Want this question answered?
The degree of temperature and exertion of pressure by the molten materials (magma) within the mantle is directly proportional to its depth. This means that, the deeper you go down the mantle the higher the degree of temperature and pressure exerted.
Increasing the temperature the number of particles remain constant and the pressure increase.
thez nuts
In a closed system with constant pressure and no input or output of heat, the gas temperature will remain constant. In that same system, if the pressure is increased, then the gas temperature will also increase. If pressure is decreased, then the gas temperature will decrease.
Because the temperature of the mantle is fairly constant and a decrease in a materials confining pressure will decrease its melting tempreature so mantle upwelling will lead to only small changes in tempraeture but a large decrease in confining pressure therefore the pressure loss is the dominat factor in melting.
The degree of temperature and exertion of pressure by the molten materials (magma) within the mantle is directly proportional to its depth. This means that, the deeper you go down the mantle the higher the degree of temperature and pressure exerted.
The weight of the rocks above the mantle results in high pressure.Diamonds need high temperatures and pressure to form from carbon. Diamonds form in the mantle in certain zones where conditions are right for them to do so.There just happens to be the right critical temperature-pressure-mineral environment in the mantle in certain zones for their formation.
The weight of the rocks above the mantle results in high pressure.Diamonds need high temperatures and pressure to form from carbon. Diamonds form in the mantle in certain zones where conditions are right for them to do so.There just happens to be the right critical temperature-pressure-mineral environment in the mantle in certain zones for their formation.
The melting temperature of materials is dependent on the pressure that is applied, whereby the higher the pressure, the higher the melting temperature. As such the rocks in the mantle are experiencing such a high pressure, that their melting point is driven up beyond the temperature within the Earth's mantle so they remain solid.
This happens at the Sun's center, where both the temperature and the pressure are greatest.This happens at the Sun's center, where both the temperature and the pressure are greatest.This happens at the Sun's center, where both the temperature and the pressure are greatest.This happens at the Sun's center, where both the temperature and the pressure are greatest.
The melting temperature of materials is affected by their confining pressure. The higher the pressure the higher the melting temperature. As such as you move deeper into the mantle, the tempraeture will increase, but because of the overlying material so to will the confining pressure which drives up the melting temperature. When high temperature mantle material moves nearer to the surface such as near a mid-ocean-ridge the confining pressure falls faster than the materials temperature and this can cause the melting point to drop below the temperature of the material leading to melting.
Mineralogy, pressure, temperature, and density differences exist among the 'layers' of the mantle.
Temperature Density and Pressure
The temperature ranges from 932 to 1,652-degrees F, at the top, where it meets the crust, to 7,230-degrees F at the lower mantle. Temperature and pressure increase with depth.
Answer The pressure increases when the temperature rises.
Their different properties are due to their chemistry, pressure, and temperature.
Increasing the temperature the number of particles remain constant and the pressure increase.