Localized quantification of anhydrous calcium carbonate polymorphs using micro-Raman spectroscopy

Micro-Raman spectroscopy is a powerful technique for qualitative and quantitative analysis of different mineral mixtures. In this paper, micro-Raman spectroscopy was used for quantification in local regions (180 × 180 μm area) of ternary mixtures of the synthetic calcium carbonate (CaCO₃) polymorphs (vaterite, aragonite, calcite) as well as CaCO₃ formed during the carbonation of nanolime suspension. The obtained results of localized quantification were in agreement with the detected concentrations obtained from bulk quantitative phase analysis of X-ray powder diffraction patterns. The detection limits were found to be below 0.5 wt.% for each CaCO₃ polymorphs. Through the use of 2D mapping, localized quantification of CaCO₃ polymorphs can be achieved. This information could be potentially useful for conservation of valuable Cultural Heritage objects, as it might influence the consolidation treatment chosen.     

The impact of various drug ferrying additives on phase transitions behavior of Calcite,Vaterite and Aragonite

The study aimed to explore the influence of eleven excipients (in three groups) on the phase transition of CaCO3. The groups were; Group 1: Ca-TEG (CaCO3- Tetraethylene Glycol), Ca-PVP (Polyvinylpyrollidone), Ca-LUT (Lutrol Micro 127 MP), Ca-HPMC (Hydroxypropylmethyl Cellulose) and Ca-Blank, Group 2: Ca-G44/14 (Gelucire 44/14), Ca-CRH40 (Cremophor RH40), Ca-SHS (Solutol HS15), Ca-LAB (Labrasol) and Group 3: Ca-GE (Garlic extract), Ca-CAS (Casein), Ca-TCT (Transcutol). Group 1 confers the characteristics of only Calcite, while, Group 2, gave the highest mole fraction of Vaterite. Group 3 gave the highest mole fraction of Vaterite followed by Calcite/Aragonite. FESEM of Ca-CRH40 illustrated numerous parallel stacks of nano-hexagonal vaterite columns building the inner structure of bacillus type Vaterite, while that of Ca-TCT suggested the presence of sunflower shaped Vaterite particles and rhombohedral calcite. The % dissolution efficiency was found maximum for Ca-TEG (90.65%) followed by Ca-PVP (86.13%), Ca-HPMC (76.25%), Ca-LUT (52.12%) and CaBlank (22.96%).     

常温0.1～2GPa压力下文石的拉曼光谱研究

利用碳化硅压腔结合拉曼光谱分析技术,研究了常温0.1～2GPa压力下文石的拉曼光谱特征,并得出文石拉曼位移与压力之间的关系:ν153(cm-1)=0.0035p(MPa)+154.0,ν206=0.0060p+206.3,ν704=0.0021p+704.2,ν1085=0.0035p+1085.3。在实验的压力范围内,未观察到文石的相变。另外,与其他碳酸盐矿物(菱镁矿、白云石)类似,0～2GPa压力下文石的对称伸缩振动拉曼位移随压力变化的dν1025/dp值大于超高压条件下的dν1025/dp值,表明碳酸盐矿物[CO3]基团中C—O键的可压缩性和压力有关,其可压缩性在0.1～2GPa时较大,压力升高可压缩性降低。     

Incorporation of Mg<Superscript>2+</Superscript>, Sr<Superscript>2+</Superscript>, Ba<Superscript>2+</Superscript> and Zn<Superscript>2+</Superscript> into aragonite and comparison with calcite

We have investigated the presence of foreign ions into the bulk structure and the external surfaces of aragonite using periodic ab-initio methods. Four cations isovalent to Ca²⁺ were studied: Mg²⁺, Sr²⁺, Ba²⁺ and Zn²⁺. The calculations were performed at structures (bulk, surface) that contain four and eight CaCO₃ units. Our results, at the Hartree-Fock level, show that the incorporation of those ions into aragonite depends strongly on their size. Mg²⁺ and Zn²⁺, due to their smaller size, can substitute Ca²⁺ ions in the crystal lattice while the incorporation of Sr²⁺ and Ba²⁺ into aragonite is energetically less favoured. Examination of the [011], [110] and [001] surfaces of aragonite revealed that the surface incorporation reduces the energetic cost for the larger ions. These systems provide challenging examples for most shape analysis methods applied in Mathematical Chemistry.     

Quantitative analysis of synthetic calcium carbonate polymorphs using FT-IR spectroscopy

Fourier Transform Infrared Spectroscopy (FT-IR) was used successfully for the simultaneous quantitative analysis of calcium carbonate phases (calcite, aragonite, vaterite) in ternary mixtures. From the FT-IR spectra of pure calcite, aragonite and vaterite powders with KBr, the absorptivities, α, of the absorption bands at 713 cm⁻¹ for calcite, 745 cm⁻¹ for vaterite, 713 and 700 cm⁻¹ for aragonite, were determined. In order to overcome the absorption band overlapping a set of equations based on Beer's law was developed. The detection limits were also established and found to be 1.1×10⁻⁴ mg calcite per mm² of pellet at 713 cm⁻¹, 3.6×10⁻⁴ mg aragonite per mm² of pellet at 700 cm⁻¹, 1.8×10⁻⁴ mg aragonite per mm² of pellet at 713 cm⁻¹ and 3.1×10⁻⁴ mg vaterite per mm² of pellet at 745 cm⁻¹. Analysis of a known ternary mixture of calcium carbonate polymorphs tested the validity of the method.     

