Mechanical Properties of FluidsMind Map

Pressure is the normal force acting per unit area. In a fluid at rest, pressure at a point acts equally in all directions and always normal to any surface. Hydrostatic pressure increases with depth because lower layers support the weight of fluid above them. At depth h below an open surface, pressure is P = P0 + ρgh, where P0 is atmospheric pressure. Pascal's law states that pressure applied to an enclosed incompressible fluid is transmitted equally and undiminished throughout the fluid. This explains hydraulic lift and hydraulic press, where a small force on a small piston produces a large force on a larger piston. The machine multiplies force, not energy.

Fluid flow describes the motion of liquids and gases. In streamline flow, each fluid particle follows a smooth path, and the velocity of fluid at a point remains constant with time. In turbulent flow, the motion is irregular, chaotic and contains eddies. The equation of continuity is based on conservation of mass. For steady incompressible flow, the volume of fluid crossing every cross-section per second is the same, so A1v1 = A2v2. Thus, fluid moves faster through narrow sections and slower through wider sections. The volume flow rate is Q = Av. Ideal fluid assumptions include incompressible, non-viscous, steady and irrotational flow, which are important before applying Bernoulli's principle.

Bernoulli's principle is the conservation of mechanical energy for ideal fluid flow. For steady, incompressible, non-viscous flow along a streamline, the sum P + 1/2ρv² + ρgh remains constant. These terms represent pressure energy, kinetic energy and potential energy per unit volume. At the same height, when fluid speed increases, pressure decreases. This pressure-velocity relationship explains many applications: a venturimeter measures flow speed using pressure difference, airplane wings produce lift due to pressure difference, and atomizers and carburetors use fast air to reduce pressure and draw liquid into the air stream. NEET frequently asks direct formulas and conceptual applications.

Viscosity is the internal friction of a fluid that opposes relative motion between its layers. A more viscous fluid, such as honey, flows slowly compared with water. The coefficient of viscosity, η, measures the viscous nature of a fluid. When a small spherical body moves slowly through a viscous fluid, it experiences viscous drag given by Stokes' law: F = 6πηrv. As a sphere falls through a fluid, its speed increases until weight is balanced by buoyant force and viscous drag. Then acceleration becomes zero and it moves with terminal velocity. Reynolds number predicts whether fluid flow is streamline or turbulent. These ideas are important in raindrops, sedimentation, blood flow and oil flow.

Surface tension is the property of a liquid surface by which it behaves like a stretched elastic membrane. It arises because molecules at the surface experience unbalanced cohesive forces. Surface tension is defined as force per unit length or surface energy per unit area. It explains spherical drops, floating needles, soap bubbles and insects walking on water. The angle of contact decides whether a liquid wets a solid surface. In a narrow capillary tube, liquid may rise or fall depending on adhesive and cohesive forces. Water rises in glass because angle of contact is acute, while mercury falls because its angle is obtuse. Curved liquid surfaces create excess pressure inside drops and bubbles, which is very important for NEET.