Environmental Engineering Reference
In-Depth Information
At highly elevated WT (approximately >25-50 °C), photoinduced and micro-
bial degradation of DOM and POM is extremely enhanced, with extremely high
generation of H 2 O 2 , CO 2 and DIC. It has been shown that [CO 2 ] aq is significantly
higher (~10-120 M) at 25 °C than at 15 °C (~5-110 M) or at 9 °C (~5-50 M) in
marine waters (Hinga et al. 1994 ). This effect can cause extremely high photo-
synthesis and high primary production. This can be supported by the synergistic
effect of high H 2 O 2 , combined with high seawater temperature, which can cause
a 134 % increase in respiration rates. Such an increase surpassed the effect of
either H 2 O 2 or high seawater temperature alone (Higuchi et al. 2009 ). High tem-
perature, driven by strong solar intensity, is responsible for high production of
H 2 O 2 (see also chapter Photoinduced and Microbial Generation of Hydrogen
Peroxide and Organic Peroxides in Natural Waters ) (Mostofa and Sakugawa
2009 ), which is directly linked with photosynthesis. Simultaneously, this pro-
cess can also generate a high amount of ROS such as O 2
, 1 O 2 , H 2 O 2 , and HO
.
The latter is a strong oxidizing agent, produced either from H 2 O 2 (via direct
photo-dissociation by sunlight or photo-Fenton reaction) or other sources, such
as the direct photolysis of NO 2
(see the chapters Photoinduced and
Microbial Generation of Hydrogen Peroxide and Organic Peroxides in Natural
Waters , Photoinduced Generation of Hydroxyl Radical in Natural Waters
and Photoinduced and Microbial Degradation of Dissolved Organic Matter in
Natural Waters ”). This effect can significantly degrade algal or phytoplankton
cells, thereby decreasing the photosynthetic efficiency. All these processes should
be able to significantly promote the photosynthetic efficiency in waters with high
contents of DOM and POM.
and NO 3
Temperature Effects on Higher Plants
Plants need an optimum temperature for photosynthesis. The stress represented by
extremely high- or low-temperature has a significantly negative effect on the growth
and productivity of plants (Allen and Ort 2001 ; Adams et al. 2002 ; Adams Iii et al.
2004 ; Öquist and Huner 2003 ; Yang et al. 2009 ). It has been shown that suboptimal and
above-optimal temperatures can promote photoinhibition, caused by an over-excitation
of photosystems (Powles 1984 ; Öquist et al. 1993 ; Huner et al. 1998 ). Effects of tem-
perature on the photosynthesis of plants have been discussed as follows: First, low tem-
perature stress or chilling stress (generally at 0-12 °C) can highly inhibit growth and
development of most plants, and in particular of those coming from tropical and sub-
tropical regions (Allen and Ort 2001 ; Yang et al. 2009 ; D'Ambrosio et al. 2006 ).
The chilling stress or lower temperatures can affect several physiological func-
tions and induce water deficiency. Commonly observed effects are decrease of leaf
water potential, of electron transport rate, of total Chl contents, of CO 2 uptake and
of the carotenoid content; stomatal closure; inhibition of thylakoid electron trans-
port and photophosphorylation; Rubisco inactivation; inhibition of carbohydrate
metabolism; and finally, a significant decrease of the maximum quantum effi-
ciency of PSI and PSII primary photochemistry (Allen and Ort 2001 ; Yang et al.
2009 ; D'Ambrosio et al. 2006 ; Berry and Bjorkman 1980 ; Eamus 1986 ; Sage and
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