Preparation of high-temperature stabilized beta-tricalcium phosphate by heating deficient hydroxyapatite with Na4P2O7 x 10H2O addition

In this paper, the high-temperature stabilized beta-tricalcium phosphate (betaTCP, beta-Ca3(PO4)2) were prepared by heating the deficient HAP (d-HAP, Ca10-x(HPO4)x(PO4)6-x(OH)2-x) with tetra-sodium diphosphate decahydrate (NP, Na4P2O7 x 10H2O) addition. The betaTCP, d-HAP and d-HAP doped with 2.5, 5, 7.5 and 10 wt % NP were heated to different temperatures and were investigated by X-ray diffraction analysis (XRD) and Fourier-transformed infrared spectroscopy (FTIR). The results demonstrated that the HPO4(2-) of d-HAP condensed into P2O7(4-) occurred before 650 degrees C. The P2O7(4-) ions could be traced in the FTIR spectrum when the d-HAP was heated up to 750 degrees C. The reaction of P2O7(4-) with OH- did not occur instantly but over a wide range of temperatures. The d-HAP doped with NP would decrease the decomposition temperature of d-HAP. NP doped into d-HAP not only induced the d-HAP decomposition at lower temperature but also stabilized the betaTCP crystal structure at higher-temperature. It could also increase the conversion temperature of betaTCP to alphaTCP from 1180 degrees C up to 1300 degrees C. We could successfully prepare high-temperature (up to 1300 C) stabilized ffTCP by heating NP doped d-HAP.     

Formation of calcium-deficient hydroxyapatite from alpha-tricalcium phosphate

This study investigated the factors influencing the kinetics of Ca9HPO4(PO4)5OH (calcium deficient hydroxyapatite or CDHAp) formation from alpha-Ca3(PO4)2 (alpha-TCP). The kinetics of CDHAp formation were investigated by isothermal calorimetry at constant temperatures ranging between 30 and 75 degrees C and by changes in pH at 37.4 and 70 degrees C. The calorimetric curves were characterized by two reaction peaks. Activation energies were calculated for the events resulting in these peaks. Values obtained were 48.4 and 67.7 kJ mol(-1), respectively, indicating nucleation and growth mechanisms for both events. Temperature had a significant effect on the growth rate as indicated by a decrease in surface area (26.5-15.0 m2 g(-1)) of the CDHAp with increasing temperature (30-75 degrees C). A linear relationship between hydrolysis temperature and CDHAp surface area was observed. The morphology of the CDHAp was plate-like and the crystallites became more regular as the reaction temperature was increased. A rapid elevation in pH upon mixing with water indicated the synthesis method initially used did not entirely eliminate slight compositional variations within the alpha-Ca3(PO4)2. Rapid elevation in pH retarded subsequent reaction. This effect was eliminated by increasing the duration of high-temperature firing during alpha-TCP synthesizing.     

Inter-relationships of carbonate, phosphate, monohydrogen phosphate, calcium, magnesium and sodium in uraemic bone: comparison of dialysed and non-dialysed patients

1. Chemical and morphological features of uraemic bone disease were studied by comparison of bone composition in 44 patients with uraemia (12 dialysed and 32 non-dialysed) and 36 control subjects. The significant changes included decreased bone mineral carbonate associated with calcium, a concomitant increase in phosphate, and an increase in magnesium. There was also an increase in osteoid and a reduction in the specific gravity of the compact bone. 2. The most marked changes in bone composition were observed in patients with uraemia of more than 1 year's duration, who had been dialysed. Bone mineral sodium concentrations were not significantly altered in any group. 3. The changes in bone mineral composition appeared to be the result of several simultaneous and/or successive mechanisms: (i) loss of fixed base, calcium carbonate; (ii) replacement of carbonate by phosphate; (iii) the addition of immature bone mineral, which contains high concentrations of phosphate and relatively low concentrations of carbonate. 4. These observations are consistent with earlier views of the bone salt as an indefinite calcium/phosphate/carbonate complex. Variations in bone composition may arise from a reciprocal relationship between phosphate and carbonate. The bone mineral analogue that best explains these variations in bone composition is octacalcium phosphate carbonate [Ca4 (PO4)2(HPO4)x(CO3)1-x,zH2O].     

