Next Article in Journal
Mineralogical and Geochemical Compositions of the Lopingian Coals and Carbonaceous Rocks in the Shugentian Coalfield, Yunnan, China: with Emphasis on Fe-Bearing Minerals in a Continental-Marine Transitional Environment
Next Article in Special Issue
CO2 Absorption and Magnesium Carbonate Precipitation in MgCl2–NH3–NH4Cl Solutions: Implications for Carbon Capture and Storage
Previous Article in Journal
A Review of the Carbon Footprint of Cu and Zn Production from Primary and Secondary Sources
 
 
Font Type:
Arial Georgia Verdana
Font Size:
Aa Aa Aa
Line Spacing:
Column Width:
Background:
Article

Connecting the Morphological and Crystal Structural Changes during the Conversion of Lithium Hydroxide Monohydrate to Lithium Carbonate Using Multi-Scale X-ray Scattering Measurements

Department of Civil and Environmental Engineering, Environmental Chemistry and Technology Program, University of Wisconsin, Madison, WI 53706, USA
Minerals 2017, 7(9), 169; https://doi.org/10.3390/min7090169
Submission received: 25 August 2017 / Revised: 10 September 2017 / Accepted: 11 September 2017 / Published: 14 September 2017
(This article belongs to the Special Issue Carbon Capture and Storage via Mineral Carbonation)

Abstract

:
While CO2 storage technologies via carbon mineralization have focused on the use of earth-abundant calcium- and magnesium-bearing minerals, there is an emerging interest in the scalable synthesis of alternative carbonates such as lithium carbonate. Lithium carbonate is the carbonated end-product of lithium hydroxide, a highly reactive sorbent for CO2 capture in spacecraft and submarines. Other emerging applications include tuning the morphology of lithium carbonates synthesized from the effluent of treated Li-bearing batteries, which can then be reused in ceramics, glasses, and batteries. In this study, in operando Ultra-Small-Angle, Small-Angle, and Wide-Angle X-ray Scattering (USAXS/SAXS/WAXS) measurements were used to link the morphological and crystal structural changes as lithium hydroxide monohydrate is converted to lithium carbonate. The experiments were performed in a flow-through reactor at PCO2 of 1 atm and at temperatures in the range of 25–500 °C. The dehydration of lithium hydroxide monohydrate to form lithium hydroxide occurs in the temperature range of 25–150 °C, while the onset of carbonate formation is evident at around 70 °C. A reduction in the nanoparticle size and an increase in the surface area were noted during the dehydration of lithium hydroxide monohydrate. Lithium carbonate formation increases the nanoparticle size and reduces the surface area.

1. Introduction

Carbon mineralization, which involves the conversion of CO2 to carbonates that are thermodynamically stable, environmentally benign, and insoluble in water, has been proposed as a pathway to safely and permanently store CO2 via natural and engineered pathways [1,2,3,4,5,6,7,8,9,10]. While various earth-abundant calcium and magnesium silicates have been extensively investigated for the permanent storage of CO2 [3,4,5,7,11,12] given their availability in nature [13,14,15], there is an increasing interest in the scalable synthesis of alternative carbonates such as lithium carbonates. Lithium carbonate is the end-product of the carbonation of lithium hydroxide, a highly reactive sorbent for CO2 capture in spacecraft and submarines. Other emerging applications include tuning the morphology of lithium carbonates synthesized from the effluent of treated Li-bearing batteries, which can be recycled back into batteries and used in ceramics and glasses. With increasing concerns around the availability of lithium that can be directly mined from the environment, there is an emerging interest in developing technologies [16,17,18,19,20] for closing elemental loops by combining multiple waste streams for sustainable resource and environmental management.
Some of the factors that influence the morphology of lithium carbonate are the reactive precursors and water. Previous studies have suggested that the kinetics of LiOH conversion to lithium carbonate is accelerated in the presence of water via the formation of lithium hydroxide monohydrate, LiOH·H2O as an intermediate [21,22,23], while Zho and co-workers [24] suggested that the carbonation of lithium hydroxide is an order of magnitude faster compared to lithium hydroxide monohydrate. The differences in the reactivity of lithium hydroxide monohydrate and lithium hydroxide with CO2 arise from the water released during the reaction [25]. Three times as many water molecules are produced during the carbonation of lithium hydroxide monohydrate compared to lithium hydroxide, as shown by the following reactions:
2LiOH(s) + CO2(g) –> Li2CO3(s) + H2O(g)
2LiOH·H2O(s) + CO2(g) –> Li2CO3(s) + 3H2O(g)
The role of water is important to consider, since most flue gas streams contain moisture which may lead to the formation of lithium hydroxide monohydrate as an intermediate. Since the kinetics of lithium hydroxide and lithium hydroxide monohydrate have been reported in previous studies [21,22,23,24,25], this study focuses on connecting the morphological and structural changes in lithium hydroxide monohydrate as it is reacted with CO2 to form lithium carbonate using multi-scale X-ray scattering measurements, which encompass Ultra-Small-Angle, Small-Angle, and Wide-Angle X-ray Scattering (USAXS/SAXS/WAXS) [26,27].
The structural changes that occur during the conversion of lithium hydroxide monohydrate to lithium carbonate, which are observed in WAXS, are related to the surface area and the size and geometry of the larger scattering features determined from the USAXS/SAXS measurements. These combined scattering techniques, which span more than four decades in spatial resolution, provide a nondestructive approach to connect nano-scale and micron-scale morphological changes with the structural changes in Angstrom scale in complex materials. The measurements reported in this study are performed in a flow-through reactor containing lithium hydroxide monohydrate and 1 atm of continuously flowing CO2 as the temperature is linearly ramped up from 25 °C to 500 °C. The reaction-driven chemo-morphological changes as lithium hydroxide monohydrate is converted to lithium carbonate are discussed in the context of lithium carbonate conversion kinetics.

