Phosphorus-containing compounds regulate mineralization

Phosphorus is the main constitutive element of minerals and fat in the body. The process of mineral formation is defined as mineralization. The minerals in the body are mainly apatite, which is the inorganic phase that composes bones and teeth. It is worth noting that people with high fat content tend to cause excessive bone mineralization, which leads us to believe that different phosphorus-containing compounds in the body are mutually transformed and can regulate mineralization in different ways. The conversion and regulation of different phosphorus-containing compounds on the mineralization are essential for formation of a complex hierarchical structure and adaptation of the bone to various mechanical environments. Therefore, this review introduces the natural phosphorus-containing compounds in the body, introduces the hierarchical structure of the bone, and summarizes recent studies on different phosphorus-containing compounds (inorganic, organic, and phosphorus-containing proteases) involved in the biomineralization. We also discuss potential research directions of the biomineralization, offering the basis for future investigation of advanced bone substitute materials.     

Experimental and theoretical study of the hydration of phosphate groups in esters of biological interest

We have studied the influence of different groups esterified to phosphates on the strength of the interaction of the PO bond with one water molecule. Experimental vibrational spectra of PO(4)3-, HPO4(2-), H2PO4-, phosphoenolpiruvate (PEP) and ortho-phosphocholamine (o-PC) were obtained by means of FTIR spectroscopy. Geometry calculations were performed using standard gradient techniques and the default convergence criteria as implemented in GAUSSIAN 98 Program. In order to assess the behaviour of such DFT theoretical calculations using B3LYP with 6-31G* and 6-311++G** basis sets, we carried out a comparative work for those compounds. The results were then used to predict the principal bands of the vibrational spectra and molecular parameters (geometrical parameters, stabilisation energies, electronic density). In this work, the relative stability and the nature of the PO bond in those compounds were systematically and quantitatively investigated by means of Natural Bond Order (NBO) analysis. The topological properties of electronic charge density are analysed employing Bader's Atoms in Molecules theory (AIM). The hydrogen bonding of phosphate groups with water is highly stable and the PO bond wavenumbers are shifted to lower experimental and calculated values (with the DFT/6-311++G** basis set). Accordingly, the predicted order of the relative stability of the hydrogen bonding of the water molecule to the PO bond of the investigated compounds is: PO(4)3->HPO4(2-)>H2PO4->phosphoenolpiruvate>phosphocholamine for the two basis sets used.     

Black painted pottery, Kildehuse II, Odense County, Denmark

This work aimed at characterization of a black layer covering a Bronze Age (period VI) pot surface. To solve research problems plane polarized light microscopy (PLM), scanning microscopy with X-ray microanalyser (SEM/EDS), Raman and FTIR microspectroscopies were applied. Observation of the black layer under the PLM suggests that we deal with an opaque, isotropic layer, purposely put on leather-hard, burnished surface of a pot. No traces of organic substances that might have modified a pot surface before painting were detected. The black layer coats the pot with a continuous 0.2-0.4 μm thick layer. The black layer must have been applied while warm or hot. It is recognized that the black layer is a true painting layer. Spectroscopic analyses (Raman and FTIR) point that birch tar or a birch-pine tar had been applied. Carbon black should be definitely excluded. The analyzed organic substance is structurally ordered in various degrees, due to varying temperature influence. Some Raman spectra reveal, in second-order region of the spectrum (>2000 cm(-1)), the graphite presence. Scarce points reveal the presence of inorganic admixtures: clay minerals, feldspars and quartz. The next question is: Is it an organic paint or a carbon-based, "mixed" paint? Inorganic admixtures are only casual. Relatively high concentration of alumina is expected to have appeared due to aluminum mobility in acidic environment and this was provided by organic tar/pitch substances. Phosphorus (usually with calcium) mostly concentrates together with clay minerals. Thus, hypothesis on bone powder or ash addition to tar/pitch should be excluded. Some elements may originate not only from inorganic substances but also from wood ashes.     

