Definition Of Densityρ=mV\rho = \frac{m}{V}ρ=Vm Mass per unit volume Units: kg/m3 Characterizes materials Important for buoyancy calculations Definition of Density
Definition Of PressureP=FAP = \frac{F}{A}P=AF Force per unit area Units: Pa (Pascal) = N/m2 Also use: atm, mm Hg, bar 1 atm = 101.3 kPa = 760 mm Hg Definition of Pressure
Absolute Vs Gauge Pressure Absolute pressure: Total pressure (including atmosphere) Gauge pressure: Pressure above atmospheric pressure Pabs=Pgauge+PatmP_{abs} = P_{gauge} + P_{atm}Pabs=Pgauge+Patm Tire gauges and blood pressure gauges typically read gauge pressure Absolute vs Gauge Pressure
Hydrostatic Pressure FormulaP=P0+ρghP = P_0 + \rho ghP=P0+ρgh Pressure increases with depth in fluid P0P_0P0: pressure at surface ρ\rhoρ: fluid density hhh: depth below surface Explains water pressure increases with depth Hydrostatic Pressure Formula
Pressure Vs Depth Relationship Linear increase in pressure with depth Deeper = higher pressure Dependent on fluid density Independent of container shape Same horizontal level: same pressure (connected vessels) Pressure vs Depth Relationship
Pascal's Principle Pressure applied to enclosed fluid transmitted undiminished F1A1=F2A2\frac{F_1}{A_1} = \frac{F_2}{A_2}A1F1=A2F2 Hydraulic lifts operate on this principle Used in hydraulic brakes, jacks, presses Pascal's Principle
Archimedes' Principle Buoyant force equals weight of fluid displaced FB=ρfluidVdisplacedgF_B = \rho_{fluid} V_{displaced}gFB=ρfluidVdisplacedg Upward force on submerged object Explains why objects float or sink Archimedes' Principle
Buoyant Force FormulaFB=ρfluidVsubmergedgF_B = \rho_{fluid}V_{submerged}gFB=ρfluidVsubmergedg Depends on fluid density and submerged volume Not equal to object's weight Can support objects that would otherwise sink Buoyant Force Formula
Floating And Sinking Conditions Floats: ρobject<ρfluid\rho_{object} < \rho_{fluid}ρobject<ρfluid Partially submerged: Vsub=ρobjρfluidVtotalV_{sub} = \frac{\rho_{obj}}{\rho_{fluid}}V_{total}Vsub=ρfluidρobjVtotal Sinks: ρobject>ρfluid\rho_{object} > \rho_{fluid}ρobject>ρfluid Entirely submerged (if completely submerged) Accelerates downward if not supported Neutrally buoyant: ρobject=ρfluid\rho_{object} = \rho_{fluid}ρobject=ρfluid Floating and Sinking Conditions
Apparent Weight In Fluids Apparent weight = actual weight - buoyant force Wapp=mg−ρfluidVsubgW_{app} = mg - \rho_{fluid}V_{sub}gWapp=mg−ρfluidVsubg Object feels lighter in fluid Explains why lifting in water is easier Basis for buoyancy devices Apparent Weight in Fluids
Characteristics Of Ideal Fluids Incompressible (constant density) Non-viscous (no internal friction) Irrotational (no rotation) Steady flow (velocity at each point constant over time) Simplified model for real fluids Characteristics of Ideal Fluids
Continuity EquationA1v1=A2v2=constantA_1v_1 = A_2v_2 = \text{constant}A1v1=A2v2=constant Flow rate constant throughout pipe Product of area and velocity constant Narrower section -> higher velocity Wider section -> lower velocity Volume flow rate: Q=AvQ = AvQ=Av (m3/s) Continuity Equation
Volume Flow RateQ=AvQ = AvQ=Av Volume of fluid passing point per unit time Units: m3/s Constant in steady flow (incompressible fluid) Same flow rate at all pipe cross-sections Volume Flow Rate
Bernoulli's PrincipleP+12ρv2+ρgh=constantP + \frac{1}{2}\rho v^2 + \rho gh = \text{constant}P+21ρv2+ρgh=constant Conservation of energy per unit volume Pressure + kinetic energy + potential energy constant along streamline Higher velocity -> lower pressure Height differences affect pressure Bernoulli's Principle
Conservation Of Energy In Fluids Energy conservation for ideal fluids Pressure energy + kinetic energy + potential energy Explains: venturi effect, airplane lift Basis for flow measurement devices Conservation of Energy in Fluids
Torricelli's Lawv=2ghv = \sqrt{2gh}v=2gh Speed of fluid exiting tank Same as free-fall speed from height h Torricelli's law Assumes no friction/viscosity Torricelli's Law
