382
O. Kruger et aI.
Table 1. Measurements in the surroundings of the factory premises of BSL Werk Schkopau in mean
distance from the source areas L66, 154/H56 and F44
wind- Ioc:aIioa :
Ioc:aIioa :
IoCIIioa :
IocaIioa :
IoCIIioa :
Ioc:aIioa :
Ioc:aIioa :
Ioc:IIioa :
diJecL
N
NO
0
SO
S
SW
W
NW
dilL I TOM dilL I TOM dilL I TOM dilL TOM dill. I TOM kIlL I TOM !dIlL '1'011 IdilL/TGM
N
500 1 605
1500 1128
800 1531J
1200 I 18
N
1000 1 805
800 /450
1200 I 35
N
800 1415
1200 I 40
N
1000 I 35
2000 1129
N
1000 I 43
2000 I 16
N
1000 /83
2000 / 17
N
1000 /95
2000 / 18
N
1000 /83
2000 / 15
N
1000 1261
2500 / 17
N
1000 1210
2500 I 28
N
I disIaatc (m) 1 TGM (nr/lll3)
1000 /152
N
I
1200 I 26
N
1200 /300
N
1200 /193
N
1500/235
N
2000 I 27
N
2000 I 20
N
3000 I 91
N
6000 I 11
S
1500 1 63
1000 I 8,8 1000 I 33 1000 I 4,8
1000 I 6.0
2000 1605 1000 I 805
S
4000 I 6.8 2500 I 505
2500 11.2 3500 I 4.4
S
4000 I 405
SW
1000 162
5000 I 7J)
1500 /32
1000 163
SW
2000 I 56
3500 I 5.3
sw
3000 rn
4000 I 705
SW
3500 110
SW
4000 144
SW
5000 I 2.6
SW
120001 3,2
SW
150001 2,4
w
1000 1161
800 I 41
W
1500 I 5.7 800 I 25
W
7000 I 5.4 800 I 35
W
1000 166
W
2500 I 6.3
W
100001 4J)
W
120001 6.0
NW
500 I 8,8 1200 I 38
1200 120
NW
1000 111
1500 146
I
NW
1500 123
1500 I 78
NW
5000 1 4,6 1500 I 39
NW
1500 I 7.9
NW
2000 I 9.0
NW
4500 1 38
3
Dispersion Modelling
The local atmospheric transport of gaseous mercury originating from emissions
at the BSL Werk Schkopau was calculated for distances of a maximum of 10 km.
A numerical model for simulating transport from individual point sources was
applied. Earlier results of this transport model (Eppel et al. 1991) compared well
with measurements within a spatial range of a maximum of 100 km.
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