Secondary-ion intensity of sputtered Si
9433
ion bombardment seem to indicate that the sputtering process in Si conforms to the linear
cascade theory. More recent angle resolved Si+ emission by Pellet et al [25] also confirms
the linear cascade behaviour to some degree. The linear cascade theory has been applied to
several metals by Vasile [1] with a wide range of surface binding energies.
For the present set of data, the effect of the linear cascade expression on the ionization
probability has been examined. Two other values for the power factor of the denominator in
expression (5) have been used, namely 2.75 and 2.5. The procedure for fitting the spectrum is
the same as before, i.e. by first fitting the high-energy part of the spectrum to expression (1)
and obtaining the value of A in the exponential, and then fitting with expression (7) to
obtain n. In both cases, the value of A obtained is 2.0 × 104 m s−1, close to that obtained
above. The lack of sensitivity in A to the neutral distribution has also been noted by Vasile
[1]. However, the values of n obtained show quite a large variation. For the power factor
of 2.75 the value of n is 1.16, giving Te = 3700 K, while for the power factor of 2.5 the
value of n is 0.73, giving Te = 5800 K. Thus it appears that high temperatures persist in
the electronic excitations and that Sroubek’s estimate of 2600 K may be somewhat low.
5. Conclusion
In conclusion, the charge exchange process in Si+ secondary-ion emission from Si(100)
was found to exhibit a strong dependence on escape velocity, particularly over the high-
emission-energy portion (>19 eV). Such a trend is consistent with the electron tunnelling
model which is based on the electronic interaction of the sputtered ion with an undisturbed
metal band structure (Te = 0 K). At lower emission energies (<19 eV), the ionization
probability for Si+ exhibits a reduced velocity dependence. Agreement between experiment
and theory can be improved if electronic excitations in the collision cascades are considered.
References
[1] Vasile M J 1984 Phys. Rev. B 29 3785
[2] Garrett R F, MacDonald R J and Connor D J O 1984 Surf. Sci. 138 432
[3] Krauss A R and Gruen D M 1980 Surf. Sci. 92 14
[4] Hart R G and Cooper C B 1980 Surf. Sci. 94 105
[5] Norskov J K and Lundqvist B I 1979 Phys. Rev. B 19 5661
[6] Brako R and Newns D M 1981 Surf. Sci. 108 253
[7] Lang N D 1983 Phys. Rev. B 27 2019
[8] Yu M L and Lang N D 1983 Phys. Rev. Lett. 50 127
[9] Low M H S, Huan C H A, Wee A T S and Tan K L 1995 Nucl. Instrum. Methods B 103 482
[10] Dahl D A and Delmore J E EG&G Idaho, ID 83415, USA
[11] Wittmaack K 1979 Surf. Sci. 90 557
[12] Sigmund P 1969 Phys. Rev. 184 383
[13] Thompson M W 1968 Phil. Mag. 18 377
[14] Oechsner H 1970 Z. Phys. 288 433
[15] Bernhardt F, Oechsner H and Stumpe E 1976 Nucl. Instrum. Methods 132 329
[16] Wright R B, Pellin M J and Gruen D M 1981 Surf. Sci. 110 151
[17] Wucher A and Oechsner H 1988 Surf. Sci. 199 567
[18] Alay J L and Vandervorst W 1994 Phys. Rev. B 50 15 015
[19] MacDonald R J and Garrett R F 1978 Surf. Sci. 78 371
[20] Sroubek Z 1984 Appl. Phys. Lett. 45 849
[21] Sroubek Z, Zdansky K and Zavadil J 1980 Phys. Rev. Lett. 45 580
[22] Sroubek Z 1982 Phys. Rev. B 25 6046
[23] Sroubek Z 1989 Spectrochim. Acta. B 44 317
[24] Zalm P C 1983 J. Appl. Phys. 54 2660
[25] Pellet C, Schwebel C and Resseguier C 1993 Nucl. Instrum. Methods B 78 294