1998
DOI: 10.1046/j.1365-2818.1998.00345.x
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Quantitative and qualitative characterization of aquatic iron oxyhydroxide particles by EF‐TEM

Abstract: Electron energy-loss spectroscopy (EELS) and elemental imaging under the energy-filtered transmission electron microscope are powerful tools for the characterization of iron-rich particles present in natural waters. Features present in EEL spectra (Fe-M 2,3 Fe-L 2,3 and O-K ionization edges) of goethite (a-FeOOH) have been studied with an energy filter operated at 80 keV to determine optimal quantification and elemental imaging of Fe-rich natural aquatic particles in the 30-200 nm range of thickness. For quant… Show more

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Cited by 11 publications
(4 citation statements)
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“…Wang et al (2004) employed this method to image Fe(III)-doped TiO 2 nanoparticles (2-4 nm) in an aqueous environment with a special sample holder. Mavrocordatos and Perret (1998) embedded iron-rich particles (30-200 nm) in resin and then sectioned these samples for visualization by TEM and EELS (Mavrocordatos and Perret 1998).…”
Section: Microscopy and Microscopy-related Techniquesmentioning
confidence: 99%
“…Wang et al (2004) employed this method to image Fe(III)-doped TiO 2 nanoparticles (2-4 nm) in an aqueous environment with a special sample holder. Mavrocordatos and Perret (1998) embedded iron-rich particles (30-200 nm) in resin and then sectioned these samples for visualization by TEM and EELS (Mavrocordatos and Perret 1998).…”
Section: Microscopy and Microscopy-related Techniquesmentioning
confidence: 99%
“…including microscopy approaches [8,9], chromatography [10,11], centrifugation [12], laser scattering [13] filtration [14][15][16], spectroscopic [17,18] and related techniques. Generally, difficulties arise due to a lack of analytical tools capable of characterizing and quantifying particles at environmentally relevant concentrations (low ppb) or in complex environmental matrices that may induce heterodisperse particle size distributions [19].…”
Section: Introductionmentioning
confidence: 99%
“…The value extrapolated to zero thickness is 0.778, compared with a theoretical value of 0.72. The dependency of the partial cross‐session ratios of O‐K and Fe‐L edges on sample thickness is different from that determined for aquatic iron oxyhydroxide particles (Mavrocordatos & Perret, 1998), in which a deconvolution could be performed in order to correct for a multiple scattering effect in their raw spectra. Using k‐factors corresponding to experimental thicknesses estimated by using the ratio of ZL and LL intensities, the ratio of oxygen and iron can be quantified in EELS spectra of core‐loss and LL energy regions from quenched molten iron at high pressures and temperatures (e.g.…”
Section: Resultsmentioning
confidence: 99%