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Meyniana

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Sediment dynamics and hydrodynamics...... 125<br />

Fig. 5: Salinity [psu] and temperature changes in profiles W1- W6 during high tide calm<br />

conditions.<br />

The particulate matter was found to be mainly in form of flocks, probably bounded<br />

with organic matter.<br />

Bottom sediments<br />

Surface sediments (0-0.5 cm layer) are dominated by the sand fraction (fig. 7).<br />

Aggregates of fine material, which are bounded probably by organic matter are observed<br />

very often on the surface as flocks – similar material up to 2 cm in size is found in<br />

the sediment traps. In many cases, the surface sediments are also enriched in<br />

small admixtures of fines, and in small organisms. Except at the W1 location,<br />

which is dominated by mud, the remaining locations are composed of sand: fine<br />

sand at the W2 station, medium, and medium to coarse sand further offshore. At the<br />

most distal stations, the surface sediments are classified as silty sand. Surface<br />

sediments are characterized by poor sorting, which is an effect of mixing of sands<br />

and fine material, and are usually dark, olive gray, dark brown and green. Relatively<br />

few carbonate organic fragments were found in these samples.<br />

Subsurface sediments (0.5 to about 5 cm layer) are also dominated by the sand<br />

fraction, except for sediments from W1 station, which are muds. In general, an<br />

offshore coarsening trend is observed from mud, fine silt to medium sand. On the<br />

locations close to the Hon Tre Island, the trend is relatively modified and coarse<br />

sands are found close to caps and fine sands in a bay. The sediments are usually<br />

very well sorted. In places, some intercalations of more silty sand similar to that<br />

found on the contemporary surface, are observed. Among the components of the<br />

sand fraction, the lithoclasts dominate. Carbonate fragments of shells and skeletons<br />

of organisms are of secondary significance.<br />

Analysis of satellite images<br />

Satellite scenes are commonly used for the water-quality studies as long as they<br />

register the wavelengths of sunlight efficiently penetrating the water. Landsat<br />

Thematic Mapper (TM) and Enhanced Thematic Mapper (ETM) scanners have four<br />

spectral bands useful for water surface and water column studies, and reasonable<br />

resolution of the pixel (30 m x 30 m). This allow successful presentations of spatial

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