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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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 />
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