In order to study the mode of development of needle crystals in the feldspar grains composing porcelain bodies, 10 (weight)% coarse potash or soda feldspar grains were mixed with 90% kaolinite or halloysite bodies and fired. Thin sections of the fired bodies were microscopically observed with following results.
(1) The temperatures at which needle crystals start to deposite within the feldspathic glass grains, are lower in the potash feldspar grains than in the soda ones, in the kaolinite bodies than in the halloysite ones, and furthermore, in the case of the slower heating rate than in the case of the faster (Table 2).
(2) In the potash feldspar grains, the needles are initially deposited at boundary parts with kaolinitic matrix and orientated normally to the boundary face. While, in the soda feldspar grains, the crystals are, from the earliest stage, deposited not only in the boundary parts, but also within the inner parts of the grains. The needles are scarcely normally orientated in the latter case.
(3) The needles grow with firing temperatures and holding time. Generally, they are longer in the soda feldspar grains than in the potash ones, and also in the kaolinite bodies than in the halloysite ones (Figs. 1 & 3).
(4) The amounts of the crystals are also increased with firing temperatures and holding time. Commonly, the crystals are more abundantly formed in the potash feldspar grains than in the soda ones, and also in the kaolinite bodies than in the halloysite ones (Figs. 2 & 4).
(5) It seems that diffusion of some components from the kaolinitic matrix is indispensable for the deposition of the needle crystals within the grains. The diffusion may have taken place through comparatively long distance within the kaolinitic matrix. This is inferred from the fact that the crystal growth in a feldspar grain is markedly decreased if it is located close to another grains.
(6) The crystals are grown either from the grains of decomposed clay minerals coming in contact with the feldspar glass, or from the crystalline kern formed within the melt. The former occurs when the diffusion is rather slow, thus resulting in a high concentration gradient, while the latter occures in the reversed case.
(7) The mechanism of the formation of the needle crystals may, principally, be similar for potash and soda feldspars, but, usually a remarkable difference is observed between the aspects of their crystal growth. The difference seems to be due to differences between the properties of their melts, especially viscosity.
(8) From the environment of their formation, as well as from their optical properties observed, the needle crystals are to be inferred as mullite.
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