Structure of GeO₂ Glass under Compression Using Molecular Dynamics Simulation

Nội dung text: Structure of GeO₂ Glass under Compression Using Molecular Dynamics Simulation

1. VNU Journal of Science: Mathematics – Physics, Vol. 37, No. x (2021) 91-101 Original Article Structure of GeO2 Glass under Compression Using Molecular Dynamics Simulation Nguyen Mai Anh*, Nguyen Thi Thu Trang, To Thi Nguyet, Nguyen Van Linh Ha Noi University of Science and Technology, 1 Dai Co Viet, Hai Ba Trung, Hanoi, Vietnam Received 14 December 2019 Revised 11 June 2020; Accepted 15 August 2020 Abstract: We have investigated the behavior of GeO2 at the temperature of 300 K and the pressure from 0 to 100GPa by using the molecular dynamics simulation (the model with 5499 atoms). The results show that the Ge-Ge, Ge-O bond distance increase but O-O bond distance decreases when increasing the pressure. We find that the peak splitting of Ge-Ge at high pressure corresponds with the Ge-O-Ge and O-Ge-O bond angles. We also find that O-Ge-O bond angle decreases, and Ge-O- Ge bond angle increases with pressure. The core-sharing-bond is major at ambient pressure, but fractions of edge and face-sharing-bonds increase with pressure. Keywords: GeO2, High pressure, Microstructure, Radial distribution functions (RDFs), Molecular Dynamics simulation, clusters. 1. Introduction Germanium dioxide (GeO2) is a compound formed as a passivation layer on pure germanium in contact with atmospheric oxygen. In different temperatures and pressures, GeO2 exists in α -quartz trigonal structure, rutile-like structure with tetragonal structure and an amorphous [1]. An amorphous form of GeO2 is similar to fused silica. The α-quartz-type structure has been studied by using both experiment [2- 4], simulation [5-7] and theory [8, 9]. The calculations of the geometric structure and the physical properties of rutile-type GeO2 phase are also investigated in many studies [10]. The amorphous form of GeO2 is researched in [2, 11]. ___ Corresponding author. Email address: anh.nm175671@sis.hust.edu.vn https//doi.org/ 10.25073/2588-1124/vnumap.4445 91
2. 92 N.M. Anh et al. / VNU Journal of Science: Mathematics – Physics, Vol. 37, No. x (2021) 91-101 Because of its importance in industry, GeO2 glass has been extensively studied both experimentally and theoretically. In ref.[2], Dong et.al investigate the pressure-induced structural changes and polyamorphism of GeO2 glasses by using X-ray and Neutron diffraction. Extended X-Ray Absorption Fine Structure (EXAFS) experiment reveals that structural transformation in GeO2 glass occurs in a wide pressure range up to 54 GPa. At low pressure ( 72.5 Gpa). In ref.[5], the authors also study the first peak splitting of Ge-Ge pair RDF. They investigate short range order (SRO) and intermediate range order (IRO) of GeO2 at 3500 K using molecular dynamics (MD), in pressure from 0 to 100 GPa. They found that GeO4 tetrahedra link to each other to form a tetrahedral network. As pressure increases, tetrahedral network transits to octahedral network (GeO6) via GeO5 polyhedra. At a middle pressure, GeO2 exists in three forms GeO4, GeO5, GeO6. GeO5-cluster reaches the maximum at 15-20 GPa. The authors found that it exists as an immediate configuration in structural transition process. Investigation shows that at low pressure, GeOx (x=4,5,6) link to each other by one common oxygen ( corner-sharing bond, see figure 11) and at high pressure, by a corner-sharing bond, edge-sharing bond (two common oxygenssee figure 11), and face-sharing bond (three common oxygens, see figure 11). At high pressure, the GeO5, GeO6 polyhedra are dominant and tend to link each other by edge-sharing and face-sharing bonds, which become edge-sharing and face-sharing clusters. In ref.[12], the structure of GeO2 glass is investigated at pressures up to 17.5(5) GPa using insitu time-of-flight neutron diffraction with a Paris–Edinburgh press employing sintered diamond anvils. At low pressure (5 GPa), it exists mainly in GeO4 units. In 5 to 10 GPa GeO4 units are replaced predominantly by GeO5 ones. At pressure beyond 10 GPa, GeO6 units begin to form. Shanavas et.al investigated GeO2 at the high-pressure and temperature using molecular dynamics simulations [6]. They found that GeO2 system has a stable phase at ambient conditions of rutile type, in which the Ge-O are octahedrally coordinated. The rutile phase transforms to the tetrahedrally coordinated α-quartz phase as the temperature increases up to around 1280 K. Heating α-quartz, it transforms to β-quartz at above 1020 K and melts at 1378 K to form a network-structure liquid. At 9 