❤️🔥Heat and Mass Transfer Unit 3 – Convection Heat Transfer
Convection heat transfer involves fluid motion enhancing heat exchange compared to conduction alone. It's crucial in engineering applications like heat exchangers and cooling systems. The process depends on fluid properties, flow characteristics, and temperature differences, quantified by Newton's law of cooling.
Convection types include forced, natural, and mixed. Boundary layers, dimensionless numbers, and empirical equations help analyze and predict convective heat transfer. Real-world applications span automotive, HVAC, electronics, and food industries, showcasing convection's importance in thermal management across various fields.
Convection involves the transfer of heat through the movement of fluids (liquids or gases)
Fluid motion enhances heat transfer compared to conduction alone
Convective heat transfer occurs due to the combined effects of conduction and fluid motion
The rate of convective heat transfer depends on the fluid properties, flow characteristics, and temperature differences
Convection plays a crucial role in various engineering applications (heat exchangers, cooling systems, HVAC)
The driving force for convective heat transfer is the temperature gradient between the surface and the fluid
Convective heat transfer can be quantified using Newton's law of cooling: Q=hA(Ts−T∞)
Q is the convective heat transfer rate (W)
h is the convective heat transfer coefficient (W/m²·K)
A is the surface area (m²)
Ts is the surface temperature (K)
T∞ is the fluid temperature far from the surface (K)
Types of Convection
Convection can be classified into two main categories: forced convection and natural (or free) convection
Forced convection occurs when an external means (pump, fan) is used to drive the fluid motion
Examples include air flow over a car's radiator or water flowing through a pipe
Natural convection arises from buoyancy forces due to density differences caused by temperature variations in the fluid
Hotter fluid rises while cooler fluid sinks, creating a circulatory motion
Mixed convection is a combination of forced and natural convection, where both mechanisms influence the heat transfer process
The Rayleigh number (Ra) determines the relative importance of natural convection to forced convection
Convection can also be classified as external (flow over a surface) or internal (flow within a confined space)
Boundary Layer Concepts
The boundary layer is a thin region near a surface where the fluid velocity changes from zero at the surface to the free-stream velocity
Boundary layers develop due to the no-slip condition, which states that the fluid velocity is zero at the surface
The velocity boundary layer thickness (δ) is defined as the distance from the surface where the velocity reaches 99% of the free-stream velocity
The thermal boundary layer thickness (δt) is the distance from the surface where the temperature difference between the fluid and the surface reaches 99% of the total temperature difference
The Prandtl number (Pr) relates the velocity and thermal boundary layer thicknesses: Pr=αν
ν is the kinematic viscosity (m²/s)
α is the thermal diffusivity (m²/s)
Boundary layers can be laminar or turbulent, affecting the heat transfer characteristics
Laminar boundary layers have smooth, parallel streamlines and lower heat transfer rates
Turbulent boundary layers have chaotic, mixing flow and higher heat transfer rates
Dimensionless Numbers in Convection
Dimensionless numbers are used to characterize and analyze convective heat transfer problems
The Reynolds number (Re) represents the ratio of inertial forces to viscous forces: Re=μρVL
ρ is the fluid density (kg/m³)
V is the fluid velocity (m/s)
L is the characteristic length (m)
μ is the dynamic viscosity (kg/m·s)
The Nusselt number (Nu) represents the ratio of convective to conductive heat transfer: Nu=khL
h is the convective heat transfer coefficient (W/m²·K)
L is the characteristic length (m)
k is the thermal conductivity (W/m·K)
The Prandtl number (Pr) represents the ratio of momentum diffusivity to thermal diffusivity: Pr=αν
The Grashof number (Gr) represents the ratio of buoyancy forces to viscous forces in natural convection: Gr=ν2gβ(Ts−T∞)L3
g is the acceleration due to gravity (m/s²)
β is the volumetric thermal expansion coefficient (1/K)
Forced Convection Equations
Forced convection equations are used to calculate the heat transfer coefficient and Nusselt number for various flow configurations
For external flow over a flat plate, the local Nusselt number can be calculated using the Dittus-Boelter equation: Nux=0.0296Rex4/5Pr1/3
Valid for 0.6≤Pr≤60 and Rex≥105
For internal flow in a circular tube, the Nusselt number can be calculated using the Sieder-Tate equation: Nu=0.027Re0.8Pr1/3(μsμ)0.14
Valid for 0.7≤Pr≤16,700 and Re≥10,000
μ is the fluid viscosity at the bulk temperature
μs is the fluid viscosity at the surface temperature
The Gnielinski correlation can be used for turbulent flow in a circular tube: Nu=1+12.7(f/8)1/2(Pr2/3−1)(f/8)(Re−1000)Pr
Valid for 0.5≤Pr≤2000 and 3000≤Re≤5×106
f is the friction factor, which can be calculated using the Colebrook equation or Moody chart
Natural Convection Principles
Natural convection occurs due to buoyancy forces arising from density differences caused by temperature variations
The driving force for natural convection is the Grashof number (Gr), which represents the ratio of buoyancy forces to viscous forces
The Rayleigh number (Ra) is the product of the Grashof and Prandtl numbers: Ra=GrPr
It characterizes the flow regime in natural convection (laminar, transitional, or turbulent)
For natural convection over a vertical plate, the Nusselt number can be calculated using the Churchill and Chu correlation: Nu=(0.825+[1+(0.492/Pr)9/16]8/270.387Ra1/6)2
Valid for Ra≤1012
For natural convection in enclosures (rectangular cavities), the Nusselt number depends on the aspect ratio and Rayleigh number
Correlations for natural convection in various geometries (horizontal plates, cylinders, spheres) are available in the literature
Heat Transfer Coefficients
The heat transfer coefficient (h) quantifies the rate of heat transfer between a surface and a fluid
It depends on the fluid properties, flow characteristics, and surface geometry
Heat transfer coefficients are typically determined experimentally or estimated using empirical correlations
The overall heat transfer coefficient (U) accounts for the combined effects of conduction and convection in a system
It is used in the design of heat exchangers and other thermal systems
The thermal resistance concept can be used to analyze convective heat transfer in series or parallel arrangements
Thermal resistances are analogous to electrical resistances in a circuit
The Biot number (Bi) is a dimensionless parameter that relates the internal conduction resistance to the external convection resistance: Bi=khLc
Lc is the characteristic length (m)
It helps determine whether lumped system analysis can be applied
Real-World Applications
Convective heat transfer is encountered in numerous real-world applications across various industries
In the automotive industry, convective heat transfer is crucial for engine cooling, radiator design, and cabin air conditioning
HVAC (Heating, Ventilation, and Air Conditioning) systems rely on convective heat transfer to maintain comfortable indoor environments
Natural convection plays a role in passive cooling strategies (natural ventilation)
Forced convection is used in air handling units, fan coil units, and ductwork
Heat exchangers, used in power plants, chemical processing, and refrigeration systems, utilize convective heat transfer to efficiently transfer heat between fluids
Electronic devices (computer chips, power electronics) require effective convective cooling to dissipate heat and maintain optimal operating temperatures
Heat sinks and fans are designed to enhance convective heat transfer
In the food industry, convective heat transfer is employed in cooking, baking, and drying processes
Ovens, fryers, and dryers rely on forced convection to uniformly heat or remove moisture from food products
Renewable energy systems, such as solar thermal collectors and geothermal heat pumps, harness convective heat transfer to capture and utilize thermal energy from the environment