2. Materials and Methods

Lithium hydroxide monohydrate procured from Himedia Laboratories (West Chester, PA, USA) is loaded into a quartz capillary cell with an internal diameter of 1.3 mm and thickness of 0.2 mm (Friedrich & Dimmock Inc., Millville, NJ, USA). The capillary cell is loaded into a sample environment cell as described by Chupas and co-workers for non-ambient experiments [28]. The starting and final temperatures are set to 26 °C and 500 °C, respectively. The temperature ramp rate is set to 2.4 °C/min. The partial pressure and flow rate of CO2 are set to 1 atm and 10 cc/min, respectively. The flow rate of CO2 at 1 atm is set to 10 cc/min.
The X-ray scattering measurements are performed at sector 9-ID at the Advanced Photon Source (APS), Argonne National Laboratory, Argonne, IL [29,30]. The USAXS, SAXS, and WAXS data are collected sequentially at each temperature of interest. The data acquisition times for the USAXS, SAXS, and WAXS measurements are 90 s, 30 s, and 30 s, respectively. Uncertainties from sampling geometry are eliminated by not changing the sample configuration in the beam path. The beam size is defined by the high-resolution X-ray slits, which are set to 0.8 mm × 0.8 mm for USAXS and 0.2 mm × 0.2 mm for SAXS and WAXS. This latter setting allows the detector pixel size, 172 μm × 172 μm for both the SAXS and WAXS detectors, to provide an outgoing scattered or diffracted beam resolution comparable to those for the incident beam collimation and flux. The sample-to-detector distances for SAXS and WAXS are set to 540 mm and 303.5 mm, respectively. The total X-ray flux at the sample is 1013 photon mm−2·s−1. The q values (q = (4π/λ)sinθ, where λ is the X-ray wavelength and θ is half the scattering angle) and the sample-to-detector distances (and geometry) are calibrated using silver behenate for SAXS and the NIST standard reference material, SRM 640d (Si) [31] for WAXS. The X-ray energy is 21.0 keV, corresponding to an X-ray wavelength of 0.59 Å.
The USAXS, SAXS, and WAXS data collected are reduced and analyzed using the Irena [32] and Nika [33] software packages written in Igor Pro (Wavemetrics, Portland, OR, USA). The USAXS measurement configuration is slit-smeared [34]. The slit-smeared USAXS and SAXS data are combined and analyzed to determine the morphological changes in the materials. The structural changes in the materials are determined from the WAXS data. Standard deviation uncertainties in the reduced data are represented by vertical bars in the figures (where visible). Estimated or computed standard deviation uncertainties in our fit results are typically ±5% of the value, unless indicated otherwise. The surface morphological features are determined using a Hitachi 3400 Variable Pressure Scanning Electron Microscope (Hitachi High Technologies, Schaumburg, IL, USA). The pore sizes are determined using the BET method (Quantachrome Autosorb-1 BET, Boynton Beach, FL, USA).

3. Results and Discussion

3.1. Structural Changes during the Carbonation of Lithium Hydroxide Monohydrate

Significant structural changes are evident during the carbonation of lithium hydroxide monohydrate in the presence of CO2 with increasing temperature. The dehydration of lithium hydroxide monohydrate on heating is evident from the reduction in the intensity of the characteristic peak that corresponds to d = 2.67 Å, q = 2.35 Å−1, or CuKα 2θ = 33.54° (h k l: (−2 2 0)) [35] (Figure 1a). The dehydration of lithium hydroxide monohydrate is rapid on heating to temperatures above 70 °C, and the characteristic peak disappears on heating to 108 °C (Figure 1b). The onset of the lithium hydroxide peak that corresponds to d = 2.74 Å, q = 2.28 Å−1, or CuKα 2θ = 32.6° (h k l: (1 0 1)) [36] occurs on heating lithium hydroxide monohydrate above 70 °C (Figure 2a). The highest integrated intensity of lithium hydroxide is noted at 147 °C, which decreases on further heating. A significant reduction in the characteristic lithium hydroxide peak is noted at temperatures above 250 °C (Figure 2b). The characteristic lithium hydroxide peak collapses at around 450 °C.
The appearance of the lithium carbonate peak at 59 °C (Figure 3a) is concurrent with the dehydration of lithium hydroxide monohydrate to form lithium hydroxide. The characteristic lithium carbonate peak that corresponds to d = 2.83 Å, q = 2.22 Å−1, or CuKα 2θ = 31.6° (h k l: (0 0 2)) [37] (Figure 3a) increases in intensity as the reaction temperatures increase from 71 °C to 499 °C. The integrated intensity of the characteristic lithium carbonate peak continues to increase with an increase in temperature to about 450 °C, after which it remains relatively unchanged (Figure 3b). The relatively unchanging integrated intensity of the lithium carbonate peak at temperatures above 450 °C corresponds to the collapse of the lithium hydroxide peak around 450 °C, as shown in Figure 3b.
Following the structural changes as lithium hydroxide monohydrate is converted to lithium carbonate provides a few mechanistic insights. In an environment characterized by continuously increasing temperature, the conversion of lithium hydroxide monohydrate to lithium carbonate does not occur directly, and proceeds via the formation of lithium hydroxide. These changes in chemical composition influence the scattering contrast, which is needed to quantify the morphological changes represented by the USAXS/SAXS curves, as discussed in the following section.