GPa, α-GeO2 transforms to a monoclinic phase. Their simulations on vitreous GeO2 displays a smoth variation of mixed coordinated state of 4, 5, 6 coordination in pressure between 6 to 10 GPa, as being reported by Guthrie et.al. The research also showed that at high pressures, liquid GeO2 transitions to a six-coordinated amorphous solid-like phase. Shanavas et.al [6] shows that Ge-O-Ge peak at 135o in the α-phase (at 300 K) and at 145o in β-phase (at 1100 K). The intertetrahedral Ge-O-Ge angle bond increases with temperature in 300 – 900 K temperature range. At higher temperature (900-1000 K) it increases strongly. However, it almost changes from 1000 K to 1500 K, decreases suddenlly from 1500 K to around 1600K and decrease to 1900K. When increasing the temperature, O-Ge-O angle does not change, but from 1500 to 1900K, it increases a little. At pressure from 0 to 20 GPa, O-Ge-O angle has
3. N.M. Anh et al. / VNU Journal of Science: Mathematics – Physics, Vol. 37, No. x (2021) 91-101 93 a peak at 90o and another small peak at 170o. At pressure from 0 to 20 GPa at 300 K and 1650 K, the interpolyhedral Ge-O-Ge angle has a small peak at 85o ascribable to edge-shared tetrahedra. Increasing the pressure, another peak appears around 90o, due to edge-shared octahedra. The study [7] using MD simulation (in the micro-canonical ensemble, with systems at densities ranged from 3.16 to 6.79 g/cm3, using a pairwise potential) shows that at around 3–7 GPa the main structural changes in amorphous GeO2 occur, changing from a network composed basically of GeO4 tetrahedra to the one composed of GeO6 octahedra. In the study of Mei and Shen et.al [4], GeO2 is investigated by using X-ray in pressure up to 15.7 GPa, the results show monotonic increase of the average coordination number of oxygen atoms around Ge with pressure from 4.2 at 5.1 GPa to 5.5 at 15.7 GPa. This reveals the structural transsition of silica glass under compression. However, the detail about the structural transformation is still not clarified. In this paper, we investigate the GeO2 model at different pressures, at 300K to find the change of RDFs, CN, angles of bonds and the connect of angles, distances and kinds of sharing bonds. We explain the peak splitting of Ge-Ge at high pressure, O-Ge-O bond angle decreases, and Ge-O-Ge bond angle increases with pressure. 2. Calculation Method We construct the models of germania glass with the two-body potential developed by Oeffner– Elliott (OE). The detail parameters of the potential are given in ref. [13]. The OE potential has been used in many works for a long time and is known to reproduce the main structural and mechanical properties of GeO2, see refs. [2, 6, 14-18]. In particular under pressure, the OE potential is known to reproduce the model with structure properties in good agreement with experiment [1-3, 12]. The glass models considered here contain 5499 atoms in cubic periodic simulation cells. They were obtained from a melt equilibrated at 6000 K. After that the model is cooled to 3500 K and compressed to different pressures in 0-100 GPa range. Next, the models are cooled to 300 K at cooling rate of 2.5 K/ps. Next, the models at different pressures are relaxed for a long time (106 time steps) to get equilibrated state. The structural properties are calculated by averaging over 1000 configurations during the last 5x104 time steps. 3. Results and Discussion In the present paper, we analyze the results of molecular dynamic simulation for amorphous GeO2 in 0-100 GPa pressure range, at 300 K. The structure of GeO2 glass under compression will be clarified. Coordination units: Figure 1 shows the pressure dependence of concentration of GeOx (x=4, 5, 6) and OGex (x=2, 3, 4). At 0 GPa, most of the Ge atoms have four-fold coordination (93.24%). The concentration of GeO4 decreases monotonously with the increase of pressure. At 100 GPa, its concentration is about 0.17%. At pressure of 0 GPa, the concentration of GeO5 is 5.9%, then increases to maximum value (50.6%), then decreases gradually to 23.8% at 100GPa. With increasing the pressure, the fraction of GeO6 monotonously increases from 0.86% at 0 GPa to 77.03% at 100 GPa. At high pressure (p>=60 GPa) , most of the Ge atoms have five-fold and six-fold coordination. The concentration of OGex (x=2, 3, 4) also depends on the pressure. At the pressure from 0 to 100 GPa, the fraction of OGe4 is small, it monotonously increases from 0% at 0GPa to 9.66% at 100 GPa. The fraction of OGe3 increases with pressure from 8.82% at 0GPa to 69.48% at 100GPa. The fraction of OGe2 monotonously decreases from 91.18% to 20.88% at pressure of 0-100GPa.
