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Kite Hill Stormwater
Management
C. Bury, J. Davis, A. Hough, R. Middlewarth, J. Ossorio
Clemson University - Biosystems Engineering
BE 4750 Fall 2015 Senior Design Presentation
November 23, 2015
http://www.clemson.edu/public/hunnicutt/about.html
Recognition of Problem
Stormwater runoff from Kite Hill and Kite Hill parking lot
resulting in:
● Erosion
● Pollution transportation
● Destruction of downstream ecology of Hunnicutt Creek
watershed
Photo Credit: Conor Bury, 2015
Photo Credit: Conor Bury, 2015
Photo Credit: Conor Bury, 2015
Photo Credit: Conor Bury, 2015
Define Problem
Lack of infiltration
Pollution runoff
Damage to Hunnicutt Creek
Goals of the Project
The goal of this project is to biologically treat stormwater runoff, and
increase infiltration back into the ground to improve the water quality of
the downstream watershed of Hunnicutt Creek.
● Reduce peak flow rates
● Slow velocity
● Improving quality
○ Reducing soil erosion
○ Treating pollution
■ Microbiological and Phytological processes
■ Physical mechanical filtration and ionic exchange capacity
within the soil layers itself
Constraints and Considerations
Constraints
Existing Infrastructure
Future Construction
Theoretical data/ Experimental Data
Multiple advisors
Budget
http://fisheyestudios.com/gallery-categories/aerial/
Considerations
Safety
Entering for maintenance
Safety around the area
Prohibiting pollution to groundwater
Sustainability
Self-sustaining
Biological Filtration
Possible Implementation
MS4 Regulations
Riparian Corridor Master Plan
Aesthetics
3 Questions
User - Clemson University
1. Is this going to limit where people can park on campus?
2. How much maintenance is required? What does this entail?
3. Will the design be aesthetically pleasing?
4. What reduction of runoff can be expected?
Client - Clemson University Facilities, Subcontractor/Developer, Stormwater Project Team
1. Can the design system elements be implemented at different times?
2. What is the approximate cost of the design and installation of the project?
3. What is the expected lifetime of the structures and systems being proposed?
Designer - Stormwater Project Team
1. What regulations must we work within?
2. Is the design system resilient?
3. What funding is available for this project? What requirements would need to be met for this design to be implemented?
http://nypost.com/2014/09/24/frat-activities-banned-at-clemson-university/
Source: Basemap: Google Maps; Highlighted Areas: J. Davis
Elements of Design
● Kite Hill Erosion Control
● Parking Lot Median
BMPs
● Enhanced Swale
● End of Pipe BMPs
Basemap: Google Maps; Highlighted Areas: J. Davis
Sub-Goals of Hill Redesign
1.Reduce Erosion from Kite Hill by 75%
per yr
2.Reduce Runoff Volume by 50 % for a
25 yr- 24 hr storm
3.Safe Driving Option: Gameday parking
Area
Section
Area of Section
(m2)
Slope
Percent
1 394 14 %
2 272 20 %
3 560 12 %
4 828 11.5 %
5 1052 9.5 %
6 479 19 %
7 1101 8.2 %
8 642 17 %
9 423 5 %
10 290 18 %
Source: Basemap: Google Maps; Area Analysis: J. Ossorio
Area of Interest Defined
Universal Soil Loss Equation
T= R*K*LS*C*P
R- Rain factor = 250 (Pickens, SC)
K- Soil Erodibility Factor = 0.17 (Web Soil Survey)
C- Cropping Factor = 0.01 (For complete Meadow)
P- Conservation Practice = 1 (Assume not preventive practice)
LS- Length Slope Factor = (Calculated separately for each area)
Area
Section
Length Slope
Factor
1 2.5
2 2.7
3 2.2
4 2.5
5 1.3
Estimated Soil Loss
T=(250)*(.17)*(.01)*(1)*(22.6) = 9.5625 tons/ acre/ year
