16 Jan 2014: Forsgren J, Frykstrand S, Grandfield K, Mihranyan A, Strømme M (2014) Correction: A Template-Free, Ultra-Adsorbing, High Surface Area Carbonate Nanostructure. doi: info:doi/10.1371/annotation/0878101b-450f-44a9-abd5-b2434957a698 View correction
We report the template-free, low-temperature synthesis of a stable, amorphous, and anhydrous magnesium carbonate nanostructure with pore sizes below 6 nm and a specific surface area of ∼ 800 m2 g−1, substantially surpassing the surface area of all previously described alkali earth metal carbonates. The moisture sorption of the novel nanostructure is featured by a unique set of properties including an adsorption capacity ∼50% larger than that of the hygroscopic zeolite-Y at low relative humidities and with the ability to retain more than 75% of the adsorbed water when the humidity is decreased from 95% to 5% at room temperature. These properties can be regenerated by heat treatment at temperatures below 100°C.The structure is foreseen to become useful in applications such as humidity control, as industrial adsorbents and filters, in drug delivery and catalysis.
Citation: Forsgren J, Frykstrand S, Grandfield K, Mihranyan A, Strømme M (2013) A Template-Free, Ultra-Adsorbing, High Surface Area Carbonate Nanostructure. PLoS ONE 8(7): e68486. doi:10.1371/journal.pone.0068486
Editor: Richard G. Haverkamp, Massey University, New Zealand
Received: April 15, 2013; Accepted: May 30, 2013; Published: July 17, 2013
Copyright: © 2013 Forsgren et al. This is an open-access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.
Funding: The Carl Trygger Foundation (www.carltryggersstiftelse.se) and the Swedish Research Council (www.vr.se)are acknowledged for financing our work. The funders had no role in study design, data collection and analysis, decision to publish, or preparation of the manuscript.
Competing interests: The authors have declared that no competing interests exist.
Nanotechnology is starting to influence most scientific areas and this key enabling technology is foreseen to significantly impact all materials science dependent industries during the coming decades –. The interest in high surface area nanostructured materials from 1990 onwards has increased exponentially for all classes of porous materials and at the beginning of 2013, according to the ISI Web of Knowledge, there were in total about 60,500 records on zeolites, 20,500 records for mesoporous silica and 13,100 records on metal organic framework (MOF) materials, whereas before 1990 these numbers were insignificant. The most common way to produce high surface area materials with micro-mesoporous structures, i.e., pores with diameters below 50 nm, is by using soft templates and building around them a more rigid structure after which the template is eluted with a solvent or burnt away to produce the rigid porous material.
In the current work we will show that it is possible, at low temperatures and without the use of templates, to synthesize a unique high surface area nanostructure with a well-defined pore-size distribution of sub 6 nm pores of a widely used, non-toxic and GRAS (generally-recognised-as-safe)-listed material that is already included in the FDA Inactive Ingredients Database ; viz. magnesium carbonate.
Magnesium is the eighth most abundant element in the earth’s crust and essential to most living species. It can form several structures of hydrated carbonates such as nesquehonite (MgCO3·3H2O), and lansfordite (MgCO3·5H2O), a number of basic carbonates such as hydromagnesite (4 MgCO3·Mg(OH)2·4 H2O), and dypingite (4 MgCO3·Mg(OH)2·5 H2O), as well as the anhydrous and rarely encountered magnesite (MgCO3) . In contrast to other alkali earth metal carbonates, chemists have found anhydrous magnesium carbonate difficult to produce, particularly at low temperatures. Above 100°C, magnesite (crystalline MgCO3) can be obtained from Mg(HCO3)2 solutions by precipitation. However, at lower temperatures, hydrated magnesium carbonates tend to form, giving rise to what has been referred to as “the magnesite problem” .Yet, not only chemists have been intrigued by magnesium carbonates. Although abundant in nature, where crystalline forms exist as traces in most geological structures, pure magnesium carbonate is seldom found on its own in larger deposits, a fact that has puzzled geologist for more than a century .
