THE LAMONT-DOHERTY-GEOLOGICAL-OBSERVATORY ISOLAB-54 ISOTOPE RATIO MASS-SPECTROMETER

被引:28
作者
ENGLAND, JG
ZINDLER, A
REISBERG, LC
RUBENSTONE, JL
SALTERS, V
MARCANTONIO, F
BOURDON, B
BRUECKNER, H
TURNER, PJ
WEAVER, S
READ, P
机构
[1] VG ISOTOPES,WINSFORD CW7 3BX,CHESHIRE,ENGLAND
[2] COLUMBIA UNIV,DEPT GEOL SCI,NEW YORK,NY 10027
[3] CUNY QUEENS COLL,DEPT GEOL,FLUSHING,NY 11367
[4] TURNER SCI,WARRINGTON WA4 4ST,CHESHIRE,ENGLAND
[5] ALFRED UNIV,DEPT GEOL,ALFRED,NY 14802
[6] VG ISOTECH,MIDDLEWICH CW10 0HT,CHESHIRE,ENGLAND
来源
INTERNATIONAL JOURNAL OF MASS SPECTROMETRY AND ION PROCESSES | 1992年 / 121卷 / 03期
关键词
THERMAL ION MASS SPECTROMETRY; SECONDARY ION MASS SPECTROMETRY; NEGATIVE THERMAL ION MASS SPECTROMETRY; SPUTTER-INDUCED RESONANCE IONIZATION MASS SPECTROMETRY;
D O I
10.1016/0168-1176(92)80063-7
中图分类号
O64 [物理化学(理论化学)、化学物理学]; O56 [分子物理学、原子物理学];
学科分类号
070203 ; 070304 ; 081704 ; 1406 ;
摘要
The Lamont-Doherty Geological Observatory (LDGO) Isolab 54 is a double focussing isotope ratio mass spectrometer that allows the measurement of thermal ions produced on a hot filament, (thermal-ionization mass spectrometry (TIMS)), secondary ions produced by sputtering a sample using a primary ion beam, (secondary ion mass spectrometry (SIMS)), and sputtered neutrals resonantly ionized using laser radiation, (sputter-induced resonance ionization mass spectrometry (SIRIMS)). Sputtering is carried out using an Ar primary beam generated in a duoplasmatron and focussed onto the sample using a two-lens column. Resonance ionization is accomplished using a frequency-doubled dye laser pumped by an excimer laser. The Isolab's forward geometry analyzer, consisting of an electrostatic followed by a magnetic sector, allows the simultaneous collection of different isotopes of the same element. This instrument is the first to have a multicollector that contains an ion-counting system based on a microchannel plate as well as traditional Faraday cups. A second electrostatic sector after the multicollector is equipped with an ion-counting Daly detector to allow high abundance sensitivity for measurements of large dynamics range. Selectable source, collector, alpha and energy slits on the instrument allow analyses to be made over a range of mass resolving powers and analyzer acceptances. Recent applications of the instrument have included the analyses of U by TIMS, Hf, Th and Re by SIMS and Re and Os by SIRIMS.
引用
收藏
页码:201 / 240
页数:40
相关论文
共 34 条
[1]  
Anderson Roy, COMMUNICATION
[2]   SEPARATION OF TRACE AMOUNTS OF URANIUM AND THORIUM AND THEIR DETERMINATION BY MASS-SPECTROMETRIC ISOTOPE-DILUTION [J].
ARDEN, JW ;
GALE, NH .
ANALYTICAL CHEMISTRY, 1974, 46 (06) :687-691
[3]   U-234 ANOMALIES IN CORALS OLDER THAN 150,000 YEARS [J].
BARD, E ;
FAIRBANKS, RG ;
HAMELIN, B ;
ZINDLER, A ;
HOANG, CT .
GEOCHIMICA ET COSMOCHIMICA ACTA, 1991, 55 (08) :2385-2390
[4]  
BENNINGHOVEN A, 1987, SECONDARY ION MASS P, P443
[5]  
BENNINGHOVEN A, 1987, SECONDARY ION MASS S, P287
[6]   NEGATIVE THERMAL ION MASS-SPECTROMETRY OF OSMIUM, RHENIUM, AND IRIDIUM [J].
CREASER, RA ;
PAPANASTASSIOU, DA ;
WASSERBURG, GJ .
GEOCHIMICA ET COSMOCHIMICA ACTA, 1991, 55 (01) :397-401
[7]   SCINTILLATION TYPE MASS SPECTROMETER ION DETECTOR [J].
DALY, NR .
REVIEW OF SCIENTIFIC INSTRUMENTS, 1960, 31 (03) :264-267
[8]  
DRUMMOND IW, 1968, THESIS U CAMBRIDGE
[9]  
DRUMOND I, 1969, P INT C ION SOURCES, P459
[10]  
ENGE H, 1981, INTRO NUCLEAR PHYSIC, P237