Importance of intrinsic calf vasodilator capacity in determining distribution of skeletal muscle perfusion during supine bicycle exercise in patients with left ventricular dysfunction

Although there is interest in forming synthetic analogs of hard tissues at physiologic temperature, significant gaps in knowledge exist with respect to the mechanisms by which precursor solids convert to apatites and also with respect to the apatite compositions that may be formed. In this study calcium-deficient HAp [Ca9(HPO4)(PO4)5OH] was prepared by hydrolysis of tricalcium phosphate (TCP), alpha-Ca3(PO4)2. The kinetics of HAp formation were studied as a function of temperature by isothermal calorimetry. TCP hydrolyzed completely within about 12 h, and the hydrolysis reaction evolved 133 kJ/mol of HAp formed. Although the kinetics of hydrolysis exhibited a strong temperature dependence, the mechanistic path taken appeared independent of temperature. The fluoridation of hydroxyapatite compositions having Ca/P ratios higher than 1.59 previously has been investigated. However, little work has been done on the fluoridation of more calcium-deficient hydroxyapatite. Ca9(HPO4)(PO4)5OH was formed at temperatures between 37.4 degrees and 55 degrees C to vary its morphology. These preparations then were reacted in NaF solution and the kinetics of fluoride incorporation studied. Solution chemical analyses were used to determine the amounts of fluoride incorporated. The extent of hydroxyl replacement by fluoride ranged from 17 to 72% and correlated with the surface area of the parent HAp.     

New Zincophosphite with Infinite One-dimensional [Zn(HPO3)(H2PO3)]- Chains: Synthesis, Characterizations and Spectral Properties

With dimethylamine as a template, a new one-dimensional zincophosphite (C2H8N)·[Zn(HPO3)(H2PO3)]was prepared under hydrothermal conditions and characterized by single-crystal X-ray diffraction, FTIR spectrametry, elemental analysis, powder X-ray diffraction, and thermogravimetric analysis. The compound crystallized in the Monoclinic space group P2(1)/c, with cell parameters, a=0.78410(9)nm, b=1.54744(2)nm, c=0.81418(1) nm, β=105.8150(1)°, V=0.95049(2) nm3 and Z=4. The connectivity of the ZnO4 tetrahedron and HPO3 pseudo pyramid resulted in inifinite corner-sharing 4-membered ring chains, which were further linked by the protonated amine molecules to form a 3D structure via hydrogen bonds. To the best of our knowledge, this is the first existence of a zincophosphite with the anionic framework composition of [Zn(HPO3)(H2PO3)]-. The compound exhibits intense photoluminescence at room temperature.     

ATP-Induced phosphorylation of the sarcoplasmic reticulum Ca2+ ATPase: molecular interpretation of infrared difference spectra

Time-resolved infrared difference spectra of the ATP-induced phosphorylation of the sarcoplasmic reticulum Ca2+-ATPase have been recorded in H2O and 2H2O at pH 7.0 and 1 degrees C. The reaction was induced by ATP release from P3-1-(2-nitro)phenylethyladenosine 5'-triphosphate (caged ATP) and from [gamma-18O3]caged ATP. A band at 1546 cm-1, not observed with the deuterated enzyme, can be assigned to the amide II mode of the protein backbone and indicates that a conformational change associated with ATPase phosphorylation takes place after ATP binding. This is also indicated between 1700 and 1610 cm-1, where bandshifts of up to 10 cm-1 observed upon protein deuteration suggest that amide I modes of the protein backbone dominate the difference spectrum. From the band positions it is deduced that alpha-helical, beta-sheet, and probably beta-turn structures are affected in the phosphorylation reaction. Model spectra of acetyl phosphate, acetate, ATP, and ADP suggest the tentative assignment of some of the bands of the phosphorylation spectrum to the molecular groups of ATP and Asp351, which participate directly in the phosphate transfer reaction: a positive band at 1719 cm-1 to the C==O group of aspartyl phosphate, a negative band at 1239 cm-1 to the nuas(PO2-) modes of the bound ATP molecule, and a positive band at 1131 cm-1 to the nuas(PO32-) mode of the phosphoenzyme phosphate group, the latter assignment being supported by the band's sensitivity toward isotopic substitution in the gamma-phosphate of ATP. Band positions and shapes of these bands indicate that the alpha- and/or beta-phosphate(s) of the bound ATP molecule become partly dehydrated when ATP binds to the ATPase, that the phosphoenzyme phosphate group is unprotonated at pH 7.0, and that the C==O group of aspartyl phosphate does not interact with bulk water. The Ca2+ binding sites seem to be largely undisturbed by the phosphorylation reaction, and a functional role of the side chains of Asn, Gln, and Arg residues was not detected.     

