At high temperature, limestone undergoes thermal decomposition. The word equation is calcium carbonate decomposes when heated to calcium oxide and carbon dioxide. The chemical equation is CaCO3 + heat --> CaO + CO2.
Different types of limestone have varying amounts of calcium carbonate due to differences in their formation processes. Factors such as environmental conditions, mineral composition, and the presence of impurities can contribute to variations in calcium carbonate content. Additionally, geological processes such as pressure and temperature can also affect the composition of limestone.
Heat and pressure turn limestone into marble through the process of metamorphism, where the mineral composition and texture of the rock are changed. This transformation occurs as a result of high temperature and pressure altering the original calcium carbonate minerals of limestone into the interlocking crystals that characterize marble.
Yes, temperature can affect the production of ammonia from ammonium chloride. Generally, higher temperatures can increase the rate of the reaction, leading to more ammonia production. However, excessively high temperatures can also cause decomposition of ammonia.
Marbles ARE solid.
The process where limestone loses oxygen is called calcination. This involves heating the limestone to high temperatures, causing it to release carbon dioxide and leaving behind calcium oxide, also known as quicklime.
The limestone turns into marble because of the tremendous pressures and high temperatures.
Yes, temperature can affect the weathering of limestone. Higher temperatures can increase the rate of chemical weathering of limestone due to enhanced dissolution of minerals in the rock. Freeze-thaw cycles, which occur in areas with fluctuating temperatures, can also lead to physical weathering of limestone through the expansion and contraction of water within cracks.
High temperature=low viscosityLow temperature=high viscosity
Limestone can turn into the metamorphic rock called marble through a process of metamorphism involving high pressure and high temperature.
High temperature=low viscosityLow temperature=high viscosity
High temperature=low viscosityLow temperature=high viscosity
High temperature makes the volume greater.
It will decompose according to: CaCO3(s) --> CaO(s) + CO2
Sublimation is accelerated at high temperature.
At high temperature the solubility is increased.
Marble is a solid at room temperature. It is a type of metamorphic rock that forms from the recrystallization of limestone under high pressure and temperature.
If limestone undergoes contact metamorphism, it will typically turn into marble. Marble forms from the recrystallization of limestone under high temperature and pressure conditions.