Abstract:A flow-through cell for hydrothermal phase transformation studies by in situ and time-resolved neutron diffraction has been designed and constructed. The cell has a large internal volume of 320 ml and can operate at temperatures up to 573 K under autogenous vapor pressures (ca 8.5 Â 10 6 Pa). The fluid flow is driven by a thermosyphon, which is achieved by the proper design of temperature difference around the closed loop. The main body of the cell is made of stainless steel (316 type), but the sample compartm… Show more
“…Leucite crystals contain inherent 3D ordered networks of nanometer-sized lamellar twins (Fig. 7c and 7e), and Xia et al [49,51] demonstrat- these analcime nanocrystals have uniform size and crystallographic orientation due to epitaxial nucleation and growth facilitated by the similarity of the crystal lattice between leucite and analcime. The morphology of the nanocrystals is tuneable by ed that such highly ordered 3D patterns could be precisely preserved during hydrothermal pseudomorphic replacement reactions in pH-buffered NaCl solutions, resulting in 3D ordered arrays of analcime nanocrystals (Fig.…”
Section: Transformation Of Leucite (Kalsi 2 O 6 ) To Analcite (Naalsimentioning
confidence: 99%
“…[54] Leucite (KAlSi 2 O 6 ) was used as the precursor to synthesize analcime NaAlSi 2 O 6 . H 2 O as an illustration of this new synthesis route, [49,51] because leucite crystals are abundant in Nature, and their 3D ordered lamellar twinning has been studied in detail. [55] Conclusions CDR reactions are often extremely complex, since they result from a complex dynamic interplay between dissolution and precipitation, controlled critically by phenomena such as surface nucleation, porosity creation/destruction, and transport of aqueous species to and from the reaction front.…”
Section: Transformation Of Leucite (Kalsi 2 O 6 ) To Analcite (Naalsimentioning
Replacement reactions ('pseudomorphism') commonly occur in Nature under a large range of conditions (T 25 to >600 ˚C; P 1 to >5 kbar). Whilst mineral replacement reactions are often assumed to proceed by solid-state diffusion of the metal ions through the mineral, many actually proceed via a coupled dissolution and reprecipitation (CDR) mechanism. In such cases, a starting mineral is dissolved into a fluid and this dissolution is coupled with the precipitation of a replacement phase across the reaction front. In cases where there are close relationships between the crystal structures of the parent and newly formed minerals, the replacement can be topotactic (interface-coupled dissolution and reprecipitation). The kinetics and chemistry of the CDR route are fundamentally different from solid-state diffusion and can be exploited i) for the synthesis of materials that are often difficult to synthesise via traditional methods and ii) to obtain materials with unique properties. This review highlights recent research into the use of CDR for such synthetic challenges. Emphasis has been given to i) the use of CDR to synthesise compounds with relatively low thermal stability such as the thiospinel mineral violarite ((Ni,Fe) 3 S 4 ), ii) preliminary work into use of CDR for the production of roquesite (CuInS 2 ), a potentially important photovoltaic component and, iii) examples where the textures resulting from CDR reactions are controlled by the nature and texture of the parent phase and the reaction conditions; these being the formation of micro-porous gold and three-dimensional ordered arrays of nanozeolite of uniform size and crystallographic orientation.