3.2. Morphological Changes during the Carbonation of Lithium Hydroxide Monohydrate

The microstructural changes are modeled from the combined Ultra-Small-Angle and Small-Angle X-ray Scattering (USAXS/SAXS) curves represented in Figure 4. Scattering as a function of q is related to the Fourier transform of the real-space electron density distribution. Scattering at low and high q represent the nano-scale and coarser features, respectively. A significant increase in the scattering intensity, particularly in the q range of 10−1 to 10−3 Å−1, is noted during the reaction of lithium hydroxide monohydrate with CO2 as the temperature is increased from 26 °C to 222 °C. For example, the scattering intensity increased 50-fold from ambient temperature to 222 °C at q = 0.01 Å−1, suggesting an increase in the scattering features. Further, a reduction in the scattering intensity is noted as the reaction temperature increases from 222 °C to 500 °C, suggesting fewer and coarser features. The surface morphology of the lithium hydroxide monohydrate and lithium carbonate are evident from the scanning and transmission electron microscopy images shown in Figure 5.
While the particle size of unreacted lithium hydroxide monohydrate is in the range of 100–700 μm (Figure 5(a-1)), nanoparticles smaller than 500 nm are attached to the surfaces of the large objects (Figure 5(a-2)). At 83 °C, the partial dehydration of lithium hydroxide monohydrate to produce lithium hydroxide results in a rougher morphological interface (Figure 5(b-1),(b-2)). Lithium carbonate formed at 499 °C shows globular nano-scale features connected to larger-scale features (Figure 5(c-1),(c-2)). BET analyses showed that the average pore sizes of the lithium hydroxide monohydrate and lithium carbonate are in the range of 2–3 nm, with a negligible number of pores greater than 10 nm (Figure S1). Therefore, the nano-scale features in the q range of 0.006–0.025 Å−1 correspond to the scattering from the particles as opposed to the pores. While the microscopy images and BET data provide insights into the morphologies of these materials and the porosity, USAXS and SAXS provided quantitative microstructural information as lithium hydroxide monohydrate is converted to lithium carbonate.

3.2.1. Contrast Variation

Applying the appropriate contrast factor is critical for quantifying the morphological features represented by the USAXS/SAXS curves. The calibrated scattering intensity is proportional to the scattering contrast factor, |Δρ|2, which is the square of the difference in scattering length density (SLD or ρ) between the pore space and the outside solid phase. The scattering length density is determined by the chemical composition and the density of the phase, which vary as the reaction progresses. In addition to the scattering contrast factor, the measured intensity for a given population of scatterers is proportional to its overall volume fraction normalized to the total sample volume, ΦVi, and the mean volume of its individual pores, VPi (at low and intermediate q), to its surface area per unit sample volume, SVi (at high q).
In this study, the scattering contrasts are determined based on the changing chemical composition of the reacting solid with CO2 with increasing temperature. It is evident from Figure 1 that the characteristic peak of lithium hydroxide monohydrate completely disappears on heating to 108 °C and is accompanied by the simultaneous formation of lithium hydroxide and lithium carbonate as noted in Figure 2 and Figure 3. The changes in the compositions of lithium hydroxide and lithium carbonate as the reaction temperature increases to 500 °C are used to determine the appropriate contrast factor for each USAXS/SAXS curve. The scattering length density, ρ, of lithium hydroxide monohydrate, lithium hydroxide, and lithium carbonate are 13.4 × 1010, 12.4 × 1010, and 17.4 × 1010 cm−2, respectively. Since the contrasting phase is the empty pore space with an SLD of 0, the overall scattering contrast factor is calculated as: Δ ρ o v e r a l l 2 = i = 1 3 ( x i ρ i ) 2 , where x and ρ represent the weight fraction and the scattering length density for each phase, i . In this study, the composition,   x i , of any or all of the three phases, which are lithium hydroxide monohydrate, lithium hydroxide, and lithium carbonate, at a given reaction temperature is represented in the determination of the overall scattering contrast factor.
The compositions of each phase are determined from the structural changes in the material from the WAXS measurements. The scattering contrast factor as a function of the reaction temperature is shown in Figure 6. As the reaction temperature increases from 26 °C to 83 °C, the dehydration of lithium hydroxide monohydrate to form lithium hydroxide reduces the scattering contrast factor from 180.4 × 1028 m−4 at 26 °C to 154.1 × 1028 m−4 at 83 °C. As the temperature increases to 450 °C, the scattering contrast factor increases to 304.1 × 1028 m−4 at 450 °C, which represents pure lithium carbonate. Subsequent increases in temperature do not change the lithium carbonate phase, so the scattering contrast factor is unchanged in the temperature range of 450–500 °C. The determination of the appropriate model and the role of the scattering contrast factor in describing the morphological features as lithium hydroxide monohydrate is converted to lithium carbonate are discussed in the following section.

