136
\l
••
B. J. Haupt· K. Stattegger . D. Seidov
Fig.17 Sediment sources prescribed as initial
conditions (see Table 1).
/l(J~ In the case of conversions the sediment density Ps = 2.6 cm- 3 and
the porosityy = 0.75
were used (Zanke 1982)
003
0.035 0095 0_099
so
85
110
I1S
120
150
155
sediment Input [Vkm>yrl
Table 1 Surver of used sediment sources. In case of conversions the sediment density
Ps = 2.6 g/cm and the porosityy = 0.75 were used (Zanke 1982). The lower sediment input
is used in case of a given range (Fig. 17)
Region
Area [x10 6 km 2 ]
Sediment input [t/km 2 yr]
Reference
northern
n.a.
3.156 x 10- 2
Honjo 1990 I
North Atlantic
Miller et al. 1977
East -Greenland
n.a.
6.96 x 10- 2
Enos 1991
Iceland
n.a.
6.1 x 10- 2 -1.085 x 10- 1
Enos 1991
Norwegian coast
n.a.
6.06 x 10- 2 -6.93 x 10- 2
Enos 1991
Elbe
0.13
84
Milliman I
Syvitski 1992
Weser
0.038
33
Milliman I
Syvitski 1992
Seine
0.065
114.2
Milliman I
Syvitski 1992
Loire
0.155
150
Milliman I
Syvitski 1992
southern England n.a.
<10
Einsele 1992