The composition of ash can be divided into acidic and basic oxides according to their chemical properties, including L'oxides, alkaline, and so on. When the acid content exceeds 80% to 85%, the melting point is usually refractory; conversely, when the content of alkaline metal oxide in the ash increases, the melting point decreases. The melting of the ash depends mainly on its composition. The chemical melting point is higher and the melting point is higher. On the contrary, the melting point of ash is higher. Reduced ash always contains a certain amount of iron in different gas media (oxidizing or reducing), and exists under different valence conditions, iron is trivalent in oxidizing media, and iron is divalent in low reducing gases , Metallic iron is converted into high-metallic iron. The three melting points of the Duke of temperature in the high-temperature medium are the smallest, the highest intermediate and the smallest silicate silicate can produce a lower melting point in the ash. Therefore, in addition to the chemical composition of coal ash, the oxidation-reducibility of the external atmosphere is also an extremely important influencing factor, especially the high content of coal ash, the more significant the impact, some of the The ash melting point difference of coal ash measured in different atmospheres is 300℃.
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