Internal energy (U) is defined as the total energy of a closed system in chemistry and physics.
The sum of the system’s potential energy and kinetic energy is known as internal energy. When a reaction is run at constant pressure, the change in internal energy (U) is equal to the amount of heat gained or lost (enthalpy change).
What is internal energy?
Internal energy is a wide concept that is difficult to quantify. Transfers of chemical compounds or energy as heat, as well as thermodynamic work, are thermodynamic processes that characterise internal energy. Changes in the system’s several variables, such as entropy, volume, and chemical composition, are used to measure these processes. Considering all of the system’s inherent energies, such as the static rest mass energy of its constituent materials, isn’t always necessary. The first law of thermodynamics describes the change in internal energy as the difference between the energy provided to the system as heat and the thermodynamic work done by the system on its surroundings when mass transfer is restricted by impermeable enclosing walls. The system is said to be isolated if neither substance nor energy passes through the confining walls, and its internal energy cannot alter.
Internal energy is an equivalent representation of entropy, both cardinal state functions of just extensive state variables, and describes the full thermodynamic information of a system.
As a result, its value is solely determined by the current state of the system, rather than by a specific decision among the many conceivable processes via which energy can enter or exit the system.
It’s a potential for thermodynamics. The kinetic energy of microscopic motion of the system’s particles from translations, rotations, and vibrations, as well as the potential energy associated with microscopic forces, such as chemical bonds, can be examined microscopically.
Factors affecting internal energy:
The entropy S, volume V, and number of heavy particles in a system determine its internal energy.
The Internal Energy Formula
We can represent it mathematically,
ΔU=q+w
Where,
The entire change in internal energy of a system is denoted by U.
The heat exchanged between a system and its environment is referred to as q.
The work done by or on the system is denoted by the letter w.
Internal energy change
Thermodynamics is primarily concerned with internal energy changes .
The changes in internal energy for a closed system, with matter transfer omitted, are attributable to heat transfer Q, and thermodynamic work , W performed by the system on its surroundings. As a result, given a process, the internal energy change ,∆U may be written as follows:
∆U= Q -W (Closed system )
When a closed system gets energy in the form of heat, the internal energy is increased. It’s split up into microscopic kinetic and microscopic potential energies. Thermodynamics, in general, does not trace this distribution. Because all of the extra energy in an ideal gas is kept only as tiny kinetic energy, it causes a temperature increase; this heating is called sensible.
The doing of work on its surroundings is a second type of mechanism for changing the internal energy of a closed system. Such work could be purely mechanical, such as when the system expands to drive a piston, or it could be more complex, such as when the system changes its electric polarisation to drive a change in the electric field around it.
An Ideal Gas’s Internal Energy
An ideal gas’s internal energy is a good representation of a real-world system. In such a system, the particles in an ideal gas are seen as point objects colliding with each other in totally elastic collisions. The real behaviour of monatomic gases (such as helium and argon) is consistent with this hypothesis.
Internal energy in an ideal gas is proportional to the number of particles per mole and the temperature:
U = cnT
U stands for internal energy,
c for heat capacity at constant volume,
n for moles,
and T for temperature.
Definition of internal energy as per the first law of thermodynamics:
The internal energy (E) is defined by the first rule of thermodynamics as the difference between the heat transfer (Q) into a system and the work (W) done by the system.
E2 – E1 = Q – W
Conclusion :
The sum of the system’s potential energy and kinetic energy is known as internal energy. When a reaction is run at constant pressure, the change in internal energy (U) is equal to the amount of heat gained or lost (enthalpy change). Because the possible energies between molecules and atoms are crucial, internal energy is important for understanding phase shifts, chemical reactions, nuclear events, and many other microscopic phenomena. Both Macroscopic and microscopic energy the objects have in vacuum.
Pressure, volume, and temperature all have an impact on internal energy. This list’s variables are all state functions. State functions include mass, volume, pressure, temperature, density, and entropy.