Identifying the presence of a disulfide linkage in peptides by the selective elimination of hydrogen disulfide from collisionally activated alkali and alkaline earth metal complexes

We report a new method for identifying disulfide linkages in peptides using mass spectrometry. This is accomplished by collisional activation of singly charged cationic alkali and alkaline earth metal complexes, which results in the highly selective elimination of hydrogen disulfide (H2S2). Complexes of peptides possessing disulfide bonds with sodium and alkaline earth metal are generated using electrospray ionization (ESI). Isolation followed by collision induced dissociation (CID) of singly charged peptide complexes results in selective elimination of H2S2 to leave newly formed dehydroalanine residues in the peptide. Further activation of the product yields sequence information in the region previously short circuited by the disulfide bond. For example, singly charged magnesium and calcium ion bound complexes of [Lys8]-vasopressin exhibit selective elimination of H2S2 via low-energy CID. Further isolation of the product followed by CID yields major b- and z-type fragments revealing the peptide sequence in the region between the newly formed dehydroalanine residues. Numerous model peptides provide mechanistic details for the selective elimination of H2S2. The process is initiated starting with a metal stabilized enolate anion at Cys, followed by cleavage of the S-C bond. An examination of the peptic digest of insulin provides an example of the application of the selective elimination of H2S2 for the identification of peptides with disulfide linkages. The energetics and mechanisms of H2S2 elimination from model compounds are investigated using density functional theory (DFT) calculations.     

Weak alkali and alkaline earth metal complexes of low molecular weight ligands in aqueous solution

This work is aimed at reviewing the chemical literature dealing with thermodynamic aspects of the weak complex formation (species with log K values less than about 3) between alkali and alkaline earth metal ions with low molecular weight inorganic and organic ligands in aqueous solution. The following ligands (up to hexavalent anions) were examined in detail: (i) hydroxide, chloride, sulfate, carbonate and phosphate as inorganic, and (ii) carboxylates, amines, amino acids, complexones and nucleotides as organic ligands. The paper also identifies the main reasons responsible for the dispersion of the stability data on ion pairs in the literature. When possible, the trend of stability for the different metal ions interacting with the same ligand will be considered to find predictive interaction relationships. Since the stability of weak alkali and alkaline earth metal complexes are mainly due to electrostatic interaction, simple empirical relationships were obtained between log K and the charge of the anionic ligand. The interest for alkali and alkaline earth cations rises since they are used in study of basic science as components of the supporting electrolyte and are widely diffused in natural fluids. Some examples of application of this science were presented too, to show the role of weak complex formation in the modelling process of natural systems.     

Metal complex formation with dicarbonyl-ligands. Calculations on glyoxal complexes with alkali and alkaline earth metal ions

Ab initio MO SCF calculations on the complexes of Li, Na, K, Be, Mg and Ca ions with glyoxal have been performed. These calculations represent the first part of a series of theoretical investigations on the dependence of complex formation properties of ligands containing two carbonyl groups on the structure of the cordinative center. Special attention has been paid to the chelate effect, which is found to increase with increasing atomic number within the series of ions. The calculated values are compared with our recent data obtained from UV spectroscopy of ion complexes with dicarbonyl ligands.     

Thermal stability of alkali metal borates and alkaline earth metal borates

The correlation between the enthalpies of formation of alkali metal and alkaline earth metal borates and the composition of the vapor in equilibrium with their melts is considered. The thermal stabilities of the studied borates have been estimated. A method is suggested for determination of the relative composition of the vapor over borate melts on the basis of their enthalpies of formation.

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Zusammenfassung Es wurde die Beziehung zwischen den Bildungsenthalpien von Alkali- (Erdalkali-)metallboraten und der Zusammensetzung der sich mit der Schmelze im Gleichgewicht befindlichen Gasphase betrachtet. Die thermische Stabilität der untersuchten Borate wurde geschätzt. Es wurde ein Verfahren entwickelt, die relative Zusammensetzung der Gasphase über Boratschmelzen auf Grund ihrer Bildungsenthalpien zu bestimmen.

