Environmental Engineering Reference
In-Depth Information
Table 4 (
continued)
Type of samples/locations
Origin of DOM
Filtration
Irradiation
time
(h/days)
Solar
intensity
(MJm
−
2
)
Changes in luorescence intensities
References
Photoirradiation
Microbial
Photoirradiation
Microbial
size/type (
μ
m)
Peak C-region
Peak T- and T
UV
-regions
%
%
Baltic Sea, BY32: 0-50 m depth
Allochthonous/
autochthonous
0.20 (uniltered)
12
nd
−
(61-70)
nd
nd
nd
Skoog et al. (
1996
)
Baltic Sea, BY32: 0-50 m
+
chloroform
Allochthonous/
autochthonous
0.20 (uniltered)
12
nd
−
(59-81)
nd
nd
nd
Skoog et al. (
1996
)
nd
Baltic Sea, BY32: 100-190 m
depth
Allochthonous/
autochthonous
0.20 (uniltered)
12
nd
−
(73-75)
nd
nd
Skoog et al. (
1996
)
Baltic Sea, BY32: 100-
190 m
+
Chloroform
Allochthonous/
autochthonous
0.20 (uniltered)
12
nd
−
(83-84)
nd
nd
nd
Skoog et al. (
1996
)
Baltic Sea, F15: 0-50 m depth
Allochthonous/
autochthonous
0.20 (uniltered)
4
nd
−
(48-49)
nd
nd
nd
Skoog et al. (
1996
)
Baltic Sea, F15: 0-50 m depth
Allochthonous/
autochthonous
0.20 (uniltered)
4
nd
−
50
nd
nd
nd
Skoog et al. (
1996
)
Baltic Sea, F15: 0-50 m depth
Allochthonous/
autochthonous
0.20 (iltered)
4
nd
−
(50-51)
nd
nd
nd
Skoog et al. (
1996
)
Baltic Sea, F15: 100 m depth
Allochthonous/
autochthonous
0.20 (iltered)
4
nd
−
56
nd
nd
nd
Skoog et al. (
1996
)
−
22
(
+
) 8
Mediterranean Sea, 42°N: Canet
lagons
Allochthonous/
autochthonous
0.20 (iltered)
8 h (summer)
nd
nd
nd
Abboudi et al. (
2008
)
Mediterranean Sea, 42°N: Leucate
lagons
Allochthonous/
autochthonous
0.20 (iltered)
8 h (summer)
nd
−
9
(
+
) 0.4
nd
nd
Abboudi et al. (
2008
)
Mediterranean Sea, 42°N: coastal
waters (SOLA)
Allochthonous/
autochthonous
0.20 (iltered)
8 h (summer)
nd
−
34
−
2
nd
nd
Abboudi et al. (
2008
)
Seawater, Gotland Deep: 40 m,
57ºN
Allochthonous/
autochthonous
0.45
13 (UV-B lamp) nd
−
32
nd
nd
nd
Lepane et al. (
2003
)
nd
not detected,
na
not applicable,
np
no signiicant luorescence peak observed in samples
(
−
) and (
+
) means a decrease in luorescence and an increase in luorescence, respectively, of the respective peaks