In 1908, Neuberg and Rewald tried to synthesise magnesite in alcohol suspensions of MgO . However, it was concluded that MgCO3 cannot be obtained by passing CO2 gas through such suspensions due to the more likely formation of magnesium dimethyl carbonate (Mg(OCOOCH3)2). Subsequent studies by Kurov in 1961  and Buzágh in 1926  only reiterated the assumption that MgO preferentially forms complex dimethyl carbonates when reacted with CO2 in methanol. A further overview of early works is provided in detail in Text S1 and Figure S1.
Yet, by changing the synthesis conditions in comparison to what has been described earlier, we here report the successful formation of a magnesium carbonate, hereafter referred to as Upsalite, in a reaction between MgO, methanol and CO2 resulting in an anhydrous, micro-mesoporous and large surface area structure. We further show that the moisture sorption of the material is featured by a unique set of properties including an adsorption capacity ∼50% larger than that of the hygroscopic zeolite-Y at low relative humidities and with the ability to retain more than 75% of the adsorbed water when the humidity is decreased from 95% to 5% at room temperature. The humid material is easily regenerated to regain its moisture sorption characteristic upon storage at only 95°C.
Results and Discussion
The synthesis is carried out well below 100°C, while previously reported amorphous structures of magnesium carbonate have been formed at higher temperatures by thermal decomposition of hydrated magnesium carbonates – or of a double salt of magnesium ammonium carbonate . In the current work, CO2 is not bubbled through the methanolic suspension, instead the reaction vessel is pressurised with CO2 to moderate relative pressures (1–3 bar). Initially, the temperature is kept at 50°C in order to facilitate a reaction between MgO and methanol, and after ∼ 3 h the temperature is decreased to room temperature. This results in formation of a rigid gel in the reaction vessel after ∼ 4 days. When dried in air at 70°C, the gel solidifies and collapses into a white and coarse powder that is primarily X-ray amorphous with traces of unreacted and crystalline MgO, see XRD pattern in Figure 1a. The sharp peaks at 2 θ equal to 43° and 62° originate from the unreacted MgO , while the halo peak between 2 θ values of 25° and 40° is indicative of at least one amorphous phase.
a) XRD pattern. The halo at 2 θ∼30° indicates the presence of at least one amorphous phase and the sharp peaks at higher scattering angles pertain to crystalline MgO. b) Raman spectrum. The band observed at ∼1100 cm−1 stems from vibration of the CO3 group and the halo cantered at 100 cm−1 is a Boson peak. c) FTIR spectrum. The three visible absorption bands (1440 cm−1, 1100 cm−1 and 850 cm−1) are all due to vibrations of the CO3 group. d) and e) XPS Mg2p and O1s peaks. The Mg2p peak at 52.1 eV and the O1s peak at 533.5 eV stem from MgCO3, the O1s peak at 531.0 eV from MgO and the O1s peak at 535.6 eV from surface adsorbed water. The solid lines represent the measured spectrum. The coloured lines are calculated using the CasaXPS software and represent the fitted curves (obtained using Gaussian-Lorentzian functions) and the subtracted background (obtained using a Shirley function).
Raman spectroscopy reveals that the powder indeed is composed of a carbonate (Figure 1b), where the band at ∼1100 cm−1 corresponds to vibration of the carbonate group . Moreover, a broad halo, or the so-called Boson peak, with a maximum at ∼100 cm−1, is further witness to the amorphous character of the powder .
When examined with Fourier transform infrared spectroscopy (FTIR, Figure 1c) the material displayed absorption bands at ∼1440 cm−1, ∼1100 cm−1 and ∼850 cm−1, which all correspond to the carbonate group . No water of crystallisation is visible in this spectrum , . The anhydrous character of the bulk material is further confirmed by Thermal Gravimetric Analysis (TGA) (see Figure S2).
