Hydraulics is a science dealing with the physical properties and movement phenomena of liquids (water)
Hydrostatics
The part of hydraulics dealing with the laws of quiescent liquids
Hydrodynamics
The part of hydraulics that examines the laws of flowing fluids (water movements)
The most important physical properties of water
3 states (liquid, solid, gaseous)
Boiling and melting points depend on pressure and solute content
Density
Ratio of mass (m) to volume (V), sign: ρ (Greek letter), temperature and pressure dependent
The maximum density of water at standard atmospheric pressure is the highest at 4 oC
At atmospheric pressure, in a normal environment, the change in density of water is negligible, so we consider the density of water as 1000 kg/m3
Specific gravity/weight
Sign: γ (gamma), unit of measure: N/m³, weight per volume unit, expressed as density: γ=ρ∙g, where g is gravity acceleration
Specific weight of water, at 5 ºC, at sea level: 9.807 kN/m³
Surface tension
A fundamental property of liquids, they strive to create the smallest specific surface area (sphere) if no external force field acts on them, due to cohesive force
Wetting
The degree of wetting can be described by the wetting edge angle (Θ, theta), if <90 degrees it is partial wetting, if >90 degrees it is partial non-wetting
Water
Due to adhesion exceeding cohesive force, the resultant points outside the wall, so the water surface shows a concave shape from above
Mercury
Due to higher cohesion, the resultant points inside the wall, so the mercury surface is convex from above
Capillarity
The phenomenon related to surface tension, where adhesion affects the liquid level against gravity, resulting in capillary rise or capillary sinking
Capillary rise of water: hcap=30/d (mm), where d is the pipe diameter
Capillary descent of mercury: hcap=10/d (mm)
Capillarity is strongly, but reversely correlating with the grain size of the sediment
Detergent washes due to reducing the surface tension of water, forming a "bridge" between water and fat particles
Viscosity
Internal friction, characterized by sliding stress, directly proportional to the velocity gradient, dynamic viscosity: η (Pa∙s), kinematic viscosity: ν=η/ρ (m2/s)
Kinematic viscosity of water: at 10 °C ν10 = 0.013 cm2/s; At 20 °C ν20 = 0.01 cm2/s = 10-6 m2/s
Ideal fluid
A fluid that fills the space and has zero viscosity, homogeneous, incompressible and frictionless
Quiescent fluid space
Absolute rest, when the fluid parts are stationary in the terrestrial coordinate system, or relative rest, when the liquid parts are stationary in the coordinate system fixed to the wall of the container
Basic theorems of hydrostatics
Stationary liquid only exerts a perpendicular effect on the wall of the containment vessel
At any internal point of the quiescent liquid, the pressure acts in all directions and at one point has the same magnitude regardless of direction
Pascal's law: the effect (pressure) of external forces acting on the fluid space at rest propagates and prevails in the fluid space without loss
Hydrostatic pressure
Pressure due to the weight of the liquid, described by Pascal's theorem: P= hγ [N/m2=Pa] where h is liquid column height, γ is specific gravity/weight of the liquid, and ρ is density of the liquid
Absolute pressure
pabs=p0+hγ, where p0 is air pressure (≈100kPa)
Buoyancy
The resultant of the vertical pressure components acting on a body immersed in water points upwards, and its magnitude is the weight of water of the same volume as the body (Archimedes' law)
The line of action of the buoyant force passes through the center of gravity of the displaced water volume
Inertia
The tendency of an object to resist changes in its motion. It's described by Newton's first law of motion, which states that an object at rest will stay at rest, and an object in motion will stay in motion, unless acted upon by an external force.
Buoyant force
The force that makes objects float in a fluid (like water or air). It's equal to the weight of the fluid that the object displaces. The line of action of the buoyant force always passes through the center of gravity of the displaced fluid volume.