Definition Of Densityρ=mV\rho = \frac{m}{V}ρ=Vm Mass per unit volume Units: kg/m3 Characterizes materials Important for buoyancy calculations Definition of Density
Definition Of PressureP=FAP = \frac{F}{A}P=AF Force per unit area Units: Pa (Pascal) = N/m2 Also use: atm, mm Hg, bar 1 atm = 101.3 kPa = 760 mm Hg Definition of Pressure
Absolute Vs Gauge Pressure Absolute pressure: Total pressure (including atmosphere) Gauge pressure: Pressure above atmospheric pressure Pabs=Pgauge+PatmP_{abs} = P_{gauge} + P_{atm}Pabs=Pgauge+Patm Tire gauges and blood pressure gauges typically read gauge pressure Absolute vs Gauge Pressure
Hydrostatic Pressure FormulaP=P0+ρghP = P_0 + \rho ghP=P0+ρgh Pressure increases with depth in fluid P0P_0P0: pressure at surface ρ\rhoρ: fluid density hhh: depth below surface Explains water pressure increases with depth Hydrostatic Pressure Formula
Pressure Vs Depth Relationship Linear increase in pressure with depth Deeper = higher pressure Dependent on fluid density Independent of container shape Same horizontal level: same pressure (connected vessels) Pressure vs Depth Relationship
Pascal's Principle Pressure applied to enclosed fluid transmitted undiminished F1A1=F2A2\frac{F_1}{A_1} = \frac{F_2}{A_2}A1F1=A2F2 Hydraulic lifts operate on this principle Used in hydraulic brakes, jacks, presses Pascal's Principle
Archimedes' Principle Buoyant force equals weight of fluid displaced FB=ρfluidVdisplacedgF_B = \rho_{fluid} V_{displaced}gFB=ρfluidVdisplacedg Upward force on submerged object Explains why objects float or sink Archimedes' Principle
Buoyant Force FormulaFB=ρfluidVsubmergedgF_B = \rho_{fluid}V_{submerged}gFB=ρfluidVsubmergedg Depends on fluid density and submerged volume Not equal to object's weight Can support objects that would otherwise sink Buoyant Force Formula
Floating And Sinking Conditions Floats: ρobject<ρfluid\rho_{object} < \rho_{fluid}ρobject<ρfluid Partially submerged: Vsub=ρobjρfluidVtotalV_{sub} = \frac{\rho_{obj}}{\rho_{fluid}}V_{total}Vsub=ρfluidρobjVtotal Sinks: ρobject>ρfluid\rho_{object} > \rho_{fluid}ρobject>ρfluid Entirely submerged (if completely submerged) Accelerates downward if not supported Neutrally buoyant: ρobject=ρfluid\rho_{object} = \rho_{fluid}ρobject=ρfluid Floating and Sinking Conditions
Apparent Weight In Fluids Apparent weight = actual weight - buoyant force Wapp=mg−ρfluidVsubgW_{app} = mg - \rho_{fluid}V_{sub}gWapp=mg−ρfluidVsubg Object feels lighter in fluid Explains why lifting in water is easier Basis for buoyancy devices Apparent Weight in Fluids
Characteristics Of Ideal Fluids Incompressible (constant density) Non-viscous (no internal friction) Irrotational (no rotation) Steady flow (velocity at each point constant over time) Simplified model for real fluids Characteristics of Ideal Fluids
Continuity EquationA1v1=A2v2=constantA_1v_1 = A_2v_2 = \text{constant}A1v1=A2v2=constant Flow rate constant throughout pipe Product of area and velocity constant Narrower section -> higher velocity Wider section -> lower velocity Volume flow rate: Q=AvQ = AvQ=Av (m3/s) Continuity Equation
Volume Flow RateQ=AvQ = AvQ=Av Volume of fluid passing point per unit time Units: m3/s Constant in steady flow (incompressible fluid) Same flow rate at all pipe cross-sections Volume Flow Rate
Bernoulli's PrincipleP+12ρv2+ρgh=constantP + \frac{1}{2}\rho v^2 + \rho gh = \text{constant}P+21ρv2+ρgh=constant Conservation of energy per unit volume Pressure + kinetic energy + potential energy constant along streamline Higher velocity -> lower pressure Height differences affect pressure Bernoulli's Principle
Conservation Of Energy In Fluids Energy conservation for ideal fluids Pressure energy + kinetic energy + potential energy Explains: venturi effect, airplane lift Basis for flow measurement devices Conservation of Energy in Fluids
Torricelli's Lawv=2ghv = \sqrt{2gh}v=2gh Speed of fluid exiting tank Same as free-fall speed from height h Torricelli's law Assumes no friction/viscosity Torricelli's Law