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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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