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D8 advance eco powder diffractometer

Manufactured by Bruker

The D8 Advance ECO powder diffractometer is a laboratory instrument designed for X-ray powder diffraction analysis. It is used to identify and characterize crystalline materials by their unique diffraction patterns. The instrument provides reliable and reproducible data for a wide range of applications, including materials science, geology, and pharmaceuticals.

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2 protocols using d8 advance eco powder diffractometer

1

Fiber Characterization via Multimodal Analysis

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Fiber morphology and diameter were examined using scanning electron microscopy (Zeiss Gemini 500 SEM) with an accelerating voltage of 2 kV. ImageJ™ open source software (National Institutes of Health) was used to measure the mean fiber diameters. Fifty measurements were taken for each sample from three separate images. Energy Dispersive X-ray spectroscopy (EDX) spectra were collected with an accelerating voltage of 10 kV. Samples were sputter coated with carbon for SEM and EDX. Chemical structure was analyzed with Attenuated Total Reflection-Fourier Transform Infrared (ATR-FTIR) spectroscopy (ATR-FTIR Spectrometer PerkinElmer Frontier) at each reaction step. Each spectrum was an average of 128 scans obtained between 4000 and 600 cm−1 at a resolution of 4 cm−1. Four spectra were collected per sample. Alkyne substitution was confirmed with Raman spectroscopy (Renishaw InVia Confocal Raman microscope). Each spectrum was obtained between 3250 and 200 cm−1 with an excitation wavelength of 785 nm and a resolution of ~1 cm−1. Three spectra were collected per sample. Crystalline structure was analyzed with X-ray diffraction (Bruker D8 Advance ECO powder diffractometer, 1 kW Cu-Kα source). Three spectra were collected per sample.
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2

Quantifying Mineral Content in Bone Scaffolds

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X-ray diffraction (pXRD) was used to determine the relative mineral portion per quarter moving axially along the bone plug. Four partially demineralized bone scaffolds were lyophilized and quartered perpendicular to the axis, moving from mineralized to demineralized portions of the scaffold. Corresponding quarters from the four bone scaffolds were ground under liquid nitrogen using a mortar and pestle. The four powders were analyzed with pXRD using a Bruker D8 Advance ECO Powder Diffractometer (Bruker, Billerica, MA). The X-ray exposure were taken at a distance of 250 mm, 40 kV and 25 mA with Cu K-α radiation with a detector slit opening of 9 mm. The XRD data were processed using MATLAB and Microsoft Excel. This experiment was performed four times to determine consistency.
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