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Figure 8


Fig. 8. The index of compaction of all models at the highest unidirectional flow speed (73 cm s-1). Values are means ± s.d., N=6. Only the most flexible models were significantly compacted, and backreef models more so than forereef models, as determined by Kruskall-Wallis non-parametric analysis (H=30.23, d.f.=11, P<0.05) and Nemenyi post-hoc multiple comparisons (Zar, 1999). Letters that are different indicate significant differences between groups as determined by Nemenyi post-hoc multiple comparisons (Zar, 1999).





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