An infrared and Raman spectroscopic study of natural zinc phosphates

Zinc phosphates are important in the study of the phosphatisation of metals. Raman spectroscopy in combination with infrared spectroscopy has been used to characterise the zinc phosphate minerals. The minerals may be characterised by the patterns of the hydroxyl stretching vibrations in both the Raman and infrared spectra. Spencerite is characterised by a sharp Raman band at 3516 cm(-1) and tarbuttite by a single band at 3446 cm(-1). The patterns of the Raman spectra of the hydroxyl stretching region of hopeite and parahopeite are different in line with their differing crystal structures. The Raman spectrum of the PO4 stretching region shows better band separated peaks than the infrared spectra which consist of a complex set of overlapping bands. The position of the PO4 symmetric stretching mode can be used to identify the zinc phosphate mineral. It is apparent that Raman spectroscopy lends itself to the fundamental study of the evolution of zinc phosphate films.     

N,N-二甲基正十二烷基胺/无机含氧酸体系的相态结构研究

利用拟三元相图法研究了N,N-二甲基正十二烷基胺(DMDA)多元体系的相态结构,并用电导、偏光显微镜以及红外、紫外可见光谱等手段进行了表征.发现N,N-二甲基正十二烷基胺体系随水相含量的增加,铵盐发生不同形式的有序缔合,分别形成了W/O型微乳液、“节-结”型链状缔合体、层状液晶和O/W型微乳液;在层状液晶中,SO₄^2-主要以桥式双齿配位形式存在,中性胺分子有利于体系中液晶的形成;层状液晶于500nm波长处有一吸收峰,在430nm附近发生“光短路”现象,该现象可能对测定层状液晶的层间距有重要意义.     

From synthetic to biogenic Mg-containing calcites: a comparative study using FTIR microspectroscopy

The formation mechanism of the thermodynamically unstable calcite phase, very high Mg calcite, in biological organisms such as sea urchin or corallina algae has been an enigma for a very long time. In contrast to conventional methods such as KBr pellet Fourier Transform infrared (FTIR) spectroscopy and X-ray diffraction (XRD), FTIR microspectroscopy (FTIRM) provides additional information about a local disorder such as an amorphous phase or the occlusion of Mg ions in the calcite lattice. In this work, we characterise for the first time systematically synthetic and biogenic Mg-containing calcium carbonate samples (especially sea urchin teeth--SUT) in detail by using two FTIRM instruments and compare these samples with KBr pellet FTIR measurements. Furthermore, we present spectra from geogenic calcite and dolomite minerals, recorded with both FTIRM systems, as well as KBr pellet FTIR spectra as references. We analyse the spectra by applying multi-peak curve fitting on the in-plane-bending (ν(4)) and out-of-plane (ν(2)) bands. Based on the obtained results we attribute the two singlet bands at ～860-865 cm(-1) and ～695-704 cm(-1) observed in the SUT FTIRM spectra to the existence of amorphous calcium carbonate (ACC), and report for the first time the existence of ACC at the mature end of SUT. In the other three studied biominerals, however, we did not find any ACC. Also, based on the FTIRM results, we observe that not only ν(4), but also ν(2) shifts to higher wavenumbers if more calcium ions are replaced by magnesium ions in the calcite lattices.     

无机材料的仿生合成

生物矿化重要的特征之一是细胞分泌的有机基质调制无机矿物的成核和生长, 形成具有特殊组装方式和多级结构特点的生物矿化材料(如骨、牙和贝壳)。仿生合成就是将生物矿化的机理引入无机材料合成, 以有机物的组装体为模板, 去控制无机物的形成,制备具有独特显微结构特点的无机材料, 使材料具有优异的物理和化学性能。仿生合成已成为无机材料化学的研究前沿。本文综述了无机材料仿生合成的发展现状。     

仿生矿化增强材料

近年来,随着材料科学领域的发展,机械性能优异且具有特定功能的有机-无机复合材料成为了研究热点。而天然的生物矿化过程产生了在自然界中分布广泛、结构特征多样性、机械性能优异的天然生物矿物,比如牙齿、骨骼、珍珠、贝壳、海胆刺、海洋红虫颚等。这些天然复合增强材料中的矿化组织结构特点和矿化机理为仿生设计与合成具有特定结构、特定功能和优异机械性能的材料提供了理论依据。通过模拟天然过程的仿生矿化方法,利用有机基质调控无机矿物成核生长为固态矿物,最终能够定向组装具有特定有序结构和先进功能的有机-无机复合材料。本文主要综述了自然界中通过生物矿化过程得到的高强度、高韧性的天然复合增强材料,以及受生物矿化增强现象的启发,在化学与材料仿生矿化合成中出现的一些有机-无机复合的增强材料。     

