D8 advance
The D8 Advance is a versatile X-ray diffractometer (XRD) designed for phase identification, quantitative analysis, and structural characterization of a wide range of materials. It features advanced optics and a high-performance detector to provide accurate and reliable results.
Lab products found in correlation
3 394 protocols using d8 advance
Characterization of NCM85 Doped Samples
Powder X-ray Diffraction Analysis
where I110 is the maximum intensity of the crystalline region at 20° and Iam is the maximum intensity of amorphous diffraction at 16°.
Structural Characterization of Ta2O5/TaC Composite
Characterization of Membrane Materials
The sample was adhered to the test bench with conductive adhesive for gold spraying; the operating voltage range was 10–20 kV. The thermal stability of the membranes was examined using thermal gravimetric analysis (TGA, STA449 C, NETZSCH, Selb, Bavaria, Germany) and differential thermal gravimetric (DTG). The tensile properties of materials were tested on an Instron 5566 universal testing machine (Intron, Boston, MA, USA). The tensile rate is 2.00 mm/min, the spline standard is 10×80 mm, and the film thickness is 0.50 to 0.80 mm.
X-ray Diffraction Analysis of Mixed and Pure Oxides
In-situ and Operando X-ray Analysis of P2 Phase Synthesis
condition for the desired P2 phase, in situ X-ray
diffraction (XRD) for synthesis was performed using an HTK1200N temperature
chamber installed on a Bruker D8 Advance diffractometer. At each designed
temperature, the temperature was held for 1 h for the XRD pattern
collection. Operando XRD of the samples was performed
on the Bruker D8 Advance diffractometer equipped with a molybdenum
source (λ = 0.709 Å). The in situ cell
was charged/discharged within a voltage domain of 1.5–4.5 V
at a rate of C/30. Each scan covered a 2θ range of 6.5–23°
in a time duration of 5000 s. The electrochemical cell used for the operando XRD measurement is similar to those used in our
previous publication.28 (link) Selected powder
samples were also tested using the synchrotron radiation source (λ
= 0.4539 Å) at beamline 17-BM at the Advanced Photon Source (APS)
at Argonne National Laboratory (ANL). Some additional synchrotron
experiments were also performed using 28-ID-2 beamline of the National
Synchrotron Light Source II (NSLS-II) at Brookhaven National Laboratory
and the 7-2 beamline of Stanford Synchrotron Radiation Lightsource
(SSRL). Morphological investigation and energy-dispersive X-ray spectroscopy
(EDS) mapping analysis of the samples was conducted using a field
emission scanning electron microscopy (FE-SEM, Zeiss, Ultra60).
Characterization of Calcium Phosphate Coatings
Quantitative Mineralogy of Dolostone
X-ray Diffraction Analysis of Co2FeO4 Catalyst
patterns were recorded with a Bruker D8 Advance using a Cu X-ray source
in the Bragg–Brentano configuration with a variable primary
divergence slit using an energy-dispersive position-sensitive LynxEye
XE-T detector (Bruker). The powder measurements and the quantification
of the crystallinity were conducted by mixing a CeO2 reference
(NIST SRM674b) and our powder sample in a 1:1 mass ratio. After rigorous
blending, the mixtures were deposited in a Si low background sample
holder. The mass fraction of the X-ray amorphous phase was calculated
via Rietveld refinement, in which the zero error, sample displacement,
lattice parameters, and size-induced broadening were taken into account.
The Rietveld refinement was jointly performed for the diffractograms
of the two Co2FeO4 samples mixed with the CeO2 standard as well as for the pure CeO2 standard
measured alone using the same structural parameters for the CeO2 as well as the zero error and the background signals from
the sample holder.
To record the diffractograms of Co2FeO4 before and after OER, the samples were prepared on
a carbon foil (0.125 mm, 99.95% purity, GoodFellow) and measured with
a Bruker D8 Advance in parallel beam configuration with a Goebel mirror
and an equatorial Soller slit (0.3°). The applied electrochemical
protocol is described in
Mineralogical Analysis of Sedimentary Samples
T(a) = Mass percentage of the oxide of the chemical element (a) in the sample
Mi = Mass percentage of mineral i in the material studied;
Pi (a) = Mass proportion of the oxide of the element (a) in the mineral i deduced from the ideal formula attributed to this mineral i.
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