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Embley

Marine - part 1 (PDF 960 KB) - Rio Tinto Alcan

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Rio Tinto AlcanEnvironmental Impact StatementSouth of <strong>Embley</strong> Project360 0315>. 270z225CCw180135asa)2 9045Mean Dirbuoy = 0.8875 Mean Dirport + 10045 90 135 180 225 270 315 360Mean Dir, SoE port siteFigure 6-15Modelled Mean Wave Direction at Proposed Port vs Measured at Buoy10080604020IINE E SE S SWWave direction (propagating from)NWNFigure 6-16Modelled Wave Direction Frequency of Occurrence at Proposed PortSite6.1.5 Sediment MovementThe beach either side of the proposed port site is relatively straight as shown in Plate 6-1.Longshore transport of beach sand occurs during storm events and the extent depends onwave height, direction, and storm duration. Calculations, using modelled wave data, show thatover time there has been a net movement of approximately 12,000m3 of beach sand percyclone season transported towards Boyd Point. The largest single sand movement event of86,000m3 towards Boyd Point occurred during Tropical Cyclone Dominic in April 1982.Mobilisation of fine sediments surrounding the dredge area is a function of the cohesive or noncohesivenature of the material and the bed stresses that are able to be developed underprevailing current and wave conditions. The material within the dredge area mainly consists ofcohesive sediments at least out to about 4km from shore where sediments increase significantlyin sand content (refer Section 6.5.4.2). Once the current and wave conditions overcome thecritical bed-shear stress, sediments will begin to move.Normally the critical bed-shear stress is not greater than 0.3N/m2 for a weakly consolidatedmud and 1.2N/m2 or greater for a moderately consolidated mud (mud is the combined silt andclay fractions).Section 6 Marine Page 6-14

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