9.5625 tons/ acre/ yr *1.54 acres = 14.726 tons =
13.36 metric tonnes of SOIL LOSS per year
Area
Section
Length Slope
Factor
6 3
7 1.1
8 3.5
9 0.7
10 3.1
Photo Credit: Conor Bury, 2015
Runoff Volume Estimates
Soil-Cover Complex Method
CN- Curve Number= 61 (Urban Area Grass Cover Open Area, HSG B, <75% grass cover)
P- Rainfall for 25 yr -24 hr storm = 6.77 in (Rain Data obtained from Tony Putnam)
S- Surface Storage
Q- Runoff
Vr- Volume of Runoff
S = (1000/CN)-10 = 6.39 in
Q= (P - 0.2S)2/(P + 0.8S) = 2.538 in of runoff
Vr = 2.538 in * (1.54 acres) = 21,850 ft3 =
618.7 m3 of Runoff during a 25 yr - 24 hr storm
Photo Credit: Conor Bury, 2015
Runoff Flow Rate Estimates
Peak Runoff Rate
Qp = qp*A*Q
Q = 2.538 in
S = 6.39 in
tL= L0.8(S +1) 0.7/(1900γ0.5)
tc = tL/0.6
Area
Section
Flow
Length
(ft)
Slope
(%)
tC
(min)
qp
(cfs/acre-in)
qp *A
(cfs/in)
1 256 14 4.8 1.8 0.18
2 155 20 2.7 2 0.2
3 282 12 5.6 1.6 0.224
4 325 11.5 6.4 1.5 0.30
5 360 9.5 7.7 1.4 0.364
Area
Section
Flow
Length
(ft)
Slope
(%)
tC
(min)
qp
(cfs/acre-in)
qp *A
(cfs/in)
6 252 19 4.1 1.85 0.222
7 450 8.2 9.8 1.3 0.351
8 330 17 5.6 1.6 0.256
9 411 5 11.8 0.8 0.08
10 375 18 5.8 1.6 0.16
Weighted qp = 1.517 (cfs/ac-in)
Qp= (1.517 cfs/ac-in *2.538 in *1.54 ac = 5.93 cfs
= 0.168 m3/s is the FLOW RATE of Runoff during a 25 yr -24 hr Storm
Design Option 1: Terracing with Existing
Driveway at Recycling Center
SDR- Soil Delivery Ratio = 14 %
LS for 60 ft - 13% = 3
LS for 15 ft - 13% = 1
3 = 9.5625 ton/ac/yr
1 = (⅓) * 9.5625 ton = 3.1875 tons per terrace
Source: Basemap: Google Maps; Area Analysis: J. Ossorio
3 - 15 ft Terraces have the potential to reduce Soil Loss
per year from 9.5625 ton/ ac to 0.518 ton/ac, a 95 %
reduction in erosion.
Terrace Designs that encourage more
infiltration and velocity reductions
Design Option 1: Terracing with Existing
Driveway at Recycling Center
Source: Basemap: Google Maps; Area Analysis: J. Ossorio www. intechopen.com
Driveway already exists, but the proposal is to
allow access to this entrance after hours by
changing Recycling Center enclosure
Design Option 2: Create an entrance
driveway to Kite Hill
Driveway allows for safe maneuvering on
and off of Kite Hill
The Paved Area should mimic current
runoff behaviors
Permeable
Surface Storage (S) 6.39 in/ac and Q =
2. 538 in 25 yr- 24 hr to avoid runoff
increase
Asphalt
Has Surface Storage (S) of 0.204 in
[CN = 98] and Q = 6.538 in
Need to decrease curve number of
other areas to compensate
Overall Runoff increased from
2.54 in to 2.94 in
Source: Basemap: Google Maps; Area Analysis: J. Ossorio
Design Option 2: Create an entrance
driveway to Kite Hill
Erosion Control (Goal: Reduce by 75%)
Universal Soil Loss
T=R*K*LS*C*P
P: The addition of a Conversation
practice like contouring can reduce
on a slope of 9-12 %
P factor will decrease from 1 to
0.60 for that area
LS: The factor will decrease because
the slope % will need to be cut down
to 12% or less a safe drive
C: Heavier vegetation (erosion control
covers) can be added on sides to
allow for less erosion
Runoff Velocity and Volume (Reduce
Volume by 50%)
Soil-Cover Complex Method
CN: By implementing different land cover
with lower Curve Numbers can reduce the
volume and velocity
Peak Runoff Rate
S: To implement the driveway the % slope
will be decreased, which will help slow
velocities
Kite Hill Erosion Reduction
Design Comparison
Option 1
Pros
-Reduce erosion significantly
-Preserve green space of Kite Hill
-Potential to slow velocity and reduce runoff
-Discourages driving up side of Kite Hill
Cons
