Large O2 Cluster Ions as Sputter Beam for ToF-SIMS Depth Profiling of Alkali Metals in Thin SiO2 Films

被引:16
作者
Holzer, Sabine [1 ,2 ]
Krivec, Stefan [1 ]
Kayser, Sven [3 ]
Zakel, Julia [3 ]
Hutter, Herbert [2 ]
机构
[1] Infineon Technol Austria AG, Siemensstr 2, A-9500 Villach, Austria
[2] Vienna Univ Technol, Inst Chem Technol & Analyt, Getreidemarkt 9, A-1060 Vienna, Austria
[3] ION TOF GmbH, Heisenbergstr 15, D-48149 Munster, Germany
关键词
SILICON; SODIUM; INSULATORS; MIGRATION; C-60; NA;
D O I
10.1021/acs.analchem.6b04222
中图分类号
O65 [分析化学];
学科分类号
070302 ; 081704 ;
摘要
A sputter beam, consisting of large 02 clusters, was used to record depth profiles of alkali metal ions (Me) within thin SiO2 layers. The O-2 gas cluster ion beam (O-2-GCIB) exhibits an erosion rate comparable to the frequently used O-2+ projectiles. However, because of its high sputter yield the necessary beam current is considerably lower (factor 50), resulting in a decreased amount of excess charges at the SiO2 surface. Hence, a reduced electric field is obtained within the remaining dielectric layer. This drastically mitigates the Me+ migration artifact, commonly observed in depth profiles of various dielectric materials, if analyzed by time-of-flight secondary ion mass spectrometry (ToF-SIMS) in dual beam mode. It is shown, that the application of O-2-GCIB results in a negligible residual ion migration for Na+ and K+. This enables artifact-free depth profiling with high sensitivity and low operational effort. Furthermore, insight into the migration behavior of Me+ during O-2+ sputtering is given by switching the sputter beam from O-2(+) to O-2 clusters and vice versa. K+ is found to be transported through the SiO2 layer only within the proceeding sputter front. For Na+ a steadily increasing fraction is observed, which migrates through the unaffected SiO2 layer toward the adjacent Si/SiO2 interface.
引用
收藏
页码:2377 / 2382
页数:6
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