Encyclopedia of Environmental Science and Engineering, Volume I and II

(Ben Green) #1

396 EUTROPHICATION


varies with the organism and with the type of nitrogen. For
ammonia nitrogen the optimum range varies from 0.3 to 5.3
ppm and for nitrate nitrogen the optimum range falls between
0.3 and 0.9 ppm. Below these values the growth rate decreases
as the concentration of nitrogen decreases.
Apparently the use of the various forms of nitrogen by
algae is not constant throughout the year. Tests conducted
at Sanctuary Lake in Pennsylvania (1965) indicate that the
order of preference for the three forms of nitrogen—ammonia-
nitrogen, nitrate-nitrogen, and nitrite-nitrogen—are defi ned
by three seasonal periods, which are:

Spring (1) Ammonia nitrogen
(2) Nitrate nitrogen
(3) Nitrite nitrogen
Midsummer (1) Ammonia nitrogen
(2) Nitrite nitrogen
(3) Nitrate nitrogen
Fall (1) Ammonia nitrogen
(2) Nitrate nitrogen
(3) Nitrite nitrogen

The amount of nitrogen in the aquatic environment is
important to algae because it determines the amount of chlo-
rophyll that may be formed. Too much nitrogen, however,
inhibits the formation of chlorophyll and limits growth.
Laboratory studies on algae conducted by Gerloff indicate
that of all the nutrients required by algae, only nitrogen, phos-
phorus and iron may be considered as limiting elements, and
of these three, nitrogen exerts the maximum limiting infl u-
ence. Approximately 5 mg of nitrogen and 0.08 mg of phos-
phorus were necessary for each 100 mg of algae produced.
The corresponding nitrogen/phosphorus ratio is 60 to 1.
Hutchinson cites phosphorus as being the more impor-
tant element since it is more likely to be defi cient. When
phosphorus enters a body of water, only about 10% is in the
soluble form readily available for algal consumption. During
midsummer total phosphate may increase greatly during the
formation of algal blooms, while soluble phosphate is unde-
tectable due to rapid absorption by the growing algae. Very
often during warm weather these blooms are stimulated by
the decomposition and release of soluble phosphates from
the bottom sediments, deposited by the expired blooms of
previous seasons. Thus when phosphates are added to a
lake, only a portion of the phosphates are used in produc-
ing blooms. The blooms thrive and consume phosphates for
only a short time, and a signifi cant amount fi nds its way to
the bottom sediments where it will be unavailable to further
growth of aquatic vegetation.
Prescott examined a number of algae and concluded
that most blue-green algae are highly proteinaceous.
Aphanizomenon fl os-aquae, for example, was shown to con-
tain 62.8% protein. Green algae were found to be less pro-
teinaceous. Spirogyra and cladophora, for example, contain
23.8 and 23.6% respectively. Thus it can be concluded that
the nitrogen requirement (for the elaboration of proteins)
depends on the class of algae, and that blue-green algae
would require more nitrogen than green algae.

Provasoli examined 154 algal species to determine the
requirements for organic micronutrients. He found that
although 56 species required no vitamins, 90 species were
unable to live without vitamins such as B 12 , thiamin and
biotin, either alone or in various combinations. He concluded
that these vitamins are derived from soil runoff, bottom muds,
fungi and bacterial production (B 12 ), and from a natural resid-
ual in the water.
Ketchum and Pirson conducted a series of examina-
tions on the inorganic micronutrient requirements of algae
and concluded that a number of elements are necessary for
growth. No numerical values were assigned to the require-
ment levels. Those elements shown to be essential were C,
H, O, P, H, S, Mg, Ca, Co, Fe, K and Mo. Those elements
which may be essential (subject to further study) were Cu,
An, B, Si, Va, Na, Sr, and Rb.
In summation, absolute values and nutrient thresholds
cannot be set at this time because too little is known regard-
ing the requirements of individual species. It might be stated
in general terms, however, that nitrogen and phosphorus are
two essential nutrient elements related to the production of
blooms, and that if they are present in the neighborhood
of 0.2 ppm and 0.05 ppm, respectively, algal growths will
increase signifi cantly.

NUTRITIONAL THRESHOLDS FOR THE GROWTH
OF AQUATIC PLANTS

Studies conducted by Harper and Daniel indicate that sub-
merged aquative plants contain 12% dry matter of which
1.8% are nitrogen compounds and 0.18% are phosphorus
compounds. Hoagland indicates that when the nitrate content
of water is high, nitrates may be stored in aquatic plants to
be reduced to the usable ammonia nitrogen form as required.
Subsequent investigations show that ammonia nitrogen can
be substituted for nitrate nitrogen and used directly. Light
apparently is not a necessary factor in the reduction of the
nitrogen.
Muller conducted a number of experiments on both algae
and submerged aquatic plants, and concludes that exces-
sive growths of plants and algae can be avoided in enriched
waters if the concentration of nitrate nitrogen is kept below
0.3 ppm, and if the concentration of total nitrogen remains
below 0.6 ppm.

OXYGEN BALANCE

Recently, attention has been given to the effect of the intense
growths of algae on the oxygen balance of natural water-
ways. It has been established that the dissolved oxygen
concentrations may exhibit wide variation throughout the
course of the day. This variation is attributed to the ability of
algae to produce oxygen during the daylight hours, whereas
they require oxygen for their metabolic processes during the
hours of darkness.

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