T13N3

Contents

 

153 Волкович С.В. К семидесятипятилетию со дня рождения

 

 

155 Шарафутдинова Д.Р. К шестидесятипятилетию со дня рождения

 

 

156 О присуждении награды имени Курта Брюне 2016 г. в области масс-спектрометрии

 

 

 Milman_Graf

157 The «low-molecular» approach to identification
of microorganisms by MALDI mass spectrometry

B.L. Milman, Yu.Yu. Ilyasov, N.V. Lugovkina,
A.A. Golovina, A.V. Dmitriev

 

 

Kosevich_Graf

167 Mass spectrometric observation of charged nanoclusters
of silver with inclusion of hydrogen formed under reduction
of AgNO3 in ethylene glycol

O.A. Boryak, M.V. Kosevich, V.V. Chagovets,
V.S. Shelkovsky 

 

 

Antoshkin_Graf

176 Determination of the geographical region of growing
the coffee beans by gas chromatograph-combustion – isotope
ratio mass spectrometry

A.M. Antokhin, V.F. Taranchenko, S.V. Vasilevsky,
A.V. Aksenov, Ju. B. Aksenova, O.V. Kuznetsova,
I.V. Lapko, M.A. Glushkova

 

 

Chijov_Graf

183 Gas-phase fragmentation studies of biotinylated,
hexaethylene glycol-spacered oligosaccharides — molecular
probes — using electrospray mass spectrometry
on hybrid high-resolution mass spectrometer

A.O. Chizhov, D.A. Argunov, M.L. Gening,
E.V. Sukhova, E.A. Khatuntseva, A.A. Karelin,
B.S. Komarova,M.V. Orekhova, V.B. Krylov,
D.V. Yasunskii, Yu.E. Tsvetkov, N.E. Nifantiev

 

 

Terentev_Graf

193 Interpretation and simulation of negative ion mass spectra
of some phosphorus organoelement compounds

А.G. Terentyev, R.V. Khatymov, M.A. Lyogkov,
A.V. Dudkin, I.V. Rybal’chenko

 

 

Chervyakovskiy_Graf

203 New method of mathematical correction of the results
of analysis, obtained by inductively coupled plasma mass spectrometry,
allowing the elimination of a double charged ions interference

K.I. Chervyakovskii

 

Gas-phase fragmentation studies of biotinylated, hexaethylene glycol-spacered oligosaccharides — molecular probes — using electrospray mass spectrometry on hybrid high-resolution mass spectrometer

T13N3

A.O. Chizhov, D.A. Argunov, M.L. Gening, E.V. Sukhova, E.A. Khatuntseva, A.A. Karelin,
B.S. Komarova, M.V. Orekhova, V.B. Krylov, D.V. Yasunskii, Yu.E. Tsvetkov, N.E. Nifantiev

Electrospray ionization high-resolution mass spectra of biotinylated, hexaethylene glycol spacered molecular probes bearing biologically relevant carbohydrate moieties in positive and negative modes were recorded and interpret. Collisionally-induced decay mass spectra (positive mode) reveal different patterns depending on the charge of the parent ion, attached cations (or ions), the composition, and the sequence of carbohydrate fragment. The most intense peaks (two series) originate from the sequential cleavage of glycoside bonds resulting in charge location on the “reducing” end (Y series, observed for all compounds studied) or “non-reducing” end (B series). Fragmentation of the hexaethylene glycol chain giving rise to the cleavage of the C—O bond remoted from the biotin moiety is observed. Other fragment ions lighter than the mentioned above on the difference of (C2H4O)n were absent or much smaller. Similar fragmentation was found for all of the non-sulfated, biotinylated glycosides with the hexaethylene glycol spacer thus demonstrating that this type of fragmentation was characteristic for such molecular probes. Similar cleavages along with decay of biotin moiety via elimination of H2S and H2CS were observed for negative ions in collisionally-induced decay mass spectra of sulfated and neutral molecular probes.

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Determination of the geographical region of growing the coffee beans by gas chromatograph-combustion – isotope ratio mass spectrometry

T13N3

A.M. Antokhin, V.F. Taranchenko, S.V. Vasilevsky, A.V. Aksenov, Ju.B. Aksenova, O.V. Kuznetsova,
I.V. Lapko, M.A. Glushkova

Gas chromatography –combustion –isotope ratio mass spectrometry has been used to study the changes in carbon isotopic composition of chlorogenic acid and caffeine extracted from samples of coffee beans of different origin. It has been shown that depending on the region of coffee beans growing, the relative characteristics of carbon isotopic composition, namely δ13C, ‰, changed significantly for both caffeine and chlorogenic acid. There was a decrease in the 13C isotope observed in the following order: Africa –South America –Central America. It has been found that the δ13C values for caffeine and chlorogenic acid, when mutually considered, provide the statistically significant identification of a region where the coffee beans grow.

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