-Expensive Soil Conservation Practice
-Construction and Maintenance of terraces
-Failure to maintain terraces can result in
degradation of bench (possible landslide)
-Adds heavy traffic volume at the Recycling
Center
Option 2
Pros
-Allows for two entrances for heavy traffic
-Reduce Erosion with implementations
-Allows for safer travel up side of Kite Hill
Cons
-Driveways require slope % of 12 % or less for
safety
-Require extensive cut and fill into the Hill
-If driveway is permeable, extra maintenance to
prevent clogging of the pores
-Reinforce permeable pavement
-May increase runoff velocity
Flow Diversion Techniques
Flow Diversion Options:
Concrete cut with apron & stabilization
Grated Trench Drain
Flow Diverting Speed Bumps
Must handle QR=0.168 m3/s
Photo Credit: Conor Bury, 2015 Source: Basemap: Google Maps; Area Analysis: R. Middleswarth
Curb Cut with Apron
Divert flow into swale
Must set stabilizers and apron
Concrete
GCL
Erosion Mat
May disturb swale function
Source: www.lastreetblog.org
Photo Credit: Conor Bury, 2015
Grated Trench Drain
Q=(k*A*R2/3*S1/2)/n
Q- volumetric flowrate
A- cross sectional area of drain
R - Hydraulic Radius
S- Slope
n - coefficient of friction
Source: www.trenchdrainsupply.com
Source: www.lastreetblog.org
Enhanced Swale Design
500ft stretch options:
Grassy Swale
Riprap Swale
Check Dam Swale
Source: Basemap: Google Maps; Area Analysis: R. Middleswarth
Trapezoidal Swale
Used for unlined channels because of side
slope stability
Easy to cut grass and maintain
Large surface area for infiltration
Enhanced Grassy and Rocky Swale
Q=(k*A*R2/3*S1/2)/n
Q- volumetric flowrate
A- cross sectional area of drain
R - Hydraulic Radius
S- Slope
n - coefficient of friction
For soil group B reduction
- TSS = 60%
- TP = 32%
- TN = 36%
Source: www.bae.ncsu.edu
Source: www.bae.ncsu.edu
Enhanced Grass Swale
V=Q/A
V - velocity (m/s)
Q - Peak Flow rate (m3/s)
A - Cross-sectional area (m2)
Factors affecting velocity include:
- Manning’s coefficient n
- Cross-sectional area
- Slope
- designed hydraulic radius
Source: www.bae.ncsu.edu
Enhanced Rock Swale
Rip-rap lined swales have varying n values
Source: www.bae.ncsu.edu
Check Dam Design
Primary Design Benefits:
Soil Erosion
Sediment Control
Total Suspended Solids (TSS)
Flow Attenuation
Secondary Benefits:
Runoff Volume Reduction
Phosphorous
Nitrogen
Heavy Metals
Floatables
BOD
Source: www.riverlink.org
Check Dam Design
33 ft intervals @ 6% slope
⅓ - ⅔ of the swale depth
~66% slope on upstream side of dam
Acts as terracing to reduce sedimentation and
velocity
Flow Through a dam
Q = h1.5/(L/D + 2.5 + L2)0.5
L = (ss)*(2d - h)
Q- flow rate exiting check dam
h - flow depth
L - length of flow
D - average stone diameter in feet
ss - check dam side slope (maximum 2:1)
d = height of dam
McMillan Road Enhanced Swale
Design Comparison
Check Dams
Pros
- Inexpensive
- Reduces erosion and sediment transport
- Allows infiltration
- May discourage illegal parking
Cons
- Requires periodic repair and sediment
removal
- Allows infiltration
- Doesn’t treat oils
Grassy / Riprap Swale (dry)
Pros
- Simple Installation
- Easy Maintenance
- Aesthetically Pleasing
Cons
- May form rills
- Higher velocity
- Less treatment and infiltration than other
methods
Alternatives
Sources: www.austintexas.gov
Source: www.thisoldhous.com
Source: www.lakesuperiorstreams.com
Sub-Goals of Median Redesign
1.Reduce the Velocity of Runoff
2.Allow Infiltration into Medians
3.Prevent Sediment Loss
Area of Interest Defined
Parking Lot Medians
123
4
5
6
7
Area
(m2)
Slope (%)
H.
Slope (%)
V.
