ABSTRACT The topographical complexity and multi-scale nature of biofouling makes the use of current drag-topography correlations over regular topographical arrangements impractical. In order to address this problem, we synthesise biofouling-type surfaces of tubeworm-type populations in various percentage coverages and distributions. To acquire the resulting flow field we utilise topography-resolving direct numerical simulations. The surface synthesis is performed by an in-house surface generation/analysis package, AdRoS, in which individual biofouling organisms are used as building blocks to synthesise surfaces that resemble those found on ship hulls. Our synthesis algorithm allows for a parametric study to be performed with respect to selected parameters characterising the topography. In this work we focus on the frontal solidity, λ f , in order for its impact to the mean flow to be investigated. Results indicate that both the boundary layer growth-rate, as well as the roughness function, Δ U + , scale with the frontal solidity, λ f , in a proportional fashion, indicating the significance of the frontal solidity parameter. The organism-characteristic height, h , proves to also have a significant impact to the mean flow and even counter-act against the frontal solidity. Interestingly, typical flow separation patterns such as those found on isolated wall-mounted objects were detected, which were found to be mitigated or amplified depending on the planar, λ p , and frontal, λ f , solidity.
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