Sentence examples for mineral distribution is from inspiring English sources
The observed mineral distribution is most likely controlled by the weathering of clay minerals in the uppermost part of the profile and translocation of clay fractions down the profile (lessivage).
A polarization of mineral distribution was therefore generated between the lower and higher mineralized portion.
Mineral distribution was polarized between the lower and the higher mineralized portion of enamel by charged oxygen free radicals due to activation of permeated hydrogen peroxide.
A large mineral distribution was allowed in the range 2700 3200 mg/cm3 even in the dense mineralized outermost enamel surface rather than the deeper region of the ROI (Figs 1f, 2b).
The mineral distribution was measured in two-dimensions by chemical mapping using energy dispersive X-ray spectroscopy scanning electron microscopy (SEM EDX).
In accordance with the results obtained from the in vitro studies, matrix mineral distribution was disorganised, showing a woven appearance in tibial severe OA subchondral bone derived from patients undergoing knee replacement surgery.
This distribution is the result of the complicated interaction between water, ice and the mineral skeleton during the freezing process.
The elemental composition of mineral phases, and elemental distribution were determined using both energy-dispersive X-ray spectroscopy (EDX) within the SEMs above, and wavelength-dispersive spectrometry (WDS) using a Cameca SX-100 electron microprobe (EPMA) at the NHM.
In summary, mineral distribution of enamel is polarized by high-concentration hydrogen peroxide with an energizing source.
Growth, in particular reorganization of the root system architecture, mineral homeostasis and root hormone distribution were studied in Arabidopsis thaliana upon copper excess.
In particular knowledge of the mineral distribution along the pore walls is particularly scarce, despite the fact that mineral exposed in the pore space will be crucial in determining the rock-fluid interactions that occur during core-flooding experiments.