次亚磷酸根离子在多晶铂电极上氧化的原位红外光谱研究

次亚磷酸根离子在多晶铂电极上氧化的原位红外光谱研究;电氧化;电催化;SNIFTIRS     

DyCl_3对原代培养的成骨细胞增殖、分化和矿化功能表达的影响(英文)

采用MTT法、碱性磷酸酶活性测定、油红O的染色和定量测定、矿化功能的测定以及qRT-PCR等手段在细胞和分子水平上研究了DyCl3对原代培养的成骨细胞增殖、分化和矿化功能的影响。研究结果表明,在测试浓度范围内,DyCl3均抑制成骨细胞增殖。浓度为1×10-8,1×10-6和1×10-5mol·L-1的DyCl3促进成骨细胞分化。在测试浓度范围内,DyCl3均抑制成骨细胞横向分化为脂肪细胞。浓度为1×10-5mol·L-1的DyCl3促进成骨细胞矿化结节的形成,而浓度为1×10-7mol·L-1和1×10-6mol·L-1的DyCl3抑制成骨细胞矿化结节的形成,进一步降低浓度为1×10-8mol·L-1,它则对成骨细胞矿化功能没有影响。浓度1×10-6mol·L-1的DyCl3显著降低PPAR-γmRNA表达水平,但相同浓度DyCl3则显著上调RUNX-2mRNA表达水平。实验结果提示,DyCl3对体外培养的成骨细胞增殖、分化及矿化功能的影响与浓度和作用时间有关,而且,它们是影响其生物效应从毒性到活性,从损伤到保护,从上调到下调转变的关键因素。这些结果对深入理解稀土离子对骨代谢的影响具有重要的价值。     

FTIR spectroscopic, thermal and XRD characterization of hydroxyapatite from new natural sources

The inorganic constituents of 5 different plants (leaves and stalks) were investigated by using Fourier transformer infrared spectroscopy (FTIR), X-ray diffraction (XRD) and thermal analysis including thermal gravimetric analysis (TGA), derivative thermogravimetry (DTG) and differential scanning calorimetry (DSC). These plants are Catha edulis (Khat), basil, mint, green tea and trifolium. The absorption bands of carbonate ions CO(3)(2-) was exhibited at 1446 cm(-1), and the phosphate ions PO(4)(3-) was assigned at 1105 and 1035 cm(-1). At high temperatures (600, 700 and 600°C) further absorption bands of the phosphate ions PO(4)(3-) was assigned at the frequencies 572, 617, 962, 1043 and 1110 cm(-1) and the vibrational absorption band of the carbonate ions CO(3)(2-) was assigned at 871, 1416 and 1461 cm(-1). X-ray diffraction and thermal analysis confirm the obtained results of FITR. Results showed that the main inorganic constituents of C. edulis and basil leaves are hydroxyapatite whereas the hydroxyapatite content in the other plant samples is less than that in case of C. edulis and basil plant leaves.     

Analysis of bone minerals by time-of-flight secondary ion mass spectrometry: a comparative study using monoatomic and cluster ions sources

Time-of-flight secondary ion mass spectrometry (TOF-SIMS) is an important tool for the analysis of bone minerals at implant surfaces. Most studies have been performed with monoatomic primary ion sources such as Ga(+) with poor secondary molecular ion production efficiency and only elemental distributions and minor fragments of bone minerals have been reported. By using cluster ion sources, such as Au(1-3) (+) and Bi(1-3) (+), identification of larger hydroxyapatite species at m/z 485, 541, 597 and 653, identified as Ca(5)P(3)O(12), Ca(6)P(3)O(13), Ca(7)P(3)O(14) and Ca(8)P(3)O(15), respectively, became possible. The ions appear to be fragments of the hydroxyapatite unit cell Ca(10)(PO(4))(6)(OH)(2). Each ion in the series is separated by 55.9 m/z units, corresponding to CaO, and this separation might reflect the columnar nature of the unit cell.     

Mammalian Cell Spheroids on Mixed Organic–Inorganic Superhydrophobic Coating

Three-dimensional cell culture has become a reliable method for reproducing in vitro cellular growth in more realistic physiological conditions. The surface hydrophobicity strongly influences the promotion of cell aggregate formation. In particular, for spheroid formation, highly water-repellent coatings seem to be required for the significant effects of the process. In this work, surfaces at different wettability have been compared to observe their influence on the growth and promotion of aggregates of representative mammalian cell lines, both tumoral and non-tumoral (3T3, HaCat and MCF-7 cell lines). The effect of increased hydrophobicity from TCPS to agarose hydrogel to mixed organic–inorganic superhydrophobic (SH) coating has been investigated by optical and fluorescence microscopy, and by 3D confocal profilometry, in a time scale of 24 h. The results show the role of less wettable substrates in inducing the formation of spheroid-like cell aggregates at a higher degree of sphericity for the studied cell lines.     

