Abstract
The dehydration dynamics of the of the Ca-saturated <1 μm size fraction of SWy-1 (low-charge montmorillonite) were studied at the crystal scale under isothermal conditions using X-ray diffraction with a position-sensitive detector (XRD-PSD) in the 30.170 °C temperature range. A total of 630 XRD patterns were modeled between 30 and 125 °C using a trial-and-error approach based on the direct comparison of experimental and calculated XRD patterns. The proportion of layers with different hydration states (bihydrated, mono-hydrated, and dehydrated) were determined in the temperature-time space as well as small variations of layer thickness within each hydration state. The results showed that dehydration produces complex structures with heterogeneous hydration states, some of which are stable (not transient) and remain at the end of the experiment. The evolution of other structural parameters (interlayer water content, layer thickness fluctuation) was consistent with previous reports of smectite hydration. For bihydrated layers, the amount of water molecules per interlayer cation indicated the presence of water molecules both coordinated and non-coordinated to the interlayer cation. The transition from bi- to mono-hydrated layers produced the maximum structural heterogeneity, with (1) strong interlayer thickness fluctuation (in individual layers), and (2) the presence of several elementary mixed-layer structures. In contrast, the transition from mono-hydrated to dehydrated layers occurs homogeneously within layers. Finally, the decrease in thickness of mono-hydrated layers only implied the removal of some water molecules forming the hydration shell of the interlayer cation.
© 2015 by Walter de Gruyter Berlin/Boston
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Articles in the same Issue
- Experimental evidence of sixfold oxygen coordination for phosphorus
- Dehydration of Ca-montmorillonite at the crystal scale. Part I: Structure evolution
- Dehydration of Ca-montmorillonite at the crystal scale. Part 2. Mechanisms and kinetics
- The high-pressure crystal structure of potassium hydrogen carbonate (KHCO3)
- Effect of Al3+ and H+ on the elastic properties of stishovite
- Investigation of synthetic Mg1.3V1.7O4 spinel with MgO inclusions: Case study of a spinel with an apparently occupied interstitial site
- Thermal expansion of deuterated hopeite, Zn3(PO4)2·4D2O
- Compression, thermal expansion, structure, and instability of CaIrO3, the structure model of MgSiO3 post-perovskite
- Crystal chemical relationships in the tourmaline group: Structural constraints on chemical variability
- The energetics of hematite dissolution in iron-oxide-rich melts: In situ high-temperature calorimetric studies
- A simple model of oscillatory zoning in magmatic plagioclase: Development of an isothermal undercooling model
- TEM investigation of Ca-rich plagioclase: Structural β uctuations related to the I1-P1 phase transition
- Crystal-chemistry of Ni in marine ferromanganese crusts and nodules
- Effect of structural transitions on properties of high-pressure silicate melts: 27Al NMR, glass densities, and melt viscosities
- Material conversion from paper-sludge ash in NaOH, KOH, and LiOH solutions
- High-pressure phase relations and crystal chemistry of calcium ferrite-type solid solutions in the system MgAl2O4-Mg2SiO4
- Origin of atoll garnets in eclogites and implications for the redistribution of trace elements during slab exhumation in a continental subduction zone
- Determination of the refractive index of particles in the clay and sub-micrometer size range
- Crystal chemistry of synthetic Ca2Al3Si3O12OH–Sr2Al3Si3O12OH solid-solution series of zoisite and clinozoisite
- Thermal infrared spectroscopy and modeling of experimentally shocked basalts
- P-V and T-V Equations of State of natural biotite: An in-situ high-pressure and high-temperature powder diffraction study, combined with Mössbauer spectroscopy
- Cation ordering in MgTi2O5 (karrooite): Probing temperature dependent effects with neutrons
- An order-disorder model for omphacitic pyroxenes in the system jadeite-diopsidehedenbergite- acmite, with applications to eclogitic rocks
- The high-pressure structural configurations of Ca0.2Sr0.8Al2Si2O8 feldspar: The I1̅-I2/c and I2/c-P21/c phase transitions
- Mechanisms of diamond oxidation and their bearing on the fluid composition in kimberlite magmas
- Brittle fracturing and fracture healing of zircon: An integrated cathodoluminescence, EBSD, U-Th-Pb, and REE study
- Galaxite, MnAl2O4, a spectroscopic standard for tetrahedrally coordinated Mn2+ in oxygen-based mineral structures
- Magmatic paragonite in trondhjemites from the Sierra del Convento mélange, Cuba
- Valence state partitioning of Cr and V between pyroxene-melt: Estimates of oxygen fugacity for martian basalt QUE 94201
- Crystal-structure refinement of Na-bearing clinopyroxenes from mantle-derived eclogite xenoliths
- High-pressure transition of CaCO3