On the sea bottom at the Galapagos Rift, water heated to 350 °C gushes out of hydrothermal vents at a depth of 3000 m. Will this water boil or remain liquid at this depth? Assume the enthalpy of vaporization for water to be independent of pressure and temperature.
On the sea bottom at the Galapagos Rift, water heated to 350 °C gushes out of hydrothermal vents at a depth of 3000 m. Will this water boil or remain liquid at this depth? Assume the enthalpy of vaporization for water to be independent of pressure and temperature.
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