The effects of magnesium on hydroxyapatite formation in vitro from CaHPO4 and Ca4(PO4)2O at 37.4 degrees C

The effects of magnesium ion on the formation of calcium-deficient hydroxyapatite [Ca9HPO4(PO4)5OH, CDHAp] from CaHPO4 and Ca4(PO4)2O dissolution were investigated using two magnesium sources: Mg3(PO4)2 (chemical system 1) or MgCl2 . H2O (chemical system 2) solutions. Because chloroapatite does not form from aqueous solutions, the use of two magnesium sources facilitated the determination of magnesium's role during synthetic hydroxyapatite formation in vitro and possible related effects during biomineralization. Isothermal calorimetry determined the progress of reactions. Two peaks are observed as heat is evolved during the formation of CDHAp in water at 37.4 degrees C. The nucleation and growth of CDHAp are the corresponding mechanisms. Although the time for complete reaction and total heat-of-reaction DeltaHr remain constant, the height of the first peak is reduced as the concentration of magnesium ion approaches 4 mM in either chemical system. Magnesium does not substitute into CDHAp even though there are calcium vacancies available. Subsequent increases cause the remaining heat peak to broaden and the time required for complete reaction to approach 24 hours as the initial MgCl2 concentration reaches 100 mM. Supersaturation limits chemical system 1 to Mg3(PO4)2 concentrations below 10 mM. A MgCl2 concentration of 3.16 M precludes CDHAp from forming for over 3 months; rather newberyite, MgHPO4 . 3H2O, precipitates. The morphology and surface area of the CDHAp formed in 100 mM MgCl2 solution are comparable to those of CDHAp formed in water. The surface areas are approximately 80 m2/g. Magnesium concentrations below 4 mM only inhibit nucleation whereas those above 4 mM inhibit growth as well. Magnesium phosphate complexes are more inhibitory than magnesium chloride complexes. Increasing the liquid-to-solids ratio or agitation significantly increases the induction period before reaction initiates. Increasing the liquid-to-solids ratio increases the time span for growth whereas increasing agitation decreases the time span for growth. The large inhibitory effect of agitation suggests quiescent systems are more suitable for determining the kinetics of HAp formation. A magnesium inorganic chemical activity (alphaMg = gammaMg[Mg2+]) many times greater than that in biological fluids is required before inhibition of hydroxyapatite formation is realized.     

The Interacting v6 = 2 Levels of D3Si35Cl: A Tool to Determine Ground State Constants from High-Resolution Spectra in the 440-590 and 900-1100 cm-1 Regions

High-resolution FTIR spectra of monoisotopic D3Si35Cl have been recorded in the regions 440-590 cm-1 (nu3/nu6) and 900-1100 cm-1 (2nu6/nu3 + nu6/2nu3). A detailed rovibrational study was done for the 2nu06, 2nu-/+26, and 2nu3 overtone bands and for the 2nu+/-26-nu+/-16, 2nu06-nu-/+16, and (nu3 + nu+/-16)-nu+/-16 hot bands. For the first time the interactions occurring between the v6 = 2, v3 = v6 = 1, and v3 = 2 levels of any trideuterated silyl halide have been analyzed. The (nu3 + nu+/-16)-nu+/-16 hot band served to obtain accurate energies of the v3 = v6 = 1 level, the nu3 + nu6 combination band not being detectable on our spectra. The first experimental determination of A0 and D0K for this molecule was undertaken by a well-established method, using the nu6, 2nu+/-26-nu+/-16, and 2nu-/+26 bands. Ground state energy differences DeltaK(J) = E0(J, K) - E0(J, K - 3) were calculated for K values from 2 to 16. By a least-squares fit of 163 such differences, the A0 and D0K values thus obtained were (in cm-1): A0 = 1.4278230(8) and D0K = 5.3916(31) x 10(-6). Copyright 1999 Academic Press.     

