Open Channel Hydraulics Study Guide

PE Water Resources Depth (PM) Exam Preparation

5 Exam Questions Water Resources Depth (PM)

Overview

PE depth exam study guide for open channel hydraulics: Manning's equation, critical depth, specific energy, hydraulic jump, gradually varied flow, and weir/orifice flow.

This topic accounts for 5 out of 40 questions on the PE Civil Water Resources Depth (PM) exam.

Key Concepts

Normal Depth and Manning's Equation

Normal depth occurs when gravity and friction forces balance (uniform flow). V = (1.486/n) x R^(2/3) x S^(1/2). For a given Q, n, S, and channel geometry, solve iteratively for normal depth. Trapezoidal: A = (b + zy)y, P = b + 2y*sqrt(1+z^2). Circular: use geometric tables for partial flow.

Critical Depth and Specific Energy

Critical depth: Fr = 1. For rectangular channels: yc = (q^2/g)^(1/3) where q = Q/b. Specific energy: E = y + V^2/(2g) = y + Q^2/(2gA^2). At critical depth, specific energy is minimum. Alternating depths (same E): subcritical (y > yc) and supercritical (y < yc) are conjugate depths on the E-y curve.

Hydraulic Jump

Occurs when supercritical flow transitions to subcritical. Conjugate depth: y2/y1 = 0.5(-1 + sqrt(1 + 8Fr1^2)). Energy loss: deltaE = (y2-y1)^3/(4y1y2). Momentum equation: used for force analysis on structures. Hydraulic jumps dissipate energy and are used in stilling basins downstream of spillways.

Weir and Orifice Flow

Sharp-crested rectangular weir: Q = Cd x (2/3) x sqrt(2g) x L x H^(3/2). Typical Cd = 0.62. V-notch weir: Q = Cd x (8/15) x sqrt(2g) x tan(theta/2) x H^(5/2). Broad-crested weir: Q = Cd x L x sqrt(g) x (2H/3)^(3/2). Orifice: Q = Cd x A x sqrt(2gH), Cd typically 0.61. Submerged orifice: use difference in head.

Common Exam Question Types

Exam Tips & Strategies

Normal depth: use Manning's and iterate. Critical depth for rectangular: yc = (q^2/g)^(1/3)
Froude number < 1 is subcritical (deep, slow), > 1 is supercritical (shallow, fast)
Weir discharge: sharp-crested uses H^(3/2), V-notch uses H^(5/2)
Hydraulic jump always goes from supercritical to subcritical (y1 < yc < y2)

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