3.2.2. USAXS and SAXS Data Interpretation Using the Unified Fit Model

The combined USAXS/SAXS data is interpreted based on the unified fit model proposed by Beaucage (1995) [38]. This theory was proposed to describe multiple levels of related scattering features in complex systems. Each scattering regime is described by a Guinier, which describes the structure corresponding to a specific scattering regime, i , and an associated Porod power law. The Porod scattering power law corresponding to a given structural level provides insights into the associated geometry of that structural arrangement. The summation of the Guinier’s exponential form and the power law for a given structural level, i , is represented by the following equation [38]:
I ( q ) =   i   [ G i exp ( q 2 R g 2 / 3 ) +   B i ( ( e r f ( q R g 6 ) ) 3 q ) P i ]
At the smallest q in small angle scattering or the largest length scale, the residual background intensity, B g , has to be added to Equation (1) above to yield Equation (2) listed below:
I ( q ) =   i   [ G i exp ( q 2 R g 2 / 3 ) +   B i ( ( e r f ( q R g 6 ) ) 3 q ) P i ] +   B g
In the above equations, G i is the Guinier exponential prefactor, B i is a constant prefactor for the power law scattering, R g i is the radius of gyration, and P i is the power law exponent for a specific structural regime i . Power law exponents indicate the geometries of the scattering features. A power law exponent of 4 is indicative of a smooth surface. Power law exponents between 3 and 4 are indicative of roughness in surface fractal geometries. Mass fractals typically display power laws smaller than 3 [34]. The validity of these parameters in describing the physical system is checked using complementary techniques such as microscopy. The scanning electron microscopy images show that the morphological features to the order of microns have a smoother interface at room temperature (Figure 5(a-1),(a-2)). Increasing the reaction temperature to 83 °C partially dehydrates lithium hydroxide monohydrate to produce lithium hydroxide and results in rougher interfaces (Figure 5(b-2)). The changes in the surface fractal geometry of these interfaces can be quantified using the porod slope.
One of the advantages of the unified fit approach is that it allows us to describe the morphological features for a given structural regime, i , using no more than two parameters each for Guinier exponential, which are G i and R g i , and power law fits, B i and P i . In this study, the combined USAXS/SAXS curves are modeled to determine the nanostructural features and the morphology of the larger scale features. The microscopy images show that the nano-scale features can be approximated in size to globules (Figure 5(b-2),(c-2)). These features are represented by the q region of 0.006–0.025 Å−1 (Figure 4). The scattering observed in the q region smaller than 0.006 Å−1, which corresponds to larger features, is indistinguishable between the pores and particles (Figure 4). Nevertheless, the porod scattering in this region provides insights into the surface or mass fractal geometry of the scattering features.
The two unified fit parameters that directly describe the shape and the geometry of the scattering features are the guinier radius, R g , and the porod slope, P , respectively. In the larger q-region of 0.006–0.025 Å−1, R g describes the radius of gyration of the nanoparticles, and the porod slope, P , provides insights into the surface or mass fractal geometry of the scattering objects. The geometric radius of the sphere is related to the radius of gyration of a sphere through the following relationship: R g e o = 3 5   R g . In the smaller q-region, where the scattering from the pores and particles is indistinguishable, describing the size and shape of the scattering objects using the Guinier exponential prefactor does not provide physically meaningful insights into the morphology. Therefore, in this region, the scattering is described only using the Porod scattering slope. Further, the scattering from the nano-scale pores is independent of the scattering from the larger objects at smaller q, so the Rg,cutoff function in Irena is implemented.
In the larger q-region of 0.006–0.025 Å−1, which corresponds to the nanoparticles, the porod slope, P , across the entire temperature range of 26–500 °C is 4, indicating that the surfaces of the nanoparticles are smooth. For smooth interfaces, the average surface area, S , the average number of particles per unit volume, N , the scattering contrast factor, ρ 2 , and the scattering vector, q , are related to the scattering intensity, I   ( q ) , through the following relationship:
I   ( q ) = 2 π N ρ 2 S q 4 .
In addition, the volume fraction for a given structural level can be determined independently of the morphology or the geometric arrangement [39], using the following relationship:
Q P =   0 Q 2 d Σ d Ω ( Q ) d Q =   2 π 2 φ   ( 1 φ ) | ρ | 2 .
Here Q P , ϕ, and ρ 2 represent the scattering invariant, the total nanoparticle volume fraction, and the scattering contrast factor, respectively.

