Articles | Volume 33, issue 1
https://doi.org/10.5194/ejm-33-39-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/ejm-33-39-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Review article
| 
05 Feb 2021
Review article |
| 05 Feb 2021
| 05 Feb 2021
Influence of water on the physical properties of olivine, wadsleyite, and ringwoodite
Key Laboratory of Geoscience Big Data and Deep Resource of Zhejiang
Province, School of Earth Sciences, Zhejiang University, Hangzhou 310027,
China
Qun-Ke Xia
Key Laboratory of Geoscience Big Data and Deep Resource of Zhejiang
Province, School of Earth Sciences, Zhejiang University, Hangzhou 310027,
China
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Wendi Liu, Yan Yang, and Qunke Xia
Eur. J. Mineral., 32, 305–310, https://doi.org/10.5194/ejm-32-305-2020, https://doi.org/10.5194/ejm-32-305-2020, 2020
Related subject area
Physical properties of minerals
Shear properties of MgO inferred using neural networks
Studies on the local structure of the F ∕ OH site in topaz by magic angle spinning nuclear magnetic resonance and Raman spectroscopy
Equation of state and sound wave velocities of fayalite at high pressures and temperatures: implications for the seismic properties of the martian mantle
Intracrystalline melt migration in deformed olivine revealed by trace element compositions and polyphase solid inclusions
Sequential dehydration of the phosphate–sulfate association from Gura Dobrogei Cave, Dobrogea, Romania
Anisotropic thermal transport properties of quartz: from −120 °C through the α–β phase transition
Determination of the H2O content in minerals, especially zeolites, from their refractive indices based on mean electronic polarizabilities of cations
Ashim Rijal, Laura Cobden, Jeannot Trampert, Hauke Marquardt, and Jennifer M. Jackson
Eur. J. Mineral., 35, 45–58, https://doi.org/10.5194/ejm-35-45-2023, https://doi.org/10.5194/ejm-35-45-2023, 2023
Short summary
Short summary
Using neural networks with experimental data, we infer the relationship between pressure, temperature and shear properties of MgO. Fixing the form of the relationship, which is a common practice, provides the properties that are largely constrained by the form and not the data. Our approach provides realistic uncertainties in shear properties, which should improve uncertainty quantification in interpretations of observed shear wave speed to infer the structure and dynamics of the Earth’s mantle.
Anselm Loges, Gudrun Scholz, Nader de Sousa Amadeu, Jingjing Shao, Dina Schultze, Jeremy Fuller, Beate Paulus, Franziska Emmerling, Thomas Braun, and Timm John
Eur. J. Mineral., 34, 507–521, https://doi.org/10.5194/ejm-34-507-2022, https://doi.org/10.5194/ejm-34-507-2022, 2022
Short summary
Short summary
We investigated the effect that fluoride and protons have on each other as structural neighbors in the mineral topaz. This was done using spectroscopic methods, which measure the interaction of electromagnetic radiation with matter. The forces between atoms distort the spectroscopic signals, and this distortion can thus be used to understand the corresponding forces and their effect on the physical properties of the mineral.
Frédéric Béjina, Misha Bystricky, Nicolas Tercé, Matthew L. Whitaker, and Haiyan Chen
Eur. J. Mineral., 33, 519–535, https://doi.org/10.5194/ejm-33-519-2021, https://doi.org/10.5194/ejm-33-519-2021, 2021
Short summary
Short summary
We performed experimental measurements of elastic parameters of fayalite. The idea is to better define the effect of olivine Fe content on these parameters and test how sensitive these are when adjusting mineralogical models to seismic data. The trend of the olivine shear modulus with Fe content is well defined, but that of the bulk modulus remains less constrained, and more experiments on olivines with different Fe compositions are needed.
Valentin Basch, Martyn R. Drury, Oliver Plumper, Eric Hellebrand, Laura Crispini, Fabrice Barou, Marguerite Godard, and Elisabetta Rampone
Eur. J. Mineral., 33, 463–477, https://doi.org/10.5194/ejm-33-463-2021, https://doi.org/10.5194/ejm-33-463-2021, 2021
Short summary
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This paper investigates the possibility for melts to migrate within extensively deformed crystals and assesses the impact of this intracrystalline melt percolation on the chemical composition of the deformed crystal. We here document that the presence of melt within a crystal greatly enhances chemical diffusive re-equilibration between the percolating melt and the mineral and that such a process occurring at crystal scale can impact the large-scale composition of the oceanic lithosphere.
Delia-Georgeta Dumitraş and Ştefan Marincea
Eur. J. Mineral., 33, 329–340, https://doi.org/10.5194/ejm-33-329-2021, https://doi.org/10.5194/ejm-33-329-2021, 2021
Short summary
Short summary
The low-temperature transformations of phosphate and sulfate sequences in the fossil guano from a Romanian cave were investigated using a mineralogical and chemical approach, resulting in the finding of a quite exotic mineral association, including the rare minerals francoanellite and monetite. The dehydration process of primary guano minerals seems driven by exothermic reactions at local scale (e.g., oxidation of ammonia, organic matter, allogenic pyrite or other organic compounds).
Simon Breuer and Frank R. Schilling
Eur. J. Mineral., 33, 23–38, https://doi.org/10.5194/ejm-33-23-2021, https://doi.org/10.5194/ejm-33-23-2021, 2021
Short summary
Short summary
The knowledge of physical properties of quartz as an abundant rock-forming mineral in the Earth’s crust allows for a better understanding of its dynamic processes. The thermal transport properties of single-crystal quartz are studied between –120 °C and 800 °C using a laser flash method. First, low-temperature data as well as the role of the low-to-high quartz phase transition (e.g. a transition-related non-ballistic radiative transfer) and size effects on thermal diffusivity are discussed.
Reinhard X. Fischer, Manfred Burianek, and Robert D. Shannon
Eur. J. Mineral., 32, 27–40, https://doi.org/10.5194/ejm-32-27-2020, https://doi.org/10.5194/ejm-32-27-2020, 2020
Short summary
Short summary
It is shown here that the H2O content of hydrous minerals can be determined from their mean refractive indices with high accuracy. This is especially important when only small single crystals are available. Such small crystals are generally not suitable for thermal analyses or for other reliable methods of measuring the amount of H2O. The results are compared with the observed H2O content evaluating 157 zeolite-type compounds and 770 non-zeolitic hydrous compounds, showing good agreement.
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Short summary
Water plays an important role in the physical properties (i.e., diffusivity, electrical conductivity, thermal conductivity, sound velocity, and rheology) of olivine, wadsleyite, and ringwoodite. Remarkably, there are numerous discrepancies and debates between experimental and theoretical studies. Here we provide a comprehensive review of the recent advances in the influence of water on the physical properties of olivine, wadsleyite, and ringwoodite, together with their applications.
Water plays an important role in the physical properties (i.e., diffusivity, electrical...
