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The morphology of calcite crystals grown in a porous medium doped with divalent cations
Institution:1. Institut für Mineralogie, University of Münster, Corrensstrasse 24, 48149 Münster, Germany;2. Nanochemistry Research Institute, Department of Chemistry, Curtin University, Perth 6845, Australia;3. The Institute for Geoscience Research (TIGeR), Curtin University, Perth 6845, Australia;1. Aix-Marseille Université, CNRS, CINaM UMR 7325, Marseille, France;2. Institut Ciències Mar, CSIC, 08003 Barcelona, Spain;3. Mediterranean Institute of Oceanography (MIO) UM 110, CNRS/INSU, IRD, Aix-Marseille Université, Université du Sud Toulon-Var, Marseille, France;4. Division of Chemistry, California Institute of Technology, Pasadena, CA, USA;5. Department of Chemistry and Applied Biosciences, ETH Zürich, Wolfgang Pauli Strasse 10, Hönggerberg, HCI, G113, CH-8093 Zurich, Switzerland;6. UBP-OPGC-CNRS, 5 rue Kessler, 63038 Clermont-Ferrand, France;7. Institut f. Geochemie und Petrologie, ETH Zürich, NW E 85, Clausiusstrasse 25, 8092 Zürich, Switzerland;1. Department of Chemistry, Wright State University, 3640 Colonel Glenn Highway, Dayton, OH 45435, USA;2. Earth Sciences Division, Lawrence Berkeley National Lab, 1 Cyclotron Road, Berkeley, CA 94720, USA
Abstract:Calcite crystals were grown in the presence of small concentrations (50, 200, and 600 ppm) of divalent cations (Ba2+, Sr2+, Co2+ and Mn2+) in a silica hydrogel medium. The calcite crystals grown in the presence of cations larger than Ca2+ (Ba2+ or Sr2+) developed rhombohedral habits defined by {101¯4} form, similar to the morphology of calcite grown in a pure gel. SEM images show that growth on {101¯4} occurs by lateral advancement of layers bounded by macroscopic dendritic or jagged steps. In the case of calcite crystals grown in a gel doped with cations smaller than Ca2+ (Co2+ or Mn2+), a variety of morphologies was obtained, ranging from blocky crystals (at lower concentrations: 50 and 200 ppm) to peanut-like aggregates, spheres and spherulites (at 600 ppm). The macroscopic morphological characteristics of such doped calcite crystals reflect closely the growth behaviour of calcite {101¯4} surface at a nanoscale, reported by previous AFM studies. Morphological features have been interpreted on the basis of the modification of growing steps characteristics as a consequence of asymmetrical cation incorporation. The use of such morphologies as a criterion of biological activity is, therefore, unreliable.
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