X-ray photoelectron spectroscopy (XPS) confirms the anhydrous nature of the MgCO3. Energy resolved spectra were recorded for the Mg2p and O1s peaks (Figure 1d,e) which were found to be positioned at 52.1 eV and 533.5 eV, respectively, which is indicative of MgCO3 . Further, the O1s peak does not contain any components for crystal water which, expectedly, would have appeared at 533–533.5 eV . The shoulder seen at 535.6 eV is located between the binding energies for liquid water (539 eV) and ice (533 eV)  and is, therefore, representative of surface adsorbed water as previously described for adsorbed water on carbon fibres , . The shoulder seen at 531.0 eV shows the presence of MgO in the powder. No presence of Mg(OH)2 was observed in the bulk, which would have resulted in a peak at 532.4 eV .
Having proved the formation of amorphous anhydrous MgCO3 by XRD, Raman, FTIR, and XPS, we postulate the following simplified route of synthesis, based on the presence of HOMgOCH3 as an intermediate (as confirmed with FTIR in Figure S3) and the necessity of heat treatment in the last synthesis step:(1a)(1b)(1c)(1d)
The presence of a hydroxyl group in the vicinity of the methoxy group in HOMgOCOOCH3 makes the compound labile and will therefore favour internal transition to a solvate MgCO3·CH3OH and loss of methanol upon heating to 70°C:(1e)
As it is evident from the above cascade scheme, the postulated reaction of MgCO3 formation goes through several steps, some of which are equilibrium reactions, namely 1a and 1b. A schematic description of the reaction steps is presented in Figure 2.
i) In the first step MgO (s) is mixed with methanol under 3 bar CO2 pressure at 50°C. ii) After 2.5 h the HOMgOCH3 is formed in the solution, the pressure is lowered to 1 bar and the heating is turned off. At the same time the methanol reacts with the CO2 and forms CH3OCOOH (methyl hemicarbonic acid). iii) HOMgOCH3 reacts with CH3OCOOH and forms water and H3COCOOMgOCH3 (methyl esther of magnesium methyl carbonate). At this point the solution changes colour from white to light yellow. iv) H3COCOOMgOCH3 reacts with the water formed in step iii) and forms HOMgOCOOCH3 (or MgCO3·CH3OH) which upon v) heating at 70°C releases CH3OH and forms MgCO3.
In order to analyse the pore structure and water sorption capacity of Upsalite, N2 and H2O vapour sorption analyses were performed. Figure 3a shows the N2 sorption isotherm for Upsalite, which exhibits a typical Type 1 shape according to the IUPAC classification . The SSA of 800 m2 g−1 for the material (Table 1) was derived from such isotherms according to the Brunauer-Emmet-Teller (BET) equation , substantially surpassing the SSA of all previously described alkali earth metal carbonates, where crystalline forms of magnesium carbonates typically have a SSA of 4–18 m2 g−1 . This high SSA places Upsalite in the exclusive class of high surface area nanomaterials including mesoporous silica, zeolites, MOFs, and carbon nanotubes.
a) N2 sorption isotherm at 77 K. b) Incremental pore volume (violet) and cumulative pore volume (blue) obtained from N2 sorption isotherm. c) Moisture sorption isotherm at room temperature for Upsalite (blue), Mg5(CO3)4(OH)2·4H2O (green), Aerosil (red) and Zeolite Y (black). The arrows indicate the direction of the pressure change.
Figure 3c displays the H2O vapour sorption isotherm for Upsalite and, based on the large amount of H2O adsorbed at low RHs, it is evident that the material is highly hydrophilic . The limited desorption of moisture from the material when the vapour pressure is reduced from 95% is further proof of the strong interaction between water molecules and the material. It should, however, be noted that no signs of hydrate formation in the material are seen using XRD after the sorption isotherm is completed, and that the sorption isotherm can be repeated with undistinguishable results after heat treatment at moderate temperatures (95°C) under vacuum. This contrasts to the regeneration of moisture sorption properties of, e.g., Zeolites typically requiring heat treatments at temperatures between 150°C and ∼600°C.
