2015
DOI: 10.1515/msp-2015-0008
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Synthesis of SiO2 nanopowders containing quartz and cristobalite phases from silica sands

Abstract: In this study, extraction and synthesis of SiO 2 nanoparticles from silica sands have been conducted by means of two different methods, i.e. dry method (method 1) and hydrothermal process (method 2). The basic difference between the two methods is in the extraction step. The two methods were compared in terms of being more efficient, economical, and superior in obtaining SiO 2 nanoparticles. The SiO 2 nanoparticles were characterized in terms of phase purity, crystallinity, Si-O functional bonding as well as p… Show more

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Cited by 79 publications
(36 citation statements)
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References 22 publications
(34 reference statements)
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“…Silica is an enormously abundant indigenous material; e.g. it is the main component from beach sand and can be extracted easily [28,29] (Fig. S1) and used directly without size selection (see Fig.…”
Section: Silica Integrationmentioning
confidence: 99%
“…Silica is an enormously abundant indigenous material; e.g. it is the main component from beach sand and can be extracted easily [28,29] (Fig. S1) and used directly without size selection (see Fig.…”
Section: Silica Integrationmentioning
confidence: 99%
“…Bands between 1 200 -1 180 cm -1 was assigned to the longitudinal optical (LO) modes of the Si-O-Si asymmetric stretching vibrations, bands at the interval of 1 128 -1 060 cm -1 was assigned to the transversal optical (TO) modes of the Si-O-Si asymmetric stretching vibrations, while a weak band around 657 cm -1 was assigned to Si-O stretching of the SiO 2 and finally the 468 cm -1 band was associated with Si-O symmetrical bending vibration. The detected vibrations reveal the presence of quartz [24]. Figure 2b shows the XRD patterns of the sands which are in total accordance with reflections corresponding to quartz SiO 2 ((JCPDS # 01-083-2465).…”
Section: Characterization Of Raw Materialsmentioning
confidence: 53%
“…The FT-IR spectrum of the silica reveals the silanol groups between 950-964 cm −1 , which are the characteristic FT-IR bands of the αquartz. The predominant absorbance bands at 1077 cm −1 were assigned to Si-O-Si asymmetric stretching vibrations [24,25]. On the other hand, the FT-IR spectrum of the β-carotene exhibits a narrow band at 1400 cm −1 associated with C-H stretching vibration mode, the bands observed between 1000-1200 cm −1 were attributed to the presence of the C-O and C-C-O stretching vibration modes.…”
Section: Characterization Methodsmentioning
confidence: 98%