3.2.3. Quantification of the Morphological Features from Unified Fit Analyses

The morphological information from the unified fit model in conjunction with the changes in the structure of the lithium hydroxide monohydrate as it is reacted with CO2 to form lithium carbonate provide important insights into reaction driven chemo-morphological changes in complex materials. At the nanostructural level in the q range of 0.006–0.025 Å−1, the porod slope of 4 allows us to apply Equation (3) to determine the specific surface area of the nanoparticles. The dehydration of lithium hydroxide monohydrate to produce lithium hydroxide reduces the Guinier radius of the nanoparticles, R g , from 30 nm at 26 °C to 23 nm at 83 °C, and increases the specific surface area of these nanoparticles from 1938 cm2/cm3 to 16,180 cm2/cm3 (Figure 7a).
In this study, the scattering invariant, which represents the total integrated scattering intensity in the q range 0.006–0.025 Å−1, as shown in Equation (4) also increases as the dehydration of lithium hydroxide monohydrate produces lithium hydroxide in the range of 26 °C to 83 °C (Figure 7b). The corresponding increase in the volumes of the nanoparticles from 0.1% to 0.6% is noted as the reaction temperature is increased from 26 °C to 83 °C (Figure 7b). In this temperature range, the increase in the nanoparticle volume distribution and the reduction in the average nanoparticle size are shown in Figure 8. Noda and Koga [25] suggested that the formation of lithium carbonate from lithium hydroxide monohydrate at lower temperatures may proceed via the presence of a liquid phase at the reaction interface. However, in our reaction system, the gas flow rates are sufficiently high to drive away the water formed during the dehydration process.
In the temperature range of 100 °C to 150 °C, changes in the intensity and integrated intensity of the lithium hydroxide and lithium carbonate peaks (Figure 2 and Figure 3) show that the lithium hydroxide peak reaches a maximum intensity at 147 °C while the lithium carbonate peak continues to increase in intensity. These data suggest that the composition of lithium hydroxide dominates lithium carbonate in the temperature regime of 100 °C to 150 °C. The radius of gyration of the nanoparticles at 97 °C decreases from 20 nm to 14 nm at 147 °C, while the corresponding surface areas increase from 31,370 to 103,370 cm2/cm3. The increase in the volume fractions as the sizes of the nanoparticles become smaller in the temperature range of 100–147 °C is noted in Figure 8. Noda and Koga [25] alluded to morphological self-regulation during the conversion of lithium hydroxide to lithium carbonate based on their kinetic models without providing quantitative microstructural insights. Our data suggest that dehydration decreases the size of the reacting particles, which in turn reduces mass transfer limitations allowing CO2 to access the core of the particle. The enhanced surface area and volume fractions of the reacting nanoparticles also provide CO2 with greater access to the reactive sites.
At temperatures in the range of 196 °C to 450 °C, the increase in the intensity of the lithium carbonate peak (Figure 3) corresponds to the reduced intensity of the lithium hydroxide peak (Figure 2). The conversion of lithium hydroxide to lithium carbonate increases the Guinier radius, R g , of the particles from 14 nm at 196 °C to 15 nm at 449 °C. A significant reduction in the surface area, from 108,900 cm2/cm3 at 196 °C to 24,560 cm2/cm3 at 449 °C, is noted. Further, the volume fraction of the nanoparticles changes from 2.34% to 0.64%. These data indicate the formation of a dense lithium carbonate phase with reduced surface area, which is consistent with the observations reported by Noda and Koga [25]. At 449 °C, the lithium hydroxide phase completely disappears and the scattering is entirely from the lithium carbonate phase (Figure 2 and Figure 3). As the reaction temperature is increased from 449 °C to 499 °C, the agglomeration of the lithium carbonate nanoparticles is noted from the increase in the Guinier radius from 15 nm to 17 nm, and the reduction in the surface area from 24,560 cm2/cm3 at 449 °C to 19,280 cm2/cm3 at 499 °C. The shift in the nanoparticle volume distribution towards larger sizes as the reaction temperature increases from 449 °C to 499 °C is also evident in Figure 8.
In addition to the changes in the nanoparticle structure, insights into the micron-scale morphology are obtained from the scattering data in the q range of 0.0002–0.006 Å−1. As discussed in Section 3.2.2, the scattering observed in this region is indistinguishable between the pores and the particles, so describing the size of the scattering objects using a Guinier radius is not physically meaningful. Instead, the porod exponent provides insights into the fractal geometry of the larger features and the evolution of this geometry as lithium hydroxide monohydrate is converted to lithium carbonate.
The porod slope for the larger scattering features in the lower Q regime of 0.006 Å−1 to 0.002 Å−1 provides insights into relative smoothness or roughness of the larger interfaces as lithium hydroxide monohydrate is converted to lithium hydroxide and then to lithium carbonate. The porod slope of the larger scattering features at 26 °C is 3.7, and dehydration results in a rougher surface characterized by a porod slope around 3 (Figure 9). As the temperature increases from 108 °C to 499 °C, which is characterized by the depletion of the lithium hydroxide phase and formation of lithium carbonate, the increase in the porod slope to 3.4 suggests enhanced smoothness of the surface fractal geometry (Figure 9). These data suggest that the dehydration of lithium hydroxide monohydrate results in rougher nano-scale interfaces, while the formation of lithium carbonate results in smoother surface fractal interfaces at the micron scale.

4. Conclusions

In this study, the morphological and chemical changes as lithium hydroxide monohydrate is converted to lithium carbonate are determined using in-operando USAXS/SAXS/WAXS measurements. The increase in the reaction temperature from 26 °C to 147 °C reduces the Guinier radius of the nanoparticles from 30 nm to 14 nm, while the surface area and the volume fraction of these features increases. The dehydration of lithium hydroxide monohydrate to form lithium hydroxide and the onset of lithium carbonate is noted in this temperature range. At higher reaction temperatures in the range of 222 °C and 500 °C, formation of the denser lithium carbonate phase reduces the surface area and volume fraction of the nanoparticles, and increases the Guinier radius of the nanoparticles from 14 nm to 17 nm. Further, the interfaces at the nanoparticles are smooth, while the larger scattering features at smaller q are characterized by surface fractals representing rough interfaces. The dehydration of lithium hydroxide monohydrate to form lithium hydroxide increases the surface roughness, while the progressive formation of lithium carbonate at higher temperatures results in smoother interfaces. These in operando scattering measurements show the chemo-morphological feedbacks during the conversion of lithium hydroxide monohydrate to lithium carbonate, and the potential for tuning the lithium carbonate’s morphology by changing the reaction temperature, gas composition, and the moisture content for various industrial applications.

Supplementary Materials

The following are available online at www.mdpi.com/2075-163X/7/9/169/s1. Figure S1: The pore volume distributions of lithium hydroxide monohydrate and lithium carbonate determined using the BET method.

Acknowledgments

The author would like to acknowledge the assistance of William Schneider and Meishen Liu in collecting the electron microscopy data. G.G. gratefully acknowledges the support of the Wisconsin Alumni Research Foundation, and the assistance of Jan Ilavsky and Ross Andrews, X-ray Science Division, Argonne National Laboratory, for providing experimental support for the combined USAXS/SAXS/WAXS measurements at the Advanced Photon Source. The use of the Advanced Photon Source, an Office of Science User Facility operated for the U.S. Department of Energy (DOE) Office of Science by Argonne National Laboratory, is supported by the U.S. DOE under Contract DE-AC02-06CH11357.

Conflicts of Interest

The author declares no conflict of interest.

