minerals
Article
A Novel Open-System Method for Synthesizing Muscovite
from a Biotite-Rich Coal Tailing
Hamid Khoshdast
1,
*, Vahideh Shojaei
1
, Ahmad Hassanzadeh
2
, Tomasz Niedoba
3,
*
and Agnieszka Surowiak
3
Citation: Khoshdast, H.; Shojaei, V.;
Hassanzadeh, A.; Niedoba, T.;
Surowiak, A. A Novel Open-System
Method for Synthesizing Muscovite
from a Biotite-Rich Coal Tailing.
Minerals 2021, 11, 269. https://
doi.org/10.3390/min11030269
Academic Editor: Stavros Kalaitzidis
Received: 28 December 2020
Accepted: 2 March 2021
Published: 6 March 2021
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4.0/).
1
Department of Mining Engineering, Higher Education Complex of Zarand, 7761156391 Zarand, Iran;
v.shojaei@uk.ac.ir
2
Independent Scholar, Am Apostelhof 7A, 50226 Frechen, Germany; a.hassanzadeh@gmx.de
3
Department of Environmental Engineering, Faculty of Mining and Geoengineering, AGH University of
Science and Technology, al. Mickiewicza 30, 30-059 Krakow, Poland; asur@agh.edu.pl
* Correspondence: khoshdast@zarand.ac.ir (H.K.); tniedoba@agh.edu.pl (T.N.); Tel.: +48-126-172-056 (T.N.)
Abstract: According to the wide application of muscovite in various industries, many studies have
focused on its fabrication. However, the process of its synthesis faces long-standing challenges
mainly related to the elevated temperature and pressure ambient, together with time and cost-
consuming processes. This research work aims at synthesizing muscovite through a straightforward
and direct wet thermal oxidation of an ash sample produced from biotite-rich coal tailings. For this
purpose, the lab ash powder was mixed with 35% H
2
O
2
at the room temperature of 25
◦
C while
stirring at 480 rpm. Then, the temperature was gradually raised to 80
◦
C, and the process ran for
180 min. The dried product and the raw lab ash were characterized by the X-ray diffraction (XRD),
scanning electron microscopy (SEM) and Fourier-transform infrared spectroscopy (FTIR) methods.
The XRD results indicated that the biotite was efficiently converted to the muscovite as the number
of relevant peaks was significantly increased in the synthesized product’s pattern. The SEM and
FTIR results showed some structural changes, from pseudo-hexagonal in the starting material to
amorphous pseudo-crystals in the synthetic product, as well as the growth of the product’s crystals.
The crystallographic study and lattice parameter calculations revealed that the starting material
and product peaks matched to International Center for Diffraction Data (ICDD reference patterns of
01-080-1110 and 01-082-2450 for the biotite and the muscovite, respectively. Moreover, the calculation
of the mean crystallite size of the starting material and treated samples were obtained as 55 nm and
87 nm, respectively. Finally, according to the characterization properties of synthesized muscovite,
the presented method was introduced as an effective technique. Therefore, we highly suggest it for
further consideration and its development in future investigations.
Keywords: synthetic muscovite; biotite; oxidation; coal tailing; crystal structure
1. Introduction
Biotite and muscovite are two phyllosilicate minerals within the mica family that
are commonly found in igneous and metamorphic rocks. Biotite has a small number of
commercial uses, while muscovite has the greatest commercial value due to its special
properties. Muscovite mineral is chemically inert, dielectric, elastic, flexible, hydrophilic,
lightweight, reflective and refractive [1]. In addition, it is stable when exposed to electricity,
light, moisture and extreme temperatures. Muscovite, either in the form of sheet or ground,
is used in joint compound, paint, drilling mud, plastics, rubber, asphalt proofing and
electronic devices [2].
The generalized chemical compositions for biotite and muscovite as a potassium-
rich mica are K(Mg,Fe)
3
(AlSi
3
O
10
)(OH,F)
2
and KAl
2
(AlSi
3
O
10
)(OH)
2
, respectively [2].
Biotite is not very resistant to weathering and transforms into clay minerals. In contrast,
muscovite is more resistant to weathering than biotite. In addition to weathering, the
Minerals 2021, 11, 269. https://doi.org/10.3390/min11030269 https://www.mdpi.com/journal/minerals