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Several submarine canyons have developed offshore of the Aramata region of the Shimoni-ikawa coast in Toyama&#x0D;Bay, which is one of the three deep bays in Japan. The Kurobe River with a steep bed slope flows into the sea&#x0D;immediately north of this region, and a large amount of sediment has been supplied to this area, which has been&#x0D;transported by southward longshore sand transport. However, beach erosion has occurred owing to the decrease in sediment supply from the Kurobe River. Furthermore, since the construction of detached breakwaters as a measure&#x0D;against beach erosion, offshore sand transport has accelerated and beach erosion has become more severe. In this&#x0D;study, aerial photographs and bathymetric survey data were analyzed, then the mechanism of offshore sand transport&#x0D;was investigated using the BG model proposed by Serizawa et al. (2007).

MECHANISM OF OFFSHORE SAND DISCHARGE INTO SUBMARINE CANYON TRIGGERED BY CONSTRUCTING DETACHED BREAKWATER CLOSE TO SHORELINE