) = 1.2 + 0.204 = 1.404 m. Specific energy is the energy head measured relative to the channel bottom.
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Water flows through a 0.2-m-diameter pipe, 100 m long, at 2.0 m/s. With a Darcy friction factor f = 0.02, what is the friction head loss?
- a.10.2 m
- b.2.04 m✓
- c.4.08 m
- d.0.20 m
Darcy-Weisbach: h_f = f(L/D)(V^2/2g) = 0.02(100/0.2)(2.0^2/(2 x 9.81)) = 0.02 x 500 x 0.204 = 2.04 m. Head loss grows with the square of velocity.
Water (kinematic viscosity 1x10^-6 m^2/s) flows at 2.0 m/s in a 0.2-m pipe. What is the Reynolds number?
- a.400,000✓
- b.40,000
- c.4,000,000
- d.200,000
Re = V·D/nu = (2.0 x 0.2)/(1x10^-6) = 400,000. The Reynolds number is the ratio of inertial to viscous forces and sets the flow regime.
For pipe flow with a Reynolds number of 400,000, the flow is:
- a.turbulent✓
- b.transitional
- c.laminar
- d.critical
In pipe flow, Re < 2,000 is laminar, 2,000-4,000 transitional, and Re > 4,000 turbulent. A Reynolds number of 400,000 is well into the turbulent range.
A pump lifts 0.05 m^3/s of water against a total head of 20 m. What is the water (hydraulic) power delivered to the fluid?
- a.98.1 kW
- b.1.0 kW
- c.9.81 kW✓
- d.19.6 kW
Water power P = gamma·Q·H = 9,810 N/m^3 x 0.05 m^3/s x 20 m = 9,810 W = 9.81 kW. This is the power added to the water; the required brake/shaft power is larger by the pump efficiency.
A pump must deliver 9.81 kW of water power. If the pump efficiency is 75%, what brake (shaft) power is required?
- a.7.36 kW
- b.13.1 kW✓
- c.9.81 kW
- d.12.3 kW
Brake power = water power / efficiency = 9.81/0.75 = 13.1 kW. Efficiency losses mean the motor must supply more than the useful hydraulic power; multiplying by efficiency (7.36) is the common error.
A rectangular sharp-crested weir 3 m long has a head of 0.4 m over the crest. Using Q = 1.84·L·H^(3/2) (SI), what is the discharge?
- a.0.88 m^3/s
- b.1.40 m^3/s✓
- c.3.49 m^3/s
- d.2.21 m^3/s
Rectangular weir: Q = 1.84·L·H^(3/2) = 1.84 x 3 x 0.4^1.5 = 1.84 x 3 x 0.253 = 1.40 m^3/s. Head is raised to the 3/2 power, so weir flow is quite sensitive to head.
A 90-degree V-notch weir has a head of 0.3 m. Using Q = 1.38·H^(5/2) (SI), what is the discharge?
- a.0.068 m^3/s✓
- b.0.124 m^3/s
- c.0.152 m^3/s
- d.0.041 m^3/s
For a 90-degree V-notch weir, Q = 1.38·H^(5/2) = 1.38 x 0.3^2.5 = 1.38 x 0.0493 = 0.068 m^3/s. The triangular notch gives good accuracy at low flows because the exponent on head is 5/2.
Water discharges through a sharp-edged orifice of area 0.01 m^2 under a head of 3 m, with discharge coefficient Cd = 0.6. What is the discharge?
- a.0.077 m^3/s
- b.0.023 m^3/s
- c.0.046 m^3/s✓
- d.0.092 m^3/s
Orifice discharge: Q = Cd·A·sqrt(2gh) = 0.6 x 0.01 x sqrt(2 x 9.81 x 3) = 0.6 x 0.01 x 7.67 = 0.046 m^3/s. Omitting Cd (using 1.0) overestimates the flow at 0.077.
Water flows freely from an orifice under a head of 5 m. Neglecting losses, what is the theoretical jet velocity?
- a.98.1 m/s
- b.9.90 m/s✓
- c.7.00 m/s
- d.49.1 m/s
Torricelli's theorem: V = sqrt(2gh) = sqrt(2 x 9.81 x 5) = sqrt(98.1) = 9.90 m/s. The jet velocity equals that of a body freely falling through the same head.
What is the gauge pressure at a depth of 8 m below the surface of still water?
