
Chemical elements with low boiling points that easily evaporate, such as zinc, sodium, and potassium.Volatile elements are chemical elements and compounds with low boiling points that easily evaporate or sublimate at relatively low temperatures. In planetary science, this includes substances like water, carbon dioxide, nitrogen, and noble gases, as well as elements like zinc, sodium, and potassium that have low condensation temperatures. These materials are crucial for understanding planetary formation, as they tend to remain gaseous or icy in the outer regions of protoplanetary disks but condense closer to the star.
The term 'volatile' in a geological context dates back to the 19th century, but its importance in planetary science was established in the mid-20th century with the study of meteorite compositions and the development of condensation sequence models.
The behavior of volatiles is governed by their vapor pressure, which increases sharply with temperature. When a planet forms, the heat from accretion and radioactive decay can drive volatiles out of rocks and into the atmosphere, where they may escape into space if the planet's gravity is too weak or if the solar wind is strong. This process, called volatile loss, explains why inner planets like Earth are depleted in volatiles compared to outer planets and comets.
Understanding volatiles is essential for assessing the resources available on the Moon or Mars for future space missions, as water ice and other volatiles can be used for life support and rocket fuel.
Zinc, a volatile element, is so depleted in the Moon's rocks compared to Earth's that scientists use its isotopic ratios as evidence that the Moon formed from a giant impact that vaporized much of the early material.







