Unraveling the atomic structure of biogenic silica: evidence of the structural association of Al and Si in diatom frustules
By M. Gehlen, L. Beck, G. Calas, A. Flank, A. J. Bennekom, J. V. Beusekom. 2002
181 citations recorded by the source corpus.
Subfields: Biomaterials, Geochemistry and Petrology, Paleontology
View Paper: https://www.semanticscholar.org/paper/cacd2814886f24756a4c126c03cb542c11aa1642
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Citations in the corpus
- Iron (III)-silica interactions in aqueous solution: Insights from X-ray absorption fine structure spectroscopy (2003, background): “…about the structural environment around silicon (and similar light elements like Al, P; e.g., Rose et al., 1997a; Ildefonse et al., 1998; Gehlen et al., 2002) can be also obtained at the Si K-edge ( 1800 eV), the low energy provides a short spectral range, and usually requires high Si…”
- A Review of the Stable Isotope Bio-geochemistry of the Global Silicon Cycle and Its Associated Trace Elements (2018, background): “…spectra at the Al-K edge show that Al occurs in 4-fold co-ordination, with tetrahedra inserted inside the bSiO2 framework, although samples of diatom bSiO2 taken from natural marine waters show both 4- and 6- fold co-ordination, possibly as a result of clay contamination (Gehlen et al., 2002).”