Jökull

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Jökull - 01.12.1980, Qupperneq 30

Jökull - 01.12.1980, Qupperneq 30
station in the receding phase of the jökul- hlaup. For discharge in this jökulhlaup see Rist (1976). In the jökulhlaup of 1972 S3-samples only were taken, at several places, including two stations (the outlet and bridge sites), where samples were collected in 1976. Fig. 5 presents sediment rating for samples obtained in 1972. The correlation coefficient of the rating curve (equation (1)) for all the samples taken in that jökulhlaup is 0.697. If a few points from an abnormal sediment load peak are omitted the correlation coefficient rises to 0.913. The cor- relation coefficient for all the S3 taken in 1976 is 0.924, or not very much better than in 1972. For discharge see Rist (1973). The sediment transport curves for two grain size fractions, coarse and fine silt, are shown in Fig. 6. The curves indicate a certain regularity in the sediment load of the jökulhlaup of 1972. First the load gradually increased, almost simultaneously with the discharge, and having reached a maximum it receded in a fairly regular manner. Concentration on the other hand varied greatly from one place to another both as regards coarse and fine grain sizes. The sediment load reached its maximum at the outlet, but at the bridge site the concentration is far less at the western bank than at the eastern one. Two or three days after the peak in the discharge a short but marked peak occurred in the sediment load. The samples taken in this peak (discussed by Tómasson 1974) are the kg/» 60000 - 50000 40000 ■ 1 A 4 ▲ 2 0 5 © 3 • 6 ® A / / 'o A° > i> i \ \ 1 i í A / / 9) *, \ o \ A X', 1 i i k ■5 0000 ' 2 X ? a! 9ÖÖ° * \ 1 k A 7f \ 1 js 6000 í \* 1 \ !• ' / \ V \ D <[$ / \ 1 t tf) 3000 2000 1000 900 800 700 600 / / ( ö Vj \ 1 1 7 // / T •ö 1 1. 4 / Q. 3 O Jt E X 16 l 8 20 Daga Da 22 m a ys of smár Mar 24 aðar h /9 1972 72 26 28 30 Fig. 6. Coarse (0.2—0.02 mm) and fine (0.02—0.002 mm) silt in suspended load in Skeiðará jökulhlaup 1972. Key: 1. coarse silt at glacier outlet and Skafta- fell; 2. coarse silt at dikes and bridge site, eastern shore; 3. coarse silt at bridge site, western Iceland; 4. fine silt at glacier outlet and Skaftafell; 5. fine silt at dikes and bridge site, eastern shore; 6. fine silt at bridge site, western shore. — Mynd 6. Aurrit mós (0.2—0.02 mm) og mélu (0.02—0.002 mm) í Skeiðarár- hlaupi 1972. 1. Mór við Otfall og Skaflafell. 2. Mór við garða og brúarstáði austurland. 3. Mór við brúarstœði vesturland. 4. Me'la við Otfall og Skaftafell. 5. Méla við garða og brúarstœði austurland. 6. Méla við brúarstceði vesturland. 28 JÖKULL 30. ÁR
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