The mineralogical constitution of the alumina cements of various composition (Table 1) were investigated by comparing the peaks of the X-ray patterns with those of the mixture of the synthetic minerals, CA, C
5A
3, C
3A
5, C
2AS and glassy substance (Fig. 1, Table 2).
The samples, except C and D (Table 1) were produced by an electric furnace. They, therefore, contained a small amount of FeO. The following results were obtained:
(1) CA was found to be the principal mineral of the cement.
(2) The samples with more than 35% CaO and less than 56% Al
2O
3 contained C
5A
3.
(3) The samples with more than 57% Al
2O
3 and less than 34% CaO contained C
3A
5.
(4) All samples contained C
2AS. The samples with more than 35% CaO contained a small amount of C
2AS together with β-C
2S.
(5) Fairly large crystals of C
2AS were found in the samples with more than 5.2% SiO
2, while no such large crystals did not exist in the samples with less than 5% SiO
2.
(6) The residue insoluble in N/2 HCl was CaTiO
3. Also C
3A
5 was slightly soluble in N/2 HCl (Fig. 2).
Shrinkage on heating the castable refractories prepared from these cement and usual or light weight chamotte was tested.
At 1200°C the component of the cement acted upon the cristoballite of the chamotte to form C
2AS, while above 1300° CAS
2 was formed together with glassy substance. The more the CaO content of the cement the more was the amount of CAS
2 thus formed.
When 72 parts of the chamotte and 28 parts of the CaO rich (37-39% CaO) cement were used the refractories swelled in the case of usual chamotte, or shrinked slightly in the case of light weight chamotte. However, such cement caused the softening of the refractories at lower temperature. When the refractories were heated under small load, i.e. 110-190g/cm
2, those prepared with CaO rich cement deformed easily.
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