Further, both the N2 and the H2O vapour sorption isotherms were analysed in order to establish the microporous properties of the material according to the Dubinin-Astakhov (D-A) model , see Table 1. The hydrophilic nature of the material is further reflected in the greater characteristic energy for adsorption of H2O compared to N2. The discrepancy in the limiting micropore volume (w0) – in which the value obtained from the N2 sorption isotherm is to be regarded as the “true” value – and modal equivalent pore size obtained from the two sorption isotherms is most likely due to site-specific interaction between the H2O species and the material, not only in the micropores but also on the exterior of the material and in pores larger than 2 nm .
Figure 3b shows the incremental and cumulative pore volume obtained through density functional theory (DFT) calculations on the N2 sorption isotherm. From these calculations it infers that about 98% of the pore volume is inherent to pores with a diameter smaller than 6 nm, while the remaining pore volume is made up of pores with a broad size distribution between 8 and 80 nm centred at ∼16 nm.
When examined with scanning electron microscopy (SEM), these pores in the larger size range are clearly visible (Figure 4a–b). Furthermore, the highly porous nature of the material is evident from the scanning transmission electron microscopy (STEM) tomography work available in the Supporting Information (see Video S1 and S2 and Figure S4; S4.1). Such three-dimensional reconstructions allow for visualisation of the internal pore structure of the material via a series of slices through the volume. Measurements from these slices, which essentially represent cross-sections, confirm that pore widths are consistently 16 nm, while pore heights vary between 8 and 50 nm. However, these larger pore networks that are visible with SEM and STEM are not noted throughout the entire material, which is consistent with the limited contribution from these pores to the total pore volume as determined by DFT. In the transmission electron microscopy (TEM) image in Figure 4c the smaller pores, dominating the contribution to the total pore volume sensed by nitrogen sorption, can be distinguished. An enlargement of pores was found to take place under the electron beam where the sample was unstable for long periods of time. This enlargement is most likely due to remaining organic groups leaving the sample. A representative image recorded after a longer period (∼ 1 min) under the electron beam is shown in Figure S4 (S4.2).
a) SEM micrograph of Upsalite. Scale bar, 1 µm. b) Higher magnification SEM of a region in a) clearly showing the textural porosity of the material. Scale bar, 200 nm. c) Representative TEM image of Upsalite showing contrast consistent with a porous material. The image is recorded with under-focused conditions to enhance the contrast from the pores. Scale bar, 50 nm.
The water sorption capacity of the material is interesting from an industrial and technological point of view and it is, hence, compared to three commercially available desiccants, namely fumed silica (SSA: 196 m2 g−1), hydromagnesite (SSA: 38 m2 g−1) and the microporous Zeolite Y (SSA: 600 m2 g−1, silica/alumina ratio 5.2∶1), see Figure 3c. For comparison, all samples were degassed at 95°C under vacuum for 10 h prior to analysis. The H2O vapour adsorption isotherm for Upsalite displays similarities with the hydrophilic zeolite at very low RHs (<1%) and shows an even higher adsorption capacity compared to the zeolite at RHs between 1 and 60%. This behaviour contrasts largely to that of the other two non-porous materials, i.e. fumed silica and hydromagnesite, which mainly adsorb H2O at RH >60%.
Amorphous magnesium carbonates produced by high temperature thermal decomposition of hydromagnesite, nesquehonite, or magnesium ammonium carbonate double salt have previously been reported to be unstable upon hydration , . In particular, instability of the hydromagnesite decomposed material was evident by a weakening of the carbonate bond . Such weakening was observed by a shift towards lower temperatures, as well as by the development of a shoulder and a split into two or more peaks, of the carbonate decomposition peak located above 350°C in differential TGA (dTGA) spectra . In this respect, Upsalite appears to remain stable upon hydration. After 11 weeks of storage at RT and 100% RH no peak split, shoulders or movement of the carbonate decomposition peak towards lower temperatures is observed in dTGA spectra (see Figure S5). In fact, the decomposition peak for the carbonate bond is shifted towards higher temperatures as compared to the as-synthesized material (Figure S2 and S5), indicating a strengthening of the carbonate bond.