Structure of selected basic zinc/copper (II) phosphate minerals based upon near-infrared spectroscopy--implications for hydrogen bonding

The NIR spectra of reichenbachite, scholzite and parascholzite have been studied at 298 K. The spectra of the minerals are different, in line with composition and crystal structural variations. Cation substitution effects are significant in their electronic spectra and three distinctly different electronic transition bands are observed in the near-infrared spectra at high wavenumbers in the 12,000-7600 cm(-1) spectral region. Reichenbachite electronic spectrum is characterised by Cu(II) transition bands at 9755 and 7520 cm(-1). A broad spectral feature observed for ferrous ion in the 12,000-9000 cm(-1) region both in scholzite and parascholzite. Some what similarities in the vibrational spectra of the three phosphate minerals are observed particularly in the OH stretching region. The observation of strong band at 5090 cm(-1) indicates strong hydrogen bonding in the structure of the dimorphs, scholzite and parascholzite. The three phosphates exhibit overlapping bands in the 4800-4000 cm(-1) region resulting from the combinations of vibrational modes of (PO(4))(3-) units.     

Raman spectroscopy of newberyite, hannayite and struvite

The phosphate minerals hannayite, newberyite and struvite have been studied by Raman spectroscopy using a thermal stage. Hannayite and newberyite are characterised by an intense band at around 980cm(-1) assigned to the v(1) symmetric stretching vibration of the HPO(4) units. In contrast the symmetric stretching mode is observed at 942cm(-1) for struvite. The Raman spectra are characterised by multiple v(3) anti-symmetric stretching bands and v(2) and v(4) bending modes indicating strong distortion of the HPO(4) and PO(4) units. Hannayite and newberyite are defined by bands at 3382 and 3350cm(-1) attributed to HOPO(3) vibrations and hannayite and struvite by bands at 2990, 2973 and 2874 assigned to NH(4)(+) bands. Raman spectroscopy has proven most useful for the analysis of these 'cave' minerals where complex paragenetic relationships exist between the minerals.     

New cembranoid diterpenes from the Vietnamese soft coral Sarcophyton mililatensis stimulate osteoblastic differentiation in MC3T3-E1 cells

Chemical investigation of the Vietnamese soft coral Sarcophyton mililatensis resulted in the isolation of four new cembranoid diterpenes, namely (-)-7beta-hydroxy-8alpha-methoxydeepoxysarcophytoxide (1), (+)-7beta,8beta-dihydroxydeepoxysarcophytoxide (2), (-)-17-hydroxysarcophytonin A (3) and sarcophytol V (4), along with two known compounds, (+)-sarcophine (5) and sarcophytoxide (6). The NMR spectral data of the new compounds were completely assigned by using a combination of 2D NMR experiments including (1)H-(1)H COSY, HSQC, HMBC, and ROESY. To investigate the bioactivities of compounds, which act on bone metabolism, we studied the effects of compounds on the function of osteoblastic MC3T3-E1 cells. Compound 1 caused a significant elevation of alkaline phosphatase activity, collagen content, and nodules mineralization compared to those of the control (p<0.05). These results suggest that newly isolated compound 1 has a direct stimulatory effect on bone formation in vitro and may contribute to the prevention for osteoporosis.     

Giant vesicles of a single-tailed chiral cationic surfactant, (1R,2S)-(-)-N-dodecyl-N-methylephedrinium bromide, in water

Self-assembly properties of a single-tailed chiral cationic surfactant, (1R,2S)-(-)-N-dodecyl-N-methylephedrinium bromide (DMEB), have been studied in water. The molecular self-assemblies of the amphiphile have been characterized by surface tension, fluorescence probes, light scattering, and microscopic techniques. The results have been compared with those of dodecyltrimethylammonium bromide (DTAB) surfactant. The critical aggregation concentration of DMEB was found to be much less than that of DTAB. Surface tension and fluorescence probe studies have suggested formation of micellar structures at low temperature (<28 degrees C) and spontaneous formation of giant vesicles in water above 28 degrees C. The mean size of the aggregates has been measured by a dynamic light scattering method. The micropolarity and microviscosity of the self-assemblies were determined by fluorescence probe technique. The (1)H NMR and FTIR spectra were recorded to elucidate the role of the hydrophobic head group towards the formation of bilayer structures. The phase transition temperatures of the vesicular aggregates were determined by measurement of fluorescence anisotropy at various temperatures.     

