Classical thermodynamics problem.

The discussion centers on calculating the global increase in entropy when two identical masses of water at temperatures T1 and T2 reach thermal equilibrium. The initial formula proposed by the user, Dimi, is ΔS = m*C*ln(T2/T1), which is incorrect. The correct formula for the increase in entropy is 2m*C*ln[(T1+T2)/2√(T1*T2)], as provided in the textbook. The key to solving the problem lies in understanding the equilibrium temperature and the change in entropy for each mass of water.

• Understanding of classical thermodynamics principles
• Familiarity with the concept of entropy
• Knowledge of thermal equilibrium
• Basic mathematical skills for logarithmic calculations

• Study the derivation of the entropy formula in thermodynamics
• Learn about thermal equilibrium and its implications in heat transfer
• Explore the concept of specific heat capacity (C) in thermodynamic calculations
• Investigate real-world applications of entropy in thermodynamic systems

Students studying thermodynamics, educators teaching classical thermodynamics concepts, and professionals in engineering fields requiring a solid understanding of entropy and thermal processes.