[key-uh-luh-nahyt] /ˈkeɪ ə ləˌnaɪt/
a very common mineral, hydrated aluminum disilicate, Al 2 Si 2 O 5 (OH) 4 , formed by the alteration of other minerals, especially feldspar: the most common constituent of .
a white or grey clay mineral consisting of hydrated aluminium silicate in triclinic crystalline form, the main constituent of kaolin. Formula: Al2Si2O5(OH)4
A soft, white triclinic mineral occurring in friable masses. Kaolinite forms as the result of the hydrothermal alteration or weathering of feldspar. It is used in the ceramic industry. Chemical formula : Al2Si2O5(OH)4.
[key-uh-luh-nahyz] /ˈkeɪ ə ləˌnaɪz/ verb (used with object), kaolinized, kaolinizing. 1. to convert (minerals containing kaolinite) into by weathering.
kaolinosis ka·o·lin·o·sis (kā’ə-lə-nō’sĭs) n. Pneumoconiosis caused by the inhalation of clay dust.
[key-on] /ˈkeɪ ɒn/ noun, Physics. 1. a meson with strangeness +1 and either positive or zero electric charge, or its antiparticle, with strangeness −1 and either negative or zero electric charge. Symbol: K. /ˈkeɪɒn/ noun 1. a meson that has a positive or negative charge and a rest mass of about 966 electron masses, or […]
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