19 research outputs found
Behavior of Fe<sup>2+/3+</sup> Cation and Its Interference with the Precipitation of Mg<sup>2+</sup> Cation upon Mineral Carbonation of Yallourn Fly Ash Leachate under Ambient Conditions
A variety
of leachates derived from the acid leaching of a unique
Fe-rich fly ash, namely Yallourn from the Latrobe Valley of Australia
at different temperatures, have been processed to achieve two key
goals: synthesis of Fe-rich precipitate and mineral carbonation of
alkaline earth metal cations for the storage and utilization of carbon
dioxide (CO2). The behavior and interference of unprecipitated
Fe-bearing cations on the carbonation stage was for the first time
examined by us. The research findings are also applicable to the leachate
derived from other industry wastes and even natural minerals, which
also contain varying amounts of iron as one impure metal. To precipitate
Fe out of the leachate, sodium hydroxide (NaOH) was added to adjust
the pH to 4. Subsequently, the pH of the resultant supernatant was
further increased to ∼13 and bubbled with CO2 to
precipitate the remaining cations. As has been confirmed through the
characterization of solid products by synchrotron Fe K-edge X-ray
adsorption spectroscopy (XAS), quantitative X-ray diffraction (Q-XRD),
and scanning electron microscopy (SEM), Fe was precipitated out as
a mixture that was predominantly ferrihydrite with a nanoscale size
for its primary nuclei. Its composition and size also varied largely
with the leachate, i.e. the acid leaching temperature. For the unprecipitated
Fe2+ that is predominant in the high-temperature leachate
(i.e., ≥150 °C), it was preferentially oxidized and converted
into nanoscale magnetite during the carbonation process, providing
seed/nuclei for the crystallization and growth of magnesian calcite
(Ca0.2Mg0.8CO3). Accordingly, the
carbonation of Mg2+ was enhanced remarkably and reached
completion in 20 min at room temperature. In addition, all the resulting
products, Fe-precipitate (i.e., ferrihydrite), magnetite, and magnesian
calcite, are relatively pure, presenting cheap and suitable precursors
for a variety of value-added environmental applications
MSE middle-range ion interaction parameters in this study.
<p>MSE middle-range ion interaction parameters in this study.</p
Normalized Ni K-edge XANES spectra of nickel complexes as a function of concentration (thin lines).
<p>Baseline-removed pre-edges are shown as a function of concentration in inset for clarity. Thick lines are the calculated (convoluted) XANES spectra for Ni aqueous species using fully hydrated regular (re.) and distorted (dis., DFT optimized), as well as [NiCl(H<sub>2</sub>O)<sub>5</sub>]<sup>2+</sup> (ADF., DFT optimized) octahedral configuration models from literature [<a href="http://www.plosone.org/article/info:doi/10.1371/journal.pone.0119805#pone.0119805.ref005" target="_blank">5</a>].</p
Distribution of Ni(II) species in NiCl<sub>2</sub>-H<sub>2</sub>O (a, b), and NiCl<sub>2</sub>-MgCl<sub>2</sub>-H<sub>2</sub>O (c) solutions and average number of ligand in the first shell of Ni<sup>2+</sup> as a function of NiCl<sub>2</sub> solution concentration.
<p>In (a) and (c), the distributions of species are calculated with the formation constant and MSE parameters determined in this study (all lines); in (b), the distributions of species was calculated for NiCl<sub>2</sub> solutions using the model and parameters from literature [<a href="http://www.plosone.org/article/info:doi/10.1371/journal.pone.0119805#pone.0119805.ref010" target="_blank">10</a>]; In (a), the calculated average numbers of ligands in the first shell of Ni<sup>2+</sup> are compared with the number of ligands extracted by EXAFS (Cl ligand, empty circles with error bar; O ligand, triangles with error bar) and XRD [<a href="http://www.plosone.org/article/info:doi/10.1371/journal.pone.0119805#pone.0119805.ref021" target="_blank">21</a>,<a href="http://www.plosone.org/article/info:doi/10.1371/journal.pone.0119805#pone.0119805.ref025" target="_blank">25</a>] (Cl ligand, filled circles) analysis are shown for comparison; and (b) the result using the model and parameters from literature [<a href="http://www.plosone.org/article/info:doi/10.1371/journal.pone.0119805#pone.0119805.ref010" target="_blank">10</a>].</p
Molar absorptivity spectra of individual Ni(II)-chloride species obtained from the analysis of two absorptive band (left, 350–550 nm and right 580–850 nm) spectroscopic data for NiCl<sub>2</sub>-H<sub>2</sub>O and NiCl<sub>2</sub>-MgCl<sub>2</sub>-H<sub>2</sub>O systems at room temperature.
<p>The molar spectrum for Ni(ClO<sub>4</sub>)<sub>2</sub> solution at room temperature is plotted as solid line for comparison.</p
Comparison experimental and predicted water activity for NiCl<sub>2</sub> solution at room temperature.
<p>The line is predicted one in this work and the dot line represents the prediction one without considering effect of complexes in system, corresponding to the dot line in <a href="http://www.plosone.org/article/info:doi/10.1371/journal.pone.0119805#pone.0119805.g009" target="_blank">Fig 9</a>; the circles are literature values [<a href="http://www.plosone.org/article/info:doi/10.1371/journal.pone.0119805#pone.0119805.ref063" target="_blank">63</a>].</p
The solubility product of solid phase in MSE and Pitzer model and the formation constant of NiCl<sup>+</sup> and [NiCl<sub>2</sub>]<sup>0</sup> species determined in this study.
<p>The association constant of [HCl]<sup>0</sup> aqueous species used in the calculation is also listed.</p><p>Uncertainty limits are given in parentheses.</p><p>* The solubility products were converted from mole fraction-scale in the literatures to molality-scale.</p><p><sup>£</sup> Value was calculated by Pitzer−Simonson−Clegg (PSC) model [<a href="http://www.plosone.org/article/info:doi/10.1371/journal.pone.0119805#pone.0119805.ref046" target="_blank">46</a>].</p><p><sup>§</sup> Values were calculated by HSC software (H = enthalpy, S = entropy, C = heat capacity) in literature [<a href="http://www.plosone.org/article/info:doi/10.1371/journal.pone.0119805#pone.0119805.ref048" target="_blank">48</a>].</p><p><sup>¶</sup> The activity coefficient model assumed <i>γ</i><sub>ion</sub> = <i>γ</i><sub><i>±</i></sub>,<sub>ion</sub>.</p><p>The solubility product of solid phase in MSE and Pitzer model and the formation constant of NiCl<sup>+</sup> and [NiCl<sub>2</sub>]<sup>0</sup> species determined in this study.</p
Experimental data used for parameters estimation.
<p>* Water activity data</p><p>** Solid liquid equilibrium data</p><p>Experimental data used for parameters estimation.</p
Ni K-edge <i>k</i><sup>3</sup>-weighted EXAFS (a), and the amplitude (b) and imaginary part (c) of their Fourier transforms of the two solid compounds and four NiCl<sub>2</sub> solutions.
<p>The dot line is the position of Ni-O and Ni-Cl peaks.</p
Normalized Ni K-edge XANES spectra for the two solid compounds.
<p>Normalized Ni K-edge XANES spectra for the two solid compounds.</p
