Fluid mechanics is all about how liquids and gases behave. This section dives into the key properties that make fluids unique, like density and viscosity . It's like learning the personality traits of water, air, and other fluids.
We'll also explore how fluids exert pressure and force when at rest. This knowledge is super useful for designing everything from dams to floating ships. It's the foundation for understanding how fluids interact with their surroundings.
Key Fluid Properties
Density and Specific Weight
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Density (ρ) measures mass per unit volume of fluid expressed in kg/m³ or slug/ft³
Affects fluid behavior and forces
Example: Water has a density of 1000 kg/m³ at 4°C
Specific weight (γ) measures weight per unit volume of fluid in N/m³ or lbf/ft³
Related to density by acceleration due to gravity (g)
Calculated using the formula γ = ρ g γ = ρg γ = ρ g
Temperature significantly impacts density
Most substances decrease in density as temperature increases (water is an exception between 0-4°C)
Viscosity and Surface Tension
Viscosity (μ) quantifies fluid's resistance to flow and deformation
Dynamic viscosity expressed in Pa·s or lb·s/ft²
Kinematic viscosity (ν) represents ratio of dynamic viscosity to density
Example: Honey has a higher viscosity than water, flowing more slowly
Surface tension (σ) measures fluid surface's resistance to external forces
Caused by cohesive forces between molecules
Typically measured in N/m or lbf/ft
Enables water striders to walk on water surface
Temperature affects viscosity and surface tension
Generally, both properties decrease as temperature increases
Compressibility and Other Properties
Compressibility measures volume change in fluid under pressure
Negligible for liquids but significant for gases
Example: Air in tires compresses under increased pressure, while water in hydraulic systems remains nearly incompressible
Bulk modulus quantifies fluid's resistance to compression
Inverse of compressibility
Higher bulk modulus indicates lower compressibility
Vapor pressure represents pressure at which liquid begins to vaporize
Increases with temperature
Critical in preventing cavitation in hydraulic systems
Hydrostatic Pressure and Force
Hydrostatic Pressure Principles
Hydrostatic pressure results from fluid weight at rest
Increases linearly with depth according to p = ρ g h p = ρgh p = ρ g h
h represents depth, ρ is fluid density, g is gravitational acceleration
Pascal's law states applied pressure transmits equally in all directions
Enables hydraulic systems like car brakes and elevators
Total pressure at a point combines atmospheric and gauge pressure
Atmospheric pressure results from weight of air column above
Gauge pressure measures pressure relative to atmospheric pressure
Hydrostatic Force Calculations
Hydrostatic force on submerged planar surface calculated by integrating pressure over area
Resultant force acts at center of pressure
Force magnitude: F = ρ g h A F = ρghA F = ρ g h A , where A is surface area
Curved surfaces require separate horizontal and vertical force component calculations
Use projected areas for each component
Example: Dam design considers both horizontal and vertical forces on curved surfaces
Pressure prisms visually represent pressure distribution on submerged surfaces
Aid in force calculation and visualization
Triangular for vertical surfaces, trapezoidal for inclined surfaces
Stability of Floating Objects
Buoyancy and Archimedes' Principle
Archimedes' principle states buoyant force equals weight of displaced fluid
Applies to submerged or partially submerged objects
Buoyant force acts vertically upward through center of buoyancy
Center of buoyancy represents centroid of displaced fluid volume
Position changes as object orientation changes
Buoyant force calculation: F b = ρ g V F_b = ρgV F b = ρ g V , where V is displaced fluid volume
Example: A 1000 kg boat displacing 1 m³ of water experiences 9810 N buoyant force
Stability Analysis
Stability determined by relative positions of center of gravity and metacenter
Metacenter intersects buoyant force vector and object's centerline
Metacentric height measures distance between center of gravity and metacenter
Positive for stable equilibrium
Negative for unstable equilibrium
Zero for neutral equilibrium
Submerged object stability achieved when center of buoyancy directly above center of gravity
Reserve buoyancy represents volume between waterline and uppermost watertight deck
Crucial for vessel design and safety
Affects ship's ability to remain afloat when damaged
Manometers and Pressure Measurement
Manometer Types and Principles
Manometers measure pressure differences using fluid column height
Simple manometers use single fluid
U-tube manometers compare two pressures
Inclined manometers increase sensitivity for small pressure differences
Pressure difference calculated using Δ p = ρ g h Δp = ρgh Δ p = ρ g h
h represents height difference between fluid levels
Multi-fluid manometers require considering density and height of each fluid section
Example: Mercury-water manometer uses density difference to measure larger pressure ranges
Pressure Measurement Devices
Barometers measure atmospheric pressure
Typically use mercury due to high density
Standard atmospheric pressure: 101.325 kPa or 760 mmHg at sea level
Pressure gauges measure relative to atmospheric pressure (gauge pressure)
Bourdon tubes use curved tube that straightens under pressure
Diaphragm gauges use flexible membrane displacement
Absolute pressure combines gauge pressure and atmospheric pressure
Important distinction in pressure measurements and calculations
Example: Tire pressure often measured in gauge pressure, while vacuum systems use absolute pressure