The boiling point of water is the temperature at which water changes from a liquid to a gas. This occurs when the vapor pressure of the liquid is equal to the atmospheric pressure.
The boiling point of water in degrees Celsius is 100 degrees. This is equivalent to 212 degrees Fahrenheit and 373.15 Kelvin.
The boiling point of water decreases at higher altitudes because the atmospheric pressure is lower. This means that the vapor pressure of the liquid only needs to reach a lower point to equal the atmospheric pressure and cause boiling.
Yes, the boiling point of water can change with the amount of dissolved substances. This is because the dissolved substances can alter the vapor pressure of the liquid, making it harder or easier to reach the boiling point.
The boiling point of water is an important physical property that is used in many everyday applications. It is also used in scientific experiments and can help determine the purity of a substance.