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Mireille Consalvey PhD Thesis - University of St Andrews

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Bi<strong>of</strong>-11111<br />

lol-Illatioll Lind dc\ clopnicill<br />

disturbance. As the site started to recover, patches <strong>of</strong> the golden brown colour<br />

associated with diatom bi<strong>of</strong>ilms were noted, these occurred throughout the site<br />

and were not localised to the edges. 14 days after the disturbance, cells had<br />

retumed to the top mm <strong>of</strong> the sediment and could be seen on and below the<br />

sediment surface (Figure 3.31)). There was a visible increase in the bed height<br />

over time at the disturbed site.<br />

Water content<br />

Associated with the removal <strong>of</strong> the surface layer <strong>of</strong> sediment was a<br />

significant decrease in the water content <strong>of</strong> 42 % (FI, 4 ý 11.03, p=0.029) from<br />

81+ 12 to 39 +4%. Subsequently the water content significantly increased over<br />

the remaining 14 days (F4,1<br />

0=3.96, p=0.03 5; Figure 3.4).<br />

Chlorophyll a<br />

After the removal <strong>of</strong> the surface sediment there was significantly less<br />

chlorophyll a in the system (t = 9.18, n=3, p=0.012), falling from 176 + 18 to 8<br />

3 pg chl a g-1 fdw, a decrease <strong>of</strong> 95%. The chlorophyll a content in the top I<br />

mm <strong>of</strong> the sediment significantly increased subsequent to the disturbance event<br />

(F6,13 ý 17.96; p

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