Mechanical properties and structure of Haliotis discus hannai Ino and Hemifusus tuba conch shells： a comparative study

Haliotis discus hannai Ino （abalone shell） and Hemifusus tuba conch shell have been studied for the purpose to comparatively investigate the mechanisms by which nature designs composites. It is shown that both shells are composed of aragonite and a small amount of proteins while the conch shell shows finer microstructure but lower strength than aba- lone shell. It is also shown that the fresh shells exhibits better property than those after heat-treatments. It is therefore sup- posed that the size of inorganic substance is not a dominant factor to improve strength, while both proteins in shells and the microstructure of inorganic matter also play important roles.     

显微红外反射光谱法快速鉴别珍珠粉真伪

珍珠是名贵的装饰品和中药材,在我国对其已有2000多年的应用历史。研究发现,贝壳内层的化学组成与珍珠相似,主要含有碳酸钙和各种氨基酸。贝壳粉也可在临床上做药用,但其药用价值远低于珍珠粉。然而,珍珠粉和贝壳粉外观特性极为相似,元素组成和形貌检测无法对其进行有效地鉴别。由于贝壳粉的成本低,常常冒充珍珠粉流入市场,侵害了消费者的利益。本研究通过珍珠粉和贝壳粉在不同温度下煅烧一定时间后显微红外反射光谱的差异实现珍珠粉真伪鉴别。实验结果表明,在一个大气压下经过400 ℃煅烧30 min后,珍珠粉中文石型碳酸钙部分转化为方解石型,而贝壳粉中文石型碳酸钙完全转化为方解石型。这种不同的相转变过程可以被显微红外反射光谱很好的区别。因此,可在此条件下利用红外反射光谱鉴别珍珠粉和贝壳粉相变差异。和传统的透射式红外光谱法相比,这种显微反射红外光谱法无需压片制样、快速灵敏。本研究也讨论了该方法针对其他常见伪品的适用性,如牡蛎粉和石决明粉,结果表明该方法能够简单、高效和准确地鉴别珍珠粉真伪。     

Temperature fluctuations in a LiNbO3 melt during crystal growth

The synthesis of calcium carbonate (CaCO₃) crystals from aqueous solutions containing sodium dodecyl sulfate (SDS), poly(N-vinyl-1-pyrrolidone) (PVP), or SDS/PVP complexes has been performed through a slow titration method. It was found that aragonite and calcite co-existed in the prepared crystals. The formation of aragonite in the precipitation systems without magnesium ions indicates that at ambient temperature ca. 26.0°C, initially formed amorphous CaCO₃ could also transfer into aragonite in the sedimentary phase, which indicates the controlling factor of organic additives in the nucleation and growth process of CaCO₃ crystals. The appearance of hexagonal crystals in the suspensible phase confirmed the hexagonal crystallization cell of vaterite, and revealed the colloidal-dispersion function of the SDS/PVP complex in the crystallization process of CaCO₃.     

Crystallization habit of calcium carbonate in presence of sodium dodecyl sulfate and/or polypyrrolidone

The synthesis of calcium carbonate (CaCO₃) crystals from aqueous solutions containing sodium dodecyl sulfate (SDS), poly(N-vinyl-1-pyrrolidone) (PVP) or SDS/PVP complexes has been performed through a slow titration method. It was found that aragonite and calcite coexisted in the prepared crystals. The formation of aragonite in the precipitation systems without magnesium ions indicates that at ambient temperature ca. 26.0°C, initially formed amorphous CaCO₃ could also transfer into aragonite in the sedimentary phase, which indicates the controlling factor of organic additives in the nucleation and growth process of CaCO₃ crystals. The appearance of hexagonal crystals in the suspensible phase confirmed the hexagonal crystallization cell of vaterite, and revealed the colloidal-dispersion function of the SDS/PVP complex in the crystallization process of CaCO₃.     

Phase transformations in calcite from electrical impedance measurements

The phase transformation in calcite I-IV-V and calcite ? aragonite have been characterized by electrical impedance measurements at temperatures 600–1200°C and pressures 0.5–2.5?GPa in a piston cylinder apparatus. The bulk conductivity σ has been measured from Argand plots in the frequency range 10⁵–10^?2?Hz in an electric cell representing a coaxial cylindrical capacitor. The synthetic polycrystalline powder of CaCO₃ and natural crystals of calcite were used as starting materials. The transformation temperature T_c was identified from resistivity-temperature curves as a kink point of the activation energy. At pressure above 2?GPa in ordered phase calcite I, the activation energy E _σ is c. 1.05?eV, and in disordered phase calcite V E _σ is c. 0.75?eV. The pressure dependence of T_c for the rotational order–disorder transformation in calcite is positive for pressures <1?GPa and negative for pressures >1?GPa. The transformation boundary of calcite 1–IV is observed only during first heating in samples after a long annealing at low temperatures. The activation energy of calcite I???IV decreases gradually from 1.8 to 1.05?eV with the pressure increase from 0.5 to 2?GPa. The kinetics of calcite ? aragonite transformation has been monitored by measuring a time-variation of the electrical resistance of a calcite sample at 10³?Hz in the stability P-T field of aragonite. The variation of the impedance correlates with the degree of phase transformation, estimated from X-ray powder diffraction studies on quenched products of experiments. The kinetics of calcite ? aragonite transformation may be fitted to the Avrami kinetics with the exponent m???1–1.5.