Dan Myers Thesis Defense July 17, 2018 Indian Mill Creek - - PowerPoint PPT Presentation
Dan Myers Thesis Defense July 17, 2018 Indian Mill Creek - - PowerPoint PPT Presentation
Dan Myers Thesis Defense July 17, 2018 Indian Mill Creek Northwest side of Grand Rapids Agricultural headwaters Urbanized lower reaches Coldwater trout stream Impaired Altered hydrology and sedimentation (Sigdel
Indian Mill Creek
Northwest side of Grand
Rapids
Agricultural headwaters Urbanized lower reaches Coldwater trout stream Impaired
Altered hydrology and
sedimentation (Sigdel 2017)
Elevation Gradient
Upper Watershed (Agricultural)
Middle Watershed (Urban / Natural)
Lower Watershed (Urban)
Flashy Flows, Eroding Banks, and High Bedload Sediment Transport
Schematic diagram of factors leading to habitat loss in Indian Mill Creek (Source: Sigdel 2017)
Outline
Intro Study #1: Habitat, Fish, and Bugs Study #2: Watershed Modeling Study #3: Streambank Erosion Synthesis and Conclusion Q & A
Study #1
“Impacts of an
Agricultural/Urban Land Cover Gradient in a Coldwater Stream”
DT Myers, RR Rediske, JN McNair, AD Parker, and EW Ogilvie
Objective and Hypothesis
Objective: Assess stream habitat and biological
community integrity across a gradient of agricultural and urban land cover.
Hypothesis: Stream habitat and biological community
structure are correlated with landscape, hydrologic, and geomorphic variables.
Methods
Stream Habitat Survey
Geomorphic units Streambed substrate Woody debris Riparian conditions
Methods
- Sediment Monitoring
Methods
Stream Temperature Loggers
Methods
Macroinvertebrate and Fish Surveys
Procedure 51 Multivariate Statistics
Streambed Substrate Results
Site Median Particle Size (mm) Median Particle Type Richmond Park 5-8 Fine Gravel Sharp Dr. (Lower) 33-64 Very Coarse Gravel Sharp Dr. (Upper) 17-32 Coarse Gravel Scout Pavilion 0.26 - 0.50 Medium Sand Five Mile Rd. 0.06 - 0.125 Very Fine Sand West Branch 0.26 - 0.50 Medium Sand East Branch 0.126 - 0.25 Fine Sand Blandford Nature Center 0.26 - 0.50 Medium Sand Walker Ditch <0.06 Silt / Clay
Lower Reaches Headwaters Tributaries
Sediment Loading Results
Lower Reaches Headwaters Tributaries
Site Suspended load (kg day-1) Bedload (kg day-1) Richmond Park 523 2,687 Sharp Dr. (Lower) 110 233 Sharp Dr. (Upper) 120 9 Scout Pavilion 110 112 Five Mile Rd. 36 61 West Branch 7 31 East Branch 16 33 Blandford Nature Center 5 86 Walker Ditch 1 13
Procedure 51 Fish Results
Site Total Score Fish Community Rating Turner Ave.
- 1
Poor (<50 fish) Richmond Park (Tamarack)
- 5
Poor (<50 fish) Richmond Park (Dam)
- 4
Poor (<50 fish) Sharp Dr. (Lower)
- 2
Poor (<50 fish) Sharp Dr. (Upper)
- 5
Poor 3 Mile Road
- 4
Acceptable Scout Pavilion
- 8
Poor
Lower Reaches Middle Reaches
Procedure 51 Macroinvertebrates
Site Total Score Macroinvertebrate Rating Richmond Park
- 4
Acceptable Sharp Dr. (Lower)
- 6
Poor Sharp Dr. (Upper)
- 2
Acceptable Scout Pavilion
- 4
Acceptable 5 Mile Rd.
- 6
Poor West Branch
- 8
Poor East Branch
- 4
Acceptable Blandford Nature Center
- 3
Acceptable Walker Ave. Ditch
- 5
Poor
Lower Reaches Headwaters Tributaries
Study #1 Major Findings
Aquatic habitat, fish, and macroinvertebrate
communities are degraded throughout the watershed
Fine substrate in the streambed has the strongest
association with degraded macroinvertebrate communities
Study #2
“Watershed and
Streambank Erosion Modeling in a Michigan, USA Stream Using the GWLF-E Model and MapShed GIS Plugin”
DT Myers, RR Rediske, JN McNair, and ME Allen
Objective and Hypothesis
Objective: Spatially assess runoff, field erosion, and
streambank erosion in the Indian Mill Creek watershed using a model.
Hypothesis: Agricultural areas in the upper watershed
contribute the most sediment from field erosion, urban areas in the lower watershed have the highest streambank erosion rates, and the model reliably estimates stream discharge.
GWLF-E Model (Evans et al. 2003)
Enhanced Generalized Watershed Loading Functions Mid-complexity Validated with Pennsylvania watersheds Appropriate because we are more interested in spatial
patterns than numerical targets
Model runoff, sediment loading, and streambank
erosion in 20 subbasins from 1997-2015
GWLF-E Model
GWLF-E Runoff
Flashy Flows by Outlet
Discharge Estimate Evaluation
GWLF-E Field Erosion
GWLF-E Streambank Erosion
Where Does the Sediment Go?
