Peptide studies using a fast atom bombardment high field mass spectrometer and data system. 1—Sample introduction, data acquisition and mass calibration

1983 ◽  
Vol 10 (5) ◽  
pp. 324-333 ◽  
Author(s):  
Alexander M. Buko ◽  
Lawrence R. Phillips ◽  
Blair A. Fraser
Keyword(s):  
Data Acquisition ◽  
Mass Spectrometer ◽  
High Field ◽  
Fast Atom Bombardment ◽  
Data System ◽  
Sample Introduction ◽  
Field Mass ◽  
Mass Calibration ◽  
System 1

scholarly journals The Q Exactive HF, a Benchtop Mass Spectrometer with a Pre-filter, High-performance Quadrupole and an Ultra-high-field Orbitrap Analyzer

2014 ◽  
Vol 13 (12) ◽  
pp. 3698-3708 ◽  
Author(s):  
Richard Alexander Scheltema ◽  
Jan-Peter Hauschild ◽  
Oliver Lange ◽  
Daniel Hornburg ◽  
Eduard Denisov ◽  
...  
Keyword(s):  
Mass Spectrometer ◽  
High Field ◽  
High Performance ◽  
Ultra High Field ◽  
Q Exactive ◽  
Orbitrap Analyzer

New sample introduction technique for mass spectrometer

1970 ◽  
Vol 42 (8) ◽  
pp. 950-952 ◽  
Author(s):  
Frank G. Padrta ◽  
J. J. Donohue
Keyword(s):  
Mass Spectrometer ◽  
Sample Introduction

Mass spectrometer polymer membrane sample introduction device

1983 ◽  
Vol 55 (4) ◽  
pp. 813-814 ◽  
Author(s):  
George J. Kallos ◽  
Nels H. Mahle
Keyword(s):  
Mass Spectrometer ◽  
Polymer Membrane ◽  
Sample Introduction ◽  
Membrane Sample

scholarly journals Source and origin of atmospheric trace elements entrapped in winter snow of the Italian Eastern Alps

2006 ◽  
Vol 6 (5) ◽  
pp. 8781-8815 ◽  
Author(s):  
P. Gabrielli ◽  
G. Cozzi ◽  
S. Torcini ◽  
P. Cescon ◽  
C. Barbante
Keyword(s):  
Boundary Layer ◽  
Trace Elements ◽  
Mass Spectrometer ◽  
Inductively Coupled Plasma ◽  
Major Ions ◽  
Eastern Alps ◽  
Field Mass ◽  
Inductively Coupled ◽  
Winter Snow ◽  
Snow Samples

Abstract. Trace elements concentrations were determined in shallow snow samples from 21 sites in the Italian Eastern Alps in order to identify the sources of the contaminants present in the tropospheric winter boundary layer. The collection of superficial snow layers was carried out weekly at altitudes between 1000 and 3000 m next to meteorological stations, far away from villages, roads and ski slopes. Ultra clean procedures were adopted in order to avoid contamination of the snow during the different experimental phases. Trace elements (Ag, Ba, Bi, Cd, Co, Cr, Cu, Fe, Mo, Mn, Pb, Sb, Ti, U, V and Zn) were determined by Inductively Coupled Plasma Sector Field Mass Spectrometer (ICP-SFMS). Ancillary parameters such as major ions (SO42−, NO3−, Ca2+;, Mg2+, K

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