[HTML][HTML] A critical review of magnesium silicate hydrate (MSH) phases for binder applications
Hydrated magnesium silicate materials are promising binding materials for applications as
alternative cementitious materials and may offer a lower carbon footprint than conventional …
alternative cementitious materials and may offer a lower carbon footprint than conventional …
Properties of magnesium silicate hydrates (MSH)
D Nied, K Enemark-Rasmussen, E L'Hopital… - Cement and Concrete …, 2016 - Elsevier
Investigations of synthetic magnesium silicate hydrate (MSH) samples have shown that MSH
aged for 1 year can exhibit variable compositions with molar Mg/Si ratios in the range 0.7≤ …
aged for 1 year can exhibit variable compositions with molar Mg/Si ratios in the range 0.7≤ …
Formation of magnesium silicate hydrates (MSH)
The formation of magnesium silicate hydrates (MSH) with MgO to SiO 2 ratios from 0.7 to 1.6
has been studied at 20, 50 and 70° C. TGA and XRD data reveal that initially brucite and …
has been studied at 20, 50 and 70° C. TGA and XRD data reveal that initially brucite and …
An experimental investigation of antigorite dehydration in natural silica-enriched serpentinite
Piston cylinder experiments were performed to constrain the pressure and temperature
conditions for two high-pressure antigorite dehydration reactions found in silica-enriched …
conditions for two high-pressure antigorite dehydration reactions found in silica-enriched …
Serpentinization of the oceanic lithosphere and some geochemical consequences: constraints from the Leka Ophiolite Complex, Norway
Serpentinization of ultramafic rocks is an important process which modifies the petrophysical
and geochemical properties of the affected rock. The Leka Ophiolite Complex (LOC) …
and geochemical properties of the affected rock. The Leka Ophiolite Complex (LOC) …
Ab initio elastic properties of talc from 0 to 12 GPa: Interpretation of seismic velocities at mantle pressures and prediction of auxetic behaviour at low pressure
D Mainprice, Y Le Page, J Rodgers… - Earth and Planetary …, 2008 - Elsevier
Talc is a hydrous magnesium rich layered silicate that is widely disseminated in the Earth
from the seafloor to over 100 km depth, in ultra-high pressure metamorphism of oceanic …
from the seafloor to over 100 km depth, in ultra-high pressure metamorphism of oceanic …
Hydrolytic weakening of olivine at mantle pressure: Evidence of [1 0 0](0 1 0) slip system softening from single-crystal deformation experiments
To date, most of the experiments performed to quantify the hydrolytic weakening of olivine
single crystals have been performed at low confining pressure (and low water fugacities). In …
single crystals have been performed at low confining pressure (and low water fugacities). In …
The compressional behaviour and the mechanical properties of talc [Mg3Si4O10(OH)2]: a density functional theory investigation
In this work, we modelled the structure, the compressional behaviour and the physical
properties of talc over a wide range of pressure using a quantum mechanical approach …
properties of talc over a wide range of pressure using a quantum mechanical approach …
Phase transitions and mineralogy of the upper mantle
P Fumagalli, S Klemme - Treatise on Geophysics. 2, Mineral Physics, 2015 - air.unimi.it
The Earth's upper mantle extends from below the crust to a depth of about 410 km. Here, we
review the mineralogical and chemical composition of the upper mantle, especially with …
review the mineralogical and chemical composition of the upper mantle, especially with …
On topotaxy and compaction during antigorite and chlorite dehydration: an experimental and natural study
Dehydration reactions result in minerals' replacement and a transient fluid-filled porosity.
These reactions involve interface-coupled dissolution–precipitation and might therefore lead …
These reactions involve interface-coupled dissolution–precipitation and might therefore lead …