We report herein the template-free formation of a stable, amorphous magnesium carbonate nanostructure formed at low temperature in a methanol solution of MgO with CO2. The obtained magnesium carbonate is featured with a unique structure of pores almost exclusively in the sub 6 nm size range and extraordinarily high surface area, which has never been reported before, neither for natural nor synthetic magnesium carbonates. The material described in this work is further featured with extraordinary water sorption properties that can be regenerated at temperatures below 100°C. The material is foreseen to find its use in a number of applications including humidity control and delivery systems for therapeutic or volatile agents.
Materials and Methods
In the current work 4 g magnesium MgO powder was placed in a glass bottle together with 60 ml methanol and a stirring magnet. The solution was put under 3 bar CO2 pressure and heated to 50°C. After approximately 4 hours the mixture was allowed to cool to RT and the carbon dioxide pressure was lowered to 1 bar, and the reaction continued until a gel had formed. When a gel was obtained, the carbon dioxide pressure was removed and the gel was allowed to solidify and dry at ∼70°C during 3 days. A schematic description of the synthesis is found in Fig. 2.
XRD analysis was performed with a Siemens/Bruker D5000 instrument using Cu-Kα radiation. Samples were ground and put on a silicon sample holder with zero background prior to analysis. The instrument was set to operate at 45 kV and 40 mA.
A Reinshaw Ramanscope was used for the Raman studies. The Raman instrument was calibrated with a silicon wafer using the band at 521 cm−1 prior to the studies. A 524 nm argon-ion laser with a 10 µm spot size was used for analysis.
Fourier transform infrared spectroscopy.
The FTIR studies were performed on a Bruker IFS 66v/S spectrometer using an Attenuated Total Reflectance (ATR) sample holder from SENSIR. 50 scans were signal-averaged in each spectrum and the resolution was 4 cm−1. Before the measurement a background scan was recorded and thereafter subtracted from the spectrum for the sample.
X-ray photoelectron spectroscopy.
The XPS experiments were conducted on a Phi Quantum 200 Scanning ESCA microprobe instrument. Prior to analysis, the samples were sputter cleaned using argon ions for 10 min at 200 V to remove surface adsorbed contaminations. A full spectrum was recorded together with energy resolved spectra for Mg2p and O1s. During the acquisition, an electron beam of 20 µA was used together with argon ions to neutralise the non-conducting sample. The peak fittings were made with CasaXPS software, the curves were fitted using Gaussian-Lorentzian functions and the background was subtracted using a Shirley function. The spectra were calibrated against the O1s peak for magnesium oxide (531.0 eV) instead of the C1s peak at 285.0 eV for adventitious carbon, which otherwise is commonly used as a reference. However, in the case of MgO, the binding energy for adventitious carbon is not reliable as reference since hydrocarbons interact with magnesium oxide in a way that shifts the C1s peak randomly making it unsuitable as a reference. Therefore, the O1s peak for MgO (531.0 eV) is instead proposed to be used as an internal reference . The presence of magnesium oxide in the samples was confirmed by XRD analysis prior to the XPS study.
N2 sorption analysis.
Gas sorption measurements were carried out with N2 at 77 K using an ASAP 2020 from Micromeritics. The samples were degassed at 95°C under vacuum for 10 h prior to analysis. The SSA was determined by applying the BET equation  to the relative pressure range of 0.05–0.30 for the adsorption branch of the isotherm. The D-A equation was employed on the appropriate pressure region for adsorption in micropores. The BET and D-A calculations were performed with the ASAP 2020 V3.04 software from Micromeritics delivered together with the analysis equipment. The pore size distribution was determined using DFT analysis carried out with the DFT Plus software from Micrometrics using the model for N2 at 77K for slit-shape geometry with low regularisation (λ = 0.005). The standard deviation of the DFT fit was 2.037 cm3/g.
Scanning electron microscopy.
For the SEM analyses, a Leo 1550 instrument from Zeiss equipped with an in-lens detector was used. Prior to the studies, the samples were cooled with liquid N2, crushed and put on a stub holder with double-sided carbon tape. As a last step prior to analysis the sample was sputter coated with a thin layer of gold/palladium.
