Environmental Engineering Reference
In-Depth Information
Table 2 (contniued)
Fluorescent components
Components identi-
ied and sources
Fluorescence properties
References
Peak C-region
Peak A-region
Peak T-region Peak T UV -region
Peak C
Peak M p
Peak M
Peak W
Major
Minor
EX/Em (nm)
Fulvic acid (C-like), Occoquan
Watershed (Northern
Virginia, US) RU
Component 1,
allochthonous
350/456
-
-
-
240/456
-
-
-
Holbrook et al. ( 2006 )
Mostofa et al. ( 2005b ) c
Fulvic acid (C-like),
Nishi-Mataya and Higashi-
Mataya upstreams, Japan
Component 1
330-335/
460-463
-
-
-
250-255/
460-463
-
-
-
Fuvic Acid (C-like), Yasu
River, Lake Biwa
watershed, Japan
Component 1
-
310/464
-
-
250/464
-
-
-
Mostofa et al. ( 2005b ) c
Mostofa et al. ( 2005b ) c
Fuvic Acid (C-like), 3 Rivers
(Ane, Echi and Amano),
Lake Biwa watershed, Japan
Component 1
330-335/
455-462
-
-
-
255/455-462
-
-
-
Mostofa et al. ( 2005b ) c
Fulvic acid (C-like), Lake
Biwa, epilimnion (0-20 m),
during summer period
Component 1,
allochthonous
-
295-310/
449-450
-
-
250-255/
449-450
-
-
-
Mostofa et al. ( 2005b ) c
Fuvic acid (C-like), Lake Biwa,
epilimnion (0-20 m),
during winter period
Component 1,
allochthonous
-
310/443
-
-
255-260/
443
-
-
-
Mostofa et al. ( 2005b ) c
Fulvic Acid (C-like), Lake Biwa,
hypolimnion (40-80 m),
during summer period
Component 1,
allochthonous
-
300-305/
444-461
-
-
255-260/
444-461
-
-
-
Mostofa et al. ( 2005b ) c
Fulvic acid (C-like), Lake
Biwa, epilimnion (40-80 m),
during winter period
Component 1,
allochthonous
-
305-310/
450-464
-
-
255-260/
450-464
-
-
-
Fulvic acid (C-like)?, Urdaibai
and Foz Estuaries, Iberian
Component 1,
305/439
-
-
-
260/439
-
-
-
Santín et al. ( 2009 )
 
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