2015
DOI: 10.1021/acs.cgd.5b01333
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Role of Aspartic Acid in the Synthesis of Spherical Vaterite by the Ca(OH)2–CO2 Reaction

Abstract: Vaterite crystals with a spherical shape were successfully obtained by the addition of aspartic acid (Asp) in the calcium hydroxide (Ca(OH) 2 )−carbon dioxide reaction system. Crystalline products were characterized by X-ray diffraction, field emission scanning electron microscopy, Fourier transform infrared spectroscopy, Raman spectroscopy, thermogravimetric analysis, and differential scanning calorimetry (TG-DSC). The experimental results indicate that the addition of Asp can inhibit the growth of calcite bu… Show more

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Cited by 63 publications
(38 citation statements)
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“…On the other hand, no data reporting Li + distribution into the vaterite crystals are available, to the best of our knowledge. Therefore, we hypothesize that in the systems with higher Li + content, the increasing adsorption onto the vaterite surface cause its slower dissolution and kinetic stabilization, which consequently postpone the formation of calcite, as already reported for organic molecules [46]. However, the adsorption of Li + onto the calcite can also inhibit its growth, which influences the overall course of transformation.…”
Section: Synthesis and Characterization Of Thin Tabular {001} Calcitsupporting
confidence: 60%
“…On the other hand, no data reporting Li + distribution into the vaterite crystals are available, to the best of our knowledge. Therefore, we hypothesize that in the systems with higher Li + content, the increasing adsorption onto the vaterite surface cause its slower dissolution and kinetic stabilization, which consequently postpone the formation of calcite, as already reported for organic molecules [46]. However, the adsorption of Li + onto the calcite can also inhibit its growth, which influences the overall course of transformation.…”
Section: Synthesis and Characterization Of Thin Tabular {001} Calcitsupporting
confidence: 60%
“…The existence of carboxyls was benefit to the formation of vaterite. [ 40,41 ] As presented in Figure , the spectra of all the ACCs formed at pH 11 exhibited a new peak at 1797 cm −1 which corresponded to C═O. This illustrated that the carboxyls in the PCA, FA, and SA were transformed to C═O with the increase of pH from 7 to 11.…”
Section: Resultsmentioning
confidence: 88%
“…Sixteen diffraction peaks in the XRD patterns at 2θ = 22.944, 29.311, 31.409, 35.849, 39.314, 43.045, 47.034, 47.455, 48.414, 56.463, 57.275, 60.535, 61.310, 62.909, 64.525, and 65.616° correspond to the respective planes of (012), (104), (006), (110), (113), (202), (024), (018), (116), (211), (122), (214), (119), (125), (300), (0012) of vaterite and the peaks at 2θ = 20.880, 24.883, 26.973, 32.711, 42.613, 43.767, 49.098, 49.946, and 55.768° correspond to the respective planes of (002), (100), (101), (102), (004), (110), (112), (104), and (202) for calcite. We estimated that the vaterite and calcite relative mole fractions in the CaCO 3 microparticles can be correlated to the X-ray diffraction intensity from the following expression [ 37 ]: where, C and V are the calcite and vaterite mole fractions, respectively, I C is the X-ray diffraction intensity of the corresponding planes of calcite, and I V is the X-ray diffraction intensity of planes of vaterite.…”
Section: Resultsmentioning
confidence: 99%