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Sediment transport near the Tauranga entrance to Tauranga Harbour
Authors:R. J. Davies‐Colley  T. R. Healy
Affiliation:1. Department of Earth Sciences , University of Waikato , Hamilton, New Zealand;2. Water and Soil Division , Ministry of Works and Development , Hamilton;3. Department of Earth Sciences , University of Waikato , Hamilton, New Zealand
Abstract:Abstract

Sediment transport at the Tauranga Entrance was studied in relation to tidal currents and waves. Bedforms resulting from tidal flow were investigated with scuba divers and echo‐soundings. The alignment and scale of bedforms indicated the direction and approximate rate of sediment transport. Sediment transport was measured directly using sediment traps, and results were compared with rates calculated by another method. Maximum sediment transport rates of 20 000–30 000 g.m?1 per half tidal cycle occur near the inlet gorge, but rates vary considerably in time and space, depending mainly upon power of tidal currents. A model of sediment transport for this inlet has been evolved based on tidal flow streamlines, bedform features, and the measured and calculated rates of sediment transport.
Keywords:Chrysophrys auratus  growth  populations  East Cape, New Zealand  trawling  fishery resources
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