4. 94 N.M. Anh et al. / VNU Journal of Science: Mathematics – Physics, Vol. 37, No. x (2021) 91-101 Figure 1. Concentration of GeOx (x=4, 5, 6) and Ogex (x=2, 3, 4) as a function. Bond angle distribution (BAD): The O-Ge-O bond angle distribution (see Figure 2) in GeO4 (in 0- 40 GPa range) decreases from 105o to 100o with increasing pressure. The O-Ge-O bond angle o o o distribution in GeO5 in 0-100 GPa range has a main peak at around 85 -90 and a small peak at 165 - o 170 . Investigation of O-Ge-O bond angle distribution in GeO6 at 3-100GPa shows the same results as GeO5. Figure 2. Fraction of angle of O-Ge-O in GeOx (x= 4, 5, 6). The Ge-O-Ge bond angle distribution in OGe4 has one peak and two subpeaks in the left and right (see figure 3). The position of corresponding peaks are at 75o, 90o and around 125-130o. Investigating o o OGe3 in 0-100GPa, we find that from 0 to 3 GPa, Ge-O-Ge BAD has two peaks are around 85 -90 and o o 115 -120 but from 6 to 100 GPa, the results show the same as OGe4 at pressure from 30 to 100GPa. Investigating OGe2 in 0-100GPa range, we find that from 0 to 6 GPa, Ge-O-Ge BAD has two peaks at o o o o around 85 -90 and 125 -130 but in 9-100 GPa range, the Ge-O-Ge BAD of OGe2 has one peak and two smaller peaks in the left and right at around 75o -80o, 90o-95o and 125o-130o. Corner-, edge- and face-sharing bonds: Figure 4 shows that at low pressure (0 GPa), corner-sharing- bonds are dominant (94.94%), edge-sharing bond is 4.75% and face-sharing bond is 0.31%. At 6 GPa, It exists corner- and edge-sharing bond. The concentration of corner-sharing-bonds is about 83.34%, edge-sharing bonds are about 14.25% and face-sharing-bonds are about 2.41%. In high pressure
5. N.M. Anh et al. / VNU Journal of Science: Mathematics – Physics, Vol. 37, No. x (2021) 91-101 95 (100GPa), It exists three types: corner-sharing-bond with concentration of 68.82%, edge-sharing-bond concentration of 24.69% and face-sharing-bond concentration of 6.49%. We find that concentration of corner-sharing-bond decreases, fraction of face-sharing-bond increases. Figure 3. The Ge-O-Ge bond angle distribution in GeOx (x=2, 3, 4). Figure 4. Fraction of core-, edge-, face-sharing bond in pressure range. The size distribution of clusters: Table 1 shows that size of clusters decreases with increasing pressure, GeO4 units link to each other into the largest cluster at ambient pressure. At higher pressure, size of clusters is smaller, it means that the number of GeO4 decreases with pressure and they split into many smaller cluster. We also find that at high pressure (>40 GPa), the number of GeO4 clusters and the number of atoms in each cluster decrease. At 100 GPa, it has one cluster with 5 atoms. Table 1. The cluster of GeO4 (Na is the number of atoms of the clusters, Nc is the number of clusters having Na correspondly). 0GPa 6GPa 12GPa 20GPa 40GPa 60GPa 80GPa 100GPa Nc Na Nc Na Nc Na Nc Na Nc Na Nc Na Nc Na Nc Na 2 5 24 5 145 5-20 186 5-20 48 5 22 5 14 5 1 5 1 5304 5 9 8 21-40 6 21-40 4 9 2 9 1 3857 2 41-80 1 40-45 1 13 1 80-160 1 17 3 160-430
