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PE EIE[R-Rg RESEARCH ON - HJ Andrews Experimental Forest

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more similar than between the different subsystems<br />

. For example, the processes in the<br />

water column involving exchanges betwee n<br />

nutrients, algae, shortlived zooplankton, and<br />

bacteria can better be handled by a singl e<br />

team than by several teams, each interested i n<br />

a specific trophic level. Further, this information<br />

may have to be handled on a daily o r<br />

hourly basis, whereas the higher consumer<br />

production, e .g., fish, will be handled on a<br />

seasonal basis .<br />

Studies Planned for 1973-74<br />

The individual studies tentatively planne d<br />

for 1973 and 1974 for the four lakes are<br />

shown in table 2 . These are described briefl y<br />

here. The interface study specific to th e<br />

Findley Lake watershed is described in th e<br />

previous paper .<br />

Water Column Process Studie s<br />

The categories and relationships are show n<br />

in figure 8. Much of the past work in th e<br />

Cedar River drainage lakes defined the annua l<br />

nutrient supply to Lake Sammamish an d<br />

Figure 8 . Categories and relationships of sub-syste m<br />

(C)a ; water column processes .<br />

documented its rate of recovery compared t o<br />

that of Lake Washington as a result of nutrient<br />

diversion. Recently, limnological conditions<br />

have been monitored in Chester Mors e<br />

and Findley Lakes to compare their trophi c<br />

character with that of Lakes Sammamish an d<br />

Washington . Ultimate objective is to develop a<br />

model with enough generality to encompas s<br />

the range in trophic character now observabl e<br />

among the lakes .<br />

Lake Washington responded rapidly to a<br />

diversion of over one-half its annual supply o f<br />

phosphorous . Edmondson (1970) has documented<br />

its recovery to a trophic state simila r<br />

to that recorded over 20 years ago in a matte r<br />

of only 3 years after the completion and 7<br />

years after the beginning of sewage diversion .<br />

Lake Sammamish, a mesotrophic lake wit h<br />

similar flushing time, located only 10 miles t o<br />

the east of Lake Washington, has no t<br />

responded noticeably in 3 years following<br />

nutrient diversion . Possible reasons for this<br />

difference in rate of response involve th e<br />

morphometry of the two lakes .<br />

The nutrient input to the lake and the<br />

levels of dissolved inorganic nutrients will b e<br />

related to the growth and production of<br />

phytoplankton and its consumption by zoo -<br />

plankton . These studies will be in sufficient<br />

detail to examine changes in species composition<br />

and the importance of size categories a s<br />

they may relate to optimum feeding strategies.<br />

More detailed, but less frequent estimates<br />

of the flow of carbon through all<br />

components of the food web will be made by<br />

the techniques of Saunders (1969) usin g<br />

radioactive bicarbonate, radioactive detritus ,<br />

and radioactive dissolved organics . Both of<br />

these field-oriented studies will be correlate d<br />

with the modeling on the dynamics of nutrient<br />

distribution and flow through aquatic ecosystems.<br />

A deferred study concerns the rol e<br />

of fungal parasites on algae to explore the<br />

hypothesis that algal blooms may cease<br />

through disease processes, rather than throug h<br />

the limitation of nutrients .<br />

The mathematical models which have been<br />

developed to explain the production dynamic s<br />

of phytoplankton production admit that the<br />

concentration of phytoplankton may vary continuously<br />

from the surface to the lake bottom .<br />

28

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