Thermally induced molecular disorder in human stratum corneum lipids compared with a model phospholipid system; FT-Raman spectroscopy

The molecular basis of lipid packing in human stratum corneum and a model phospholipid system has been studied as a function of temperature using Fourier Transform (FT) Raman spectroscopy. Thermally induced molecular rearrangements of the model lipid system, dipalmitoylphosphatidyl choline (DPPC), and stratum corneum were investigated using FT Raman spectroscopy coupled to a heating chamber. Spectra were recorded for a range of sample temperatures and the results for the two systems were compared, producing previously unreported information of the thermal behaviour for the different systems. Discrete thermal events were recorded for both systems by plotting band separation of the lipid v(CH2) symmetric and asymmetric stretching modes against temperature. The main thermal events observed for DPPC included a 'pre-melting' between 37 and 39 degrees C, the main transition observed between 41 and 42 degrees C, a 'post-transition' between 42 and 43 degrees C and three minor transitions at 58-60, 65-70 and 75-80 degrees C. No evidence was found for the pre-transition of DPPC, previously observed at 34-35 degrees C. The main transitions for human stratum corneum were observed at 35-45, 55, 72 and 83 degrees C, measured from lipid CH2 stretching and bending vibrations. The keratin thermal transition at about 100 degrees C exerted little effect on the lipid bands and no characterisable structural changes were reflected in the keratotic bands.     

电动力富集电解锰渣中锰的研究

采用电动力技术对电解锰渣中可溶性锰的迁移、转化和富集规律进行研究。结果表明,直接电动力和CO_2辅助电动力均可在阴极区富集锰,反应48h锰富集量分为达到3.8%和4.3%。两种方式作用下,阴极区锰的富集量随反应时间的增加而增加,阳极区锰含量随反应时间的增加逐渐减少。从阴极到阳极,锰含量逐渐减少。直接电动力作用下的反应机制为,锰在阴极区富集并与OH-反应形成Mn(OH)_2、CaMn(OH)SiO_4等难溶物。CO_2辅助电动力作用下的反应机制为,CO_2与阴极区的OH-反应形成CO_3~(2-),CO_3~(2-)进一步与迁移到阴极区的Mn~(2+)反应形成MnCO_3。     

Multiple thermotropic state transitions in erythrocyte membranes. A laser-Raman study of the CH-stretching and acoustical regions

1. We have examined the Raman scattering from erythrocyte ghosts at 2700 cm-1 -3000 cm-1 (CH-stretching region), that at low frequencies due to acoustical vibrations, as well as that due to v (-C=C-) and v (=C-C=) of beta-carotene, in the temperature range of -30 degrees C to +30 degrees C. For comparison we have also evaluated the Rama spectra of liposomes composed of lecithins+/-cholesterol. 2. Plots vs. temperature of the intensities (I) of the approx. 2880 cm-1 and 2932 cm-1 bands relative to the intensity of the thermally stable 2850 cm-1 band, i.e. the (I2880/I2850) and (I2932/I2850) ratios, revealed discontinuities in both erythrocyte membranes and liposomes. 3. In erythrocyte membranes, plots of (I approximately 2880/I2850) and (I approximately 2932/I 2850) reveal several discontinuities. Those reported by (I approximately 2880/I 2850) occur at +17 degrees C and approx. -4 degrees C. The ratio (I approximately 2932/I 2850) reveals a transition between -20 degrees C and +10 degrees C, 1/2 maximal at -8 degrees C. The ratio (I 1527/I 1158), representing the relative intensity of v (-C=C-) vs. v (=C-C=) of membrane-bound beta-carotene, changes discontinuously with the 17 degrees C transition, but is stable over the rest of the temperature change studied. 4. The data indicate that a major membrane-state transition takes place below 0 degrees C but that an additional transition occurs at approx. 17 degrees C.     