6. 96 N.M. Anh et al. / VNU Journal of Science: Mathematics – Physics, Vol. 37, No. x (2021) 91-101 Table 2 shows that in 12-40 GPa range, the GeO5 units forms clusters with size of 2000 to over 3000 atoms. At low pressure (0GPa), the number of clusters as well as their size are small. The size of GeO5 clusters increases and gets maximum at 20 GPa, then decreases with pressure. Table 2. The clusters of GeO5 (Na is the number of atoms of the clusters, Nc is the number of clusters having Na correspondly) 0GPa 6GPa 12GPa 20GPa 40GPa 60GPa 80GPa 100GPa Nc Na Nc Na Nc Na Nc Na Nc Na Nc Na Nc Na Nc Na 6- 6- 25 6-10 17 6 43 6-20 67 6-20 94 122 47 6-10 58 6-20 20 20 21- 21- 1 11-15 1 11 4 21-40 6 21-40 13 10 5 11-15 5 21-40 40 40 41- 41- 1 16-20 1 16 1 54 6 41-60 7 1 3 16-20 3 41-60 60 60 61- 1 21-25 1 33 1 86 2 61-80 6 1 78 3 21-25 4 61-80 80 81- 1 3348 1 3379 1 2432 1 1 156 1 26-30 2 81-100 100 101- 5 4 101-200 200 1 173 2 201-400 1 540 Table 3 shows that GeO6 forms clusters: At 0 GPa, the number and the size of the clusters are minimun. There are only 12 clusters, each of clusters has 7 to 14 atoms. Increasing pressure from 0 to 9 GPa, the number of clusters also the size of them increase. At 9 GPa, there are 119 clusters and the biggest cluster has 161 atoms. Then, increase the pressure, we find that the size of clusters increase and the number of clusters decreases. At 12 GPa, there are 106 clusters, the biggest cluster has 177 atoms. At pressure > 30 GPa, each cluster has more than 4000 atoms, it is maximum at 100 GPa with 5113 atoms. We find that at pressure > 40 GPa, the atoms convergeinto one cluster. The simulation model has 5499 atoms so the fraction and the concentration of GeO6 are dominant. Table 3. The clusters of GeO6 (Na is the number of atoms of the clusters, Nc is the number of clusters having Na correspondly) 0GPa 6GPa 12GPa 20GPa 40GPa 60GPa 80GPa 100GPa Nc Na Nc Na Nc Na Nc Na Nc Na Nc Na Nc Na Nc Na 9 7 94 7-20 78 7-20 12 7 1 4456 1 4851 1 4995 1 5113 2 11 4 21-40 16 21-40 1 11 1 14 1 42 6 41-60 2 13 1 45 3 61-100 1 16 2 101-200 2 18 1 20 1 41 1 3150
7. N.M. Anh et al. / VNU Journal of Science: Mathematics – Physics, Vol. 37, No. x (2021) 91-101 97 Radial distribution function (RDF): We find that the Ge-Ge RDF has many peaks at high pressure. From 0 to 3 GPa, the RDFs of Ge-Ge have one peak. The first peak of RDF shows that Ge-Ge bond length is 3.16 Å at 0 GPa. From 6 to 9 GPa, the RDFs of Ge-Ge have one main peak and a small peak on the left. At 6 GPa, Ge-Ge bond length comprises two values of 2.7 Å and 3.2 Å. From 12 to 100 GPa, the RDFs of Ge-Ge have three peaks. At 100 GPa, it consists of three peaks showing that Ge-Ge bond lengths are 2.28, 2.64 or 3.32 Å. The first peaks of RDFs of Ge-O show Ge-O bond length is about 1.74 – 1.78 Å. The first peak positions shifts to the right with increasing pressure. The RDFs of O-O show that O-O bond length is about from 2.5 to 2.8 Å. The first peak shift to the left as pressure increases. At pressure beyond 9 GPa , the O-O RDF has a small peak at around 3.6Å after the first peak. 25 Ge-Ge 240 Ge-O 50 O-O 100 GPa 220 45 200 80 GPa 20 40 180 60 GPa 35 160 40 GPa 30 GPa 15 140 30 20 GPa 120 25 15 GPa 10 100 20 12 GPa 80 15 