CdTe Thin films were deposited on glass substrates by thermal evaporation
method. The geometric thickness was calculated using interferometric method
based on reflectance curve recorded with the spectrophotometer. The XRD
analysis and optical char
acterizations of CdTe films with different optical
thicknesses reveals that the structure of the films is polycrystalline with
preferential orientation (111). The structure constant (a), crystallite size (D),
dislocation density (δ) and strain (ε) were calculated, and it is observed that the
crystallite size increases but micro-strain and dislocation density decreases with
increases in thin film thickness. The overall absorbance has been increased with
the film thickness and the direct band gap was obtained. It decreases with the
increase in the thickness of the films.
CdTe Thin films were deposited on silicon substrates by thermal
evaporation method. The geometric thickness was calculated using
interferometric method based on reflectance curve recorded with the
spectrophotometer. The Reflection of High-Energy E
lectron Diffraction
(RHEED) patterns and XRD analysis reveals that the structure of the films are
polycrystalline with preferential orientation (111). The structure constant (a),
crystallite size (D), dislocation density (δ) and strain (ε) were calculated, and it
is observed that the crystallite size increases but micro-strain and dislocation
density decreases with increases in thin film thickness. The composition of the
samples was determined by Energy Dispersive X-ray Analysis (EDX) and it is
found that the wt.% of Cd increases and the wt.% of Te decreases with the
increases of film thickness due to the re-evaporation of Te.
Mn doped tin oxide transparent conducting thin films were deposited at a
substrate temperature of 450°C by spray pyrolysis method. Structural
properties of the films were investigated as a function of various Mn-doping
levels (0, 1, 3, 5, 7 wt%) w
hile all other deposition parameters such as
substrate temperature, spray rate, carrier gas pressure and distance between
spray nozzle to substrate were kept constant.
Composition and origin of barite ores studied in Qerdaha
region. The fieldwork was done on geological sections belong to
Maastricht, from which many nodules like specimens were taken.
Both mineralogical and chemical composition of the
specimens w
ere determined using XRD. Petrological study was
done, as well.The mineralogical composition of most nodules
consisted of barite-calcite of various percentages. The nodules at
northern part of studied region consisted of barite or barite-calcite,
turned into calcite or calcite-barite phases towards south.
