- Chapter 1: Introduction
- Chapter 1.2: Dimensions, Dimensional Homogeneity, and Units
- Chapter 1.4: Measures of Fluid Mass and Weight
- Chapter 1.5: Ideal Gas Law
- Chapter 1.6: Viscosity (also see Lab Problems 1.1LP and 1.2LP)
- Chapter 1.7: Compressibility of Fluids
- Chapter 1.8: Vapor Pressure
- Chapter 1.9: Surface Tension
- Chapter 10: Open-Channel Flow
- Chapter 10.2: Surface Waves
- Chapter 10.3: Energy Considerations
- Chapter 10.4.2: The Manning Equation
- Chapter 10.4.3: Uniform FlowDetermine Flowrate
- Chapter 10.5: Gradually Varied Flow
- Chapter 10.6.1: The Hydraulic Jump
- Chapter 10.6.2, 3: Sharp-Crested and Broad-Crested Weirs
- Chapter 10.6.4: Underflow (Sluice) Gates
- Chapter 11: Compressible Flow
- Chapter 11.1: Ideal Gas Thermodynamics
- Chapter 11.2: Stagnation Properties
- Chapter 11.3: Mach Number and Speed of Sound
- Chapter 11.4: Subsonic and Supersonic Flow
- Chapter 11.5: Shock Waves
- Chapter 11.6: Isentropic Flow
- Chapter 11.7: One Dimensional Flow in a Variable Area Duct
- Chapter 11.8: Constant Area Duct Flow with Friction
- Chapter 11.9: Frictionless Flow in a Constant Area Duct with Heating or Cooling
- Chapter 12: Turbomachines
- Chapter 12.1: Introduction and Section 12.2 Basic Energy Considerations
- Chapter 12.4: The Centrifugal Pump and Section 12.4.1 Theoretical Considerations
- Chapter 12.4.2: Pump Performance Characteristics
- Chapter 12.4.3: Net Positive Suction Head (NPSH)
- Chapter 12.4.4: System Characteristics and Pump Selection
- Chapter 12.5: Dimensionless Parameters and Similarity Laws
- Chapter 12.6: Axial-Flow and Mixed-Flow Pumps
- Chapter 12.7: Fans
- Chapter 12.8: Turbines (also see Sec. 12.3)
- Chapter 12.9: Compressible Flow Turbomachines
- Chapter 2: Fluid Statics
- Chapter 2.10: Hydrostatic Force on a Curved Surface
- Chapter 2.11: Buoyancy, Flotation, and Stability
- Chapter 2.12: Pressure Variation in a Fluid with Rigid-Body Motion
- Chapter 2.3: Pressure Variation in a Fluid at Rest
- Chapter 2.4: Standard Atmosphere
- Chapter 2.5: Measurement of Pressure
- Chapter 2.6: Manometry
- Chapter 2.8: Hydrostatic Force on a Plane Surface
- Chapter 3: Elementary Fluid Dynamics The Bernoulli Equation
- Chapter 3.2: F = ma along a Streamline
- Chapter 3.3: F = ma Normal to a Streamline
- Chapter 3.5: Static, Stagnation, Dynamic, and Total Pressure
- Chapter 3.6.1: Free Jets
- Chapter 3.6.2: Confined Flows
- Chapter 3.6.3: Flowrate Measurement
- Chapter 3.7: The Energy Line and the Hydraulic Grade Line
- Chapter 3.8: Restrictions on Use of the Bernoulli Equation
- Chapter 4: Fluid Kinematics
- Chapter 4.1: The Velocity Field
- Chapter 4.2: The Acceleration Field
- Chapter 4.2.1: The Material Derivative
- Chapter 4.4: The Reynolds Transport Theorem
- Chapter 5: Finite Control Volume Analysis
- Chapter 5.1.1: Derivation of the Continuity Equation
- Chapter 5.1.2: Fixed, Nondeforming Control Volume Uniform Velocity Profile or Average Velocity
- Chapter 5.1.3: Moving, Nondeforming Control Volume
- Chapter 5.1.4: Deforming Control Volume
- Chapter 5.2.1: Derivation of the Linear Momentum Equation
- Chapter 5.2.2: Application of the Linear Momentum Equation (also see Lab Problems 5.1LP, 5.2LP, 5.3LP, and 5.4LP)
- Chapter 5.2.3: Derivation of the Moment-of-Momentum Equation
- Chapter 5.2.4: Application of the Moment-of-Momentum Equation
- Chapter 5.3.1: Derivation of the Energy Equation
- Chapter 5.3.2: Application of the Energy EquationNo Shaft Work and Section 5.3.3 The Mechanical Energy Equation and the Bernoulli Equation
- Chapter 5.3.3: Application of the Energy Equation and the Bernoulli EquationCombined with Linear Momentum
- Chapter 5.3.4: Application of the Energy Equation to Nonuniform Flows
- Chapter 5.3.5: Combination of the Energy Equation and the Moment-of-Momentum Equation