9 GPa 60 5 10 6 GPa 40 5 3 GPa 20 0 GPa Thedistributionradialfunction g(r) 0 0 0 2 3 4 5 1.7 1.8 1.9 2.0 2 3 4 Distance(Å) Figure 5. Radial distribution functions of Mg-Mg, Mg-O, and O-O pairs at different pressures. The peaks splitting of Ge-Ge RDF: The Ge-Ge distance depends on the bond type. At high pressure, we find that it has three peaks corresponding to corner-, edge- and face-sharing bonds (see figure 5). The distances of Ge-Ge are different with each sharing bond. The Ge-Ge distance depends on bond type. So, the Ge-Ge RDF has three peaks at high pressure. At low pressure (0GPa), it exists mainly corner- sharing bonds and has one peak. The distance of Ge-Ge also depends on the Ge-O-Ge bond angle. 2 2 ̂ 푒− 푒 = √ − 푒 + − 푒 + 2 ∗ − 푒 − 푒 표푠 푒 − − 푒 Figure 6 shows that at high pressure (100 GPa), The Ge-O-Ge BAD has three peaks at 75o, 90o and 130o. So, the Ge-Ge RDF has three peaks corresponding with Ge-Ge bond lengths of 2.28, 2.64 and 3.32 Å. At low pressure (0GPa), It has two peaks (one main peak and a small peak on the left), we find that the RDF has one peaks and a shoulder. We also find that the peaks of Ge-Ge RDF shift to the right with increasing the pressure. Because the distance of Ge-O increases with pressure, the distance of Ge-Ge also increases. Bond distance: Figure 7 shows that the peaks of Ge-O bond distance distribution in GeOx (x=4, 5, 6) shifts to the left with increasing the pressure. At pressure in 0-40 GPa range, Ge-O bond length in GeO4 decreases from 1.74 Å to 1.72 Å. At pressure from 3-100 GPa, Ge-O bond length in GeO5 decreases from 1.78Å to 1.76Å. At pressure from 3 to 100 GPa, the Ge-O bond length in GeO6 decreases from 1.88Å to 1.78Å.
8. 98 N.M. Anh et al. / VNU Journal of Science: Mathematics – Physics, Vol. 37, No. x (2021) 91-101 Figure 6. The Ge-O-Ge and O-Ge-O bond angle distribution at different pressures. Figure 8 shows the distance Ge-O of OGex(x=2, 3, 4). Investigating OGe4 in 20-100 GPa, we find that the Ge-O length bond decreases from 1.84Å to 1.8Å. At pressure of 0-100 GPa, the Ge-O length bond increases from 1.76Å (in 0GPa) to maximum value at 1.8Å (in 60GPa) then decreases to 1.78Å (in 100GPa). The Ge-O bond length increases from 1.74Å (in 0GPa) to maximum value at 1.78Å (in 30-40 GPa range) then decrease to 1.78Å (in 100GPa). The distance of Ge-O increases with the pressure: The Ge-O distance increases from 1.74 Å to 1.78 Å with pressure from 0 to 100 GPa. With increasing the pressure, the Ge-O CN increase, the result shows that coulomb repulsions between Ge and Ge, between O and O increase, leading to increasing Ge-O bond length. The Ge-O distances in GeOx (x=4, 5, 6) decreases with increasing pressure but the Ge-O distances in GeO6 > the ones in GeO5 > the ones GeO4 (see Figure 8). The fraction of GeO6 increases, the fraction of GeO4 and GeO5 decreases with increasing pressure so that the distances of Ge- O increases. Both of the Ge-O distances in OGe2 and OGe3 also increases with the pressure. The fraction of OGe2 and OGe3 increases with increasing pressure so the Ge-O distance increases. Figure 7. Fraction of distance of Ge-O in GeOx (x=4, 5, 6).
