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Centroid location of implanted ions in the SiO2layer of MOS structures using the photoI‐Vtechnique)

 

作者: D. J. DiMaria,   D. R. Young,   R. F. DeKeersmaecker,   W. R. Hunter,   C. M. Serrano,  

 

期刊: Journal of Applied Physics  (AIP Available online 1978)
卷期: Volume 49, issue 11  

页码: 5441-5444

 

ISSN:0021-8979

 

年代: 1978

 

DOI:10.1063/1.324510

 

出版商: AIP

 

数据来源: AIP

 

摘要:

The centroids for distributions of various ions important in Si technology (Al, P, and As) implanted at energies from 5 to 100 keV and a fluence of 1×1013cm−2into 1300–1400‐A˚‐thick SiO2layers of metal‐silicon dioxide‐silicon (MOS) structures have been located by using measurements of the photocurrent as a function of the gate voltae which is called the photoI‐Vtechnique. This technique senses trapped electrons on sites related to the implanted ions after charging by avalanche injection. A high‐temperature (1000 °C in N2for 30 min) premetallization anneal was used in order to minimize trapping on atomic displacement damage sites which could give a different centroid than that of the ion distribution. Good agreement of the trapped electron centroid deduced from the photoI‐Vtechnique with calculations of the ion centroid based on the theory of Lindhard, Scharff, and Schio&slash;tt (LSS) and with independent experimental determinations of the ion centroid from profiles using secondary ion mass spectroscopy (SIMS) or He+ion backscattering was found in most cases. The photoI‐Vtechnique is shown to have distinct advantages over most techniques which directly measure the ion distribution or centroid like SIMS and He+ion backscattering because of its nondestructive nature, minimally perturbing effect, and extremely low detectability limit of 1011charges/cm2or less. The empirical relationship observed by Chu, Crowder, Mayer, and Ziegler for ion implantation into various amorphous insulators between the LSS normalized centroid &rgr; and the LSS normalized energy &egr; of &rgr;=2.7&egr; has been shown for the first time to be valid for &egr;?0.4.

 

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