Review of Rare Earths and Fluid-Rock Interaction

As demonstrated by a great amount of geologic and experimental evidences, RE of rock systems may be mobilized during fluid-rock interaction when solutions are rich in F^-, Cl^-, CO3^2- , HCO3^-, CO2, HPO4^2- , HS^-,S^2- , SO4^2- , though little has been known about the mobilizing mechanism of these anions or ligands. The fractionation of RE resulted from hydrothermal alterations, i. e., fluid-rock interactions, are distinctive. One set of field data implies the preferential mobility of the LRE, while another set of field observations demonstrates the dominant mobilization of the HRE, and some theoretical prediction is not consistent with the field evidence. The Eu anomalies caused by fluid-rock interaction are complex and compelling explanation is not available due to inadequate experimental approaches. To know the exact behavior of RE during fluid-rock interaction and to solve the contradiction between some theoretical predictions and field observations, the following works remain to be done : ( 1 ) experimental investigations of RE mobility and fractionation as a function of fluid chemistry, e.g., the activity of F^-,Cl^-, CO3^2- , HCO3^-, CO2, HPO4^2- , HS^-, S^2- , SO4^2- , etc. ; (2) experimental determination of RE mobility and fractionation as a function of T, P, pH, Eh and water/rock ratios; (3) investigation of the mechanism and the controlling factors of RE partitioning between hydrothermal minerals and fluids. It was demonstrated that RE mobility is a potentially useful method for exploration.     

Spectroscopic studies and Rietveld refinement of strontium-britholites

Strontium-britholites whose chemical formula was Sr10-xLax（PO4）6-x（SiO4）xF2, where x=0, 1, 2, and 4 were prepared by solid state reaction. The structural refinement carried out using the Rietveld method indicated that La^3＋ ions were located into the two sites with a strong preference for metal （2） sites especially for low contents. A progressive shift of the F position along the c-axis outside the centre of the triangle formed by metal （2）-atoms was observed with the increase of x. The infrared and Raman spectra exhibited the characteristic vibration modes of PO4 and SiO4groups confirming the incorporation of this last group into the apatite structure. The 295i MAS-NMR spectra exhibited one resonance peak confirming the data obtained by X-ray diffraction, indicating that P and Si were located in the same crystallographic site.     

Nucleation of hydroxyapatite by bone sialoprotein

Bone sialoprotein (BSP) and osteopontin, the major phosphorylated proteins of mammalian bone, have been proposed to function in the initiation of mineralization. To test this hypothesis, the effects of BSP and osteopontin on hydroxyapatite crystal formation were determined by using a steady-state agarose gel system. At low calcium phosphate concentrations, no accumulation of calcium and phosphate occurred in control gels or gels containing osteopontin. Gels containing BSP at 1-5 micrograms/ml, however, exhibited a visible precipitation band and significantly elevated Ca + PO4 contents. By powder x-ray diffraction, the precipitate formed in the presence of BSP was shown to be hydroxyapatite. These findings suggest that bone sialoprotein may be involved in the nucleation of hydroxyapatite at the mineralization front of bone.     

Stability of triple-helical poly(dT)-poly(dA)-poly(dT) DNA with counterions

Structural conformation of triple-helical poly(dT)-poly(dA)-poly(dT) has been a very controversial issue recently. Earlier investigations, based on fiber diffraction data and molecular modeling, indicated an A-form conformation with C'3-endo sugar pucker. On the other hand, Raman, solution infrared spectral, and NMR studies show a B-form structure with C'2-endo sugars. In accordance with these experimental results, a theoretical model with B-form, C'2-endo sugars was proposed in 1993. In the present work we investigate the dynamics and stability of the two conformations within the effective local field approach applied to the normal mode calculations for the system. The presence of counterions was explicitly taken into account. Stable equilibrium positions for the counterions were calculated by analyzing the normal mode dynamics and free energy of the system. The breathing modes of the triple helix are shifted to higher frequencies over those of the double helix by 4-16 cm-1. The characteristic marker band for the B conformation at 835 cm-1 is split up into two marker bands at 830 and 835 cm-1. A detailed comparison of the normal modes and the free energies indicates that the B-form structure, with C'2-endo sugar pucker, is more stable than the A-form structure. The normal modes and the corresponding dipole moments are found to be in close agreement with recent spectroscopic findings.     

