degassing
Quick Summary
Degassing refers to the release of gases from Earth's interior. This process is primarily associated with volcanic activity. Volcanic gases include water vapor, carbon dioxide, sulfur dioxide, and hydrogen sulfide, along with smaller amounts of other elements and compounds. These gases can be released from fumaroles or during explosive eruptions, forming hazardous gas clouds that can cause suffocation or poisoning.1
The origin of Earth's water and atmosphere is linked to degassing. It's theorized that gases, including water vapor, escaped from Earth's interior during its early history, forming the initial atmosphere and hydrosphere. While the exact timing and extent of this early degassing are uncertain, it's believed that the hydrosphere reached its present volume early in Earth's history, with ongoing minor degassing contributing to its volume today. The composition of volcanic gases depends on factors like temperature, pressure, and the specific volatile elements present in the magma.21
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hydrosphereOrigin and evolution of the hydrosphereGains would be from continuous degassing of Earth; the present degassing rate of juvenile water has been determined as being only 0.3 cubic km (about 0.07 cubic mile) per year. Water loss in the upper atmosphere is by photodissociation, the breakup of water vapour molecules into hydrogen and oxygen due…
Read MoreGains would be from continuous degassing of Earth; the present degassing rate of juvenile water has been determined as being only 0.3 cubic km (about 0.07 cubic mile) per year. Water loss in the upper atmosphere is by photodissociation, the breakup of water vapour molecules into hydrogen and oxygen due…
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seawaterThe early oceansWhether most of this degassing took place during core formation or soon afterward or whether there has been significant degassing of Earth’s interior throughout geologic time is uncertain. Recent models of Earth formation, however, suggest early differentiation of Earth into three major zones (core, mantle, and crust) and attendant…
Read MoreWhether most of this degassing took place during core formation or soon afterward or whether there has been significant degassing of Earth’s interior throughout geologic time is uncertain. Recent models of Earth formation, however, suggest early differentiation of Earth into three major zones (core, mantle, and crust) and attendant…
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