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Ft nicolet 5700 spectrometer

Manufactured by Thermo Fisher Scientific
Sourced in United States

The FT Nicolet 5700 spectrometer is a Fourier Transform Infrared (FTIR) spectrometer designed for analytical applications. It is capable of providing high-resolution infrared spectral data for the identification and characterization of a wide range of materials.

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2 protocols using ft nicolet 5700 spectrometer

1

Infrared Spectroscopy of Mono-ICE Samples

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Infrared spectra were collected by using a Thermo Electron Corporation (Whaltham, MA, USA) FT Nicolet 5700 spectrometer with 4 cm−1 resolution. Self-supporting pellets of Mono-ICE samples were obtained by grinding a piece of silica monolith and compressing the obtained powder with a mechanical press at ca. 7 tons·cm−2. To perform the analysis, the obtained pellets were placed into an IR cell equipped with KBr windows permanently attached to a vacuum line (residual pressure ≤ 1 × 10−3 mbar), allowing all treatments (and toluene adsorption/desorption experiments) to be carried out in situ. All the spectra were collected at beam temperature (ca. 35 °C) on samples previously dehydrated at RT for 30 min to completely remove the adsorbed water.
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2

In-situ IR Adsorption Studies of Silica

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Infrared spectra were collected on a Thermo Electron Corporation FT Nicolet 5700 Spectrometer (resolution: 4 cm−1). Self‐standing pellets were placed into an IR cell with KBr windows permanently attached to a vacuum line (residual pressure: 10−4 mbar), allowing all treatments and adsorption–desorption experiments to be carried out in situ. Before the gas adsorption tests, the silica samples were outgassed at 135 °C (heating ramp: 5 °C min−1, holding: 3 h) by using an oil‐free apparatus and a grease‐free vacuum line. Afterwards the samples were cooled at room temperature for the collection of IR spectra upon CO2 adsorption. All the spectra were normalized by dividing for the density of the self‐supported pellets. Furthermore, the proper normalization of the IR spectra was verified taking as reference the intensity of the overtones and combination modes of the silica framework (bands in the 2200–1600 cm−1 range). In this way, differences in the band intensities among different samples related to intrinsic oscillators of the materials (e. g. hydroxyl groups) can be associated with actual differences in the amount of such species in the samples. As a consequence of the normalization, the absorbance values are reported as the arbitrary unit (a.u.).
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