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Adsorption desorption isotherms and pore distributions varied among Al2O3 and metal oxide-loaded Al2O3 catalysts (Fig. 4a, b).
The Alviniconcha holobiont and endosymbiont distributions varied from the northern to the southern region of the ELSC, which have somewhat different geological settings (Beinart et al. 2012).
Moreover, the overall temperature distributions varied significantly across multiple experiments, and the voltage signals possessed more chaotic behaviors than did those of the 1D and 2D CNTs structures.
There is considerable difference in terms of both fracture topographies and strains for models containing 16 particles when distributions varied from random/uniform to stringer distributions.
The particle size distributions varied from very narrow mesh sizes to full particle size distributions as they came out of commercial gas phase polymerization reactors.
This consistency is in line with our earlier findings during the simulated experiments where the bipartite caching mechanism with fixed and dynamically resizable partitions demonstrated a deviation of 1.23% and 0.96% respectively as the scope distributions varied.
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The bubble-size distributions vary widely within the contactor, deviating considerably from a standard normal distribution.
The distributions vary dramatically across centers.
We see that the interval distributions vary systematically with time.
Another hampering factor is seasonal climate; since weather is highly variable in Kenya, tsetse distributions vary similarly.
Cell size distributions vary between mutants.
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