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

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Methods<br />

The water column in Lake Sammamish wa s<br />

sampled at 2-week intervals in spring, summer,<br />

and early fall and monthly in winter during<br />

1970 and 1971 . Phytoplankton biomas s<br />

and productivity and nutrient content wer e<br />

determined in samples collected from severa l<br />

depths. Nutrient supply from surface water s<br />

was estimated by monthly sample collectio n<br />

and flow measurements from two major an d<br />

11 minor streams entering the lake .<br />

Primary productivity was determined i n<br />

situ according to procedures described b y<br />

Goldman (1961) . Water samples inoculate d<br />

with C 14 were incubated at four depths for 4<br />

hours and the results reported as integrate d<br />

productivity in the photic zone extrapolate d<br />

to daily rates assuming a 1 :1 relationship with<br />

incident light. Data are reported from on e<br />

centrally located station in each of the lakes .<br />

Methods of Strickland and Parsons (1968 )<br />

were followed for N, P, and Chlorophyll a<br />

(Chl a) analyses in water . Total and orthophosphate<br />

phosphorus were determined spectrophotometrically<br />

as a phosphomolybdat e<br />

complex. Reactive silicate was also deter -<br />

mined from a silico-molybdate complex .<br />

Nitrate and nitrite were determined spectrophotometrically<br />

following reduction in a<br />

cadmium-copper filled column and are reported<br />

together as NO 3 -N. Chl a was determined<br />

with a Turner Model 110 fluorometer .<br />

Cations were determined by atomic absorption<br />

techniques and anions by routine procedures<br />

(American Public Health Associatio n<br />

1971). All analyses except for total P wer e<br />

performed on filtered (0.451.t poresize) water<br />

samples .<br />

Surface sediments (surface to 10-cm depth )<br />

were collected with a Peterson dredge in the<br />

four lakes . Surface sediments in Lake Sammamish<br />

were sampled more extensively (2 6<br />

samples from 26 different depths) than those<br />

of the other three lakes where only four to si x<br />

samples were collected . Analyses for total C ,<br />

N, and P contents of air-dried sediments wer e<br />

performed with procedures of Baker (1970 )<br />

for C, Bremner (1960, 1965) for N, and<br />

Delfino et al. (1969) for P. The phosphomolybdate-ascorbic<br />

acid method of Strickland<br />

and Parsons (1968) was used for the determination<br />

of extracted P . Results are expresse d<br />

on an ovendried (104°C) basis .<br />

Bioassays to determine the limiting nutrient(s)<br />

were conducted in large (0 .21 m z X5m)<br />

plastic cylinders submerged in the lake for 7<br />

days. Nitrogen, P, C, and Si were added t o<br />

experimental bags separately and in combination<br />

. Phytoplankton response was determine d<br />

by daily measurements of productivity rat e<br />

and Chl a concentration . Significance of<br />

response was judged from results of analysi s<br />

of variance using a factorial design and<br />

Dunnett 's test at the 95-percent level of confidence<br />

(Steel and Torrie 1960) . Data are<br />

graphed as integrated values over time to indicate<br />

total production .<br />

Lake Sammamish<br />

Trophic Status<br />

Lake Sammamish is considered mesotrophic<br />

judging from measurements of phytoplankton<br />

productivity, biomass (Chi a), hypolimnetic<br />

oxygen deficit, and concentration s<br />

and loading of N and P . Guidelines for thes e<br />

characteristics are suggested in table 1 fo r<br />

judging the trophic status of a lake . With on e<br />

exception, values for these characteristics i n<br />

Lake Sammamish fall in between ranges typical<br />

of oligotrophy and those of eutrophy . Th e<br />

exception, mean winter ortho PO 4 -P, i s<br />

greater than the level often considered indicative<br />

of subsequent summer nuisance alga l<br />

blooms (Sawyer 1952). Of probably mor e<br />

significance than winter concentration, how -<br />

ever, is annual supply of P . In this regard ,<br />

Lake Sammamish lies clearly between safe<br />

and danger limits of eutrophication, her e<br />

construed to suggest oligotrophy an d<br />

eutrophy, respectively (Vollenweider 1968) .<br />

These ranges of measured characteristic s<br />

are at best only guidelines for judging the<br />

trophic status in lakes . Eutrophication o f<br />

lakes is a complex process and is affected b y<br />

climate, basin morphology and soil type . Differences<br />

in these factors could lead to considerable<br />

inconsistencies in judging trophi c<br />

status using the limited number of characteristics<br />

in table 1 . On the other hand, the<br />

302

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