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Boiling is the rapid vaporization process of liquid, which happens when the liquid is heated at its boiling point, which is the temperature at which the vapor pressure of the liquid is equal to the pressure exerted on the liquid by the surrounding atmosphere. There are two basic types of boiling, critical heat flux boiling and nucleate boiling. Transition boiling is intermediate with the elements of both types. The boiling point of water is 100 °C in celsius and 212 °F.
Boiling is the opposite process to condensation and is natural insofar as the sequence of states in which matter can appear as the liquid and gaseous ordered sequentially.
The fundamental explanation of the process has to do with the fact that in the liquid state, the molecules move constantly and are united to each other by attractive forces.
The molecules collide with each other, and the warming of the environment makes this agitation take place in a faster and more intense way: precisely the escape of the molecules outside the same mass to be lost in the atmosphere is the transformation to the gaseous form.
The point at which this phenomenon occurs is called the boiling temperature, and it is different for each element: in some, even at a temperature below zero degrees Celsius, this evaporation can occur.
This critical point, however, is directly associated with the atmospheric pressure conditions at which it occurs, since its definition can be said to be the point at which the vapor pressure equals the external atmospheric pressure.
See Also: Difference between evaporation and boiling
Here are some examples of the boiling process, detailing the temperature at which it occurs in each element:
See Also: Types of thermometers
1: Pressure
The greatest determinant of the boiling point of a liquid is the surrounding pressure. In an open system, the external pressure is most likely the earth’s atmosphere. Water, for example, reaches standard atmospheric pressure at 100 degrees Celsius. This measurement is taken at sea level, where the total weight of the Earth’s atmosphere presses on the water. As the elevation increases, the water may boil at a lower temperature. At the top of Mount Everest, the water boils at about 72 degrees Celsius.
2: Intermolecular Bonds
When we consider other liquids, more factors help determine the boiling point. Chief among them is the strength of the bonds between the molecules. Ethyl alcohol, for example, has a boiling point of 78.5 degrees Celsius at sea level. It is a liquid at room temperature and the bonds between its molecules are comparatively strong. In contrast, methyl ether has a “boiling” point of -25 degrees Celsius. At room temperature and sea level, methyl ether is a gas.
3: Solute, Solvents and Solutions
An effective way to raise the boiling point of a liquid is to add another ingredient. While sea-level water has a boiling point of 100 degrees Celsius, its boiling point can be increased by adding a solute, such as salt. A solvent is any substance in which another dissolves. The substance that dissolves is called the solute. When a solute dissolves in a solvent, a solution is created. A solution generally boils higher than the pure solvent.
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