Well, first of all that isn't a question. Second of all, When subjected to high temperature and pressure, such as the earth, the center of the earth is solid. as you progress outward, it becomes more liquidy.
Graphite has its own atomic structure of its basic carbon atoms. Subjecting it to very high temperature and pressure would not change its structure. Carbon, when subjected to very high temperature and pressure can be crystallized into diamond structures.
When a gas is subjected to extremely high pressure, its volume decreases and its particles are forced closer together, increasing the density of the gas. This can lead to changes in the physical properties of the gas, such as a decrease in its volume and an increase in its temperature.
The temperature varies with its pressure. If pressure high the condensing temperature also high. please be more specific, can someone please provide more specifics to this?
To make oxygen a liquid, it must be cooled to a temperature below its critical temperature of -118.57 degrees Celsius and be subjected to high pressure. This will cause the oxygen molecules to come close together and transition from a gas to a liquid state.
Temperature is more important than pressure in sterilization because high temperatures are able to denature proteins and destroy microorganisms, while pressure alone may not be sufficient to achieve sterilization. The combination of high temperature and pressure ensures that all microorganisms are killed, providing a more effective sterilization process.
High temperature and pressure can cause rocks to change their forms. This is known as metamorphic.High pressure and high temperature can cause rocks to change forms. This is known as metamorphic.
Metamorphic rocks are produced when other rocks are subjected to high temperature and pressure underground. This process causes their mineral composition, texture, and structure to change, resulting in the formation of metamorphic rocks like marble, slate, and schist.
Metamorphism can occur through contact metamorphism, where rocks are altered by heat from nearby magma; regional metamorphism, where rocks are subjected to high pressure and temperature over a large area; burial metamorphism, where rocks are subjected to increased pressure from being buried deep underground; and dynamic metamorphism, where rocks are deformed under high pressure but low temperature conditions along faults or shear zones.
Metamorphic rock is formed when existing rocks are subjected to high temperature and pressure, causing them to recrystallize and change their mineral composition without melting. Examples of metamorphic rocks include marble, slate, and schist.
Metamorphic rocks are formed when existing rocks are subjected to high pressure and temperature deep within the Earth's crust. This process causes the minerals in the original rocks to recrystallize into new forms, resulting in metamorphic rocks like marble, slate, and gneiss.
Metamorphic rocks are produced from other types of rocks (igneous, sedimentary, or existing metamorphic rocks) under high temperature and pressure conditions. The existing rocks undergo changes in mineral composition and texture without melting. Examples of metamorphic rocks include marble, schist, and gneiss.
metmorphic rack
By high pressure and temperature
Metamorphic rocks result from the alteration of existing rocks due to high temperature, pressure, and/or the presence of chemically active fluids. This process typically occurs deep within the Earth's crust where rocks are subjected to intense heat and pressure, causing them to recrystallize and reorganize into new forms.
Metamorphic rocks form when rocks are subjected to high heat, high pressure, hot mineral-rich fluids or, more commonly, some combination of these factors.
Graphite has its own atomic structure of its basic carbon atoms. Subjecting it to very high temperature and pressure would not change its structure. Carbon, when subjected to very high temperature and pressure can be crystallized into diamond structures.
Metamorphic rocks are formed from other types of rocks under high temperature and pressure. Examples of metamorphic rocks include marble, slate, and schist.