The first law of thermodynamics is a cornerstone of energy conservation in mechanical systems. It links changes in to transfer and work done, providing a framework for understanding energy transformations.
This law states that energy can't be created or destroyed, only converted between forms. It's expressed as , where U is internal energy, Q is heat added, and W is work done by the system.
Definition and concept
First law of thermodynamics establishes the fundamental principle of energy conservation in thermal systems
Relates changes in internal energy to heat transfer and work done, forming the basis for understanding energy transformations in mechanical systems
Statement of first law
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Energy cannot be created or destroyed, only converted from one form to another
Total energy of an remains constant over time
Mathematically expressed as ΔU=Q−W, where U is internal energy, Q is heat added, and W is work done by the system
Conservation of energy principle
Fundamental concept underlying the first law of thermodynamics
Energy transfers between system and surroundings must balance
Applies to all physical processes, including mechanical, thermal, and chemical interactions
Closed vs open systems
Closed systems exchange energy but not matter with surroundings
Open systems allow both energy and matter exchange
First law applies differently to each system type, accounting for mass flow in open systems
Internal energy
Microscopic kinetic energy
Contributes to internal energy through molecular motion
Includes translational, rotational, and vibrational energy of particles
Directly related to temperature, increasing as temperature rises
Microscopic potential energy
Arises from intermolecular forces and atomic bonds
Includes electrostatic interactions and chemical bond energies
Changes during phase transitions and chemical reactions
Relation to temperature
Temperature measures average kinetic energy of particles
Higher temperature indicates greater internal energy
Absolute zero represents minimum possible internal energy state
Work in thermodynamics
Pressure-volume work
Most common form of work in thermodynamic systems
Calculated as W=∫PdV, where P is pressure and V is volume
Positive work done by system when expanding against external pressure
Other forms of work
Electrical work in batteries and fuel cells
Magnetic work in superconductors
Surface tension work in liquid droplets
Gravitational work in hydrostatic systems
Sign conventions
Positive work indicates energy leaving the system
Negative work represents energy entering the system
Consistent sign convention crucial for accurate energy balance calculations
Heat transfer
Conduction vs convection vs radiation
Conduction transfers heat through direct molecular collisions
involves heat transfer by fluid motion
transmits energy via electromagnetic waves
Each mechanism dominates in different scenarios (solids, fluids, vacuum)
Heat capacity and specific heat
measures energy required to raise temperature by one degree
normalizes heat capacity per unit mass
Values vary widely among materials (water has high specific heat)
Mathematical formulation
Equation for first law
General form: ΔU=Q−W
For open systems: ΔU=Q−W+∑mihi−∑mehe
Accounts for energy flows across system boundaries
Change in internal energy
Calculated as ΔU=mcvΔT for ideal gases
Depends on specific heat capacity at constant volume (cv)
Independent of path taken between initial and final states
Work done on system
Negative of work done by system: Won=−Wby
Includes all forms of work (pressure-volume, electrical, etc.)
Path-dependent quantity, unlike internal energy change
Applications
Isochoric process
Volume remains constant (ΔV=0)
No done
All heat added goes into increasing internal energy
Isobaric process
Pressure remains constant
Work done equals W=PΔV
Commonly encountered in constant pressure heating/cooling
Isothermal process
Temperature remains constant (ΔT=0)
Internal energy unchanged for ideal gases
All heat added converted to work (or vice versa)
Adiabatic process
No heat transfer with surroundings (Q=0)
Work done entirely at expense of internal energy
Occurs in rapid compressions/expansions (diesel engines)
Limitations and assumptions
Ideal gas approximation
Assumes negligible intermolecular forces
Valid for low densities and high temperatures
Breaks down for real gases under extreme conditions
Quasi-static processes
Assumes system remains infinitesimally close to equilibrium
Allows use of equilibrium thermodynamic relations
Real processes often deviate from this idealization
Relation to other laws
Zeroth law of thermodynamics
Establishes concept of thermal equilibrium
Provides foundation for temperature measurement
Complements first law in describing heat flow direction
Second law of thermodynamics
Introduces concept of entropy and irreversibility
Limits efficiency of and
Complements first law by addressing quality of energy
Experimental verification
Historical experiments
Joule's paddle wheel experiment demonstrated mechanical equivalent of heat
Rumford's cannon boring observations linked heat to motion
Mayer's work on in biological systems
Modern laboratory techniques
Calorimetry measures heat transfer in chemical reactions
Bomb calorimeters determine energy content of fuels