Thermal gravimetric analysis.
TGA analysis was carried out under a flow of air in an inert alumina cup with sample sizes of approximately 15 mg. The samples were heated from RT to 700°C with a heating ramp of 10°C min−1 using a Thermogravimetric analyser from Mettler Toledo, model TGA/SDTA851e.
Water vapour sorption.
An ASAP 2020 instrument from Micromeritics was used for the water sorption studies. Prior to analysis the samples were degassed at 95°C under vacuum for 10 h. The D-A equation was employed on the appropriate pressure region for adsorption in micropores. The affinity coefficient (β) for water was set to 0.2 in the D-A calculations, which has been shown to be an appropriate value for analysis of polar surfaces .
Scanning transmission electron microscopy and electron tomography.
Scanning transmission electron microscopy (STEM) samples were prepared by dispersing the powder in ethanol and placing 20 µl on a Quantifoil® TEM grid. Experiments were performed on an FEI Tecnai F20 (FEI Company, The Netherlands) operated at 200 kV. Images were recorded on a high-angle annular dark-field detector (HAADF). The Dual-Axis Tomography Holder Model 2040 (Fischione Instruments, PA, USA) was used in a linear tilt scheme to acquire a single-axis tilt-series with image acquisition increments of 2°. Automated focusing, image shifting, and acquisition of HAADF STEM images over an angular range of ±62° were achieved using the Explore3D software (FEI Company, The Netherlands). The 3D reconstructions were computed using a simultaneous iterative reconstruction technique, with 20 iterations, in Inspect3D (FEI Company, The Netherlands). Models for 3D visualisation were created in Amira Resolve RT FEI (Visage Imaging Inc., USA).
Transmission Electron Microscopy (TEM).
HRTEM images were taken with a JEOL-3010 microscope, operating at 300 kV (Cs 0.6 mm, resolution 1.7 Å). Images were recorded using a CCD camera (model Keen View, SIS analysis, size 1024×1024, pixel size 23.5×23.5 µm) at 30 000–100 000× magnification using low-dose conditions on as-crushed samples.
X-ray pattern of the material obtained when water was deliberately added to the synthesis. All peaks in the pattern corresponds to nesquehonite, Mg(HCO3)(OH)·2 H2O, (PDF# 00-020-0669). No signs of residual MgO can be detected in the pattern.
Thermal Gravimetric Analysis of Upsalite. TGA and dTGA curves for Upsalite.
FTIR spectrum for the in-situ sample collected from the reaction vessel after 3 hours of reaction, together with a reference sample.
STEM Tomography and TEM. Internal pore structure from electron tomography. Slices through two electron tomographic reconstructions of the Upsalite material. Essentially representing an internal cross-section, pore size measurements from these volumetric slices indicate pore sizes with one dimension measuring on average 16 nm, and the other varying between 50 nm and 8 nm (S4.1). TEM image showing Upsalite sample after a long period (∼1 min) under the electron beam (S4.2).
Differential Thermal Gravimetric Analysis of Upsalite stored at 100% humidity and RT for different time periods.
Overview of earlier work.
Electron tomographic tilt-series. The as-acquired electron tomographic tilt-series of Upsalite comprised of HAADF STEM images taken over ±62°.
Electron tomographic reconstruction. Volumetric slices through the reconstructed volume, followed by a three-dimensional rendering, reveal the internal pore structure of Upsalite.
We thank Prof. Peter Lazor for assistance with interpretation of the Raman spectra, Dr. Alfonso E. Garcia-Bennett for recording the TEM images and Dr. Martin Sjödin for initial discussions regarding the reaction mechanism.
Conceived and designed the experiments: JF AM MS. Performed the experiments: SF KG JF. Analyzed the data: JF AM SF MS KG. Contributed reagents/materials/analysis tools: JF AM SF MS KG. Wrote the paper: JF AM SF MS KG.
- 1. Fadeel B, Kasemo B, Malmsten M, Strømme M (2010) Nanomedicine: Reshaping clinical practice. J. Intern. Med. 267: 2–8. doi: 10.1111/j.1365-2796.2009.02186.x
- 2. European Commission (2012) A European strategy for Key Enabling Technologies – A bridge to growth and jobs. Brussels: COM 341 final.
