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Uv 2600 system

Manufactured by Shimadzu
Sourced in Japan

The UV-2600 system is a high-performance UV-visible spectrophotometer designed for accurate and reliable analysis. It features a double-beam optical system, a wide wavelength range, and advanced data processing capabilities. The UV-2600 is a versatile instrument suitable for a variety of applications in various industries.

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2 protocols using uv 2600 system

1

Nanoparticle Characterization Protocol

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UV-visible spectra were acquired using a Shimadzu UV-2600 system (Shimadzu Corporation, Tokyo, Japan). FE-TEM images of nanoparticles were obtained using a JEM-3010 model (Jeol Ltd., Tokyo, Japan). To obtain the FE-TEM images, the samples were loaded on a carbon-coated copper grid (carbon type-B, 300 mesh, Ted Pella Inc., Redding, CA, USA) and dried for 24 h at ambient temperature. FT-IR spectra were acquired from powdered samples using a Varian 640 IR system in the ATR mode (Agilent Technologies, Santa Clara, CA, USA). The HR-XRD pattern was analyzed using an Ultimate IV system and a CuKα laser (λ = 0.154056 nm) (Rigaku, Japan). The hydrodynamic size and zeta potential were measured using a NanoBrook 90Plus Zeta system from Brookhaven Instruments Corporation (Holtsville, NY, USA). Sonication was conducted using a WUC-A22H system (Daihan Scientific Co. Ltd., Seoul, Republic of Korea). Centrifugation was performed using a 5424R centrifuge (Eppendorf AG, Hamburg, Germany) and the freeze-drying process was conducted using an FD8518 system (IlshinBioBase Co. Ltd., Gyeonggi, Republic of Korea).
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2

Comprehensive Materials Characterization Protocol

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XRD patterns were supplied by Bruker D8 Advance. TEM image and EDS images were captured by Tecnai G2 F20 with EDS Inca X–Max (Oxford). Scanning electron microscopy (SEM) images were given by Gemini SEM 300. In-situ XPS measurement was operated on a Kratos-Axis Ultra DLD instrument using a xenon lamp as the light source. The binding energy of C1s at 284.8 eV was used for energy calibration. VB XPS spectra and UPS of the samples were collected by Escalab Xi+ (Thermo Scientific), and UV–vis DRS was determined by the UV-2600 system (Shimadzu). The content of K and Li was obtained from ICP-OES (PE Avio 200) and the content of H was obtained from O, N, and H co-meter (LECO ONH836). AFM images and KPFM images were captured by Bruker MultiMode 8, and the probe used was a silicon probe. During the measurement, a xenon lamp was used as the light source, and the light irradiation time was 15 min. In this case, the powder sample was dispersed in an ethanol solution and then dropped onto the silicon wafer to form a uniform film for testing.
In-situ DRIFTS characterization was operated on a Nicolet iS50 FTIR spectrometer. 13C isotope tracing experiment was performed by mass spectrometry (Finnigan MAT 271). The O2 generated during the CO2 photoreduction process was detected by a gas chromatograph (GC14C, Shimadzu) with a TCD detector.
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