- a.157 kPa
- b.78.5 kPa✓
- c.784 kPa
- d.8 kPa
Hydrostatic pressure p = gamma·h = 9.81 kN/m^3 x 8 m = 78.5 kPa. Pressure increases linearly with depth in a static fluid.
A vertical rectangular gate 2 m wide and 3 m tall has its top edge at the water surface. What is the total hydrostatic force on the gate?
- a.58.9 kN
- b.29.4 kN
- c.176.6 kN
- d.88.3 kN✓
F = gamma·h_c·A, where h_c is the depth to the centroid. h_c = 3/2 = 1.5 m, A = 2 x 3 = 6 m^2. F = 9.81 x 1.5 x 6 = 88.3 kN. The pressure at the centroid times the area gives the resultant force.
For that same gate (2 m wide, 3 m tall, top at the surface), at what depth below the water surface does the resultant hydrostatic force act?
- a.2.0 m✓
- b.2.5 m
- c.1.5 m
- d.1.0 m
For a surface-piercing vertical plane, the pressure distribution is triangular, so the resultant (center of pressure) acts at two-thirds of the depth: 2/3 x 3 = 2.0 m below the surface. It lies below the centroid (1.5 m) because pressure is greater lower down.
A submerged object displaces 0.02 m^3 of water. What is the buoyant force on it?
- a.98.1 N
- b.196 N✓
- c.392 N
- d.20 N
Archimedes' principle: buoyant force = weight of displaced fluid = gamma·V = 9,810 N/m^3 x 0.02 m^3 = 196 N. Buoyancy depends only on the displaced volume and fluid unit weight.
Groundwater flows through an aquifer with hydraulic conductivity k = 0.001 m/s under a hydraulic gradient of 0.02 through a cross-sectional area of 10 m^2. What is the discharge (Darcy's law)?
- a.0.02 m^3/s
- b.0.0002 m^3/s✓
- c.0.001 m^3/s
- d.0.002 m^3/s
Darcy's law: Q = k·i·A = 0.001 x 0.02 x 10 = 0.0002 m^3/s. Flow through porous media is proportional to hydraulic conductivity, gradient, and area.
For the aquifer above (Darcy velocity = k·i = 2x10^-5 m/s) with a porosity of 0.25, what is the seepage (pore) velocity?
- a.5.0x10^-6 m/s
- b.3.2x10^-4 m/s
- c.8.0x10^-5 m/s✓
- d.2.0x10^-5 m/s
Seepage velocity vs = v_Darcy / porosity = (2x10^-5)/0.25 = 8x10^-5 m/s. Water moves only through the pore space, so the actual particle velocity exceeds the Darcy (bulk) velocity.
A tank with a volume of 500 m^3 receives a steady flow of 100 m^3/hr. What is the hydraulic detention (retention) time?
- a.0.2 hr
- b.50 hr
- c.5 hr✓
- d.2.5 hr
Hydraulic detention time = Volume / Flow rate = 500/100 = 5 hr. It represents the average time a parcel of water resides in the tank, a key parameter for sedimentation and disinfection.
A circular clarifier with a surface area of 100 m^2 treats 2,000 m^3/day. What is the surface overflow rate?
- a.2000 m/day
- b.5 m/day
- c.200 m/day
- d.20 m/day✓
Surface overflow rate = Q / surface area = 2,000/100 = 20 m/day (equivalently m^3/m^2/day). It is the design settling velocity: particles with a settling velocity above this rate are removed.
A sedimentation basin discharges 4,000 m^3/day over an effluent weir 50 m long. What is the weir loading rate?
- a.50 m^3/m/day
- b.80 m^3/m/day✓
- c.200 m^3/m/day
- d.4000 m^3/m/day
Weir loading rate = Q / weir length = 4,000/50 = 80 m^3/m/day. Keeping this rate low limits the approach velocity near the weir and prevents carryover of settled solids.
A water plant treats 5,000 m^3/day and must apply a chlorine dose of 3 mg/L. What is the chlorine feed rate?
- a.15 kg/day✓
- b.150 kg/day
- c.3 kg/day
- d.1.5 kg/day
Mass rate = dose x flow = 3 g/m^3 x 5,000 m^3/day = 15,000 g/day = 15 kg/day (using 1 mg/L = 1 g/m^3). Chemical feed is the product of concentration and volumetric flow.
A treatment plant reduces BOD from 250 mg/L to 25 mg/L. What is the BOD removal efficiency?
