saturated or saturation
It is vapor molecules in equilibrium with a liquid in a closed system exert a pressure proportional to the concentration of molecules in the vapor state.
Water is in equilibrium with water vapor when the rate of evaporation of water molecules equals the rate of condensation of water vapor molecules. This typically occurs when the relative humidity in the air reaches 100% at a given temperature, known as the dew point.
Kinetic vapor pressure is the pressure exerted by vapor molecules when a liquid is in a closed container and some of the liquid has evaporated into the gas phase due to kinetic energy. It is different from the equilibrium vapor pressure, which is the pressure at which the rate of evaporation equals the rate of condensation.
Vapor pressure increases over a liquid in a closed container until the amount of vapor molecules rejoining the liquid equals the number leaving the liquid to form vapor. This is the characteristic vapor pressure of the substance.
The maximum pressure of vapor that can build up in a closed container is the vapor pressure of the substance at the given temperature. Once the vapor pressure is reached, the system reaches equilibrium and no further increase in pressure occurs. Any additional vapor will condense back into liquid form.
It is vapor molecules in equilibrium with a liquid in a closed system exert a pressure proportional to the concentration of molecules in the vapor state.
Water is in equilibrium with water vapor when the rate of evaporation of water molecules equals the rate of condensation of water vapor molecules. This typically occurs when the relative humidity in the air reaches 100% at a given temperature, known as the dew point.
The rate of molecules overcoming attractive forces is equal to the rate of molecules entering the solid state.
Kinetic vapor pressure is the pressure exerted by vapor molecules when a liquid is in a closed container and some of the liquid has evaporated into the gas phase due to kinetic energy. It is different from the equilibrium vapor pressure, which is the pressure at which the rate of evaporation equals the rate of condensation.
Vapor pressure increases over a liquid in a closed container until the amount of vapor molecules rejoining the liquid equals the number leaving the liquid to form vapor. This is the characteristic vapor pressure of the substance.
The maximum pressure of vapor that can build up in a closed container is the vapor pressure of the substance at the given temperature. Once the vapor pressure is reached, the system reaches equilibrium and no further increase in pressure occurs. Any additional vapor will condense back into liquid form.
If a hydrate's vapor pressure is higher than the water vapor in the air, water molecules will evaporate from the hydrate into the air until equilibrium is reached. This process will continue until the vapor pressures are equalized.
The condition of equilibrium between evaporation and condensation is known as a physical equilibrium because it involves a balance between the rates of evaporation and condensation without any change in the chemical composition of the substances involved. The equilibrium is based on physical processes such as the balance of vapor pressure and temperature rather than chemical reactions.
This process is called condensation. It occurs when vapor molecules lose energy and transition back into a liquid state by interacting with other liquid molecules at the surface. This can happen when the temperature of the vapor decreases or when it comes into contact with a cooler surface.
In a system at constant vapor pressure, a dynamic equilibrium exists between the vapor and the liquid. The system is in equilibrium because the rate of evaporation of liquid equals the rate of condensation of vapor. -KarkatHorns
At equilibrium, liquid water and water vapor coexist at a specific temperature and pressure, where the rate of evaporation of the liquid equals the rate of condensation of the vapor. This dynamic balance means that the amount of water in both phases remains constant over time, despite the continuous molecular exchanges. The vapor pressure of the water is determined by the temperature, and at equilibrium, it reflects the tendency of water molecules to escape into the vapor phase versus returning to the liquid phase.
The vapor pressure of water at 50°C is significantly higher than at 10°C. As temperature increases, the kinetic energy of water molecules also increases, allowing more molecules to escape into the vapor phase. Consequently, the vapor pressure, which is the pressure exerted by the vapor in equilibrium with its liquid, rises with temperature. Therefore, at 50°C, the vapor pressure of water is much greater than at 10°C.