The crystal chemistry of Ca(10-y)(SiO4)3(SO4)3Cl(2-x-2y)F(x) ellestadite

Fluor-chlorellestadite solid solutions Ca(10)(SiO(4))(3)(SO(4))(3)Cl(2-x)F(x), serving as prototype crystalline matrices for the fixation of hazardous fly ash, were synthesized and characterized by powder X-ray and neutron diffraction (PXRD and PND), transmission electron microscopy (TEM), and Fourier transform infrared spectroscopy (FTIR). The lattice parameters of the ellestadites vary linearly with composition and show the expected shrinkage of unit cell volume as fluorine (IR = 1.33 ?) displaces chlorine (IR = 1.81 ?). FTIR spectra indicate little or no OH(-) in the solid solutions. All compositions conform to P6(3)/m symmetry where F(-) is located at the 2a (0, 0, (1)/(4)) position, while Cl(-) is displaced out of the 6h Ca(2) triangle plane and occupies 4e (0, 0, z) split positions with z ranging from 0.336(3) to 0.4315(3). Si/S randomly occupy the 6h tetrahedral site. Ellestadites rich in Cl (x ≤ 1.2) show an overall deficiency in halogens (<2 atom per formula unit), particularly Cl as a result of CaCl(2) volatilization, with charge balance achieved by the creation of Ca vacancies (Ca(2+) + 2Cl(-) →□(Ca) + 2□(Cl)) leading to the formula Ca(10-y)(SiO(4))(3)(SO(4))(3)Cl(2-x-2y)F(x). For F-rich compositions the vacancies are found at Ca(2), while for Cl-rich ellestadites, vacancies are at Ca(1). It is likely the loss of CaCl(2) which leads tunnel anion vacancies promotes intertunnel positional disorder, preventing the formation of a P2(1)/b monoclinic dimorph, analogous to that reported for Ca(10)(PO(4))(6)Cl(2). Trends in structure with composition were analyzed using crystal-chemical parameters, whose systematic variations served to validate the quality of the Rietveld refinements.     

Synthesis and Structures of Two New Molybdophosphates

A one-dimension solid and a two-dimension solid consisting of polyoxoanions bridged by {CoO3N2} and {CoO4} groups respectively have been synthesized by the hydrothermal method and structurally characterized by X-Ray crystallography. Each structure has the [(PO4)4Mo6O15]^12- cluster that is commonly observed in many molybdophosphates. In compound 1, [(PO4)4Mo6O15]^12- clusters are linked by {CoO3N2} groups to form a chain-like structure, and the chains are hydrogen-bonded into a network. Compound 2 is a layer structure with channnels constructed from [(PO4)4Mo6O15]^12- clusters and {CoO4} groups, the organic molecules and the lattice water molecules are distributed disorderly in the interlamellar region and form strong hydrogen bonds with inorganic framework. The IR and the fluorescent spectra were investigated and discussed.     

Anions bonded on the supramolecular hydrogel surface as the growth center of biominerals

In this work, a supramolecular hydrogel formed from N,N',N'-tris(3-pyridyl)-trimesic amide was reported to serve as the matrix for the growth of biominerals. The organic hydrogel scaffold contains nitrogen heterocyclic ring and amide groups that can bind anions of the mineral (specially here, carbonate ions and phosphate ions) through hydrogen bonding interactions and act as the biomineralization active sites for growing biominerals. Calcium carbonate nucleated on the site of the hydrogel fiber where carbonate ions bonded and left obvious hydrogel fiber prints on the obtained product. Calcium phosphate grew into curved platelike nanostructures along the hydrogel fibrous network. XRD pattern and FT-IR spectra confirmed the formation of minerals on the hydrogel. The results indicate that the hydrogen bonding interaction can provide strong enough binding force for the growth of the minerals on organic scaffolds. Our finding extends the organic scaffolds into biodegradable small molecule hydrogels and also extends the growth centers of the minerals from conventional carboxylate groups binding Ca(2+) to amide and pyridyl groups binding PO(4)(3-).