     

Tetraphenylborate salts of alkali and alkaline earth metal complex cations

An introductory review summarises complex formation between poly(alkyleneoxy) adducts and inorganic salts. This is followed by preparative and IR and NMR spectroscopic features of the tetraphenylborates of complexes of polyethylene glycols, nonylphenoxy(polyethyleneoxy)ethanols and polypropylene glycols with sodium, magnesium, calcium, strontium and barium ions. Generally, an alkylene oxide:cation ratio of 8.5:1 is indicated for the complexes with sodium, and 12:1 (∼10.5:1 for the polyethylene glycols)_for the complexes with the alkaline earth metals.     

Tuning aromaticity in trigonal alkaline earth metal clusters and their alkali metal salts

In this work, we analyze the geometry and electronic structure of the [X_nM₃]^n?2 species (M = Be, Mg, and Ca; X = Li, Na, and K; n = 0, 1, and 2), with special emphasis on the electron delocalization properties and aromaticity of the cyclo‐[M₃]^2? unit. The cyclo‐[M₃]^2? ring is held together through a three‐center two‐electron bond of σ‐character. Interestingly, the interaction of these small clusters with alkali metals stabilizes the cyclo‐[M₃]^2? ring and leads to a change from σ‐aromaticity in the bound state of the cyclo‐[M₃]^2? to π‐aromaticity in the XM₃^? and X₂M₃ metallic clusters. Our results also show that the aromaticity of the cyclo‐[M₃]^2? unit in the X₂M₃ metallic clusters depends on the nature of X and M. Moreover, we explored the possibility for tuning the aromaticity by simply moving X perpendicularly to the center of the M₃ ring. The Na₂Mg₃, Li₂Mg₃, and X₂Ca₃ clusters undergo drastic aromaticity alterations when changing the distance from X to the center of the M₃ ring, whereas X₂Be₃ and K₂Mg₃ keep its aromaticity relatively constant along this process. © 2009 Wiley Periodicals, Inc. J Comput Chem, 2009     

Solvent‐free alkali and alkaline earth metal complexes of di‐imine ligands

Compound [(dph‐BIAN)Mg(THF)]₂ ( 2 ) was prepared by reacting magnesium metal with 1,2‐bis[(2‐biphenyl)imino]acenaphthene (dph‐BIAN) in THF, followed by crystallization from toluene. Reaction of CaI₂ with (dpp‐BIAN)Li₂ in toluene afforded [(dpp‐BIAN)Li]₂Ca ( 3 ) (dpp‐BIAN = 1,2‐bis[(2,6‐diisopropylphenyl)imino]acenaphthene). Both complexes 2 and 3 were characterized by single crystal X‐ray diffraction. The ¹H NMR spectroscopic data obtained for complex 3 in toluene solution indicated an agostic interaction between the methyl groups of the ligand and lithium atoms. © 2005 Wiley Periodicals, Inc. Heteroatom Chem 16:663–670, 2005; Published online in Wiley InterScience ( www.interscience.wiley.com ). DOI 10.1002/hc.20168     

Modification of sulfonated polyphenylquinoxaline by alkali and alkaline earth metal cations

Salts of sulfonated polyphenylquinoxaline (SPPQ) containing alkaline earth metal ions—Mg²⁺, Ca²⁺, and Ba²⁺—were synthesized. The paper considers their solubilities, the properties of solutions, and thermal stability in comparison with analogous characteristics of SPPQ salts with alkali metals. The introduction of alkaline earth metal cations into SPPQ affords soluble polymeric salts having high thermal stability. Solutions of SPPQ salts in N-methylpyrrolidone (N-MP) containing Mg²⁺, Ca²⁺, and Ba²⁺ ions do not exhibit polyelectrolyte properties, unlike solutions of SPPQ salts in which the counterions are Li⁺, Na⁺, and K⁺. Solutions of SPPQ and its salts in N-MP can be converted to water-soluble form by dialysis. This opens up new prospects for using the polymeric salts.     

Automatic ion-exchange chromatograph for analysis of alkali and alkaline earth metal mixtures

A new automatic chromatograph for ultramicro determination of alkali and alkaline earth metals has been developed. It combines a high-sensitivity hydrogen flame-ionization detector with ion-exchange chromatography. Zirconium phosphate was chosen as ion-exchanger.     

