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 luo
r
escence intensities
References
Photoirradiation
Microbial
Photoirradiation
Microbial
size/type (
μ
m)
Peak C-region
Peak T- and T
UV
-regions
%
%
Lake Biwa, 35°N: deeper water
(70 m)
Allochthonous/
autochthonous
0.10
12 (dark)
nd
na
0
na
(
+
) 5
Mostofa et al. (
2011
)
Lake Biwa, 35°N: surface water
(2.5 m)
Allochthonous/
autochthonous
<5 kDa
12 (irradiated)
nd
−
16
na
(
+
) 4
na
Mostofa et al. (
2011
)
(
+
) 102
Lake Biwa, 35°N: surface water
(2.5 m)
Allochthonous/
autochthonous
<5 kDa
12 (dark)
nd
na
na
(
+
) 51
Mostofa et al. (
2011
)
na
Lake Biwa, 35°N: deeper water
(70 m)
Allochthonous/
autochthonous
<5 kDa
12 (irradiated)
nd
−
50
−
19
na
Mostofa et al. (
2011
)
Lake Biwa, 35°N: deeper water
(70 m)
Allochthonous/
autochthonous
<5 kDa
12 (dark)
nd
na
(
+
) 20
na
(
+
) 28
Mostofa et al. (
2011
)
Four Lakes (45ºN)
Allochthonous/
autochthonous
0.45
13
nd
−
(22-31)
−
(0-5)
nd
nd
Garcia et al. (
2005
)
Lake Taihu, China
Allochthonous/
autochthonous
0.22
12
nd
−
70
nd
−
60
nd
Zhang et al. (
2009b
)
Fulvic acid, Mill Creek: surface
water, 43ºN
Allochthonous/
autochthonous
0.45
12
nd
−
(48-79)
na
na
na
Winter et al. (
2007
)
Fulvic acid, Bannister Lake:
surface water, 43ºN
Allochthonous/
autochthonous
0.45
12
nd
−
(75-83)
na
na
na
Winter et al. (
2007
)
−
(74-77)
na
Fulvic acid and tryptophan, Lake
Erie: surface water, 42ºN
Allochthonous/
autochthonous
0.45
12
nd
na
na
Winter et al. (
2007
)
Fulvic acid, Sanctuary Pond:
surface water, 41ºN
Allochthonous/
autochthonous
0.45
12
nd
−
(71-79)
na
na
na
Winter et al. (
2007
)
Humic acid, Luther Marsh:
surface water, 43ºN
Allochthonous/
autochthonous
0.45
12
nd
−
(64-65)
na
na
na
Winter et al. (
2007
)
Humic acid, Mill Creek:
surface water, 43ºN
Allochthonous/
autochthonous
0.45
12
nd
−
(91-100)
na
na
na
Winter et al. (
2007
)