- 3. Mihranyan A, Ferraz N, Strømme M (2012) Current status and future prospects of nanotechnology in cosmetics. Prog. Mater. Sci. 57: 875–910. doi: 10.1016/j.pmatsci.2011.10.001
- 4. Varshney HM, Shailender M (2012) Nanotechnology; Current Status In Pharmaceutical Science: A Review. Int. J. Therap. Appl. 6: 14–24.
- 5. Truitt B (2009) Magnesium Carbonate. In Handbook of Pharmaceutical Excipients, 6th ed.; Rowe R, Sheskey P, Quinn M, Eds.; Pharmaceutical Press: London; 397–400.
- 6. Deelman JC (2011) In Low Temperature Formation of Dolomite and Magnesite [Online] version 2.3 ed.; Compact Disc Publications: Eindhoven, 2011. Available: www.jcdeelman.demon.nl. Accessed 2012 Apr 18.
- 7. Pohl W (1990) Genesis of Magnesite Deposits - Models and Trends. Int. J. Earth. Sci. 79: 291–299. doi: 10.1007/bf01830626
- 8. Neuberg C, Rewald B (1908) Ueber Kolloide Und Gelatinöse Verbindungen Der Erdalkalien. Colloid Polymer Sci. 2: 354–357. doi: 10.1007/bf01504380
- 9. Kurov VI (1961) Alkyl Carbonate Salts.5. Methyl Carbonate Salts of Bivalent Metals. Russ. J. Gen. Chem. 31: 9–11.
- 10. Buzágh A (1926) Ueber Kolloide Lösungen Der Erdalkalikarbonate. Kolloid Z. 38: 222–226. doi: 10.1007/bf01460833
- 11. Khan N, Dollimore D, Alexander K, Wilburn FW (2001) The Origin of the Exothermic Peak in the Thermal Decomposition of Basic Magnesium Carbonate. Thermochim. Acta 367–368: 321–333. doi: 10.1016/s0040-6031(00)00669-9
- 12. Hashimoto H, Tomizawa T, Mitomo M (1968) Exothermic Process in the Differential Thermal Analysis Curves of Basic Magnesium Carbonate. Kogyo Kagaku Zasshi 71: 480–484. doi: 10.1246/nikkashi1898.71.4_480
- 13. Sawada Y, Uematsu K, Mizutani N, Kato M (1978) Thermal Decomposition of Hydromagnesite 4 MgCO3•Mg(OH)2•4 H2O under Different Partial Pressures of Carbon-Dioxide. Thermochim. Acta 27: 45–59. doi: 10.1016/0040-6031(78)85020-5
- 14. Choudhary VR, Pataskar SG, Gunjikar VG, Zope GB (1994) Influence of Preparation Conditions of Basic Magnesium Carbonate on Its Thermal-Analysis. Thermochim. Acta 232: 95–110. doi: 10.1016/0040-6031(94)80049-9
- 15. Dell RM, Weller SW (1959) The Thermal Decomposition of Nesquehonite MgCO3•3 H2O and Magnesium Ammonium Carbonate MgCO3•(NH4)2CO3•4 H2O. Trans Faraday Soc 55: 2203–2220. doi: 10.1039/tf9595502203
- 16. Clark CB (1946) X-Ray Diffraction Data for Compounds in the System CaO-MgO-SiO2. J. Am. Ceram. Soc. 29: 25–30. doi: 10.1111/j.1151-2916.1946.tb11544.x
- 17. Rutt HN, Nicola JH (1974) Raman Spectra of Carbonates of Calcite Structure. J. Phys. C Solid State Phys. 7: 4522–4528. doi: 10.1088/0022-3719/7/24/015
- 18. Gouadec G, Colomban P (2007) Raman Spectroscopy of Nanomaterials: How Spectra Relate to Disorder, Particle Size and Mechanical Properties. Prog. Cryst. Growth Charact. Mater. 53: 1–56. doi: 10.1016/j.pcrysgrow.2007.01.001
- 19. Raade G (1970) Dypingite, a New Hydrous Basic Carbonate of Magnesium, from Norway. Am. Mineral. 55: 1457–1465.
