Watershed Characteristics
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Transcript Watershed Characteristics
Cayuga Lake Project
Rich Bowen
Jeremy Deans
Jacob Krall
Rami 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
N
<http://www.cayugawatershed.org/Cayuga%20Lake/RPP/caywaterresources.htm>.
Subwatershed
Tributaries:
Cayuga Inlet
Buttermilk
Fall Creek
Virgil
Creek
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
Different Loads of Coliform
Low River
Water Flow Rate
x
High Contaminant
Concentration
= Low Load
→ Impairment close to river input
High River
Water Flow Rate
x
Low Contaminant
Concentration
→ Slow, whole lake deterioration
Chapman, Deborah Water Quality
Assessments 1996; pg 339
= High Load
Sample Collected Information
Data Collected by the NY State
Department of Health
Phosphorous Correlation
Coliform vs Total Phosphorous
Six Mile Creek 9-22-04
y = 472.18x - 1660.2
R2 = 0.8647
40000
Coliform (col/100mL)
35000
30000
25000
20000
15000
10000
5000
0
0
10
20
30
40
50
Total Phosphorous (ug/L)
Data Collected by Six Mile Creek
Watershed Committee
60
70
80
90
Phosphorous Correlation
Coliform vs. Soluble Reactive Phosphorous
Virgil Creek, Owego Hill Road
y = -33.787x + 1984.4
R2 = 0.4195
3000
Coliform (col/100mL)
2500
2000
1500
1000
500
0
0
5
10
15
20
25
30
SRP (ug/L)
Data Collected by Volunteers of Fall
Creek Watershed Committee
35
40
45
Flow Rate Correlation
Total Coliform vs Flow rate
y = 18.948x + 2013.4
Fall Creek (10-18-02 to 7-13-04)
R2 = 0.3523
70000
Coliform (col/100mL)
60000
50000
40000
30000
20000
10000
0
0
200
400
600
800
1000
1200
Flow Rate (ft^3/s)
Data Collected by Volunteers of Fall
Creek Watershed Committee
1400
1600
1800
Precipitation Correlation
E. Coli vs. Precipitation
Fall Creek (11-20-03 to 11-10-04)
y = 963.66x + 157.23
R2 = 0.9627
1600
1400
Coliform (col/100mL)
1200
1000
800
600
400
200
0
0
0.2
0.4
0.6
0.8
1
Percipitation (inches)
Data Collected by Volunteers of Fall
Creek Watershed Committee
1.2
1.4
1.6
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
Seneca Lake
Canandaigua Lake
Cayuga Lake
(Callinan Presentation DEC)
Keuka Lake
Owasco, Skaneateles, Otisco
Lakes
Geographic Information Systems Project
Goals
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’
Further
effect on bacteria
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?