We performed in situ infrared spectroscopic measurements of OH bands in a forsterite single crystal between -194 and 200 °C. The crystal was synthesized at 2 GPa from a cooling experiment performed between 1,400 and 1,275 °C at a rate of 1 °C per hour under high silica-activity conditions. Twenty-four individual bands were identified at low temperature. Three different groups can be distinguished: (1) Most of the OH bands between 3,300 and 3,650 cm-1 display a small frequency lowering (<4 cm⁻¹) and a moderate broadening (<10 cm⁻¹) as temperature is increased from -194 to 200 °C. The behaviour of these bands is compatible with weakly H-bonded OH groups associated with hydrogen substitution into silicon tetrahedra; (2) In the same frequency r...
We performed new experiments on incorporation of hydrogen in olivine at high pressures (2–12 GPa) an...
International audienceHydroxyl defects in pure forsterite are usually ascribed to incorporation of p...
Hydroxyl defects in pure forsterite are usually ascribed to incorporation of protons fully compensat...
We performed in situ infrared spectroscopic measurements of OH bands in a forsterite single crystal ...
International audienceWater incorporation in forsterite samples synthesized under low to medium sili...
International audienceSubstitutional mechanisms involving hydrogen incorporation at vacant tetrahedr...
International audienceSubstitutional mechanisms involving hydrogen incorporation at vacant tetrahedr...
International audienceThe infrared spectroscopic properties of selected defects in forsterite are in...
Experimental and theoretical evidence for the coupled substitution of B and H in synthetic forsterit...
Experimental and theoretical evidence for the coupled substitution of B and H in synthetic forsterit...
Experimental and theoretical evidence for the coupled substitution of B and H in synthetic forsterit...
Water distribution in the deep Earth represents one of the most important topics in the field of ge...
Hydrogen incorporation in olivine involves many OH-defects, which will control the hydrogen solubili...
International audienceSynthetic hydroxylated titanium-bearing and undoped MgO-buffered forsterite cr...
The hydroxyl of the gem-grade forsterite from Pakistan was measured by the polarized spectra at room...
We performed new experiments on incorporation of hydrogen in olivine at high pressures (2–12 GPa) an...
International audienceHydroxyl defects in pure forsterite are usually ascribed to incorporation of p...
Hydroxyl defects in pure forsterite are usually ascribed to incorporation of protons fully compensat...
We performed in situ infrared spectroscopic measurements of OH bands in a forsterite single crystal ...
International audienceWater incorporation in forsterite samples synthesized under low to medium sili...
International audienceSubstitutional mechanisms involving hydrogen incorporation at vacant tetrahedr...
International audienceSubstitutional mechanisms involving hydrogen incorporation at vacant tetrahedr...
International audienceThe infrared spectroscopic properties of selected defects in forsterite are in...
Experimental and theoretical evidence for the coupled substitution of B and H in synthetic forsterit...
Experimental and theoretical evidence for the coupled substitution of B and H in synthetic forsterit...
Experimental and theoretical evidence for the coupled substitution of B and H in synthetic forsterit...
Water distribution in the deep Earth represents one of the most important topics in the field of ge...
Hydrogen incorporation in olivine involves many OH-defects, which will control the hydrogen solubili...
International audienceSynthetic hydroxylated titanium-bearing and undoped MgO-buffered forsterite cr...
The hydroxyl of the gem-grade forsterite from Pakistan was measured by the polarized spectra at room...
We performed new experiments on incorporation of hydrogen in olivine at high pressures (2–12 GPa) an...
International audienceHydroxyl defects in pure forsterite are usually ascribed to incorporation of p...
Hydroxyl defects in pure forsterite are usually ascribed to incorporation of protons fully compensat...