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D max 3c x ray diffractometer

Manufactured by Rigaku
Sourced in Japan

The D/MAX 3C X-ray diffractometer is a laboratory instrument designed for the analysis of crystalline materials. It utilizes X-ray diffraction technology to provide information about the structure and composition of solid samples. The core function of the D/MAX 3C is to measure the diffraction pattern of X-rays interacting with the crystalline structure of the sample, allowing for the identification and quantification of the present crystalline phases.

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5 protocols using d max 3c x ray diffractometer

1

Structural Characterization of Nanomaterials

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The morphology and microstructure are measured on scanning electron microscope (SEM, 15 kV, JEOL 6500F). Moreover, 4-mercaptobenzoic acid (4-MBA) is purchased from Sigma-Aldrich Co Ltd. X-ray diffraction (XRD is performed on the Rigaku D/MAX 3C X-ray diffractometer with Cu Kα radiation (λ = 1.5418 Å)). The UV-Vis spectrum is obtained by Shimadzu UV-3600 spectrophotometer (Kyoto, Japan). The Raman spectrum is collected on Renishaw Raman with a spectral resolution of 1 cm−1 (London, UK, 2000 confocal microscope spectrometer). The Raman laser wavelength is 785 nm, the power is 500 mw, and the single acquisition time is 1000 ms.
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2

Comprehensive Characterization of Materials

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SEM characterizations were performed on a JEOL-6500F (JEOL LTD., Tokyo, Japan) scanning electron microscope with an acceleration voltage of 15 kV. X-ray diffraction (XRD) patterns were obtained using a Rigaku D/MAX 3C X-ray diffractometer (Rigaku Corporation, Tokyo, Japan) with Cu Kα radiation. Raman spectra were measured with a Renishaw Raman system at a laser wavelength of 633 nm. The laser beam was focused on the sample at 50 × long-range objective for characterization. The signal acquisition time was set to 10 s. Ultraviolet-visible (UV-Vis) spectra were measured by a SHIMADTU ultraviolet spectrophotometer (UV-3600).
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3

Characterization of Ag-Heteropolyacid Composite

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The loading amounts of Ag and H3PW12O40 in the composite films were determined by a Leeman Prodigy Spec inductively coupled plasma atomic emission spectrometer. X-ray diffraction (XRD) patterns were obtained on a Rigaku D/max-3c X-ray diffractometer (Cu Kα radiation, λ = 0.15405 nm). UV-Vis diffuse reflectance spectra (UV-Vis/DRS) were recorded on a Cary 500 UV-Vis-NIR spectrophotometer. X-ray photoelectron spectroscopy (XPS) was performed on a VG-ADES 400 instrument with Mg Kα-ADES source at a residual gas pressure lower than 10−8 Pa. Raman scattering spectra were recorded on a Jobin-Yvon HR 800 instrument with an Ar+ laser source of 488 nm wavelength in a macroscopic configuration. Field-emission scanning electron micrographs (FESEM) were obtained using a JEOL 6340 F scanning electron microscope. Nitrogen porosimetry was measured by a Micromeritics ASAP 2020. Surface areas were calculated by Brunauer-Emmett-Teller (BET) equation. Pore size distributions were calculated by BJH model based on the nitrogen desorption isotherm (samples were degassed for 1 h under vacuum at 363 K, and then for 12 h at 473 K). Transmission electron microscope (TEM) micrographs, high resolution TEM (HRTEM), and selected area electron diffraction (SAED) micrographs were recorded by a JEM-2100F HRTEM at an accelerating voltage of 200 kV.
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4

Soil Characterization Using XRD Analysis

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Standard methods were used to characterize the soil physicochemical properties such as pH, soil organic matter and total nitrogen, and total and available phosphate and potassium. Soil samples for the X-ray diffraction (XRD) analysis were prepared as previously described (Moore and Reynolds 1997 ; Laird 1999 ). Briefly, soil samples were first treated with 0.1 mol·L−1 HCl to remove free carbonates and then subject to wet oxidation with 30% H2O2 in order to remove the organic matter. Next, 0.5 mol·L−1 NaOH was used to adjust pH of the suspension to 7.3, and the fraction of <2 μm was separated by sedimentation. To further purify the clay, free ionic compounds were removed by adding sodium dithionate, sodium citrate, and sodium bicarbonate at the final concentration of 1.5 mol·L−1, 0.3 mol·L−1, and 1.0 mol·L−1, respectively. Magnesium-saturated samples were prepared and oriented on glass slides by the paste method (Theissen and Harward 1962 ).
X-ray diffraction was performed on a Japan Rigaku D/max-3C X-ray diffractometer with graphite-monochromatized Cu Ka radiation (λ = 0.154178 nm) following the manufacturer's recommendation. Standard minerals were used to develop relationships between XRD integrated intensity ratios and weight fraction ratios of mineral contents (Moore and Reynolds 1997 ).
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5

Characterization of Novel Compounds via Multi-Technique Analysis

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Single-crystal X-ray diffraction data were recorded on a Supernova diffractometer (Rigaku, Japan) equipped with graphite monochromated and Mo−Kα radiation (λ = 0.71073 Å). Powder X-ray diffraction (PXRD) patterns were collected using a D/Max-3c X-ray diffractometer (Rigaku, Japan). Four transform infrared spectroscopy (FT-IR) spectra were performed on a Spectrum Two spectrometer (PerkinElmer, United States). High-resolution mass spectrometry was performed on an Exactive mass spectrometer (Thermo Fisher Scientific, Germany). Thermogravimetric analysis (TGA) was performed on a Labsys evo TG-DTA/DSC analyzer (Setaram instrument, France) under an N2 atmosphere from 25 to 1000°C with the heating rate of 10°C min−1. UV−Vis absorption spectra were recorded on a CARY ECLIPSE JASCO-720 spectrophotometer (Agilent, United States). Raman spectra were measured on a Renishaw Invia Raman spectrometer (Invia, United Kingdom).
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