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Structure of Calcium Silicate Hydrate (C‐S‐H): Near‐, Mid‐, and Far‐Infrared Spectroscopy
The mid-, near-, and far-infrared (IR) spectra of synthetic, single-phase calcium silicate hydrates (C-S-H) with Ca/Si ratios (C/S) of 0.41–1.85, 1.4 nm tobermorite, 1.1 nm tobermorite, and jenniteExpand
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Relaxation in glassforming liquids and amorphous solids
The field of viscous liquid and glassy solid dynamics is reviewed by a process of posing the key questions that need to be answered, and then providing the best answers available to the authors andExpand
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Analytical methods for volatiles in glasses
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Hydrogen in Stishovite, with Implications for Mantle Water Content
Stishovite, the highest pressure polymorph of silicon dioxide, may be an important mineral in some regions of the Earth's mantle. Fourier transform infrared spectroscopy has been used to determineExpand
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Structural controls on the solubility of CO2 in silicate melts: Part II: IR characteristics of carbonate groups in silicate glasses
The characteristics of carbonate groups dissolved in silicate glasses have been investigated using FTIR spectroscopy. Glasses of natural melt compositions are compared with simple analogues. ThisExpand
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Structural controls on the solubility of CO2 in silicate melts: Part I: bulk solubility data
Abstract CO 2 solubility data are presented for a wide range of melt compositions in the following systems: SiO 2 –Na 2 O–Al 2 O 3 +CO 2 (SNA) at 2.0 GPa and 1600°C; SNA+CaO (SNAC) and SNA+MgO+CaOExpand
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Raman spectroscopic studies of carbonates part I: High-pressure and high-temperature behaviour of calcite, magnesite, dolomite and aragonite
The room-temperature Raman spectra of aragonite, magnesite and dolomite have been recorded up to 30 GPa and 25 GPa, respectively and no phase changes were observed during compression, unlike calcite.Expand
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Solubility, speciation and dissolution mechanisms for CO2 in melts on the NaAlO2–SiO2 join
CO2 solubility and speciation in melts along the NaAlO2–SiO2 join from Ne (NaAlSiO4) to a model rhyolite (Ry) composition (NaAlSi6O14), have been investigated as a function of pressure (10 to 25 kb)Expand
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A Raman spectroscopic study of shocked single crystalline quartz
We have carried out a Raman Spectroscopic study of single crystalline quartz samples shocked to peak pressures up to 31.4GPa. Samples shocked to above 22 GPa show shifts in peak positions consistentExpand
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Water solubility in aluminosilicate melts
We have compiled water solubility data for a wide range of natural and synthetic aluminosilicate melts in a search for correlations between melt composition and solubility. The published data revealExpand
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