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When c in the BET equation is greater than 1, a type II isotherm is produced. When employing the BET approach, this is the most typical isotherm that is obtained.
isotherm, a line connecting places on a map or chart that have the same temperature. Isotherms are frequently used in meteorology to display the temperature distribution at the Earth's surface or to represent constant levels or constant pressure on a chart. The properties of heat flow into soil, for instance, are easily visualized from a graph showing temperature as a function of depth and time. They are also used to depict the time fluctuation of temperature with height in the atmosphere or with depth in soil or water. Plotting the temperature for each place as a function of day and season (vertical axis) makes it easy to compare thermal conditions (horizontal axis).
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