4 research outputs found
Grain-sizereductionmechanisms and rheologicalconsequences in high-temperaturegabbromylonites of Hidaka, Japan
International audienceThe study of microstructures and crystallographic fabrics in a granulite-facies shear zone of the Hidaka Metamorphic Belt showed that the strong shearing localized within the mylonite resulted in the asymmetrical elongation of the inherited orthopyroxene porphyroclasts and the generation of fine-grained plagioclase and orthopyroxene layers as asymmetric tails of orthopyroxene porphyroclasts. The orthopyroxene porphyroclasts and the coarse plagioclase matrix surrounding them have a strong crystallographic preferred orientation acquired through deformation by dislocation creep. In contrast, the small orthopyroxene and plagioclase grains located in the tails have equant shapes and random fabric that are interpreted as the result of deformation by grain-boundary sliding. The small orthopyroxene grains are generated on the sheared rims of the orthopyroxene porphyroclasts by subgrain rotation, inheriting the orientation of the porphyroclasts before deforming by grain-boundary sliding (GBS) and losing this fabric. Additional mechanism of grain-sizereduction is the disruption of orthopyroxene porphyroclasts by synthetic shear zones localized on clinopyroxene exsolutions. The switch in deformation mechanism from dislocation creep to GBS, associated with the grain-sizereduction, yielded estimates of deviatoric stress one order smaller than lithostatic pressure. Besides, such rheological evolution attests of the mechanical softening during deformation, which contributed to the localization of the strain within the mylonite
Grain-size reduction mechanisms and rheological consequences in high-temperature gabbro mylonites of Hidaka, Japan
Lewis-Acid Sites of TiO<sub>2</sub> Surface for Adsorption of Organic Dye Having Pyridyl Group as Anchoring Unit
Adsorption
of an organic dye having a pyridyl group as an anchoring
unit (<b>NI4</b>) is studied on nanocrystalline TiO<sub>2</sub> surface by being compared with a similar dye having a carboxyl anchor
(<b>NI2</b>). Adsorption of both dyes followed a Langmuir isotherm,
and analysis of the isotherms showed that an adsorption equilibrium
constant of <b>NI4</b> is (1.1 ± 0.1) × 10<sup>3</sup> M<sup>–1</sup>, much smaller than (0.6 ± 0.05) ×
10<sup>5</sup> M<sup>–1</sup> for <b>NI2</b>, and amounts
of adsorbed dyes at saturation are similar to each other: [(1.5 ±
0.2) and (1.7 ± 0.3)] × 10<sup>14</sup> cm<sup>–2</sup> for <b>NI2</b> and <b>NI4</b>, respectively. Coadsorption
experiments with 4-carboxy TEMPO (<b>4CT</b>) and either <b>NI2</b> and <b>NI4</b> revealed that the adsorption sites
of <b>NI2</b> and <b>NI4</b> are different from each other.
This was supported by measurements of average nearest-neighbor interspin
distances of <b>4CT</b> radicals coadsorbed on TiO<sub>2</sub> by a spin-probe ESR technique. The above findings and elaborate
FT-IR studies demonstrated that <b>NI2</b> and <b>NI4</b> adsorb, respectively, on Brønsted- and Lewis-acid sites of
TiO<sub>2</sub> surface. The number of Lewis-acid sites evaluated
from the temperature-programmed desorption experiments of TiO<sub>2</sub> was in good agreement with the amount of <b>NI4</b> adsorbed on TiO<sub>2</sub> at saturation, providing a further confirmation
for Lewis-acid sites acting as a predominant adsorption site of <b>NI4</b>