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The Mathematical Model of Interaction of Carbonaceous Fullerene Containing Mineral Shungate and Microporous Crystalline Aluminosilicate Mineral Zeolite with Water
Authors: Ignat Ignatov, Oleg Mosin
Number of views: 555
We studied the composition and structural properties of the amorphous, uncrystallized, fullerene analogous, carbon containing natural mineral shungite from Zazhoginskoe deposit in Karelia (Russian Federation) and the microporous crystalline aluminosilicate mineral zeolite (Most, Bulgaria) for evaluation of the mathematical model of interaction of these minerals with water. There are submitted data about the nanostructure, obtained with using of transmission electron microscopy (TEM-method), IR-spectroscopy (NES and DNES-method), as well as composition and physical chemical properties of these minerals. For evaluation of the mathematical model of interaction of these minerals with water, the methods of non-equilibrium spectrum (NES) and differential non-equilibrium spectrum (DNES) of water were applied. The average energy (∆EH... O) of hydrogen Н…O-bonds among individual molecules H2O after treatment of shungite and zeolite with water was measured at -0,1137 eV for shungite and -0,1174 eV for zeolite. The calculation of ∆EH... O for shungite with using DNES method compiles +0,0025±0,0011 eV and for zeolite -1,2±0,0011 eV. This result suggests the restructuring of ∆EH...O values among the individual H2O molecules in the samples, with a statistically reliable increase of local maximums in DNES-spectra.