| 摘要 |
A method of regenerating tidal mud flats which have a degraded or eroding profile includes the steps of ascertaining the ambient tidal range and wave climate of a mud flat to be regenerated and deriving from these data a new, regenerated profile for the mud flat, and depositing densified or dewatered mud or clay on the mud flat to build the new profile. The wave climate, and hence the sedimentary regime, of the mud flat is modified by breakwater or barrier means to render the mud flat receptive to deposition and retentive of the deposited mud or clay to preserve the regenerated profile. The breakwater or barrier means may be an offshore, floating breakwater adapted to suppress high and short-period waves but to permit the passage of low and long-period waves.
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