The mixtures of silicious volcanic glass (shorten as v.g., 74.76% SiO
2, 13.36% Al
2O
3, 0.60% Fe
2O
3, 1.73% CaO, 0.69% MgO, 4.00% Na
2O, 3.27% K
2O, 0.61% Ig. loss) separated from the original Shirasu and carbon black (shorten as C) were heated at temperatures from 1300 to 1450°C for 1 to 10h under N
2 gas flow. As the reaction products, Si
2ON
2*, β′-Si
3N
4, α-Si
3N
4, AlN and β-SiC were observed. Si
2ON
2* and β′-Si
3N
4 are solid solutions appeared in the system of Si
3N
4-AlN-SiO
2-Al
2O
3.
The kinds of reaction products and their amounts were altered according to C/v.g. value, reaction temperature, reaction time and impurities. Each of Si
2ON
2*, β′-Si
3N
4 and α-Si
3N
4 was mainly formed in a range of C/v.g. value, 0.2-0.3, 0.3-1 and above 1, respectively. Relative amounts of α-Si
3N
4 were increased with increasing C/v.g. value.
The nitridation of the volcanic glass by reducing process with carbon is induced below 1300°C and this temperature is lower than that of pure silica. β′-Si
3N
4 is considered to be formed via Si
2ON
2* from the volcanic glass but α-Si
3N
4 is accounted to be formed through vapour phase by the reaction between the volcanic glass and carbon under N
2 atmosphere.
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