hesheng chemical
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Silicate Melting Point
A certain study in technical research, especially in the nature of minerals, among which Silicate Melting Point is the most important. Taste the melting degree of various kinds of silicic acids, and observe the law of their variation due to temperature, pressure and composition ratio.
Every time a ore sample is obtained, its chemical composition must be analyzed in detail and accurately measured. In different temperature and pressure environments, use special devices to observe its melting. See the combination of silicon, its melting degree is not the same, or due to the mixing of alkaline earth metals and heavy metals, its lattice changes, and its melting degree is also different.
If a silicate rock is used as a test, at the beginning, it is heated, and gradually reaches its first temperature, and the ore begins to soften, and then flows. This is its melting point. If you add other substances, try again, the melting point may rise or fall. The reason is the change of the force between atoms.
After years of research, there is a lot of evidence, and the change of the melting degree of clear silica is of great importance in geological structure and mineral formation. It can be used for prospecting and metallurgy, providing evidence and rationale, so that when the industry practices, they can use this as a reference and do good things.
Every time a ore sample is obtained, its chemical composition must be analyzed in detail and accurately measured. In different temperature and pressure environments, use special devices to observe its melting. See the combination of silicon, its melting degree is not the same, or due to the mixing of alkaline earth metals and heavy metals, its lattice changes, and its melting degree is also different.
If a silicate rock is used as a test, at the beginning, it is heated, and gradually reaches its first temperature, and the ore begins to soften, and then flows. This is its melting point. If you add other substances, try again, the melting point may rise or fall. The reason is the change of the force between atoms.
After years of research, there is a lot of evidence, and the change of the melting degree of clear silica is of great importance in geological structure and mineral formation. It can be used for prospecting and metallurgy, providing evidence and rationale, so that when the industry practices, they can use this as a reference and do good things.
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