Effect of calcium carbonate on the compliance of an apatitic calcium phosphate bone cement

Clinical requirements for calcium phosphate bone cements were formulated in terms of the initial setting time, the final setting time, the cohesion time and the ultimate compressive strength. Three cement formulations were tested. The previously developed Biocement H was made of a powder containing alpha-tertiary calcium phosphate and precipitated hydroxyapatite. Biocement B2 powder was made by adding some CaCO3 to Biocement H, whereas Biocement B1 was made by adding some CaCO3 but with simultaneous adjustment of the amount of precipitated hydroxyapatite.The liquid/ powder ratio of the cement paste and the accelerator concentrations (percentage Na2HPO4) in cement liquid were varied. For Biocement H there was no combination of L/P ratio and percentage Na2HPO4 for which all clinical requirements were satisfied. However, there was an area of full compliance for Biocements B1 and B2, of which that for B1 was the largest. Therefore, Biocement B1 may be applied in clinical situations as those in orthopaedics, plastic and reconstructive surgery and oral and maxillofacial surgery, even when early contact with blood is inevitable.     

Crystal structure and infrared spectrum of thallium holmium polyphosphate, TIHo(PO3)4

Crystals of thallium-holmium polyphosphate TIHo(PO3)4 were grown by flux method technique and characterized by single crystal X-ray diffraction. Structure of TIHo(PO3)4 was solved for the first time, and it crystallized in the monoclinic P21/n space group with the following unit-cell dimensions: a=1.02225(3) nm, b=0.88536(2) nm, c=1.09541(4) nm, β=105.888(1)°, V=0.95354(5) nm3 and Z=4. The crystal structure was solved from 2174 independent reflections with final R1(F2)=0.0442 and Rw(F<2)=0.0861 refined with 164 parameters. The atomic arrangement could be described as a long chain polyphosphate organization. Holmium atoms had eighffold coordination. The structure of T1Ho(PO3)4 consisted of HoO8 polyhedra sharing oxygen atoms with phosphoric group PO4. Infrared spectrum was investigated at room temperature in the frequencies range, 350-4000 cm-1, showing some characteristic vibration bands of infinite chain structure of PO4 tetrahedra linked by bridging oxygen.     

RNA-ascorbate interaction

Ascorbic acid and divalent iron salts have been widely used to investigate the effects of reactive oxygen species in different biological targets such as nucleic acids, proteins and lipids. This study was designed to examine the interaction of yeast RNA with vitamin C in aqueous solution at physiological pH with drug/RNA(P)(P=phosphate) molar ratios of r=1/80, 1/40, 1/20, 1/10, 1/4 and 1/2. Absorption spectra and Fourier transform infrared (FTIR) difference spectroscopy were used to determine the ascorbate binding mode, binding constant, sequence selectivity and RNA secondary structure in aqueous solution. Spectroscopic evidence showed that at low drug concentration (r=1/80 and 1/40), no major ascorbate-RNA interaction occurs, while at higher drug concentrations (r>1/40), a major drug-RNA complexation was observed through both G-C and A-U base pairs and the backbone phosphate groups with k=31.80 M(-1). Evidence for this comes from large perturbations of the G-C vibrations at 1698 and 1488 cm(-1) and the A-U bands at 1654 and 1608 cm(-1) as well as the phosphate antisymmetric stretch at 1244 cm(-1). At r>1/10, minor structural changes occur for the ribose-phosphate backbone geometry with RNA remaining in the A-family structure. The drug distributions around double helix were about 55% with G-C, 33% A-U and 12% with PO2 groups. A comparison between ascorbate-RNA and ascorbate-DNA complexes showed minor differences. The ascorbate binding (H-bonding) is via anion CO and OH groups.     

