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( Salmo salar L.) in the River Spey as determined by

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Movements after <strong>the</strong> first <strong>as</strong>cent<br />

Dur<strong>in</strong>g early migration, fish movements were predom<strong>in</strong>antly crepuscular<br />

and nocturnal and appeared to take place regardless of <strong>the</strong> prevail<strong>in</strong>g flow<br />

conditions (Fig. 8). However, with<strong>in</strong> this migration daylight movements<br />

were recorded which correlated closely with <strong>in</strong>cre<strong>as</strong>ed flow rates (Table V).<br />

For much of <strong>the</strong>ir river<strong>in</strong>e migration <strong>the</strong> adult fish rema<strong>in</strong>ed at a fixed<br />

location <strong>in</strong> <strong>the</strong> river; however, this quiescent period w<strong>as</strong> often <strong>in</strong>terrupted<br />

<strong>by</strong> a fur<strong>the</strong>r up-stream movement to a new hold<strong>in</strong>g position. These later<br />

movements were analysed to determ<strong>in</strong>e if <strong>the</strong>re w<strong>as</strong> any relationship with<br />

chang<strong>in</strong>g flow rates. Where fish showed a discont<strong>in</strong>uous up.stream<br />

migration, such <strong>as</strong> F2.88 and F38.89, data from <strong>the</strong> recommencement of<br />

progress were <strong>in</strong>cluded if a period of greater than five days w<strong>as</strong> spent <strong>in</strong> a<br />

hold<strong>in</strong>g position. The movements analysed were for ma<strong>in</strong> stem movements<br />

between Boat o'Brig and Grantown; tributary movements were excluded.<br />

r Grilse Upper<br />

[ Grilse Lower<br />

Figure 11.<br />

Time [days)<br />

The average distance moved dur<strong>in</strong>g <strong>the</strong> first 15 days of <strong>the</strong> <strong>as</strong>cent<br />

ph<strong>as</strong>e <strong>by</strong> grllse rele<strong>as</strong>ed dur<strong>in</strong>g June. Grilse which progressed to <strong>the</strong><br />

upper reaches are shown separately from those that rema<strong>in</strong>ed <strong>in</strong> <strong>the</strong><br />

lower reaches.<br />

Figures 12a and 12b show <strong>the</strong> frequency of mean daily flows recorded at<br />

Boat o'Brig from May to November 1988 and from March to October 1989.<br />

The mean daily flows at which fish were recorded <strong>as</strong> mov<strong>in</strong>g were<br />

determ<strong>in</strong>ed, and are <strong>in</strong>dicated <strong>in</strong> Figures 12 a and 12b.<br />

From <strong>the</strong> results presented <strong>in</strong> Figures 12a and 12b, it appears that salmon<br />

movements occur over a wide range of flows. Only dur<strong>in</strong>g July 1988, June<br />

1989 and August 1989 were <strong>the</strong> flows at which fish commenced

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