PE EIE[R-Rg RESEARCH ON - HJ Andrews Experimental Forest
PE EIE[R-Rg RESEARCH ON - HJ Andrews Experimental Forest
PE EIE[R-Rg RESEARCH ON - HJ Andrews Experimental Forest
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climate, surrounding terrestrial environment ,<br />
prevailing winds, lake circulation dynamics ,<br />
rates of water and inorganic nutrient inflow<br />
and outflow, and chemical precipitation of<br />
essential nutrients control the productivity ,<br />
water quality, and community structure of<br />
aquatic ecosystems ; (2) the dynamics of nutrient<br />
and energy cycling through both biological<br />
and physical processes ; (3) the<br />
mechanisms by which community structure<br />
may inhibit or enhance overall productivity<br />
and water quality ; (4) the response of complex<br />
aquatic ecosystems to a variety of<br />
natural and artificially created disturbances ;<br />
and (5) the mechanisms these systems have<br />
evolved for coping with these disturbances .<br />
The nature of these questions justifies th e<br />
coordinated program which is planned. Some<br />
of the questions this program will bear upo n<br />
and how they intend to be tackled will now<br />
be discussed .<br />
The phytoplankton and bacterial communities<br />
in lakes not only provide the basis fo r<br />
complex food webs, they essentially contro l<br />
the overall water quality and the apparent<br />
state of eutrophication . The sustained abundance<br />
and species composition of the bacterial<br />
and phytoplankton communities depend<br />
to a large extent upon the rate at whic h<br />
they are supplied with essential inorganic<br />
nutrients and energy sources. Most of these<br />
compounds are introduced from the surrounding<br />
terrestrial environment and the<br />
atmosphere through biological fixatio n<br />
processes . The rate at which a lake is supplied<br />
with allochthonous materials may determin e<br />
its productivity structure . Several mechanisms<br />
may be responsible for determining a lake' s<br />
response to allochthonous nutrient input .<br />
These mechanisms relate both to the suppl y<br />
of nutrients to the phytoplankton and bacteria<br />
communities and to the physical an d<br />
biological forces which influence the production<br />
dynamics of these communities .<br />
1 . Dynamics of release of inorganic nutrients<br />
from allochthonous organic material<br />
of varying nutrient richness : The first indication<br />
is that nutrients in nutrient<br />
poor organic material, e .g., wood, are released<br />
slowly. Since the four lakes in thi s<br />
study can be characterized by the nature<br />
and extent of allochthonous input, thi s<br />
mechanism can be studied .<br />
2. Nutrient availability as a function o f<br />
thermal distribution, circulation dynamics,<br />
and cycling dynamics of other chemical<br />
compounds : Vertical density gradients<br />
(determined by vertical therma l<br />
distribution gradients) can control th e<br />
availability of essential nutrients to autotrophic<br />
organisms . The density gradient s<br />
function as a barrier to the mixing o f<br />
nutrients from deeper waters into th e<br />
productive surface waters . Since the<br />
density barrier also inhibits the passag e<br />
of oxygen from the surface into th e<br />
deeper waters the deeper waters some -<br />
times become depleted of oxygen . Thi s<br />
anerobic condition enhances the solubility<br />
of compounds which bind phosphorus<br />
in forms unavailable to phytoplankton<br />
. Thus, the deep waters may be<br />
rich in nutrients which are relatively unavailable<br />
to autotrophic organisms . Th e<br />
four lakes in this study vary greatly i n<br />
the formation of their density gradient s<br />
and thus their capacity to trap nutrients .<br />
This theory is only partially applicabl e<br />
to any particular lake since there exis t<br />
other mechanisms for distributing nutrients.<br />
The shape of the lake basin, direction<br />
and strength of prevailing winds ,<br />
internal circulation currents, disturbanc e<br />
of the bottom sediments by mechanica l<br />
mixing, and dynamics of nutrient trans -<br />
port through the reduced layer of th e<br />
sediment are all mechanisms which ar e<br />
being studied to bear upon the proble m<br />
of nutrient cycling .<br />
3.Biological cycling of nutrients : Since the<br />
communities of phytoplankton and bacteria<br />
in lakes are often limited by the<br />
availability of essential nutrients they<br />
have tended to evolve elaborate mechanisms<br />
for the conservation and recyclin g<br />
of nutrients. In the absence of these<br />
mechanisms, production would mos t<br />
likely be nil. Nutrients cycle through<br />
communities of phytoplankton, zoo -<br />
plankton, bacteria, protozoans, and<br />
littoral aquatic plants. The nature of<br />
these cycles and how they operate with -<br />
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