The depends a lot on what type of rock it is. Some will crumble eventually turning to dust. Meanwhile coal turns into diamonds. Some react violently to pressure and can explode.
What are two examples of how the solubility of gases increases at higher pressures?Read more: What_are_two_examples_of_how_the_solubility_of_gases_increases_at_higher_pressures
What are two examples of how the solubility of gases increases at higher pressures?Read more: What_are_two_examples_of_how_the_solubility_of_gases_increases_at_higher_pressures
metamorphic
Operating at even higher pressures can increase the risk of equipment failure, increase operating costs, and require additional safety measures. Additionally, operating at very high pressures may not significantly improve the process efficiency beyond a certain point, making it unnecessary to operate at even higher pressures.
By applying increasing pressures or temperatures which cause mineralogical and structural changes to the rock.
The rock cycle can recycle rocks from melting and giving pressures to sediments.
Pressure can increase the melting point of rock because higher pressures result in a higher melting point. However, if the rock is subjected to extremely high pressure without a corresponding increase in temperature, it may deform or undergo metamorphism rather than melting.
The factors that determine whether a rock behaves as a brittle or ductile material include temperature, confining pressure, strain rate, mineral composition, and presence of pre-existing fractures. Higher temperatures and lower confining pressures tend to promote ductile behavior, while lower temperatures and higher confining pressures favor brittle behavior. The strain rate, mineral composition, and presence of pre-existing fractures can also influence whether a rock will exhibit brittle or ductile behavior.
Higher pressures this gives more collisions which is a goal of the gases
(B)-slate
Rocks can deform under confining stress, but the amount of deformation depends on factors such as the type of rock, temperature, pressure, and time. In general, rocks are more likely to deform under higher temperatures and pressures. If the confining stress is higher than the rock's strength, it may deform or fail.
SAMMI shows 357 operating at higher pressures