Íslenskar landbúnaðarrannsóknir


Íslenskar landbúnaðarrannsóknir - 01.09.1978, Qupperneq 25

Íslenskar landbúnaðarrannsóknir - 01.09.1978, Qupperneq 25
THE ATLANTIC SALMON IN ICELAND 23 start until the water temperature is over 8°C. A similar experience was noted at the fishpass at Laxfoss in the river Nordurá in Iceland (Fig. 7). Information on the ascent of salmon in Icelandic rivers has been gained mainly from catch records during the early part of the salmon fishing season. In a few in- stances the salmon have been counted by fish counters, the most reliable one being a mechanical counter which has been in op- eration since 1960 at the river Ellidaár. This fish counter is mounted in a trap of a weir about 800 m above the tidal zone of the river. The counts at the weir from 1962-1971 and 1973 (Eiríksdóttir 1974) showan ob- vious trend for the peak of the run to be during the first or second week of July. The run then gradually tapers out in Au- gust and even into September (Fig. 8). The ascent varies in time from year to year. Thus the difference in time when 10% of the run has been counted can be about 1 month, at 50% 5V2 weeks and at 90% more than 6 weeks. The average cumulative catch curve from 1949-1973 (Fig. 9) (Eiríksdóttir 1974) shows that there was not as much difference in time at the 10% catch level as in the average cumulative curve of ascent for 1962-1971, and 1973, it being only IV2 weeks. At 50% it was almost 2 weeks and at 90% a little over 2 weeks. Spawning Jones (1959) states that salmon will spawn at depths from 15-120 cm, the ideal depth being 60 cm or more and that the most favorable rate of flow is 30-45 cm per sec- ond at the surface. Spawning proceeded to completion when the water temperature was between 2°C and 6°C in his tank ex- periments, but he has observed spwning in the river when temperature was as high as 10°C. Jones states furthermore that at water temperature below 1°C the cutting of beds is languid and not completed, and orgasm does not take place. In Icelandic salmon rivers there are usually large areas with gravel bottom at various depths suited for spawning. Spawning takes place at low tempera- tures. As water temperature falls first in the fall in the north and northeastern parts of the country, spawning starts there ear- lier than in the southern and western parts. Spawning time in the colder rivers would be in September and early October; salmon have even been caught in northern rivers with ripe ova in late August. In the rivers in western and southern Iceland spawning generally takes place from late September into November, but salmon have been observed to spawn as late as December in the river Sog. This river drains Thingvallavatn, the largest lake in Iceland, which is deep and it takes a long time to cool the water temperature in the autumn. The spawning beds of the river Ulfarsá near Reykjavík were surveyed in detail for six autumns during the years 1955—1963 (Gudjónsson 1964). The river is 10.4 km long and has an average discharge of 800 liters per second. It discharges from lake Hafravatn, which is 68 m above sea level, with a surface area of 1.02 km2 and into which flows a small stream, the Sel- jadalsá. In Ulfarsá spawning took place mostly during the first half of November. In many parts of the river there was gravel bottom where the salmon, mostly grilse,
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Íslenskar landbúnaðarrannsóknir

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