References

  1. Lackner, K.S.; Wendt, C.H.; Butt, D.P.; Joyce, E.L., Jr.; Sharp, D.H. Carbon dioxide disposal in carbonate minerals. Energy 1995, 20, 1153–1170. [Google Scholar] [CrossRef]
  2. Oelkers, E.H.; Gislason, S.R.; Matter, J. Mineral carbonation of CO2. Elements 2008, 4, 333–337. [Google Scholar] [CrossRef]
  3. Park, A.H.A.; Jadhav, R.; Fan, L.S. CO2 mineral sequestration: Chemically enhanced aqueous carbonation of serpentine. Can. J. Chem. Eng. 2003, 81, 885–890. [Google Scholar] [CrossRef]
  4. Park, A.H.A.; Fan, L.S. CO2 mineral sequestration: Physically activated dissolution of serpentine and pH swing process. Chem. Eng. Sci. 2004, 59, 5241–5247. [Google Scholar] [CrossRef]
  5. Gerdemann, S.J.; O’Connor, W.K.; Dahlin, D.C.; Penner, L.R.; Rush, H. Ex situ aqueous mineral carbonation. Environ. Sci. Technol. 2007, 41, 2587–2593. [Google Scholar] [CrossRef] [PubMed]
  6. Gadikota, G.; Park, A.H.A. Accelerated Carbonation of Ca- and Mg-Bearing Minerals and Industrial Wastes Using CO2. In Carbon Dioxide Utilization: Closing the Carbon Cycle; Styring, P., Quadrelli, A., Armstrong, K., Eds.; Elsevier: Oxford, UK, 2014. [Google Scholar]
  7. Gadikota, G.; Matter, J.; Kelemen, P.; Park, A.A. Chemical and morphological changes during olivine carbonation for CO2 storage in the presence of NaCl and NaHCO3. Phys. Chem. Chem. Phys. 2014, 16, 4679–4693. [Google Scholar] [CrossRef] [PubMed]
  8. Pan, S.-Y.; Chang, E.; Chiang, P.-C. CO2 Capture by Accelerated Carbonation of Alkaline Wastes: A Review on Its Principles and Applications. Aerosol Air Qual. Res. 2012, 12, 770–791. [Google Scholar] [CrossRef]
  9. Gadikota, G.; Swanson, E.J.; Zhao, H.; Park, A.H.A. Experimental design and data analysis for accurate estimation of reaction kinetics and conversion for carbon mineralization. Ind. Eng. Chem. Res. 2014, 53, 6664–6676. [Google Scholar] [CrossRef]
  10. Gadikota, G. Commentary: Ex Situ Aqueous Mineral Carbonation. Front. Energy Res. 2016, 4, 21. [Google Scholar] [CrossRef]
  11. Zhao, H.; Park, Y.; Lee, D.H.; Park, A.-H.A. Tuning the dissolution kinetics of wollastonite via chelating agents for CO2 sequestration with integrated synthesis of precipitated calcium carbonates. Phys. Chem. Chem. Phys. 2013, 15, 15185–15192. [Google Scholar] [CrossRef] [PubMed]
  12. O’Connor, W.K.; Dahlin, D.C.; Rush, G.E.; Gerdemann, S.J.; Nilsen, D.N. Final Report: Aqueous Mineral Carbonation: DOE/ARC-TR-04-002; National Energy Technology Laboratory: Albany, OR, USA, 2004. [Google Scholar]
  13. Matter, J.M.; Kelemen, P.B. Permanent storage of carbon dioxide in geological reservoirs by mineral carbonation. Nat. Geosci. 2009, 2, 837–841. [Google Scholar] [CrossRef]
  14. Kelemen, P.B.; Matter, J.; Streit, E.E.; Rudge, J.F.; Curry, W.B.; Blusztajn, J. Rates and mechanisms of mineral carbonation in peridotite: Natural processes and recipes for enhanced, in situ CO2 capture and storage. Annu. Rev. Earth Planet. Sci. 2011, 39, 545–576. [Google Scholar] [CrossRef]
  15. Gadikota, G.; Fricker, K.; Jang, S.-H.; Park, A.-H.A. Carbonation of Silicate Minerals and Industrial Wastes and Their Potential Use as. In Advances in CO2 Capture, Sequestration, and Conversion; Jin, F., He, L.-N., Hu, Y.H., Eds.; American Chemical Society: Washington, DC, USA, 2015; pp. 295–322. [Google Scholar]
  16. Contestabile, M.; Panero, S.; Scrosati, B. A laboratory-scale lithium battery recycling process. J. Power Sources 1999, 83, 75–78. [Google Scholar] [CrossRef]
  17. Granata, G.; Moscardini, E.; Pagnanelli, F.; Trabucco, F.; Toro, L. Product recovery from Li-ion battery wastes coming from an industrial pre-treatment plant: Lab scale tests and process simulations. J. Power Sources 2012, 206, 393–401. [Google Scholar] [CrossRef]
  18. Richa, K.; Babbitt, C.W.; Gaustad, G.; Wang, X. A future perspective on lithium-ion battery waste flows from electric vehicles. Resour. Conserv. Recycl. 2014, 83, 63–76. [Google Scholar] [CrossRef]
  19. Gaines, L. The future of automotive lithium-ion battery recycling: Charting a sustainable course. Sustain. Mater. Technol. 2014, 1, 2–7. [Google Scholar] [CrossRef]
  20. Nan, J.; Han, D.; Zuo, X. Recovery of metal values from spent lithium-ion batteries with chemical deposition and solvent extraction. J. Power Sources 2005, 152, 278–284. [Google Scholar] [CrossRef]
  21. Williams, D.D.; Miller, R.R. Effect of Water Vapor on the LiOH-CO2 Reaction. Dynamic Isothermal System. Ind. Eng. Chem. Fundam. 1970, 9, 454–457. [Google Scholar] [CrossRef]
  22. Boryta, D.A.; Maas, A.J. Factors Influencing Rate of Carbon Dioxide Reaction with Lithium Hydroxide. Ind. Eng. Chem. Process Des. Dev. 1971, 10, 489–494. [Google Scholar] [CrossRef]
  23. Wang, T.C.; Bricker, J.L. Combined temperature and water vapor effects on the lithium hydroxide-carbon dioxide reaction in underwater life support systems. Environ. Int. 1979, 2, 425–430. [Google Scholar] [CrossRef]
  24. Zho, Z.; Chashchin, V.A.; Vishnyakov, A.V. Carbonization kinetics of lithium hydroxide and its monohydrate. Theor. Found. Chem. Eng. 2007, 41, 577–584. [Google Scholar] [CrossRef]
  25. Noda, Y.; Koga, N. Phenomenological kinetics of the carbonation reaction of lithium hydroxide monohydrate: Role of surface product layer and possible existence of a liquid phase. J. Phys. Chem. C 2014, 118, 5424–5436. [Google Scholar] [CrossRef]
