Ocean Thermal Energy Conversion (OTEC) leverages the vastness of the world's oceans, covering two-thirds of the Earth's surface and absorbing approximately 70% of the sun's solar energy. This absorption results in a temperature disparity between the warm seawater near the surface, heated by solar energy, and the cold seawater deep below. These temperature differences create two essential reservoirs serving as a heat source and heat sink for a heat exchanger, forming the foundation for OTEC's clean and renewable energy production. Although the assumptions for OTEC plants include a tested and researched temperature difference of around 20C (potentially as high as 40C), the process relies on the cold seawater, approximately 4C, acting as a heat sink, and the warm seawater, around 26C, as the heat source. This temperature gradient is crucial for the efficiency and functionality of OTEC systems, making them promising contributors to clean and sustainable energy solutions. Analyze and calculate the cycle a. The pressure and temperature of each state. b. The properties of each state, such as, pump power, enthalpies, volumes, entropies, qualities, etc. whatever are required. c. Cycle heat input and output. d. Net work output. e. Thermal efficiency