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Quanta 650f

Manufactured by Thermo Fisher Scientific
Sourced in United States

The Quanta 650F is a field emission scanning electron microscope (FE-SEM) designed for high-resolution imaging and analysis of a variety of sample types. It features a large chamber, high-resolution electron optics, and advanced imaging capabilities to enable detailed characterization of materials at the nanoscale.

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4 protocols using quanta 650f

1

Measuring MIP Film Thickness via SEM

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An edge of the MIP films on glass was removed using a razor and the film was coated with sputtered gold. An FEI Quanta 650F field emission scanning electron microscope (FEI, Hillsboro, OR, USA) was used for imaging of the MIP film section with secondary electrons at a 70° tilt and 10 kV acceleration potential. A thickness of film (H) was estimated based on average height of seeming 90° section measured on SEM image (H′) and the tilt angle:
Thickness values for three films of the same kind were averaged.
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2

Multi-modal Imaging of Microfossils

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Conventional (light) photographs were taken with either a Canon EOS 7D Mark II camera mounted on a BK Lab Plus Lab imaging system (Dun Inc., Charlottesville, VA, USA), a Leica DVM6 microscope (Leica Microsystems GmbH, Wetzlar, Germany), or a Nikon D100 digital camera using a standard copy stand. SEM images were taken with a FEI Quanta 650F variable-pressure field-emission SEM (FEI Company, Hillsboro, OR). The FEI microscope was operated at 15 kV, with a spot size of 2.45 and working distances of about 12 to 15 mm. Notably, the high conductivity of the rocks from McGraths Flat allowed high-resolution SEM imaging without any coating. All microfossils were imaged in situ (i.e., in the matrix) rather than using acid preparation. Micro x-ray fluorescence (μXRF) was undertaken by directly sampling across the surface of a rock containing a fish spine (AM F.146602) using a benchtop M4 Tornado μXRF (Bruker Corp., Billerica, MA). This allowed us to sample both the fossil and matrix for differences in chemistry. The instrument consists of a Rh anode metal-ceramic x-ray tube. The measurement was carried out under vacuum condition (20 mbar). The following parameters were used for elemental mapping analysis: x-ray tube, 45 kV and 600 μA; area mapping point distance, 60 μm; time/pixel, 600 ms; 1 cycle; maximum energy, 40 keV; and maximum pulse throughput, 130 kilo counts per second.
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3

Characterization of Crystalline Materials

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Materials and Methods: All solvents and reagents were purchased from commercial suppliers and were used without further purification. X-ray powder diffraction (XRPD) patterns under ambient conditions were collected on an X'Pert PRO MPDP analytical diffractometer (Panalytical) at 40 kV and 40 mA using CuKα radiation (λ = 1.5419 Å). The samples were analyzed with scanning θ/2θ. Field-Emission Scanning Electron Microscopy (FESEM) images were collected on a FEI Quanta 650F scanning electron microscope, using aluminum as a support. Gravimetric water vapor sorption isotherms were measured using a DVS vacuum instrument (Surface Measurement Systems Ltd). The weight of the sample (≈ 20 mg) was constantly monitored with a high-resolution microbalance (± 0.1 µg) and recorded at 25 (± 0.2 °C) under pure water vapor pressures. Prior to the sorption experiments, samples were degassed inside the chamber under vacuum at 120 °C for 6 h. Folding angles were calculated as previously described. [16] A Bluepoint 4 ECOcure (Hönle UV Technology) UV-Vis highintensity spot lamp without a filter (300 nm to 650 nm), and a PI 450 (Optris) infrared camera (operating temperature range: 0 ºC to 250 °C), were used. Data were obtained using PI Connect software.
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4

Comprehensive Material Characterization Protocols

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All chemical reagents and solvents were purchased from commercial sources and used as received without further purification. NMR spectra were recorded on a Bruker Avance DPX-250 spectrometer and Bruker AMX-400 Wide Bore for liquid and solid-state samples respectively. Mass spectra were acquired on a micrOTOF-QII ESI-MS instrument. Purity of all bulk material batches was confirmed by X-ray powder diffraction (XRPD) patterns collected on an X'Pert PRO MPD analytical diffractometer (Panalytical) at 45 kV, 40 mA using Cu Kα radiation (λ 1.5419 Å), and compared with single crystal simulated patterns. Thermogravimetric analyses were performed under nitrogen flow using a STA 449 F1 Jupiter-Simultaneous TGA-DSC from NETZSCH with a heat rate of 5°C/min. IR spectra were recorded in transmission mode on a Bruker Tensor 27FTIR equipped with a Golden Gate diamond ATR cell. Elemental Analysis measurements were performed on a Flash EA 2000 CHNS, Thermo Fisher Scientific analyser. Inorganic Elemental Analysis measurements were performed on an ICP-MS 7500ce, Agilent Technologies. Scanning electron microscope images were acquired on a FEI Quanta 650F working at an accelerating voltage of 2 kV and a beam current of 50 pA. Transmission electron microscope images were acquired on a JEOL JEM-1400 working at an accelerating voltage of 120 kV.
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