Abstract
Resuspension rates have been measured on Long Island Sound sediments (New York/Connecticut, USA) under an oscillating grid, using a flume, and in place, using high frequency acoustics, transmissometers, and sediment traps. Despite differences, the results compare favorably. The methods all provide an order-of-magnitude estimate of the resuspension rate and increases under storm conditions can be estimated.
| Original language | English |
|---|---|
| Pages (from-to) | 159-161 |
| Number of pages | 3 |
| Journal | Geo-Marine Letters |
| Volume | 11 |
| Issue number | 3-4 |
| DOIs | |
| State | Published - Sep 1991 |
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