碱土金属与DBC-偶氮氯膦配位反应及配合物结构的研究

本文研究了DBC-偶氮氯膦在不同酸度下的存在形式、质子化情况及反应中的质子释放情况, 测定了钙、锶、钡与其形成的配合物的稳定常数。利用红外、激光Raman、核磁共振光谱等对所生成的配合物的结构进行了研究, 并根据实验结果和分子结构的几咱理论, 提出了碱土金属与其生成的配合物的结构。本文还就配位反应和配合物的成键情况进行了讨论。     

Accurate all-purpose method for the assay of alkali and alkaline earth carbonates with perchloric acid

An accurate all-purpose method is proposed for the determination of carbonate in alkali and alkali earth carbonates. A large sample size (4–9 g depending on the carbonate) is dissolved in 100.00 ml of 1.2 M perchloric acid, the solution is boiled, and the excess of acid is titrated with standard 1.0 M sodium hydroxide solution to a methyl orange end-point. Perchloric acid is preferable to hydrochloric acid because there is no danger of loss of acid during the boiling; it is preferable to sulfuric acid since insoluble sulfates of barium, strontium, and calcium are not precipitated in analyzing alkali earth carbonates. Normal alkali and alkali earth carbonates (anhydrous and hydrated) are assayed on samples previously dried by heating in an oven at 250°C for 3 h. This treatment drives off all the water but it also converts any hydrogencarbonate present into carbonate. Hydrogencarbonates are assayed on samples dried in a desiccator containing sulfuric acid for 16 h. Twelve different carbonates were analyzed. The average standard deviation of the method was 0.050%.     

Thermochemistry of 18C6 complexation with alkali,alkaline earth metal cations and ammonium ion

The object of the present study is to examine the factors governing the process of 18C6 complexation in aqueous solution by interpreting of thermodynamic parameters of the reaction in terms of observed selectivity and solvation characteristics under various temperature conditions.     

Complexation of crown-containing butadienyl dyes with alkali and alkaline earth metal cations in the ground and excited electron states

Spectrophotometry and steady-state fluorimetry were used for the study of complexation of crown-containing butadienyl dyes with alkali and alkaline earth metal cations in acetonitrile, as well as protonation of these dyes with trifluoroacetic acid. Complexation of the compounds studied with the metal cations leads to the 1: 1 product, whereas protonation with trifluoroacetic acid affords the 1: 2 product containing 2 moles of the acid per 1 mole of the dye. Stability constants of the complexes are varied from 10 to 10⁶ L mol⁻¹, basicity of the crown-containing dyes in the reaction with trifluoroacetic acid increases with the increase in the macrocycle size. On complexation, the fluorescence spectra are shifted considerably less than the absorption spectra. This indicates that photorecoordination of the cation in the complex excited molecules occurred. Based on the correlation of the spectral shifts with the metal cation charge density, three types of complexes differing in the extent of influence of the cation charge on the spectral shifts can be singled out: “tight”, “loose”, and “solvent-separated”.     

Ultrafine Na-4-mica: uptake of alkali and alkaline earth metal cations by ion exchange

The cation exchange properties of alkali and alkaline earth metal cations at room temperature were investigated on an ultrafine, highly charged Na-4-mica (with the ideal mica composition Na4Mg6Al4Si4O20F4.xH2O). Ultrafine mica crystallites of 200 nm in size led to faster Sr2+ uptake kinetics in comparison to larger mica crystallites. The alkali metal ion (K+, Cs+, and Li+) exchange uptake was rapid, and complete exchange occurred within 30 min. For the alkaline earth metal ions Ba2+, Ca2+, and Mg2+, however, the exchange uptake required lengthy periods from 3 days to 4 weeks to be completed, similar to its Sr uptake, as previously reported. Kinetic models of the modified Freundlich and parabolic diffusion were examined for the experimental data on the Ba2+, Ca2+, and Mg2+ uptakes. The modified Freundlich model described well the Ba2+ ion uptake kinetics as well as that for the Sr2+ ion, while for the Ca2+ and Mg2+ ions the parabolic diffusion model showed better fitting. The alkali and alkaline earth ion exchange isotherms were also determined in comparison to the Sr2+ exchange isotherm. The thermodynamic equilibria for these cations were compared by using Kielland plots evaluated from the isotherms.