Environmental Engineering Reference
In-Depth Information
(or not inluenced by) the settling of other particles, in a quiescent luid. So, settling is also inversely
proportional to the deviation of an object from a sphere (form resistance). Think of skydivers. If they
are falling head down with their arms by their sides, frictional (form) resistance is minimized and
their fall velocity is great (about 160-180 mph in the lower atmosphere). If the skydivers fall with
their body perpendicular to the ground and with their arms stretched out, the terminal fall velocity
is substantially decreased (to about 120 mph).
Similarly, phytoplankton may minimize their fall velocity by taking advantage of colder periods
(e.g., spring or fall in contrast to summer), minimizing the density difference between their bodies
and the water, and reducing their size. Since settling decreases nonlinearly with the square of the
radius, the most effective method for reducing settling velocities is to reduce size. A common clas-
siication system by size is illustrated in Table 15.3. So, Cyanobacteria, which include some of the
smallest phytoplankton, may have some competitive advantage over large phytoplankton in some
cases.
The ratio of surface area to volume also increases as size decreases, which may facilitate the
surface exchange of gases and nutrients as well as decrease settling rates. For picoplankton and
nanoplankton, the transfer of material to and from cells is almost entirely by molecular diffusion
(Wetzel 2001). Size may also impact the ease with which the phytoplankton may be eaten, such as
by ish and zooplankton. The microplankton and macroplankton are not as vulnerable to predation
(Wetzel 2001) but they are less eficient at nutrient uptake and more vulnerable to settling.
The size of phytoplankton may also impact the manner and accuracy of their enumeration. Sigee
(2005), for example, suggested that in the past the ecological role of picoplankton and nanoplankton
has been underestimated due to the dificulty of their detection and enumeration using conventional
microscopy.
In addition to their size, phytoplankton can also decrease their rate of settling by varying their
shape. Some of the potential strategies are to form groups or colonies, or to become asymmetrical
where the form resistance decreases with increasing asymmetry.
In addition, many phytoplankton may actively inluence settling velocities. Wetzel (2001), for
example, indicated that microphytoplankton (Table 15.3) may be separated into two broad types of
ecological strategies, those that are motile and those that are not motile. The motile forms include
those with gas vacuoles, such as some Cyanobacteria. By regulating their gas vacuoles, these algae
may become negatively buoyant and rise through the water column. Flagella may also be used
for motility. The nonmotile forms may depend on the turbulence mixing of the water column to
maintain their position within the photic zone. Other strategies include the accumulation of fats, the
reduction of density by altering the cellular ion content, and the production of gelatinous sheaths
TABLE 15.3
Size of Phytoplankton
Linear Size (Cell or
Colony Diameter, λ m)
Category
Unicellular Organisms
Colonial Organisms
Picoplankton
0.2-2
Photosynthetic bacteria, blue-green algae;
Chrysophyta
Nanoplankton
2-20
Blue-green algae, cryptophytes, small
dinolagellates and others
-
Microplankton
20-200
Dinolagellates
Diatoms
Macroplankton
>200
-
Blue-green algae
(Anabaena, Microcystis)
Source: Modiied from Sigee, D.C., Freshwater Microbiology: Biodiversity and Dynamic Interactions of Microorganisms
in the Aquatic Environment , Wiley, Chichester, UK, 2005.
 
Search WWH ::




Custom Search