Coastal Restoration Trust of New Zealand

Coastal Dune Ecosystem Reference Database

Descriptions of new native species of phanerograms Journal Paper

Author
Petrie, D.
Year
1912
Journal / Source
Transactions and Proceedings of the Royal Society of New Zealand
Volume
44
Pages
179-187
Keywords
accretion, airflow, Ammophila arenaria, foredune, suspension.
Summary
Aeolian sedimentation across an Ammophila arenaria-dominated foredune was assessed for eight months using sand traps. This research aimed to ascertain if such foredunes act as a barrier to transport between beaches and hinterland dune systems. At Mason Bay, sand was transported across the foredune at rates of up to 10 kg.hour-1 per 100 m length of coast at wind velocities of 31 m.s-1 . Results were compared with computational fluid dynamics modelled airflows and foredune volume changes. Saltation was important for up to 17 m past the stoss face. Rates of transport were well short of rates of volume gain. Approximately 2% or less of stoss face suspended sediment transport reached the hinterland. The foredune is primarily a sand sink.