“…Leucite crystals contain inherent 3D ordered networks of nanometer-sized lamellar twins (Fig. 7c and 7e), and Xia et al [49,51] demonstrat- these analcime nanocrystals have uniform size and crystallographic orientation due to epitaxial nucleation and growth facilitated by the similarity of the crystal lattice between leucite and analcime. The morphology of the nanocrystals is tuneable by ed that such highly ordered 3D patterns could be precisely preserved during hydrothermal pseudomorphic replacement reactions in pH-buffered NaCl solutions, resulting in 3D ordered arrays of analcime nanocrystals (Fig.…”
Section: Transformation Of Leucite (Kalsi 2 O 6 ) To Analcite (Naalsimentioning
confidence: 99%
“…[54] Leucite (KAlSi 2 O 6 ) was used as the precursor to synthesize analcime NaAlSi 2 O 6 . H 2 O as an illustration of this new synthesis route, [49,51] because leucite crystals are abundant in Nature, and their 3D ordered lamellar twinning has been studied in detail. [55] Conclusions CDR reactions are often extremely complex, since they result from a complex dynamic interplay between dissolution and precipitation, controlled critically by phenomena such as surface nucleation, porosity creation/destruction, and transport of aqueous species to and from the reaction front.…”
Section: Transformation Of Leucite (Kalsi 2 O 6 ) To Analcite (Naalsimentioning
Replacement reactions ('pseudomorphism') commonly occur in Nature under a large range of conditions (T 25 to >600 ˚C; P 1 to >5 kbar). Whilst mineral replacement reactions are often assumed to proceed by solid-state diffusion of the metal ions through the mineral, many actually proceed via a coupled dissolution and reprecipitation (CDR) mechanism. In such cases, a starting mineral is dissolved into a fluid and this dissolution is coupled with the precipitation of a replacement phase across the reaction front. In cases where there are close relationships between the crystal structures of the parent and newly formed minerals, the replacement can be topotactic (interface-coupled dissolution and reprecipitation). The kinetics and chemistry of the CDR route are fundamentally different from solid-state diffusion and can be exploited i) for the synthesis of materials that are often difficult to synthesise via traditional methods and ii) to obtain materials with unique properties. This review highlights recent research into the use of CDR for such synthetic challenges. Emphasis has been given to i) the use of CDR to synthesise compounds with relatively low thermal stability such as the thiospinel mineral violarite ((Ni,Fe) 3 S 4 ), ii) preliminary work into use of CDR for the production of roquesite (CuInS 2 ), a potentially important photovoltaic component and, iii) examples where the textures resulting from CDR reactions are controlled by the nature and texture of the parent phase and the reaction conditions; these being the formation of micro-porous gold and three-dimensional ordered arrays of nanozeolite of uniform size and crystallographic orientation.
“…21 Our previous in situ neutron diffraction kinetic study on this reaction was carried out at 230°C. 18 This study is to obtain the reaction kinetics at a second temperature, so that accurate reaction activation energy can be determined and thus the reaction rate under natural environments can be estimated.…”
Section: ͑2͒mentioning
confidence: 99%
“…3,16,17 To achieve a higher working temperature and pressure, and a larger fluid volume, we have previously constructed a thermosyphon driven flow-through cell and commissioned on Wombat, Australian's new high intensity powder diffractometer at the OPAL research reactor, run by Nuclear Science and Technology Organization ͑ANSTO͒. 18 The cell worked smoothly but the thermosyphon is sensitive to local temperature and air flow variations in the neutron guide hall. In practice, the temperature profile along the flow-through loop is not always stable during the course of hydrothermal reactions.…”
Section: Introductionmentioning
confidence: 99%
“…4͑b͔͒ gives rate constant k = 1.93Ϯ 0.14ϫ 10 −5 s −1 and the time exponent n = 2.04Ϯ 0.01. The reaction condition used in this study was identical to our previous in situ neutron diffraction study except the reaction temperature, 18 and the same nucleation Note that the total mass of the sample changed from 1.25 g at the beginning of the reaction to 0.92 g at the end because of the loss of small particles from the mesh tube; however, the mass of the stainless steel mesh tube remained constant at 0.57 g, so the mass fraction of ͑Fe,Ni͒ slightly increased during the process, serving as an excellent internal standard for quantification. ͑b͒ An Avrami plot yields the rate constant k and the time component n as shown in the plot.…”
The mechanism of nickel sulfide induced rapid crystallization of highly textured tungsten disulfide ( W S 2 ) thin films: An in situ real-time diffraction study J. Appl. Phys. 103, 063501 (2008) A hydrothermal cell with 320 ml internal volume has been designed and constructed for in situ neutron diffraction studies of hydrothermal crystallizations. The cell design adopts a dumbbell configuration assembled with standard commercial stainless steel components and a zero-scattering Ti-Zr alloy sample compartment. The fluid movement and heat transfer are simply driven by natural convection due to the natural temperature gradient along the fluid path, so that the temperature at the sample compartment can be stably sustained by heating the fluid in the bottom fluid reservoir. The cell can operate at temperatures up to 300°C and pressures up to 90 bars and is suitable for studying reactions requiring a large volume of hydrothermal fluid to damp out the negative effect from the change of fluid composition during the course of the reactions. The capability of the cell was demonstrated by a hydrothermal phase transformation investigation from leucite ͑KAlSi 2 O 6 ͒ to analcime ͑NaAlSi 2 O 6 ·H 2 O͒ at 210°C on the high intensity powder diffractometer Wombat in ANSTO. The kinetics of the transformation has been resolved by collecting diffraction patterns every 10 min followed by Rietveld quantitative phase analysis. The classical Avrami/Arrhenius analysis gives an activation energy of 82.3Ϯ 1.1 kJ mol −1 . Estimations of the reaction rate under natural environments by extrapolations agree well with petrological observations.
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