Watershed degradation
Habitat Fish Macroinvertebrates
Out to the Grand River
Eroding Banks Throughout!
Study #2 Major Findings
The GWLF-E model predicts high proportions of
runoff in urban areas, like Brandywine Creek, and high field erosion rates with steep slopes and erodible soils.
Streambank erosion is a major contributor to sediment
loading in lower subbasins of Indian Mill Creek and more research is needed about it.
Study #3
“Measuring Streambank
Erosion: A Comparison
- f Erosion Pins, Total
Station, and Terrestrial Laser Scanner”
DT Myers, RR Rediske, and JN McNair
Objective and Hypothesis
Objective: Compare three techniques to measure bank
erosion (erosion pins, total station, and laser scanner), then assess the spatial patterns and compare results with GWLF-E model.
Hypothesis: The three techniques will provide
significantly different estimates of streambank erosion due to their abilities to detect spatial differences. Also, measurements will be higher than GWLF-E predictions.
Study Design
Nine sites 18 study banks
Laser scans at 10
Variety of conditions
Vegetation Erosion or deposition
Measurements May 2017
to May 2018
Compared with
statistical tests
Erosion Pins, Total Station, and Laser Scanner
Laser Scanning
Significance Testing
Normal distribution
Shapiro Wilk Tests
ANOVA Random Block
Design
No detectable
differences between technique
df=2, f=0.457, p=0.639
Pearson Test for Correlations
Erosion pins and total station [A]
Not significant (R2=0.26, p=0.165)
Erosion pins and laser scanner [B]
Not significant (R2=0.16, p=0.289)
Total station and laser scanner [C]
Significant (R2=0.79, p=0.001)
- 0.10
0.00 0.05
- 0.2
0.0 0.2 0.4 Erosion Pins (m^3 / m / yr) Total Station (m^3 / m / yr)
- 0.10
0.00 0.05
- 0.03 -0.01
0.01 0.03 Erosion Pins (m^3 / m / yr) Laser Scanner (m^3 / m / yr)
- 0.2
0.0 0.2 0.4
- 0.03 -0.01
0.01 0.03 Total Station (m^3 / m / yr) Laser Scanner (m^3 / m / yr)
[A] [B] [C]
Percent Difference
Resop and Hession 2010 Erosion pins and total
station
650%
Laser scanner and
erosion pins
596%
Laser scanner and total
station
1,275%
Comparison of Techniques at Sites
Average Laser Coverage of Bank
No heavy vegetation
32.5%
Heavy vegetation
11.75%
Significantly different
P = 0.047
Tree roots also cause
data gaps
Laser Scan Coverage
Complex Banks
Bank Erosion in Watershed
East Branch (Headwaters)
Streambed dominated
by fine sand
GWLF-E predicts low
bank erosion
Surveys show some of
the highest bank erosion rates
Sharp Drive (Middle Reaches)
High gradient Severe bank erosion Coarser substrate
Richmond Park (Near Outlet)
GWLF-E predicts
highest bank erosion
Surveys show net
deposition of sediment
- n banks
Degraded fish
community
Estimation of Sediment Loading
GWLF-E estimate
Field erosion = 5,078 Mg yr-1 Bank erosion = 1,031 Mg yr-1
Erosion pin estimate
Bank erosion = 2,020 Mg yr-1 28% of total load
Study #3 Major Findings
Differing results between techniques could be due to a
combination of vegetation, undercut banks, and coverage; choice of technique is important.
Streambank erosion is a major contributor to sediment
loading which affects the quality of aquatic habitat, fish, and macroinvertebrate communities in the Indian Mill Creek watershed.
Synthesis
Land Cover Change Degraded Aquatic Habitat Increased Runoff and Sediment Loading Sediment from Eroding Streambanks Impaired Fish and Macroinvertebrates
Management Recommendations
Controlling runoff is
most important! (Walsh et al. 2005)
Restore creek to more
natural timing and volume of flows
Intense storm flows
constrain aquatic communities
Controlling Runoff
Urban low impact
development
Bioretention basins Pervious pavement Reduction in impervious
surface area
Agricultural conservation
practice standards
Riparian cover Filter strips Cover crops
Check Out Our Blog! Indianmillstudy.wordpress.com
Thank You!
Coauthors
Dr. Rick Rediske Dr. Jim McNair Aaron Parker Wendy Ogilvie Matt Allen
Funders
Annis Water Resources Institute GVSU Graduate School Lower Grand River Organization of
Watersheds
Assistance
Matt Allen Noah Cleghorn John Koches Dr. Eric Snyder Rachel Frantz Dana Strouse Eileen Boekestein Carlos Calderon Rajesh Sigdel Brian Scull Amanda Chambers Matt Claucherty Kurt Thompson Molly Lane Gene and Mary Dewys Jake Gardner