♨️Thermodynamics of Fluids Unit 1 – Intro to Fluid Thermodynamics
Fluid thermodynamics explores how heat, work, and energy interact in flowing substances. This field is crucial for understanding everything from weather patterns to engine efficiency. It combines principles of fluid mechanics with thermodynamic laws to explain how fluids behave under various conditions.
Key concepts include density, pressure, temperature, and viscosity. These properties help describe fluid behavior and are essential for applying fundamental laws like the First and Second Laws of Thermodynamics. Understanding these principles is vital for solving real-world engineering problems in areas like power generation and HVAC systems.
Thermodynamics studies the relationships between heat, work, and energy in systems
Fluids include both liquids and gases that continuously deform under shear stress
Density (ρ) is mass per unit volume, a measure of fluid compactness
Pressure (P) is force per unit area, resulting from molecular collisions within the fluid
Temperature (T) quantifies the average kinetic energy of particles in a substance
Viscosity (μ) measures a fluid's resistance to flow or internal friction
Compressibility is the ability of a fluid to change volume under pressure (gases are highly compressible, liquids are nearly incompressible)
Ideal gas assumes molecules have negligible volume and no intermolecular forces
Fundamental Laws and Principles
First Law of Thermodynamics states that energy cannot be created or destroyed, only converted from one form to another
Expressed as ΔU=Q−W, where ΔU is change in internal energy, Q is heat added, and W is work done by the system
Second Law of Thermodynamics asserts that entropy (disorder) of an isolated system always increases over time
Implies that heat flows naturally from high to low temperature and work is required to transfer heat from low to high temperature
Zeroth Law of Thermodynamics defines thermal equilibrium: if two systems are each in thermal equilibrium with a third, they are in thermal equilibrium with each other
Ideal Gas Law relates pressure, volume, temperature, and amount of gas: PV=nRT
P is pressure, V is volume, n is number of moles, R is universal gas constant, and T is absolute temperature
Dalton's Law states that in a mixture of non-reacting gases, the total pressure equals the sum of the partial pressures of the individual gases
Properties of Fluids
Fluids are characterized by their ability to flow and take the shape of their container
Density of a fluid depends on its composition, pressure, and temperature
Liquids are generally more dense than gases due to stronger intermolecular forces
Viscosity arises from intermolecular forces and quantifies a fluid's resistance to deformation
Newtonian fluids (water, air) have constant viscosity, while non-Newtonian fluids (blood, ketchup) have viscosity that varies with shear rate
Surface tension results from unbalanced molecular forces at the interface between a liquid and another substance (gas or solid)
Causes phenomena like capillary action and the formation of droplets
Compressibility is significant for gases but negligible for most liquids under normal conditions
Thermal expansion causes fluids to change volume with temperature, typically increasing for gases and liquids
Vapor pressure is the pressure at which a liquid and its vapor are in equilibrium at a given temperature
Thermodynamic Systems and Processes
A thermodynamic system is a region of the universe under study, separated from its surroundings by a boundary
Closed systems allow energy but not mass transfer, while open systems allow both
Thermodynamic equilibrium occurs when a system's properties remain constant over time
Thermal, mechanical, and chemical equilibrium must be achieved
Processes describe the path a system takes from one equilibrium state to another
Isothermal processes occur at constant temperature
Isobaric processes maintain constant pressure
Isochoric (isovolumetric) processes have constant volume
Adiabatic processes allow no heat transfer with the surroundings
Reversible processes can be reversed without any net change to the system or surroundings
Irreversible processes involve energy dissipation and cannot be fully reversed
Work is done when a system expands or contracts against an external pressure
For a quasistatic process, W=∫PdV
Heat transfer occurs due to temperature differences and can be quantified using specific heat capacities
Equations of State
Equations of state describe the relationship between pressure, volume, temperature, and composition for a substance
Ideal Gas Law is the simplest equation of state, applicable to gases at low densities and high temperatures
Assumes no intermolecular forces and negligible molecular volume
Van der Waals equation modifies the Ideal Gas Law to account for molecular size and attraction
(P+Vm2a)(Vm−b)=RT, where a and b are substance-specific constants
Virial equation expresses the compressibility factor (Z) as a power series in pressure or density
Useful for describing real gas behavior at moderate pressures
Cubic equations of state (Peng-Robinson, Soave-Redlich-Kwong) are widely used in chemical engineering for their accuracy and computational efficiency
Tabulated data and empirical correlations are often used for liquids and dense fluids due to the complexity of intermolecular interactions
Energy Transfer and Conservation
Internal energy (U) is the sum of the kinetic and potential energies of the particles in a system
Function of temperature, pressure, and composition
First Law of Thermodynamics states that the change in internal energy equals the heat added minus the work done
ΔU=Q−W for a closed system
Enthalpy (H) is a state function defined as H=U+PV
Represents the total heat content of a system
For isobaric processes, change in enthalpy equals heat transferred
Heat capacity quantifies the amount of heat required to change a substance's temperature
Specific heat capacity (c) is heat capacity per unit mass
Q=mcΔT for a constant specific heat
Latent heat is the energy absorbed or released during a phase change at constant temperature
Latent heat of fusion for solid-liquid transitions and latent heat of vaporization for liquid-gas transitions
Heat transfer occurs via conduction, convection, and radiation
Conduction is heat transfer through a solid or stationary fluid due to temperature gradients
Convection involves heat transfer by the bulk motion of a fluid
Radiation is the emission of electromagnetic waves from a surface due to its temperature
Applications in Engineering
Fluid mechanics principles are essential for designing and optimizing piping systems, pumps, and valves
Pressure drop, flow rate, and power requirements must be considered
Heat exchangers transfer thermal energy between fluids at different temperatures
Designed using principles of heat transfer and fluid mechanics to maximize efficiency
Power cycles (Rankine, Brayton) convert heat into mechanical work using a working fluid
Efficiency is limited by the Second Law of Thermodynamics
Refrigeration and air conditioning systems remove heat from a low-temperature reservoir and reject it to a high-temperature reservoir
Coefficient of Performance (COP) quantifies the efficiency of these systems
Combustion processes involve the rapid oxidation of a fuel, releasing heat and products of combustion
Adiabatic flame temperature and chemical equilibrium are key concepts
Psychrometrics studies the thermodynamic properties of moist air, crucial for HVAC design
Humidity, dew point, and wet-bulb temperature are important parameters
Compressible flow analysis is necessary for high-speed applications like jet engines and supersonic aircraft
Mach number, shock waves, and choked flow are significant phenomena
Problem-Solving Techniques
Identify the system and surroundings, specifying the type of system (open, closed, isolated)
Determine the relevant properties and processes, making appropriate assumptions and simplifications
Apply the conservation laws (mass, energy) and equations of state to the problem
First Law of Thermodynamics: ΔU=Q−W for a closed system
Steady-flow energy equation for open systems: Δh+Δke+Δpe+q+w=0
Use property tables, charts, or equations of state to find necessary thermodynamic properties
Interpolate between values when needed
Solve equations systematically, checking units and orders of magnitude for consistency
Analyze the results critically, considering the implications and limitations of the assumptions made
Validate the solution using alternative methods or by comparing it to known cases
Communicate the results effectively using appropriate terminology, units, and significant figures