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the production of thymoquinone from thymol and carvacrol

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shared oxygen atoms with various regular arrangements, to form hundreds <strong>of</strong> different<br />

three-dimensional crystal frameworks (Kaduk et al. 1995).<br />

The framework structure encloses cavities containing pores <strong>of</strong> molecular<br />

dimensions. Their frameworks are made up <strong>of</strong> 4-connected networks <strong>of</strong> atoms. One way<br />

<strong>of</strong> thinking about this is in terms <strong>of</strong> tetrahedra, with a silicon atom in <strong>the</strong> middle <strong>and</strong><br />

oxygen atoms at <strong>the</strong> corners. These tetrahedra can <strong>the</strong>n link toge<strong>the</strong>r by <strong>the</strong>ir corners as<br />

seen in Figure 2.1. Zeolite Y has a faujasite type framework structure, with three<br />

different cavities or cages which are <strong>the</strong> large supercage, <strong>the</strong> sodalite cage <strong>and</strong> <strong>the</strong><br />

double 6-ring.<br />

The structural formula <strong>of</strong> a zeolite for a crystallographic unit cell is:<br />

Mx/n((AlO2)x(SiO2)y).wH2O<br />

Where M is <strong>the</strong> cation <strong>of</strong> valance <strong>of</strong> n, w is <strong>the</strong> number <strong>of</strong> water molecules. The<br />

ratio y/x (Si/Al ratio) usually has values <strong>of</strong> 1-5 depending upon <strong>the</strong> structure. The sum<br />

(x+y) is total number <strong>of</strong> tetrahedral in <strong>the</strong> unit cell (Breck 1974).<br />

Figure 2.1. Framework structure <strong>of</strong> zeolite Y<br />

(Source: Kaduk et al. 1995)<br />

The replacement <strong>of</strong> SiO4 tetrahedra by <strong>the</strong> (AlO4) - tetrahedral in <strong>the</strong> zeolite<br />

framework causes excess negative charge. Cations are needed to neutralize.<br />

Compensation <strong>of</strong> negative charge by associated cations such as; H + , Na + , K + , Ca +2 ,<br />

5

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