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D max 2400 powder diffractometer

Manufactured by Rigaku
Sourced in Japan

The D/Max-2400 is a powder diffractometer manufactured by Rigaku. It is designed to perform X-ray diffraction analysis on powder samples. The core function of the D/Max-2400 is to collect and analyze X-ray diffraction patterns from powder materials, which can be used to identify crystalline phases and determine structural properties.

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2 protocols using d max 2400 powder diffractometer

1

Characterization of UVS and UVS-NZVI

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The microstructures of the UVS and UVS-NZVI were imaged on S-4800 scanning electron microscopy (Hitachi, Japan) and H-9500 transmission electron microscopy (Hitachi, Japan). Fourier transform infrared (FTIR) spectra were obtained on a Tensor27 FTIR spectrometer (Bruker, Germany). X-ray diffraction (XRD) was recorded on a D/Max-2400 powder diffractometer (Rigaku, Japan), operating at 40 kV and 40 mA. The specific surface area and pore structure were measured on a specific surface area and porosity analyser (ASAP 2460 analyser, Micromeritics, USA). UVS-NZVI was degassed in vacuum and characterized by N2 sorption at 77 K. The specific surface area was calculated by the Brunauer–Emmett–Teller (BET) method. Pore diameter were calculated by Barrett–Joyner–Halenda (BJH) method [26 (link),27 (link)].
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2

Detailed Characterization of Luminescent Materials

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The X-ray diffraction patterns were obtained on a Rigaku D/max-2400 powder diffractometer by using Cu Kα radiation at 40 kV and 60 mA. The luminescence decay curves were measured by a FLS-920T fluorescence spectrophotometer with a nF900 microsecond flashlamp as the light source. The photoluminescence and the long persistent luminescence spectra were recorded by FLS-920 fluorescence spectrophotometer (Edinburgh Instruments). The absorption spectra were recorded by a PerkinElmer Lambda 950 spectrometer in the region of 400–700 nm, while BaSO4 was used as a reference.
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