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Blue Lake Assessment Limnology Fall 2010. Ian Faurot Elise LaVanaway Scott Paradis Cody Settles. What we know. Small, circular lake with rapid drop-off No inflow, year-round outflow Frozen in winter Abundant population of bullhead ( Ameiurus sp. ) and a stocked rainbow trout population - PowerPoint PPT Presentation
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Blue Lake AssessmentLimnology Fall 2010
Ian FaurotElise LaVanaway
Scott ParadisCody Settles
What we knowSmall, circular lake
with rapid drop-offNo inflow, year-round
outflowFrozen in winterAbundant population
of bullhead (Ameiurus sp.) and a stocked rainbow trout population
Extensive macrophytes
What we want to learnLake classification and originsProductivitySediment compositionHabitat qualityBiological communityPotential concerns
What we need to sampleTo assess Blue Lake, we need
Physical parameters: bathymetric map, irradience, temperature, maximum and mean depth, water and sediment volume, sediment profile and composition
Chemical parameters: total and dissolved phosphorous*, specific conductivity, and dissolved oxygen profiles
Biological parameters: primary production, zooplankton community, littoral and benthic invertebrates
A
B
D
C
Study Area•East side of lake
•4 sampling sites
Methods and Materials: Bathymetry• A boat with a depth finder and GPS was taken in even
transects across the lake, north to south and east to west, to obtain a bathymetric profile
Methods and Materials: Physical properties
Photic zone/irradience
Temperature
Oxygen content
Conductivity
Methods and Materials : Chlorophyll
• Only photic zone sampled
• 3 replicates of integrated samples at our 4 sites
• Chlorophyll calculated with photo-spectrometer BF Environmental Consultants Inc.
Bathymetric Map
Volume – 58877 m3 Sediment volume – 6873 m3 Surface area – 10532 m2
Maximum depth – 10.22 mMean depth - 5.59 mSediment depth - .57m
Photic zoneSecchi depth –
2 m
Li-cor photometer estimate of photic zone – 5.69 m
Extinction coefficient – 0.81
0 20 40 60 80 100 120 1400
1
2
3
4
5
6
7
Irradience
Dep
th
Temperature profileMean
temperature – 8.99 °C
Expect inverse stratification in winter
Direct stratification in summer
5 5.5 6 6.5 7 7.5 8 8.5 9 9.5 100
2
4
6
8
10
12
Temperature (°C)
Dep
th
Dissolved oxygenSomewhat
low for good trout habitat
Potentially a problem with anoxia
0 0.5 1 1.5 2 2.5 3 3.5 40
2
4
6
8
10
12
Dissolved Oxygen (mg/L)
Dep
th
Specific conductivityMeasured in
micro-seimens per cm.
A measure of TDS
200 220 240 260 280 300 320 340 360 380 4000
2
4
6
8
10
12
Conductivity (µS)
Dep
th
Chlorophyll-a Chlorophyll levels
seem moderate
Little significant variation across lake
0
0.5
1
1.5
2
2.5
3
3.5
4
Chl-a concentrations (µg/L)
ABCDAVG
ConclusionsBlue lake formed by glacial activity
Kettle LakeMesotrophic, Dimictic classification
Chlorophyll A 3.16 ± 0.94 µg/LTP: 16.94 ± 10.81 µg/L, SP: 16.73 ± 10.07 µg/LTemp: 8.99 °CDO: 2.93 mg/LOrganic sediment content slightly higher than
mineral content
Recommendations
Avoid input of any fuel, fertilizer, sewage. Reduce levels of bullhead – spawn in lake
Catch and Keep?Continue to stock rainbow trout
Spawning/Trophic CascadeContinue study on lake in spring/summer
Oxygen levels
Literature cited Bettoli, P.W., M.J. Maceina, R.L. Noble, and R.K. Betsill. Response of a
reservoir fish community to aquatic vegetation removal. North American Journal of Fisheries Management 13:110-124.
Gall, G.A.E. and P.A. Crandell, 1992. The rainbow trout. Aquaculture 100:1-10.
Wetzel, R. G. 2001. Limnology - Lake and River Ecosystems (3rd ed) Academic Press.
Wilhelm, F. 2010a. Fish 415 Limnology, Spring Valley Lab Handout. University of Idaho, Moscow, Idaho.
Wilhelm, F. 2010b. FISH 415 Limnology, Zooplankton Identification Lab. University of Idaho, Moscow, Idaho.