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Solid state transitions of Bi2O3 nanoparticles

Published online by Cambridge University Press:  04 July 2014

Gerrit Guenther
Affiliation:
Institute of Materials Science, Technische Universität Darmstadt, Darmstadt 64287, Germany; and Otto Schott Institute of Materials Research, Friedrich Schiller University of Jena, Jena 07743, Germany
Olivier Guillon*
Affiliation:
Otto Schott Institute of Materials Research, Friedrich Schiller University of Jena, Jena 07743, Germany
*
a)Address all correspondence to this author. e-mail: o.guillon@fz-juelich.de

Abstract

The solid-state phase transitions of bismuth(III) oxide (Bi2O3) nanoparticles were investigated by complementary methods such as differential scanning calorimetry, differential thermal analysis with combined thermogravimetry and mass spectrometry, and high-temperature x-ray diffraction as compacted nanopowder. At room temperature the particles resided in the β-phase, which is usually a metastable high-temperature phase of bulk Bi2O3. The complementary experimental methods were linked and a nanophase (tetragonal β-phase) → bulk-phase (monoclinic α-phase) transition was identified which was preceded by crystal growth and evaporation of O and C containing species. It was also shown that the atmosphere (more precisely its absolute pressure) has an influence on the transition behavior. An interpretation was proposed that successfully explains all observations from this work and from literature: A sudden destabilization takes place around 735 K due to the loss of the stabilizing, carbonized surface. This leads to the observed transformation to the bulk-phase. But if the particles are smaller than a certain, critical size in the nanorange and are not allowed to grow, they remain in the nanophase until they melt.

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Articles
Copyright
Copyright © Materials Research Society 2014 
Figure 0

FIG. 1. Scheme of bismuth oxide structures. Red arrows indicate heating, blue arrows indicate cooling. The information is a composition from literature values cited in the text, mainly from Mehring73 and Klinkova et al.75 The transitions are reported to depend on multiple factors like maximum heating temperature and cooling rates. The absolute values of the temperatures and rates vary and no guarantee for the quantitative correctness can be given. Elevated temperatures in vacuum atmosphere can also provoke transitions (dashed arrows). Oxygen contents are from Klinkova et al.

Figure 1

FIG. 2. SEM micrographs of the commercial Bi2O3 powders. Nanopowder: (a) In the overview the agglomerates are visible. (b) The HR image shows the primary particles. The rough surface is caused by the sputtered AuPd film. Micrometer-size powder (c) composed of dense sintered agglomerates.

Figure 2

FIG. 3. X-ray diffractograms and Rietveld refinements measured at PETRA III, beamline P02.1 (λ = 0.207309 Å) in air. The structure of the commercial nanopowder is β-Bi2O3. The stars indicate reflexes of bismuth hydroxide which is a result of aging under ambient conditions.

Figure 3

FIG. 4. (a) DSC measurement of Bi2O3 nano- and micrometer-powder in argon at ambient pressure. Nanopowder: Minimum at 588 K and exothermic event at 738.6 K, endothermic α → δ phase transition at 1002.3 K and melting at approximately 1076 K. Micrometer-powder: The powder resides in the α-phase at RT and no exothermic events occur below 1002 K. (b) DTA-TG and MS measurement of the nanopowder between 300 and 820 K. The gravimetric curve (black) is plotted on the left and the MS signal on the right ordinate. The same transitions could be observed up to 750 K. The sample looses −1.6% of weight until 750 K and mass spectroscopy measures increased amounts of gas species. For example m = 30, 32, and 44 are shown. After the transition around 733 K mass loss and evaporation stop abruptly. The heat signal and dashed lines are just for orientation.

Figure 4

TABLE I. Temperatures for β → α, α → δ, and δ → l transitions measured with different methods and in varying atmospheres. The commercial Bi2O3 nanopowder (nano) and an ultra pure micrometer powder (micro) were measured.

Figure 5

FIG. 5. A 12° window with the major Bi2O3 reflexes during heating at 10 K/min captured in temperature steps of 15 K in (a) inert gas and (b) pumped to ∼1 Pa from ambient air. The β → α transition of the commercial Bi2O3 nanopowder took place between 717–733 K in air and inert gas and between 749–767 K in vacuum. First the (−111) and (112) reflexes of α-Bi2O3 around 29° formed and in the next step also the other reflexes had changed from the β- to the α-structure.

Figure 6

FIG. 6. Average, isotropic crystallite sizes calculated from reflex broadening of commercial β-Bi2O3 for the patterns shown in Fig. 5. It indicates grain growth started around 630 K. The crystallites grew until the temperature for the β → α transition was reached (dashed lines). In vacuum the particles were bigger and the transition occurred later. For illustration: A change from 50 to 70 nm would correspond to a doubling in volume (e.g., coalescence of two 50 nm particles).

Figure 7

FIG. 7. Scheme of the postulated stability diagram at constant T in attempt to explain the β → α transformation. No units and values are given as it is a qualitative illustration. A phase transformation occurs at G(α) = G(β) which depends on the slope of the curves. This in turn depends on the surface energy of the phase. As carbonization decreases γsv, the critical size is larger for carbonated than for decarbonated β-Bi2O3. In region (a) α-Bi2O3 is always the stable form. In the intermediate region (b) β-Bi2O3 is stable below and α-Bi2O3 above the temperature for decarbonization (∼735 K). Region (c) is the absolute stability region of β-Bi2O3. The scheme is valid for a moment of constant temperature. In reality particles will grow and change at T > 500 K. Also the partial pressures of gas species (which affect the equilibria of the decomposition reactions of the carbonate surface) are considered to be constant.