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9 Interlayer Exchange Interactions in Magnetic Multilayers

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348 9 <strong>Interlayer</strong> <strong>Exchange</strong> <strong>Interactions</strong> <strong>in</strong> <strong>Magnetic</strong> <strong>Multilayers</strong><br />

at least two reasons for this discrepancy. The first is the effect of <strong>in</strong>terface roughness,<br />

which generally tends to reduce the amplitude of the coupl<strong>in</strong>g oscillations [117];<br />

this effect is particularly pronounced for short-period oscillatory components, as is<br />

<strong>in</strong>deed confirmed experimentally [22]. The second reason is of <strong>in</strong>tr<strong>in</strong>sic character<br />

– the theoretical values of A1 given <strong>in</strong> Table 3 correspond to the asymptotic limit,<br />

whereas the experimental data have been obta<strong>in</strong>ed for spacer thicknesses below<br />

15 AL. As is clearly apparent from Fig. 6a of Ref. [129] and from Fig. 13 (bottom)<br />

of Ref. [47], the asymptotic regime is atta<strong>in</strong>ed only for thicknesses above 20 to<br />

40 AL; below this value the envelope of the oscillations deviates significantly from<br />

D −2 behavior, and the apparent amplitude <strong>in</strong> the range relevant to experiments is<br />

typically a factor of 2 smaller than the asymptotic amplitude. This pre-asymptotic<br />

correction is attributed to the strong energy-dependence of r ↓<br />

1 [47].<br />

Let us now discuss the long-period oscillatory component. As appears from Table<br />

3, the situation is quite confus<strong>in</strong>g – not only do the various theoretical results disagree<br />

with each other, but some [133, 60, 47] underestimate the coupl<strong>in</strong>g strength compared<br />

with the experimental result [20, 21, 122], a difference which cannot be expla<strong>in</strong>ed by<br />

the effect of roughness or <strong>in</strong>terdiffusion.<br />

The long-period oscillatory component arises from the center Ɣ of the two-<br />

dimensional Brillou<strong>in</strong> zone. Here aga<strong>in</strong>, for the same reason as above, |r ↑<br />

2 |≈0.<br />

The m<strong>in</strong>ority-sp<strong>in</strong> reflection coefficient, is on the other hand, considerably smaller<br />

than for the short-period oscillation, and |r ↓<br />

2 | ≈ 0.15 [74], so that |r2| ≈ 0.05<br />

[74, 133]. This very small sp<strong>in</strong>-dependent conf<strong>in</strong>ement expla<strong>in</strong>s the very small values<br />

of A2 obta<strong>in</strong>ed by authors who rely on the asymptotic expression, Eq. (29), obta<strong>in</strong>ed<br />

from the stationary phase approximation [133, 60, 47]. As seen from Fig. 2 of Ref.<br />

[135] and from Fig. 2 of Ref. [60], however, r ↓<br />

2 <strong>in</strong>creases very strongly with k and<br />

full reflection is reached at a distance 0.1 × π/a from Ɣ; <strong>in</strong>deed, the low reflectivity<br />

arises only <strong>in</strong> a narrow w<strong>in</strong>dow around Ɣ. As discussed <strong>in</strong> Ref. [136], this gives rise to<br />

a strong preasymptotic correction, and expla<strong>in</strong>s why the stationary-phase approximation<br />

yields an underestimated value of A2. If, on the other hand, the k <strong>in</strong>tegration<br />

is performed without us<strong>in</strong>g the stationary-phase approximation, as <strong>in</strong> Ref. [129], a<br />

much higher value of A2 is obta<strong>in</strong>ed; the latter is larger than the experimental value<br />

[20, 21, 122] by a factor of 2.5, which seems plausible <strong>in</strong> view of the effect of roughness<br />

and <strong>in</strong>terdiffusion.<br />

Our knowledge of the phase of the oscillations is much more restricted as this<br />

aspect of the problem has so far attracted little attention, with the notable exception<br />

of the work of Weber et al. [22]. On general grounds, for total reflection (as for<br />

r1↓), one expects the phase to vary with magnetic layer thickness and/or with the<br />

chemical nature of the magnetic layer; conversely, for weak conf<strong>in</strong>ement (as for r ↓<br />

2 ),<br />

one expects the phase to be almost <strong>in</strong>variant [74]. These general trends were, <strong>in</strong>deed,<br />

confirmed experimentally by Weber et al. [22].

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