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The fundamental unit is a tetrahedral complex consisting of a small cation such as Si tetrahedron and other mineral structures as determined by the relative sizes of the different ions.
This ionic coordination representation is no longer adapted to the requirements of geopolymer chemistry that is governed by covalent bonding mechanisms.
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100 to 1000 times faster than the polymerization of ortho-silicate, oligo-siloxo units.but since the introduction of the geopolymer concept by Joseph Davidovits, the terminology and definitions of 'geopolymer' have become more diverse and often conflicting.The examples below were taken from 2011 scientific publications, written by scientists with different backgrounds. Geopolymers consist of a polymeric Si–O–Al framework, similar to zeolites.The organic polymers comprise the classes of natural polymers (rubber, cellulose), synthetic organic polymers (textile fibers, plastics, films, elastomers, etc.) and natural biopolymers (biology, medicine, pharmacy).Raw materials used in the synthesis of silicon-based polymers are mainly rock-forming minerals of geological origin, hence the name: geopolymer.