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This is a short notes for physical chemistry for students
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Introduction to Thermodynamics in Physical Chemistry: Thermodynamics is a branch of physical chemistry that deals with the study of energy, heat, work, and how they interact within chemical systems. It provides a set of principles and laws that govern the transformation of energy in both physical and chemical processes. Thermodynamics is crucial for understanding processes such as chemical reactions, phase changes, and the behavior of gases and liquids. Key Concepts in Thermodynamics: System and Surroundings: System: The part of the universe we are focusing on, such as a reaction vessel, gas in a container, or a chemical reaction. Surroundings: Everything else outside the system that can exchange energy or matter with the system. The system is the part of the universe being studied, and the surroundings are everything else. Types of Systems: Isolated System: No exchange of energy or matter with the surroundings (e.g., thermos). Closed System: Can exchange energy (heat or work) but not matter with the surroundings (e.g., a sealed container). Open System: Can exchange both energy and matter with the surroundings (e.g., a beaker of water). State Functions and Path Functions: State Functions: Properties that depend only on the current state of the system, not on how the system got there. Examples include temperature (T), pressure (P), volume (V), enthalpy (H), entropy (S), and internal energy (U). Depend only on the current state of a system Do not depend on the path taken to reach that state Examples include temperature, pressure, volume, and internal energy Ex: Displacement The distance between two towns is a state function because it is the same for each route. Path Functions: Properties that depend on the specific process taken to change the system’s state, such as heat (Q) and work (W). Depend on the path taken to reach a particular state Are influenced by the specific conditions and steps followed during the process Examples include work and heat Ex: Work
The amount of work done on a system depends on the path taken, so work is a path function Energy (U): The internal energy of a system is the total energy contained within the system, including kinetic and potential energy at the molecular level. First Law of Thermodynamics (Conservation of Energy): ΔU=Q−W\Delta U = Q - W Where: ΔU\Delta U = Change in internal energy of the system QQ = Heat added to the system WW = Work done by the system on its surroundings Heat and Work: Heat (Q): Energy transferred between the system and surroundings due to a temperature difference. Work (W): Energy transferred when a force is applied over a distance, often related to changes in volume (e.g., gas expansion or compression). Enthalpy (H): Enthalpy is a state function defined as: H=U+PVH = U + PV Where PP is pressure and VV is volume. It’s used to describe the heat content of a system at constant pressure. For processes at constant pressure: ΔH=Qp\Delta H = Q_{\text{p}} Where ΔH\Delta H is the change in enthalpy, and QpQ_p is the heat absorbed or released at constant pressure. Entropy (S): Entropy is a measure of the disorder or randomness in a system. It quantifies the amount of energy in a system that is unavailable to do work. The Second Law of Thermodynamics states that for any spontaneous process, the total entropy of the system and surroundings always increases. ΔStotal>0\Delta S_{\text{total}} > 0 The Second Law also implies that natural processes are irreversible. Gibbs Free Energy (G): The Gibbs Free Energy is a thermodynamic potential that measures the reversible work obtainable from a system at constant temperature and pressure. Defined as: G=H−TSG = H - TS Where: HH = Enthalpy TT = Temperature SS = Entropy For a process to be spontaneous at constant temperature and pressure, the change in Gibbs free energy must be negative: ΔG<0\Delta G < 0 Spontaneous processes occur without the need for external energy input, and their spontaneity depends on the relationship between enthalpy and entropy. Third Law of Thermodynamics: As temperature approaches absolute zero (0 K), the entropy of a system approaches a minimum value, which for a perfect crystal is zero.