Electron transfer in tetrahemic cytochromes c3: spectroelectrochemical evidence for a conformational change triggered by heme IV reduction

Electron transfer in tetrahemic cytochromes c3 from Desulfovibrio vulgaris Hildenborough (D.v.H.) and Desulfovibrio desulfuricans Norway (D.d.N.) strains has been investigated by thin layer spectroelectrochemistry with visible absorption, CD, and resonance Raman (RR) monitoring. The observed splitting of the isosbestic point in the Soret absorption band indicates that the electron transfer from the (FeIII)4 state to the (FeII)4 state proceeds via an intermediate species, which corresponds to 25 and 50% reduction for the D.v.H. cyt.c3 and the D.d.N. cyt.c3, respectively. For the latter, a specific CD signal is observed at half-reduction. RR monitoring of the redox process does not reveal multiple splitting of the high-frequency RR bands, at variance with previously published results on the enzymatic reduction of cyt.c3 from Desulfovibrio vulgaris Miyazaki, a cytochrome highly homologous to D.v.H. cyt.c3 [Verma, A.L., Kimura, A., Nakamura, A., Yagi, T., Inoguchi, H., & Kitagawa, T. (1988) J. Am. Chem. Soc. 110, 6617-6623]. The low-frequency RR spectra of the intermediate species differ significantly from the ones calculated from a linear combination of the all-ferric and all-ferrous states, for the same reduction ratio. Frequency shifts of the bending modes of the cysteine and propionate heme substituents are observed, as well as changes specific to each cytochrome; most notable is the activation of two torsional modes in the case of D.d.N. cyt.c3. Comparison of the results obtained for the two cytochromes leads to the conclusion that reduction of heme IV triggers the observed conformational change. This conclusion is supported by the spectroelectrochemical investigation of the mutant D.v.H. cyt.c3 H25M, in which the sixth ligand of heme III, histidine, is replaced by a methionine.     

Characterization of vinyl-substituted, carbon-carbon double bonds by GC/FT-IR analysis

Vapor-phase infrared spectra allow the determination of the stereochemistry of carbon-carbon double bonds conjugated with a vinyl group. Cis and trans isomers of unsubstituted 1,3-alkadienes can be differentiated on the basis of the differences observed in the 900-1000 cm-1 region (spectra of cis isomers show two bands at 993 and 906 cm-1, while those of trans compounds show three absorptions at 998, 949, and 902 cm-1) and the 1590-1650 cm-1 region (the C=C stretch bands are observed at 1595 and 1642 cm-1 for cis compounds and at 1604 and 1650 cm-1 for trans compounds). Compounds bearing CH2=CHC(CH3)=CHCH2- and CH2=CHC(=CH2)-CH2- structural moieties, referred to as alpha- and beta-type compounds, are frequently encountered as natural products. For compounds bearing alpha-type groups, the cis/trans configuration of the trisubstituted double bond can be determined unambiguously. An absorption at 3095-3091 cm-1, for the =CH2 stretch vibration, is common to both of these groups; however, due to the presence of two =CH2 groups, the relative intensity of the band is much higher for beta-type compounds. For alpha-type compounds, a cis configuration at the C-3 carbon atom is characterized by a =CH2 wag absorption at 907-906 cm-1. For beta-type compounds and 3E-alpha-type compounds, this band appears at 899-897 cm-1. In addition, a wavy "fingerprint" pattern with two minima at 1632 (low intensity) and 1595-1594 cm-1 (high intensity) is characteristic for beta-type compounds. Our generalizations are based on spectra of cis and trans ocimene, myrcene, and dehydration products of many 3-methyl-1-alken-3-ols. Six isomers of farnesene can be characterized by GC/FT-IR. Furthermore, gas-phase IR allows the determination of the configuration of the trisubstituted double bond at C-3 in alpha-type farnesene congeners. For example, the homo- and bishomofarnesene isomers from Myrmica ants were shown to include a 3Z bond.