  26. Gadikota, G.; Zhang, F.; Allen, A.J. Towards understanding the microstructural and structural changes in natural hierarchical materials for energy recovery: In-operando multi-scale X-ray scattering characterization of Na- and Ca-montmorillonite on heating to 1150 °C. Fuel 2017, 196, 195–209. [Google Scholar] [CrossRef]
  27. Gadikota, G.; Allen, A.J. Microstructural and structural characterization of materials for CO2 storage using multi-scale scattering methods. In Materials and Processes for CO2 Capture, Conversion, and Sequestration; Li, L., Wong-Ng, W., Eds.; John Wiley & Sons: Hoboken, NJ, USA, 2017. [Google Scholar]
  28. Chupas, P.J.; Chapman, K.W.; Kurtz, C.; Hanson, J.C.; Lee, P.L.; Grey, C.P. A versatile sample-environment cell for non-ambient X-ray scattering experiments. J. Appl. Crystallogr. 2008, 41, 822–824. [Google Scholar] [CrossRef]
  29. Ilavsky, J.; Jemian, P.R.; Allen, A.J.; Zhang, F.; Levine, L.E.; Long, G.G. Ultra-small-angle X-ray scattering at the Advanced Photon Source. J. Appl. Crystallogr. 2009, 42, 469–479. [Google Scholar] [CrossRef]
  30. Ilavsky, J.; Zhang, F.; Allen, A.J.; Levine, L.E.; Jemian, P.R.; Long, G.G. Ultra-small-angle X-ray scattering instrument at the advanced photon source: History, recent development, and current status. Metall. Mater. Trans. A 2013, 44, 68–76. [Google Scholar] [CrossRef]
  31. Black, D.R.; Windover, D.; Henins, A.; Gil, D.; Filliben, J.; Cline, J.P. Certification of nist standard reference material 640d. Powder Diffr. 2010, 25, 187–190. [Google Scholar] [CrossRef]
  32. Ilavsky, J.; Jemian, P.R. Irena: Tool suite for modeling and analysis of small-angle scattering. J. Appl. Crystallogr. 2009, 42, 347–353. [Google Scholar] [CrossRef]
  33. Ilavsky, J. Nika: Software for two-dimensional data reduction. J. Appl. Crystallogr. 2012, 45, 324–328. [Google Scholar] [CrossRef]
  34. Beaucage, G. Small-Angle Scattering from Polymeric Mass Fractals of Arbitrary Mass-Fractal Dimension. J. Appl. Crystallogr. 1996, 29, 134–146. [Google Scholar] [CrossRef]
  35. Alcock, N.W. Refinement of the crystal structure of lithium hydroxide monohydrate. Acta Crystallogr. Sect. B Struct. Crystallogr. Cryst. Chem. 1971, 27, 1682–1683. [Google Scholar] [CrossRef]
  36. Dachs, H. Bestimmung der Lage des Wasserstoffs in LiOH durch Neutronenbeugung. Z. Krist. Mater. 1959, 112, 60–67. [Google Scholar] [CrossRef]
  37. Zemann, J. Die Kristallstruktur von Li2CO3. Acta Crystallogr. 1957, 10, 664–666. [Google Scholar] [CrossRef]
  38. Beaucage, G. Approximations leading to a unified exponential power-law approach to small-angle scattering. J. Appl. Crystallogr. 1995, 28, 717–728. [Google Scholar] [CrossRef]
  39. Glatter, O.; Kratky, O. Small Angle Scattering; Academic: New York, NY, USA, 1982. [Google Scholar]
Figure 1. Changes in (a) the characteristic lithium hydroxide monohydrate peak (d = 2.67 Å, q = 2.35 Å−1, or CuKα 2θ = 33.5°) and (b) the integrated peak intensity on reacting with CO2 in the temperature range of 26 °C to 108 °C. The relative integrated intensity represented in (b) is the integrated intensity of the characteristic lithium hydroxide monohydrate peak at a given temperature normalized to the integrated intensity at 26 °C. Vertical bars in (b) represent estimated standard deviation uncertainties.
Figure 1. Changes in (a) the characteristic lithium hydroxide monohydrate peak (d = 2.67 Å, q = 2.35 Å−1, or CuKα 2θ = 33.5°) and (b) the integrated peak intensity on reacting with CO2 in the temperature range of 26 °C to 108 °C. The relative integrated intensity represented in (b) is the integrated intensity of the characteristic lithium hydroxide monohydrate peak at a given temperature normalized to the integrated intensity at 26 °C. Vertical bars in (b) represent estimated standard deviation uncertainties.
Minerals 07 00169 g001aMinerals 07 00169 g001b
Figure 2. Changes in (a) the characteristic lithium hydroxide peak (d = 2.75 Å, q = 2.28 Å−1 or CuKα 2θ = 32.5°) and (b) the integrated peak intensity on reacting with CO2 in the temperature range of 26 °C to 499 °C. The relative integrated intensity represented in (b) is the integrated intensity normalized relative to the maximum integrated intensity of the lithium hydroxide peak at 108 °C. The movement of the peak to the left in (a) corresponds to the effects of thermal expansion. Vertical bars in (b) represent estimated standard deviation uncertainties.
Figure 2. Changes in (a) the characteristic lithium hydroxide peak (d = 2.75 Å, q = 2.28 Å−1 or CuKα 2θ = 32.5°) and (b) the integrated peak intensity on reacting with CO2 in the temperature range of 26 °C to 499 °C. The relative integrated intensity represented in (b) is the integrated intensity normalized relative to the maximum integrated intensity of the lithium hydroxide peak at 108 °C. The movement of the peak to the left in (a) corresponds to the effects of thermal expansion. Vertical bars in (b) represent estimated standard deviation uncertainties.
Minerals 07 00169 g002
Figure 3. Changes in (a) the characteristic lithium carbonate peak (d = 2.83 Å, q = 2.22 Å−1, or CuKα 2θ = 31.6°) and (b) the integrated peak intensity on reacting with CO2 in the temperature range of 26 °C to 500 °C. The movement of the peak to the left in (a) corresponds to the effects of thermal expansion. Vertical bars in (b) represent estimated standard deviation uncertainties.
