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In this regard, it is important to compare the average/peak column abundances of Na and Fe in the main layer and also within Es.
A double layer photoanode structure with TiO2 nanoparticles (P25) as main layer and composite of titanium nanotubes (TNTs) and P25 as over-layer was introduced.
Fig. 1 Typical range-time Signal-to-Noise Ratio (SNR) contours showing (a) descending layers, (b) patchy layers above/below the main layer, and (c) echoes showing a seasonal shift in the height of occurrence observed in different seasons.
The Nd-Fe-B main layer and overlayers of Nd and Mo were deposited successively at substrate temperatures of (T_{mathrm {s}^{NFB}} =) 600 °C and (T_{mathrm {s}^{Nd}} = T_{mathrm {s}^{Mo}} =) 50 °C, respectively.
The surface nonuniformity of a coating usually results from a process in which the coating is continuously deposited to the main layer and also from surface treatment of already applied coatings (laser treatment, ion implantation, etc).. Surface nonuniformity can also be caused by the use of various materials when manufacturing the coating.
This creates a +1 charge on the main layer and this positive charge is balanced by anions (A n −) in the interlayer region, which also contains water molecules.
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Therefore, in the following mining, we should further improve water flooding reserves producing degree of the non-main oil layers, updip pinch-out site of the main layers and subdivision out of thin and poor layers.
Common-volume measurements have been used to study sporadic layers, dynamical perturbations of the main layers, and meteor trails.
Increasing both penetration depth and preload level involved the main layer response and caused alterations in hyperelastic and viscoelastic parameters of the tissue, such that for both layers, the shear modulus was increased (p < 0.01) while the rate and percentage of relaxation were decreased (p < 0.01).
The mesospheric echoes often show descending layers, patchy layers above/below the main layer between 70 and 80 km, and a strong seasonal dependence in the height of occurrence.
The following are the main conclusions drawn from the present study: (1) The mesospheric echoes often show descending layers, patchy layers above/below the main layer between 70 and 80 km, and a strong seasonal dependence in the height of occurrence.
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