- Chapter 6: Differential Analysis of Fluid Flow
- Chapter 6.1: Fluid Element Kinematics
- Chapter 6.10: Other Aspects of Differential Analysis
- Chapter 6.2: Conservation of Mass
- Chapter 6.3: The Linear Momentum Equation
- Chapter 6.4: Inviscid Flow
- Chapter 6.5: Some Basic, Plane Potential Flows
- Chapter 6.6: Superposition of Basic, Plane Potential Flows
- Chapter 6.8: Viscous Flow
- Chapter 6.9.1: Steady, Laminar Flow between Fixed Parallel Plates
- Chapter 6.9.2: Couette Flow
- Chapter 6.9.3: Steady, Laminar Flow in Circular Tubes
- Chapter 6.9.4: Steady, Axial, Laminar Flow in an Annulus
- Chapter 7: Dimensional Analysis, Similitude, and Modeling
- Chapter 7.1: Dimensional Analysis
- Chapter 7.10: Similitude Based on Governing Differential Equations
- Chapter 7.3: Determination of Pi Terms
- Chapter 7.5: Determination of Pi Terms by Inspection
- Chapter 7.6: Common Dimensionless Groups in Fluid Mechanics
- Chapter 7.7: Correlation of Experimental Data
- Chapter 7.8: Modeling and Similitude
- Chapter 7.9: Some Typical Model Studies
- Chapter 8: Viscous Flow in Pipes
- Chapter 8.1: General Characteristics of Pipe Flow
- Chapter 8.2: Fully Developed Laminar Flow
- Chapter 8.3: Fully Developed Turbulent Flow
- Chapter 8.4.1.: Major Losses
- Chapter 8.4.2: Minor Losses
- Chapter 8.4.3: Noncircular Conduits
- Chapter 8.5.1: Single PipesDetermine Pressure Drop
- Chapter 8.5.2: Multiple Pipe Systems
- Chapter 8.6: Pipe Flowrate Measurement
- Chapter 9: Flow over Immersed Bodies
- Chapter 9.1: General External Flow Characteristics
- Chapter 9.2: Boundary Layer Characteristics
- Chapter 9.3: Drag
- Chapter 9.4: Lift
Fundamentals of Fluid Mechanics 8th Edition - Solutions by Chapter
Full solutions for Fundamentals of Fluid Mechanics | 8th Edition
Active continental margin
Usually narrow and consisting of highly deformed sediments. They occur where oceanic lithosphere is being subducted beneath the margin of a continent.
A fan-shaped deposit of sediment formed when a stream’s slope is abruptly reduced.
A slow motion of Earth’s axis that traces out a cone over a period of 26,000 years.
Tiny bits of particulate matter that serve as surfaces on which water vapor condenses.
An isotope resulting from radioactive decay.
A term used to describe plutons that cut across existing rock structures, such as bedding planes.
The combined effect of evaporation and transpiration.
The view that the Sun is at the center of the solar system.
One of the three main categories of meteorites. This group is composed largely of iron with varying amounts of nickel (5–20 percent). Most meteorite finds are irons.
A system for classifying climates devised by Wladimir Köppen that is based on mean monthly and annual values of temperature and precipitation.
Magma that reaches Earth’s surface.
A relatively flat, gently sloping plain consisting of materials deposited by meltwater streams in front of the margin of an ice sheet.
All geologic time prior to the Paleozoic era.
Fog formed when rain evaporates as it falls through a layer of cool air.
Fog having the appearance of steam, produced by evaporation from a warm water surface into the cool air above.
Sediments deposited by glacial meltwater.
Transform fault boundary
A boundary in which two plates slide past one another without creating or destroying lithosphere.
By international agreement, a tropical cyclone with maximum winds between 61 and 119 kilometers (38 and 74 miles) per hour.
The state of the atmosphere at any given time.
The disintegration and decomposition of rock at or near Earth’s surface.
Having trouble accessing your account? Let us help you, contact support at +1(510) 944-1054 or email@example.com
Forgot password? Reset it here