𝔖 Bobbio Scriptorium
✦   LIBER   ✦

Nondestructive determination of the concentration profile in the surface layer of AuCu alloy with the use of directional AES and Monte-Carlo simulations

✍ Scribed by S Mróz; A Mróz

Publisher
Elsevier Science
Year
1998
Tongue
English
Weight
532 KB
Volume
49
Category
Article
ISSN
0042-207X

No coin nor oath required. For personal study only.

✦ Synopsis

Ratios of M*,,VVAuger

peak heights of gold and copper for the Au~&I~,~ alloy expected for particular compositions of two surface atomic layers and for two incidence angles of the primary electron beam in an RFA spectrometer were calculated with the use of Monte-Carlo computer simulation of the process ofAuger electron transport to the sample surface, including elastic and inelastic scattering of those electrons. Those ratios were compared with the corresponding ratios obtained experimentally which gave the relative concentration of gold atoms in the first and second atomic layers equal to 0.79+ 0.05 and 0.605 0.20, respectively.

📜 SIMILAR VOLUMES

In silico profiling of tyrosine kinases
In silico profiling of tyrosine kinases binding specificity and drug resistance using Monte Carlo simulations with the ensembles of protein kinase crystal structures
✍ Gennady M. Verkhivker 📂 Article 📅 2007 🏛 Wiley (John Wiley & Sons) 🌐 English ⚖ 734 KB

## Abstract The molecular basis of the tyrosine kinases binding specificity and drug resistance against cancer drugs Imatinib and Dasatinib is elucidated using Monte Carlo simulations of the inhibitor–receptor binding with the ensembles of protein kinase crystal structures. __In silico__ proteomics

Profile measurements in the atmospheric
Profile measurements in the atmospheric near-surface layer and the use of suitable universal functions for the determination of the turbulent energy exchange
✍ Th. Foken; G. Skeib 📂 Article 📅 1983 🏛 Springer 🌐 English ⚖ 376 KB

The authors summarize their recent published studies on profile measurements including new universal functions and an error analysis with a particular view to parameterisation above soil and water. Verification of the theoretical results is given using new data of the MESP-81 Tsimlyansk experiment.