cayuga lake project rich bowen jeremy deans jacob krall rami zahr supervisor: cliff callinan, new...
DESCRIPTION
Watershed Characteristics Part of the Oswego River Basin Drains into Lake Ontario 39.3 miles long, max depth of 435 feet, shoreline of 95.3 miles, average width 1.7 milesTRANSCRIPT
Cayuga Lake ProjectRich Bowen
Jeremy DeansJacob KrallRami Zahr
Supervisor: Cliff Callinan, New York State Department of Environmental Conservation (NYSDEC)
Partner Organization Representative: Ruthanna Hawkins, Cayuga Lake Watershed Network
Cayuga Lake Project Worked with NYSDEC and Cayuga Lake Watershed Network
Problem: Fecal Coliform spikes have long been an issue in Cayuga Lake, necessitating the closing of Stewart Park Beach in 1966
Long-term goal: Fully understand the Coliform spikes and move toward a solution
This semester: Initial data compilation, research, problem definition.
Watershed Characteristics
Part of the Oswego River Basin Drains into Lake Ontario 39.3 miles long, max depth of 435 feet,
shoreline of 95.3 miles, average width 1.7 miles
<http://www.cayugawatershed.org/Cayuga%20Lake/RPP/caywaterresources.htm>.
N
Subwatershed
Tributaries: Cayuga Inlet
Buttermilk Creek Fall Creek
Virgil Creek Cascadilla Creek Six Mile Creek
<http://www.cayugawatershed.org/clwsmap.html>.
Fecal Coliform
Indicator of amount of other potentially harmful pathogens found in warm blooded animals
Pathogen easily measured (e.g. E. Coli) Fecal coliform levels should not exceed
200 col/100mL and total coliform levels 2,400 col/100mL
Possible Sources
Sewage and Municipal Waste
Agricultural Runoff
Wildlife Around Lake
Urban Runoff
Possibly Related to Fecal Coliform
Total Coliform Phosphorous Nitrogen Total Suspended Solids Water Flow Rate (tributaries) Precipitation
Differentiating Between Types of Runoff
Agricultural: Pesticides, mercury, arsenic, & selenium
Urban: Oils & trace metals used in local industry
Sewage: Surfactants and other pathogens
Chapman, Deborah Water Quality Assessments 1996; pg 339
Different Loads of Coliform Low River x High Contaminant Water Flow Rate Concentration = Low Load
→ Impairment close to river input
High River x Low Contaminant Water Flow Rate Concentration = High Load
→ Slow, whole lake deterioration
Data Collected by the NY State Department of Health
Sample Collected InformationIthaca Yacht Club 1984 - 1997 Total Coliform
0
500
1000
1500
2000
2500
3000
3500
4000
Date
Data Collected by Six Mile Creek Watershed Committee
Phosphorous CorrelationColiform vs Total Phosphorous
Six Mile Creek 9-22-04y = 472.18x - 1660.2
R2 = 0.8647
0
5000
10000
15000
20000
25000
30000
35000
40000
0 10 20 30 40 50 60 70 80 90
Total Phosphorous (ug/L)
Col
iform
(col
/100
mL)
Data Collected by Volunteers of Fall Creek Watershed Committee
Phosphorous CorrelationColiform vs. Soluble Reactive Phosphorous
Virgil Creek, Owego Hill Road y = -33.787x + 1984.4R2 = 0.4195
0
500
1000
1500
2000
2500
3000
0 5 10 15 20 25 30 35 40 45
SRP (ug/L)
Col
iform
(col
/100
mL)
Data Collected by Volunteers of Fall Creek Watershed Committee
Flow Rate CorrelationTotal Coliform vs Flow rate
Fall Creek (10-18-02 to 7-13-04)y = 18.948x + 2013.4
R2 = 0.3523
0
10000
20000
30000
40000
50000
60000
70000
0 200 400 600 800 1000 1200 1400 1600 1800Flow Rate (ft^3/s)
Col
iform
(col
/100
mL)
Data Collected by Volunteers of Fall Creek Watershed Committee
Precipitation CorrelationE. Coli vs. Precipitation
Fall Creek (11-20-03 to 11-10-04) y = 963.66x + 157.23R2 = 0.9627
0
200
400
600
800
1000
1200
1400
1600
0 0.2 0.4 0.6 0.8 1 1.2 1.4 1.6
Percipitation (inches)
Col
iform
(col
/100
mL)
Soil
Glacial till (clay, silt, and gravel) Clays are the most effective filter Bacteria are attracted to clay (cation
bridging) Sandy soils have poor retention Bacteria moves faster through coarser
soils
Movement in Soils
Storm water is the main cause of bacteria infiltration into water ways
Cracks in the bed rock increase seepage rate
Water table fluctuations can strand bacteria
Bacteria will die without proper host
Probable Solution
Marshes: cattails, red-stemmed dogwood, arrow-wood, water willow, woolgrass, reed
Intertwining roots, leaves and fibers remove sediment from slow-moving water
Marsh slows down the water and bacteria laden sediment drops out
Marsh plant’s roots and stems stop both surface and subsurface water
Removal
80-90% of sediment is removed by wetlands
65% of sediment never leaves the wetland Provide surfaces for microorganisms
(protozoans) to grow that are predators
Finger Lakes Wetlands
Conesus, Hemlock, Canadice, Honeoye Lakes
Canandaigua Lake Keuka Lake
Seneca Lake Cayuga Lake Owasco, Skaneateles, Otisco Lakes
(Callinan Presentation DEC)
Geographic Information Systems ProjectGoals
Map out sampling points:
DOH data at various sites Fall and Sixmile Creek data taken by Community Organizations USGS gages Others: WWTPs, RUSS Unit Also on map: Land Use data, watershed divisions
Link points on map to data that has been collected.
The map will serve as a tool for future groups working on this project.
Create interactive map on team website?
GIS Map
Summary
What has been done:
Compiled large amounts of data from (DOH, Local WWTPs, Non Profit Orgs)
Begun research into various topics (geology, vegetation, coliform sources, sampling techniques)
Preliminary GIS work
Future Work
Look into DNA analysis
Minerals’ effect on bacteria
Further GIS work
Seasonal population density of migratory birds and
their fecal coliform contribution
Research synthetic wetland construction
More Sources for Data Compilation
Water Treatment Plants
Wastewater Treatment Plants
Cornell Lake Source Cooling
Data Collectors – Thank You
Department of Environmental Conservation – New York State
Department of Health – New York State Six Mile Creek Watershed Committee Monitoring Volunteers for the Fall Creek
Watershed Committee
Special Thanks
Ruthanna Hawkins – Cayuga Lake Watershed Network (WN)
Cliff Callinan – NY State Department of Environmental Conservation
Nicholas Hollingshead (WN) Prof. Ruth Richardson – CEE Prof. Rachel Davidson - CEE
Questions?