- 20. Santamaria M, Di Quarto F, Zanna S, Marcus P (2007) Initial Surface Film on Magnesium Metal: A Characterization by X-Ray Photoelectron Spectroscopy (XPS) and Photocurrent Spectroscopy (Pcs). Electrochim. Acta 53: 1314–1324. doi: 10.1016/j.electacta.2007.03.019
- 21. Splinter SJ, Mcintyre NS, Lennard WN, Griffiths K, Palumbo G (1993) An Aes and Xps Study of the Initial Oxidation of Polycrystalline Magnesium with Water-Vapor at Room-Temperature. Surf. Sci. 292: 130–144. doi: 10.1016/0039-6028(93)90396-2
- 22. Siegbahn K, Nordling C, Johansson G, Hedman J, Hedén PF, et al..(1969) Esca Applied to Free Molecules. North-Holland Publishing Company: Amsterdam.
- 23. Xie YM, Sherwood PMA (1990) X-Ray Photoelectron Spectroscopic Studies of Carbon-Fiber Surfaces.11. Differences in the Surface-Chemistry and Bulk Structure of Different Carbon-Fibers Based on Poly(Acrylonitrile) and Pitch and Comparison with Various Graphite Samples. Chem. Mater. 2, 293–299.
- 24. Gardner SD, Singamsetty CSK, Booth GL, He GR, Pittman CU (1995) Surface Characterization of Carbon-Fibers Using Angle-Resolved Xps and Iss. Carbon 33: 587–595. doi: 10.1016/0008-6223(94)00144-o
- 25. Sing KSW, Everett DH, Haul RAW, Moscou L, Pierotti RA, et al. (1985) Reporting Physisorption Data for Gas Solid Systems with Special Reference to the Determination of Surface-Area and Porosity (Recommendations 1984). Pure Appl. Chem. 57: 603–619. doi: 10.1351/pac198557040603
- 26. Brunauer S, Emmett PH, Teller E (1938) Adsorption of Gases in Multimolecular Layers. JACS 60: 309–319.
- 27. Pires J, Pinto ML, Carvalho A, de Carvalho MB (2003) Assessment of Hydrophobic-Hydrophilic Properties of Microporous Materials from Water Adsorption Isotherms. Adsorption 9: 303–309. doi: 10.1023/a:1026219813234
- 28. Dubinin MM, Astakhov VA (1971) Description of Adsorption Equilibria of Vapors on Zeolites over Wide Ranges of Temperature and Pressure. In Molecular Sieve Zeolites-Ii, American Chemical Society: Washington, D C. 102: 69–85. doi: 10.1021/ba-1971-0102.ch044
- 29. Verhoeven L, Lodewyckx P (2001) In Comparison of Dubinin–Radushkevich Micropore Volumes Obtained from N2, CO2 and H2O-Adsorption Isotherms, Carbon 2001 proceedings, Lexington (KY, USA), American Carbon Society: Conference proceeding avalibe from: http://acs.omnibooksonline.com/data/papers/2001_10.2.pdf.
- 30. Botha A, Strydom CA (2003) Dta and FT-IR Analysis of the Rehydration of Basic Magnesium Carbonate. J. Therm. Anal. Calorim. 71: 987–995.
- 31. Ardizzone S, Bianchi CL, Fadoni M, Vercelli B (1997) Magnesium Salts and Oxide: An Xps Overview. Appl. Surf. Sci. 119: 253–259. doi: 10.1016/s0169-4332(97)00180-3
- 32. Dastgheib SA, Karanfil T (2005) The Effect of the Physical and Chemical Characteristics of Activated Carbons on the Adsorption Energy and Affinity Coefficient of Dubinin Equation. J. Colloid Interface Sci. 292: 312–321. doi: 10.1016/j.jcis.2005.06.017