2021
DOI: 10.1039/d1ce00365h
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A study of the effects of NH4+ on the fast precipitation of vaterite CaCO3 formed from steamed ammonia liquid waste and K2CO3/Na2CO3

Abstract: Vaterite-phase calcium carbonate (CaCO3) has many unique properties, such as high solubility, spherical shape, large surface areas, and porosity, giving it more industrial applications than calcite and aragonite-type polymorphs. However,...

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Cited by 11 publications
(6 citation statements)
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“…Na + and NO 3 − ions could be adsorbed in the original primary vaterite nanosize particles surface inside the microsphere and consequently prevent the crystal growth polymorph and phase transformation. A similar mechanism was reported using Na 2 CO 3 as a carbon source that ions such as NH 4 + ions are able to control the growth of primary particles [42]. In this case, the particle growth mechanism of spherulites of vaterite was found to be dependent on the crystal surface structure.…”
Section: The Proposed Mechanism Of Spherulitic Growth Of Caco 3 Mesoporoussupporting
confidence: 72%
“…Na + and NO 3 − ions could be adsorbed in the original primary vaterite nanosize particles surface inside the microsphere and consequently prevent the crystal growth polymorph and phase transformation. A similar mechanism was reported using Na 2 CO 3 as a carbon source that ions such as NH 4 + ions are able to control the growth of primary particles [42]. In this case, the particle growth mechanism of spherulites of vaterite was found to be dependent on the crystal surface structure.…”
Section: The Proposed Mechanism Of Spherulitic Growth Of Caco 3 Mesoporoussupporting
confidence: 72%
“…At high concentrations of SOMs (50, 500, and 1000 μg/mL), diffractions at 2θ = 24.5, 26.6, and 32.4°were observed corresponding to the presence of vaterite crystallographic planes (110), (112), and (114) (Figure 3f(iii−v); PDF # 33-0268). At the same time, the decrease in intensity of the calcite peak at 29.2°(104) 44,45 indicates the nucleation of a lower number of calcite crystals at high concentrations of SOMs (Figure 3f(iii−v), PDF # 05-0586).…”
Section: ■ Results and Discussionmentioning
confidence: 96%
“…The diffraction peak at 29.4°i s assigned to the (104) plane of the calcite lattice (Figure 6f(i)). 44 In the case of crystals grown in the presence of the peptide and Mg ions, diffraction peaks were observed at 2θ = 29.5°, 32.7°, and 45.5°, indicating the presence of aragonite crystal lattice planes of (112), (114), and (008), respectively (Figure 6f(ii−vi)). 51,52 These results are in good agreement with the data reported in the literature.…”
Section: ■ Results and Discussionmentioning
confidence: 99%
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