The equilibrium condition where a gas holds all the water vapor molecules it can is called saturation. At saturation, the rate of evaporation of water molecules into the gas phase is equal to the rate of condensation of water vapor molecules back into the liquid phase. This results in a balance where the gas is holding the maximum amount of water vapor possible at a given temperature and pressure.
The gas pressure above a liquid at equilibrium is called the vapor pressure. This is the pressure at which the rate of evaporation equals the rate of condensation, leading to a dynamic equilibrium between the liquid and its vapor.
Equilibrium vapor pressure is the pressure exerted by a vapor in thermodynamic equilibrium with its condensed phases (solid or liquid) in a closed system at a specific temperature. It represents the balance between molecules escaping from the condensed phase and re-entering it.
At the triple point, all three phases of water coexist in equilibrium: solid (ice), liquid, and gas (water vapor). This is the point where the three phases can exist simultaneously under specific conditions of temperature and pressure.
You mean vapor?
No: Vapor is defined as the gas phase of a substance that is mostly solid or liquid at equilibrium at standard temperature and pressure. Therefore, a liquid itself is never a vapor, but the liquid is in equilibrium with a vapor phase that contains the same chemical substance.
In equilibrium, the movement of water is balanced, with the rate of evaporation equal to the rate of condensation. This state occurs when the vapor pressure of water in the air is equal to the vapor pressure of water in the liquid.
The vapor pressure of water at 21.5°C is approximately 19.8 mmHg. This value represents the pressure exerted by water vapor when in equilibrium with liquid water at that temperature.
The air that contains water vapor in equilibrium at a certain temperature is called saturated air. At saturation, the air has reached its maximum water vapor capacity at that temperature, leading to a balance between evaporation and condensation.
The answer to this problem is not as simple as it seems. When water evaporates, an equilibrium exists between the water vapor and liquid water. Normally, the water vapor is disbursed into the surrounding air, causing the equilibrium to shift in the direction of the water vapor product. By covering the water, the equilibrium is not shifted in this direction. Although the molecules are not evaporating more slowly, more of them reenter the water. Thus, the loss of liquid water slows (or stops if the container is air tight), but the process of evaporation continues at the same speed; its just that the water vapor formed now reenters the solution as just as quickly as it forms.
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 equilibrium condition where a gas holds all the water vapor molecules it can is called saturation. At saturation, the rate of evaporation of water molecules into the gas phase is equal to the rate of condensation of water vapor molecules back into the liquid phase. This results in a balance where the gas is holding the maximum amount of water vapor possible at a given temperature and pressure.
Condensation commonly occurs when a vapor is cooled. Water vapor from air which naturally condenses on cold surfaces into liquid water is called dew. Water vapor will only condense onto another surface when that surface is cooler than the temperature of the water vapor, or when the water vapor equilibrium in air, i. e. saturation humidity, has been exceeded. When water vapor condenses onto a surface, a net warming occurs on that surface.
The gas pressure above a liquid at equilibrium is called the vapor pressure. This is the pressure at which the rate of evaporation equals the rate of condensation, leading to a dynamic equilibrium between the liquid and its vapor.
The pressure caused by the collisions of particles in a water vapor with the walls of a container is known as vapor pressure. It represents the equilibrium pressure exerted by a vapor in thermodynamic equilibrium with its condensed phases (liquid or solid) in a closed system. At equilibrium, the rate of evaporation equals the rate of condensation, resulting in a constant pressure.
Here we have the reaction: water(l) <-> water(g) Water in the liquid state must be in equilibrium with the gas phase, so a very small part of this liquid water will pass to the gas state in order to reach a dynamic equilibrium.
Water saturation temperature is the maximum temperature at which water can exist in a stable liquid state at a given pressure. It is the temperature at which water vapor in equilibrium with liquid water exerts a partial pressure equal to the vapor pressure of pure water at that temperature.