Figure 3. Changes in (a) the characteristic lithium carbonate peak (d = 2.83 Å, q = 2.22 Å−1, or CuKα 2θ = 31.6°) and (b) the integrated peak intensity on reacting with CO2 in the temperature range of 26 °C to 500 °C. The movement of the peak to the left in (a) corresponds to the effects of thermal expansion. Vertical bars in (b) represent estimated standard deviation uncertainties.
Minerals 07 00169 g003
Figure 4. Changes in the combined slit-smeared Ultra-Small Angle and Small-Angle X-ray Scattering (USAXS/SAXS) data on reacting lithium hydroxide monohydrate with CO2 to form lithium carbonate in the temperature range of 26 °C to 500 °C.
Figure 4. Changes in the combined slit-smeared Ultra-Small Angle and Small-Angle X-ray Scattering (USAXS/SAXS) data on reacting lithium hydroxide monohydrate with CO2 to form lithium carbonate in the temperature range of 26 °C to 500 °C.
Minerals 07 00169 g004
Figure 5. Microscopic views of lithium hydroxide monohydrate ((a-1),(a-2)) as it is partially converted to lithium hydroxide at 83 °C ((b-1),(b-2)) and completely transformed to lithium carbonate at 500 °C ((c-1),(c-2)). The surface morphology of lithium hydroxide monohydrate at 26 °C is smoother compared to lithium hydroxide at 499 °C. The micron-scale morphology of the materials represented here show rough surface interfaces, which is indicative of fractal microstructures.
Figure 5. Microscopic views of lithium hydroxide monohydrate ((a-1),(a-2)) as it is partially converted to lithium hydroxide at 83 °C ((b-1),(b-2)) and completely transformed to lithium carbonate at 500 °C ((c-1),(c-2)). The surface morphology of lithium hydroxide monohydrate at 26 °C is smoother compared to lithium hydroxide at 499 °C. The micron-scale morphology of the materials represented here show rough surface interfaces, which is indicative of fractal microstructures.
Minerals 07 00169 g005
Figure 6. Calculated contrast factors for determining morphological properties as lithium hydroxide monohydrate is converted to lithium carbonate.
Figure 6. Calculated contrast factors for determining morphological properties as lithium hydroxide monohydrate is converted to lithium carbonate.
Minerals 07 00169 g006
Figure 7. Changes in the (a) specific surface area and the radius of gyration, R g , of the nano-scale particles and (b) the scattering invariant and the volume of nanoparticles as lithium hydroxide monohydrate is converted to lithium carbonate.
Figure 7. Changes in the (a) specific surface area and the radius of gyration, R g , of the nano-scale particles and (b) the scattering invariant and the volume of nanoparticles as lithium hydroxide monohydrate is converted to lithium carbonate.
Minerals 07 00169 g007
Figure 8. Changes in the nanoparticle volume distribution as lithium hydroxide monohydrate reacts with CO2 to form lithium carbonate in the temperature range of 26 °C to 500 °C.
Figure 8. Changes in the nanoparticle volume distribution as lithium hydroxide monohydrate reacts with CO2 to form lithium carbonate in the temperature range of 26 °C to 500 °C.
Minerals 07 00169 g008
Figure 9. Changes in the porod slope of the scattering features in the q range of 0.0002–0.006 Å−1. Porod slope in the range of 3–4 indicates a surface fractal, with 4 being a smooth interface. As the reaction temperature increases to 100 °C, the dehydration of lithium hydroxide monohydrate to produce lithium hydroxide results in a rougher interface. Progressive growth of lithium carbonate with increase in reaction temperature above 100 °C reduces the roughness of the interface.
Figure 9. Changes in the porod slope of the scattering features in the q range of 0.0002–0.006 Å−1. Porod slope in the range of 3–4 indicates a surface fractal, with 4 being a smooth interface. As the reaction temperature increases to 100 °C, the dehydration of lithium hydroxide monohydrate to produce lithium hydroxide results in a rougher interface. Progressive growth of lithium carbonate with increase in reaction temperature above 100 °C reduces the roughness of the interface.
Minerals 07 00169 g009

Share and Cite

MDPI and ACS Style

Gadikota, G. Connecting the Morphological and Crystal Structural Changes during the Conversion of Lithium Hydroxide Monohydrate to Lithium Carbonate Using Multi-Scale X-ray Scattering Measurements. Minerals 2017, 7, 169. https://doi.org/10.3390/min7090169

AMA Style

Gadikota G. Connecting the Morphological and Crystal Structural Changes during the Conversion of Lithium Hydroxide Monohydrate to Lithium Carbonate Using Multi-Scale X-ray Scattering Measurements. Minerals. 2017; 7(9):169. https://doi.org/10.3390/min7090169

Chicago/Turabian Style

Gadikota, Greeshma. 2017. "Connecting the Morphological and Crystal Structural Changes during the Conversion of Lithium Hydroxide Monohydrate to Lithium Carbonate Using Multi-Scale X-ray Scattering Measurements" Minerals 7, no. 9: 169. https://doi.org/10.3390/min7090169

Note that from the first issue of 2016, this journal uses article numbers instead of page numbers. See further details here.

Article Metrics

Back to TopTop