What Is Evaporation?
Evaporation is a surface phenomenon by which a liquid changes into a vapour. The evaporation of liquid occurs at a temperature below the boiling point. The principle of evaporation states that in order for liquid molecules to evaporate, they must be close to the surface, moving in the right direction, and have enough kinetic energy to overcome the intermolecular forces present between the molecules in the liquid phase.
Evaporation Process and the Rate of Evaporation
The rate of evaporation is low when few molecules match certain requirements. Higher temperatures promote evaporation more quickly because a molecule's kinetic energy is directly related to its temperature. The more quickly moving molecules escape or evaporate, the lower the average kinetic energy of the remaining molecules and the lower is the temperature of the liquid. Evaporative cooling is another name for this process. This is also the reason why sweating causes the body to become cooler.
Higher gas-to-liquid flow rates and liquids with higher vapour pressure both tend to speed up the evaporation process. For instance, on a windy day as opposed to a calm day, washing drying on a clothesline (via evaporation) will occur more quickly. Heat, atmospheric pressure, which controls the humidity percentage, and air movement are the three main factors in evaporation. In a liquid, only a small percentage of the molecules have enough heat energy to escape as vapour. Until equilibrium is attained, where the liquid's evaporation is equal to its condensation, evaporation will continue. A liquid will evaporate in a closed space until the air is completely saturated.
The distinction between the liquid state and the vapour state is not clearly defined at the molecular level. In its place, a Knudsen layer exists where the phase is unknown. A distinct phase transition interface cannot be detected at the macroscopic scale since this layer is just a few molecules thick.
Factors Affecting Evaporation
The concentration of a chemical that is evaporating in the air: The chemical substance will evaporate more slowly if there is already a significant amount of the evaporating substance in the air.
Air flow rate: This is partially influenced by the concentration. The concentration of the substance in the air is less likely to increase over time, promoting quicker evaporation, if "fresh" air is constantly passing over the substance (air that is neither already saturated with the substance nor with other compounds). The reason for this is that when the flow rate increases, the boundary layer at the evaporation surface thins, reducing the diffusion distance in the stagnant layer.
Intermolecular forces: More energy is required to escape the force that is holding the molecules together in a liquid state. The enthalpy of vaporisation serves as a defining characteristic of this.
Pressure: If there is less pressure on the surface preventing the molecules from launching themselves, evaporation proceeds more quickly.
Surface area: A material with a greater surface area may evaporate more quickly because there are more surface molecules per unit of volume that may be able to escape.
The temperature of the substance: The molecules at its surface have more kinetic energy at higher temperatures, which causes them to evaporate more quickly.
Examples of Evaporation
Drying clothes in the sun, potholes and water drying up on the street, the cooling effect of sweat on the body, tea and other hot beverages cooling down, drying of nearby water bodies like lakes and ponds and the drying of wet hair are a few examples of evaporation.
Applications of Evaporation
Evaporation is used in numerous printing and coating processes, salt recovery from solutions, and drying a range of products like chemicals, paper, fabric, and timber.
Evaporation is frequently used as a pre-processing step for various laboratory tests, including spectroscopy and chromatography, in order to dry or concentrate materials. Centrifugal and rotary evaporators are two examples of the systems utilised for this.
Even if the air temperature is below the boiling point of water when garments are put on a washing line, water evaporates. Factors like low humidity, heat (from the sun), and wind speed up this process.
Water and other liquids are traditionally stored and cooled in the porous clay Matki/Matka, an object from India is to use evaporation to chill the water inside.
By simply passing dry air over a filter that has been soaked with water, evaporative coolers may effectively cool a building.
Naturally, evaporation of water from ponds, lakes and oceans plays a major role in the water cycle and causes rainfall.
Important Questions
1. What is evaporation? Give examples.
Evaporation is the process that changes liquid to gaseous vapour. Examples of evaporation are cooling down a hot beverage, drying clothes, sweating on a hot summer day, etc.
2. What are the factors affecting evaporation?
A liquid is transformed into a vapour by the process of evaporation. Surface area, temperature, humidity, and wind speed, the concentration of the substance in the surrounding air are a few factors that affect how quickly liquid evaporates.
Summary
When a liquid transitions from the liquid phase to the gaseous phase, evaporation takes place on the liquid's surface. High concentrations of the evaporating material in the surrounding air considerably slow down evaporation. The way that the liquid's molecules collide determines how much energy is transferred to one another.
In order to escape and enter the surrounding air as a vapour, a liquid molecule close to the surface must absorb enough energy to exceed the vapour pressure. Evaporative cooling is the process of reducing a liquid's temperature as a result of evaporation, which removes energy from the evaporated liquid.
Practice Questions
What type of change is evaporation?
Physical change
Chemical change
Electrochemical change
Thermal change
What will be the rate of evaporation if the humidity in the atmosphere is high?
Evaporation is higher
Evaporation is lower
Has no effect on evaporation
Both a and b
Answers:
(a)
(b)
FAQs on Evaporation: A Surface Phenomenon
1. How does cooling occur due to evaporation?
Cooling naturally results from evaporation. In order for matter to alter its state, it must either absorb energy or lose energy, according to the fundamental principle. To overcome their potential energy with kinetic energy when a substance changes phases from a liquid to a gas, matter molecules need energy.
As a result, the liquid absorbs this energy from its environment. When material reaches the boiling point, its molecules constantly absorb heat energy from its surroundings and cool the surroundings. Once reaching the boiling point, the molecules begin to separate from the liquid and transform into vapour.
2. Describe the meaning of condensation in the water cycle.
Gaseous water vapour turns into liquid water through the process of condensation. If the air is so full of water vapour molecules that it is unable to retain any more liquid, condensation due to saturation may happen. The emergence of clouds in the atmosphere is one example of this.
When a pocket of air can no longer contain any more water vapour, the molecules of water condense together until the air pocket begins to change into a liquid. If water vapour is cooled to the dew point or the temperature at which water vapour transforms to liquid, condensation may also take place.
3. Describe the meaning of precipitation in the water cycle.
The process through which water from the atmosphere returns to the surface of the earth is called precipitation. There are several states of matter or kinds of precipitation. For instance, there are two types of precipitation: liquid precipitation, or rain; and solid precipitation, like snow or hail.
Precipitation has many forms depending on the atmosphere's temperature. Condensation is the cause of precipitation. Water droplets in the cloud get bigger and heavier when condensation takes place and clouds form. When clouds are so densely populated with heavy water molecules, precipitation results as a result of the molecules' descent to earth.