9. N.M. Anh et al. / VNU Journal of Science: Mathematics – Physics, Vol. 37, No. x (2021) 91-101 99 Figure 8. The Ge-O bond distance distribution in GeOx (x=2, 3, 4). The distance of O-O decreases when increasing the pressure: With increasing the pressure, the O- Ge-O bond angle decreases from 105o to 85o (see Figure 5) and the distance of O-O decreases from 2.8 to 2.5 Å. O-Ge-O BAD (Figure 5) has one more peak at 170-175o at high pressure so that the RDF of O-O has one peak at 3.6Å. This distance is approximately double the distance of Ge-O. 2 2 ̂ − = √ − 푒 + − 푒 + 2 ∗ − 푒 − 푒 표푠 − 푒 − 4. Conclusion The paper reported the microstructure of GeO2 glass by using the molecular dynamic method. It showed that: i/ The fraction of GeOx (x=4,5,6) and OGex (x=2, 3, 4) changes significantly in considered pressure range; ii/ The O-Ge-O bond angle decreases with increasing pressure. The change of Ge-O-Ge BAD under compression resulting in the change of Ge-Ge and O-O distance and formation of edge-, face-sharing-bonds. The fractions of edge-, face-sharing-bonds is increase with pressure and this is the cause of the first peak splitting of Ge-Ge RDF at high pressure; iii/ The glassy network structure of GeO2 changes significantly under compression, the GeO4 units tend to link each other forming GeO4 clutsers. Similar GeO5 and GeO6 also tend to form GeO5 and GeO6 clusters. This shows the polyamorphism in GeO2 glass at high pressure. The O-O distances decreases, meanwhile Ge-O distance increases with pressure. Figure 9. The structure of GeOx (x=4, 5, 6).
10. 100 N.M. Anh et al. / VNU Journal of Science: Mathematics – Physics, Vol. 37, No. x (2021) 91-101 Figure 10. Linkage between GeOx (x=4, 5, 6) in clusters. Figure 11. The structure of core-, edge-, face-sharing bonds. References [1] M. Micoulaut, L. Cormier, G.S. Henderson, The structure of amorphous, crystalline and liquid GeO2, J. Phys.: Condens. Matter 18 (2006) R753–R784. [2] Dong et.al, Revisiting local structural changes in GeO2 glass at high pressure. Journal of Physics: Condensed Matte (2017) 29 465401, [3] Yoshio Konoa,Curtis Kenney-Bensona, Daijo Ikutaa, Yuki Shibazakib, Yanbin Wangc, and Guoyin Shena, Ultrahigh-pressure polyamorphism in GeO2 glass with coordination number >6. PNAS (2016-03-29) vol 113, no.13, 3436–3441 www.pnas.org/lookup/suppl/doi:10. 1073/pnas.1524304113/-/DCSupplementa. [4] Q. Mei, S. Sinogeikin, G. Shen, S. Amin, C. J. Benmore, and K. Ding, High-pressure x-ray diffraction measurements on vitreous GeO2 under hydrostatic conditions. Physical review. B 81, 174113 (2010), [5] Tran Thuy Duong, Toshiaki Iitaka, Pham Khac Hung, Nguyen Van Hong, The first peak splitting of the Ge-Ge pair RDF in the correlation tonetwork structure of GeO2 under compression. Journal of Non-Crystalline Solids 459 (2017) 103–110, [6] Shanavas et.al, Classical molecular dynamics simulations behavior of GeO2 under high pressures and at high temperatures, Phys. Rev. B 73 (2006), 094120 [7] Joaquín Peralta, Gonzalo Gutiérrez, Pressure-induced structural transition in amorphous GeO2: a molecular dynamics simulation. Eur. Phys. J. B 87, 257 (2014) , [8] C. Sevik, C. Bulutay, J. Mater. Theoretical study of the insulating oxides and nitrides: SiO2, GeO2, Al2O3, Si3N4, and Ge3N4, Sci. 42 (2007) 6555–6565, [9] Q.J. Liu, Z.T. Liu, L.P. Feng, H. Tian, First-principles study of structural, elastic, electronic and optical properties of rutile GeO2 and alpha-quartz GeO2 Solid State Sciences 12 (2010) 1748–1755,
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