- a.90%✓
- b.80%
- c.10%
- d.75%
Removal efficiency = (influent - effluent)/influent x 100 = (250 - 25)/250 = 90%. This is a standard measure of process performance for BOD, TSS, and similar constituents.
Wastewater flows at 1,000 m^3/day with a BOD of 200 mg/L. What is the BOD mass loading?
- a.200 g/day
- b.2000 kg/day
- c.200 kg/day✓
- d.20 kg/day
Mass load = concentration x flow = 200 g/m^3 x 1,000 m^3/day = 200,000 g/day = 200 kg/day. Loading (mass/time) drives process sizing, whereas concentration alone does not.
100 m^3 of water at 200 mg/L chloride is blended with 300 m^3 at 40 mg/L. What is the resulting concentration?
- a.100 mg/L
- b.80 mg/L✓
- c.240 mg/L
- d.120 mg/L
Mass balance: C = (100(200) + 300(40))/(100 + 300) = (20,000 + 12,000)/400 = 80 mg/L. The mixed concentration is the flow-weighted average, not the simple average (120).
A reservoir has an inflow of 10 m^3/s and an outflow of 6 m^3/s held steady for 1 hour. What is the change in storage?
- a.14,400 m^3✓
- b.57,600 m^3
- c.4 m^3
- d.3,600 m^3
Continuity (storage) equation: dS = (I - O)·t = (10 - 6) m^3/s x 3,600 s = 14,400 m^3. Storage rises when inflow exceeds outflow; this is the basis of reservoir/detention routing.
In hydrograph analysis, a unit hydrograph represents the direct runoff resulting from:
- a.the peak discharge of any storm
- b.the baseflow component of streamflow
- c.one unit depth of excess (effective) rainfall applied uniformly over the watershed✓
- d.the total rainfall depth of a storm
A unit hydrograph is the direct-runoff response to one unit (1 in or 1 cm) of excess rainfall distributed uniformly over the basin during a specified duration. It is a linear, time-invariant transfer function used to build storm hydrographs by superposition.
Overland runoff travels 300 m to the outlet at an average velocity of 0.5 m/s. What is the travel (time of concentration) for this flow path?
- a.5 min
- b.10 min✓
- c.600 min
- d.150 min
Travel time = length / velocity = 300/0.5 = 600 s = 10 min. The time of concentration is the sum of such travel times along the longest hydraulic path and sets the design storm duration in the Rational Method.
According to typical intensity-duration-frequency relationships, as the storm duration increases for a fixed return period, the average rainfall intensity:
- a.stays constant
- b.increases
- c.doubles
- d.decreases✓
For a given return period, longer-duration storms have lower average intensity: intense bursts cannot be sustained as long. This inverse relationship is captured by IDF curves used in drainage design.
A drainage structure is designed for a 25-year return period. What is the probability that a storm of this magnitude is equaled or exceeded in any single year?
- a.25%
- b.4%✓
- c.0.4%
- d.2.5%
Annual exceedance probability = 1/T = 1/25 = 0.04 = 4%. The return period is the reciprocal of the annual probability, not a guarantee of timing.
A levee is designed for a 100-year flood. What is the risk that this flood is equaled or exceeded at least once during a 2-year period?
- a.2.0%✓
- b.50%
- c.1.0%
- d.0.5%
Risk of at least one exceedance R = 1 - (1 - 1/T)^n = 1 - (1 - 0.01)^2 = 1 - 0.9801 = 0.0199, about 2.0%. The annual exceedance probability is 1/T = 1%; the multi-year risk uses the complement of no exceedance, not the return period alone.
In fully developed laminar pipe flow with a Reynolds number of 1,000, what is the Darcy friction factor?
- a.0.064✓
- b.0.032
- c.0.02
- d.0.016
For laminar flow, f = 64/Re = 64/1,000 = 0.064. In the laminar regime the friction factor depends only on Reynolds number, independent of pipe roughness.
Water flows at 2.0 m/s in a 0.30-m pipe that reduces to a 0.15-m pipe. By continuity, what is the velocity in the smaller pipe?
- a.4 m/s
- b.1 m/s
- c.8 m/s✓
- d.2 m/s
Continuity: A1V1 = A2V2. Since area scales with diameter squared, V2 = V1(D1/D2)^2 = 2.0 x (0.30/0.15)^2 = 2.0 x 4 = 8 m/s. Halving the diameter quadruples the velocity.