- 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.
An instrument that measures atmospheric pressure.
A low, elongate ridge of sand that parallels the coast.
A cloud of glowing gas excited by ultraviolet radiation from hot stars.
An igneous rock texture in which the crystals are roughly equal in size and large enough so that individual minerals can be identified with the unaided eye.
Tiny bits of particulate matter that serve as surfaces on which water vapor condenses.
A region where the rigid plates are moving apart, typified by the midoceanic ridges.
A break in a rock mass along which movement has occurred.
A vent in a volcanic area from which fumes or gases escape.
The concept of an Earth-centered universe.
Ice cap climate
A climate that has no monthly means above freezing and supports no vegetative cover except in a few scattered high mountain areas. This climate, with its perpetual ice and snow, is confined largely to the ice sheets of Greenland and Antarctica.
Localized convective lifting
Unequal surface heating that causes localized pockets of air (thermals) to rise because of their buoyancy.
A center of low pressure characterized by cyclonic winds.
The boundary between the mesosphere and the thermosphere.
Drops of water that fall from clouds that have a diameter of at least 0.5 millimeter (0.02 inch).
The steep, leeward slope of a sand dune; it maintains an angle of about 34 degrees.
Slow, downslope flow of water-saturated materials common to permafrost areas.
The columnlike form that grows upward from the floor of a cavern.
A measure of stellar distance.
Radiation with a wavelength from 0.4 to 0.7 micrometer.