Sources for Bottom Water Phosphates and Suspended Sediments in Southern Cayuga Lake, New York
Prabighya Basnet Hobart & William Smith Colleges Geneva, NY
Sources for Bottom Water Phosphates and Suspended Sediments in - - PowerPoint PPT Presentation
Sources for Bottom Water Phosphates and Suspended Sediments in Southern Cayuga Lake, New York Prabighya Basnet Hobart & William Smith Colleges Geneva, NY Outline of Todays Presentation Introduce Problem Under Investigation
Prabighya Basnet Hobart & William Smith Colleges Geneva, NY
2005 - 2007 Mean Phosphate 2 4 6 8 10 12 H
e
e C a n a n d a i g u a K e u k a S e n e c a C a y u g a O w a s c
k a n e a t e l e s Average Phosphate (SRP, ug/L, P)
2005 Surface 2006 Surface 2007 Surface 2005 Bottom 2006 Bottom 2007 Bottom
– Hypolimnion Phosporus – Upwelled to Surface – Fertilizes Algal Growth – Degrades Water Quality – Especially Southern End
– Cornell’s Lake Source Cooling – Internal Seiche Activity – Waves & Surface Currents
Fluorescence Subsurface Algae Turbidity Surface & Nepheloid
– Suspended Sediments & Phosphates from Runoff Events, esp. in Spring
– Suspended Sediments & Phosphates from Southern Shelf
– Especially in Summer – Bacteria Release SRP
Spring Runoff Events
Photos by Bill Hecht
– Sites 1 & 2 Finger Lakes Survey – Sites B, D, E & G extend mid-lake southward from Site 2
CTD Profile - SeaBird CTD SBE-25 SeaLogger
Profiles of Conductivity, Temperature, pH, Dissolved Oxygen, Turbidity, and Fluorescence
Water Samples
Surface Water Mid Depth (40m above the lake floor) Bottom Water (within a few m of the lake floor)
Onsite Analyses
Vertical and Horizontal Plankton Tow Secchi Disk Depth Conductivity, Temperature & pH Dissolved Oxygen & Alkalinity Titrations
Laboratory Analyses
Total Phosphate (TP) Soluble Reactive Phosphate (SRP) Nitrate Chlorophyll-a Total Suspended Sediments (TSS) Major Ion Concentrations.
Highest After Wind Events May & Early June Profiles Wind & Runoff Events Runoff Event? No Rain Episode Increases - Minimal Accumulation Site 1 Minimal Contribution from Algae
Total Phosphate - 2008
5 10 15 20
1S 1M 1B 2S 2M 2B B/S B/M B/B D/S D/M D/B E/S E/M E/B G/S G/M G/B
Sites TP (P, ug/L)
Dissolved Phosphate - 2008
2 4 6 8 10 12 14 16
1S 1M 1B 2S 2M 2B B/S B/M B/B D/S D/M D/B E/S E/M E/B G/S G/M G/B
Sites SRP (P, ug/L) 2005 - 2008 Mean Phosphate 2 4 6 8 10 12 H
e
e C a n a n d a i g u a K e u k a S e n e c a C a y u g a O w a s c
k a n e a t e l e s O t i s c
2005 Surface 2006 Surface 2007 Surface 2008 Surface 2005 Bottom 2006 Bottom 2007 Bottom 2008 Bottom
2006 - 2008 Mean Total Phosphates 5 10 15 20 25 H
e
e C a n a n d a i g u a K e u k a S e n e c a C a y u g a O w a s c
k a n e a t e l e s O t i s c
2005 No Data 2006 Surface 2007 Surface 2008 Surface 2005 No Data 2006 Bottom 2007 Bottom 2008 Bottom
Large Hypolimnetic SRP Reservoir
2005 - 2008 Mean Chlorophyll-a 1 2 3 4 5 H
e
e C a n a n d a i g u a K e u k a S e n e c a C a y u g a O w a s c
k a n e a t e l e s O t i s c
2005 Surface 2006 Surface 2007 Surface 2008 Surface 2005 Bottom 2006 Bottom 2007 Bottom 2008 Bottom
2005 - 2008 Mean Total Suspended Solids 1 2 3 4 H
e
e C a n a n d a i g u a K e u k a S e n e c a C a y u g a O w a s c
k a n e a t e l e s O t i s c
2005 Surface 2006 Surface 2007 Surface 2008 Surface 2005 Bottom 2006 Bottom 2007 Bottom 2008 Bottom
Chlorophyll-a - 2008
1 2 3 4 5 6 7 8
1S 1M 1B 2S 2M 2B B/S B/M B/B D/S D/M D/B E/S E/M E/B G/S G/M G/B
Sites Chlorophyll-a (ug/L)
Total Suspended Solids - 2008
1 2 3 4 5 6 7 1S 1B 2S 2B B/S B/B D/S D/B E/S E/B G/S G/B Site TSS(mg/L)
2005 - 2008 Mean Secchi Disk Depth 1 2 3 4 5 6 7 8 9 10
H
e
e C a n a n d a i g u a K e u k a S e n e c a C a y u g a O w a s c
k a n e a t e l e s O t i s c
2005 2006 2007 2008
Secchi Disc Depth - 2008
1 2 3 4 5 6 1 2 B D E G Depth (m)
TP vs TSS
R2 = 0.05
5 10 15 20 25 2 4 6 8 10 TSS (mg/L) TP (ug/L)
SRP vs TSS
R2 = 0.01
2 4 6 8 10 12 14 16 2 4 6 8 10 TSS (mg/L) SRP (ug/L)
– Other Sources of Phosphate to Lake? – Missed Early Spring Runoff Contributions? – Primarily Recycled Phosphorus by Bacteria? – High Phosphate in Hypolimnion an Ongoing Problem