Version 1
: Received: 1 October 2021 / Approved: 4 October 2021 / Online: 4 October 2021 (11:03:20 CEST)
How to cite:
Shcherbakov, I.; Makhmudov, K. The Mechanism of Destruction Under the Influence of Shock Waves. Preprints2021, 2021100047. https://doi.org/10.20944/preprints202110.0047.v1
Shcherbakov, I.; Makhmudov, K. The Mechanism of Destruction Under the Influence of Shock Waves. Preprints 2021, 2021100047. https://doi.org/10.20944/preprints202110.0047.v1
Shcherbakov, I.; Makhmudov, K. The Mechanism of Destruction Under the Influence of Shock Waves. Preprints2021, 2021100047. https://doi.org/10.20944/preprints202110.0047.v1
APA Style
Shcherbakov, I., & Makhmudov, K. (2021). The Mechanism of Destruction Under the Influence of Shock Waves. Preprints. https://doi.org/10.20944/preprints202110.0047.v1
Chicago/Turabian Style
Shcherbakov, I. and Khairullo Makhmudov. 2021 "The Mechanism of Destruction Under the Influence of Shock Waves" Preprints. https://doi.org/10.20944/preprints202110.0047.v1
Abstract
The spectra of the plasma emitted from the studied samples consist of several dozens of narrow bands superimposed on each other. Tables of spectral lines were used to interpret the spectra. It turned out that the largest number of bands corresponds to the radiation of positively charged ions and atoms of elements that make up the crystal lattices of minerals that make up the studied rocks. Thus, the spectra of the plasma emitted from quartz corresponded to the radiation of atoms and positively charged silicon ions, the charge of which varied from 1 to 4, as well as atoms and positively charged oxygen ions, the charge of which varied from 1 to 3. Positively charged ions and atoms of Si, O, K, Ca, Al and Na, which are part of the crystal lattices of quartz and feldspar, flew out of granites. Positively charged ions and Ca, C and O atoms flew out of the calcite.
Keywords
shock waves; mechanism and dynamics of destruction; quartz; granites; calcite
Subject
Environmental and Earth Sciences, Geophysics and Geology
Copyright:
This is an open access article distributed under the Creative Commons Attribution License which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.
