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It follows that the stationary value of the mean linear size of adsorbate islands decreases with the anisotropy strength growth.
At small values of the anisotropic strength, the mean linear size of adsorbate islands grows in time even at large time scales.
It is seen that at a stage when the mean linear size grows in time, one can observe both large multilayer adsorbate islands and small islands on the first layer (see Fig. 3 b at t=50).
Fig. 3 Evolution of the mean linear size of adsorbate islands 〈R〉 in units of diffusion length L D on a half-height of the growing surface at different values of anisotropy strength u (a).
Next, we will discuss a change in the mean linear size of adsorbate islands 〈R〉 on a half-height of the growing surface with an increase in the anisotropy strength u and corresponding distributions of adsorbate islands over sizes f(R/〈R〉).
It is seen that at small values of anisotropy strength (see curve with black squares at u=3), the mean linear size 〈R〉 of adsorbate islands on a half-height of a growing surface grows in time even at large time scales, when the mean adsorbate concentration takes stationary value (see dash-dot curve for u=3 in Fig. 1 a).
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HEIP of tumour size could be replicated using a weighted sum of CEIP of effective diameter, surface area and maximum linear size (mean squared deviation 56.56, p < 0.001).
While Fragment 6a does emphasize the size of intervals and their combination to form the octave, size need not mean linear magnitude and combination need not mean addition.
In grain growth experiments, if the mean spatial grain size is estimated by the mean linear intercept length, marginal reductions in the spread in grain size may be interpreted as an increased growth exponent in the grain growth equation.
To determine the differences in alveolar size, measurements of mean linear intercept (Lm) were used.
Grain size was determined by mean linear intercept method.
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