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when the vapor pressure is greater than 5 mm
An explosive eruption is caused by magma with a high content of water and silica. Non-explosive eruptions are caused by either lava because it is a thicker consistency, or magma with a low content of water and silica.
high pressure vapor
When you add a teaspoon of honey to water with vapor pressure, it will reduce the vapor pressure. The sugar in the honey leads to the pressure going down.
if a volcano is high in silica, it will be explosive. If its low in silica, it will be quiet. Two important things that determine whether an eruption will be explosive or quiet: # The amount of water vapor and other gases that are trapped in the magma. # If the magma is basaltic or grantic.
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when the vapor pressure is greater than 5 mm
The pressure is greater then 10 mm.
vapor pressure evaporation rate flashpoint upper explosive limit lower explosive limit
vapor pressure evaporation rate flashpoint upper explosive limit lower explosive limit
Lorne Elias invented the explosive dectorin 1985 Lorne Elias invented the explosive dectorin 1985
Yes. More gas trapped in magma leads to a more explosive eruption. Water vapor is the most abundant gas in magma.
For a gas or vapor to be flammable or an explosion hazard it must have a concentration in air between the Lower Explosive Limit (LEL) and the Upper Explosive Limit (UEL) for that particular gas or vapor.
At higher temperature the vapor pressure is higher.
An explosive eruption is caused by magma with a high content of water and silica. Non-explosive eruptions are caused by either lava because it is a thicker consistency, or magma with a low content of water and silica.
Lose Effloresce
high pressure vapor