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Physical and chemical properties of dust in the Pre-Aral region of Uzbekistan

Rustam BazarbayevDepartment of Physics and Mathematics, Urgench State University, Urgench, UzbekistanBiao ZhouCollege of Materials Science and Engineering, Sichuan University, Chengdu, 610065, ChinaAtabek AllaniyazovDepartment of Physics, Karakalpak State University, Nukus, Republic of Karakalpakstan, UzbekistanGuanggen ZengCollege of Materials Science and Engineering, Sichuan University, Chengdu, 610065, ChinaDamir MamedovDepartment for Solar Energy, Institute for Energy Technology, NO-2027, Kjeller, NorwayE. A. IvanitskayaDepartment of Materials Science, National Research Nuclear University (MEPhI), Moscow, RussiaQingzhu WeiHongqiang QianKomiljon YakubovDepartment of Physics and Mathematics, Urgench State University, Urgench, UzbekistanMohsen GhaliSchool of Basic and Applied Sciences, Egypt-Japan University of Science and Technology, Alexandria, EgyptSmagul KarazhanovDepartment for Solar Energy, Institute for Energy Technology, NO-2027, Kjeller, Norway. [email protected]
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Аннотация

Abstract The aim of this work is study of physical and chemical properties of dust of the Pre-Aral region of Uzbekistan such as Karakalpakstan and Khorezm that are located near the three deserts such as the Aralkum, Karakum, and Kyzylkum. The dust particles fell on glass have been collected in Karakalpakstan and Khorezm and studied systematically by employing wide range of methods. Particle volume vs size distribution has been measured with maximum around 600 nm and ~ 10 µm. The major and minor constituent materials present in the dust have been studied systematically by X-ray fluorescence spectroscopy, energy dispersive X-ray diffraction, and inductively coupled plasma optical emission spectroscopy. Main characteristic absorption bands corresponding to Si–O, Si–O-Si bonding in quartz and Fe–O bonds in hematite Fe 2 O 3 have been identified by infrared and Raman spectroscopy. Quartz, hematite, lime, corundum, magnesia, and several other trace minerals have been identified in the dust particles. X-ray diffraction peaks corresponding to quartz, hematite, and corundum are sharp and are found to be more crystalline with some level of disorder. Analysis of the particle size and crystallinity on human being has been performed: disordered or crystalline quartz can create the lung disease; the particles in the size of 0.5–0.7 µm may produce diseases such as chronic silicosis, silicosis, and silica tuberculosis whereas hematite might create lung disease. Dust particles worsen optical transmittance of glass of the panels. Graphical abstract

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