1 385.11 10.8 1.0
2 613.41 4.2 0.9
3 923.9 6.7 0.8
4 929.79 6.1 1.0
5 735.48 6.4 1.2
6 695.93 5.9 1.4
7 601.01 5.0 1.6
Source: Google Maps
Design 1 - Vegetated Filter Strip
Manning’s Equation
V = (k/n)*Rh
(⅔)*So
(½)
k: coefficient to convert units
k = 1.486 (US Customary Units)
n: Gauckler-Manning’s coefficient
short vegetation - 2 to 6 inches: 0.04
tall vegetation - 12 to 24 inches: 0.08
Rh: hydraulic radius - Rh = areaCS/wetted
perimeter
So: slope of channel length bed
Parabolic Channel Design
Slope
V (short veg
12”) f/s
V (short veg
6”) f/s
V (tall veg 12”)
f/s
V (tall veg 6”)
f/s
1 0.01 0.330 0.083 0.165 0.041
2 0.009 0.297 0.074 0.149 0.037
3 0.008 0.264 0.066 0.132 0.033
4 0.01 0.330 0.826 0.165 0.041
5 0.012 0.396 0.099 0.198 0.49
6 0.014 0.462 0116 0.231 0.058
7 0.016 0.528 0.132 0.264 0.066
Design 1: Vegetated Filter Strip
Excavation - cut and fill using paversCurb cuts versus
curb stops
http://www.lowes.com/Outdoors/Pavers-Retaining-Walls/_/N-
1z0wgaf/pl
http://www.publicdomainpictures.net/view-
image.php?image=3409&picture=parking-lot
http://www.estuarypartnership.org/sites/default/files/fieldguide/e
xamples/swale.htm
http://www.hrwc.net/stormwat
erbmps.htm
Vegetated Filter Strip
Soil - gravel layer
Plants http://www.clemson.edu/psapublishing/pa
ges/HORT/IL87.PDF
http://www.watershedmanagement.vt.gov/stormwater/htm/sw_gi_bmp_bioretention.htm
http://www.emuseum.org/alcoa-foundation-outdoor-classroom
Design 2 - Erosion Mat
Coconut Fiber Mat
Vegetation
Live stakes
T= R*K*LS*C*P
R- Rain factor = 250 (Pickens, SC)
K- Soil Erodibility Factor = 0.17 (Web Soil Survey)
C- Cropping Factor = 0.01 (For complete Meadow)
P- Conservation Practice = 1 (Assume not preventive practice)
LS- Length Slope Factor
- For the steepest slope - Control Mat 40 (Granite Environmental)
- 80% efficiency of sediment removal
http://www.in.gov/legislative/iac/20120404-IR-312120154NRA.xml.html
Erosion Mat
Permeable Pavement
Miscanthus Grass
http://www.in.gov/legislative/iac/20120404-IR-
312120154NRA.xml.html
http://www.vwrrc.vt.edu/swc/NonPBMPSpecsMarch11/VASWMBMPSpec7PERME
ABLEPAVEMENT.html
http://www.hgtvgardens.com/flowers-and-plants/maiden-grass-
miscanthus-sinensis-morning-light
Medians
Design Comparison
Option 1
Pros
-Reduce sediment, pollutants and velocity of
stormwater
-Allow more time for infiltration of stormwater
-Adds more green area to Kite Hill (aesthetically
pleasing)
Cons
-Steep slope adds more complex issue
-Maintenance
-Failure of pavers
Option 2
Pros
-Allows for more infiltration
-Reduce erosion with vegetated mat
Cons
-Failure of permeable pavement
-Sediment clogging
-Anaerobic issues
-4 to 6 year life span
-Pollutant removal
-Maintenance
End of Pipe “Solutions”
● Upstream reductions are not enough
● Most common designs are:
○Detention Basin
○ Retention basin
■ Submerged gravel wetland
Detention Pond
● Reduce peak flows
● Little filtration
● Little to no pollutant
conversion
Source: https://stormwater.files.wordpress.com/2009/05/img_4745.jpg?w=640
Retention Pond
Source: http://water.epa.gov/scitech/wastetech/upload/2002_06_28_mtb_wetdtnpn.pdf
Settling Velocities
Stokes Law for settling velocities:
where,
VS: settling velocity VP: volume of particle
ρP: density of particle CD: drag coefficient
ρ: density of fluid AP: surface area of particle
g: gravitational constant
Settling Velocities cont.
To get the VP and AP,
Approximated particle geometry as sphere
Found mean particle diameter (d50) for Cecil Sandy Loam
(low: 0.2 cm, high: 7.4 cm; Source: Web Soils Survey)
Low end value used to determine minimum settling velocity
Calculated mean particle volume (4/3·𝜋·r3) and surface area (4·𝜋·r2)
VPmin = 0.004189 cm3 APmin = 0.125664 cm2
Settling Velocities cont.
To get the ρP, ρ, and CD,
An average soil particle density value: 2.66 g/cm3
Assuming pure water at 4oC and 1 atm: 1 g/cm3
CD can be determined experimentally or using representative values
Unfortunately this value can change dramatically depending on
the number of particles falling
the true particle geometry
aggregate particles vs single particles
turbulence generated by mass particles falling
Settling Velocities cont.
Given the high level of variability,
SCDOT Stormwater Manual
Reports Cecil as d15 = 0.0066 ~ 0.0043 mm
If d15 < 0.01 mm, use simplified Stokes,
Vs = 2.81·d2
where,
d = particle diameter in mm
Vs = settling velocity in ft/s
Settling Velocities cont.
SCDOT Stormwater Manual
Reports Cecil ranging in particle sizes as 0.001 ~ 1.4 mm,
Vs = 2.81·(0.001)2 ≈ 2.81·10-6 ft/s ≈ 8.56·10-7 m/s
Vs = 2.81·(1.4)2 ≈ 5.51 ft/s ≈ 1.68 m/s
Sizing a basin is not enough.
Vegetation, microbial, and aggregate filtration necessary.
Filtration
Source:
http://www.deq.state.or.us/wq/stormwater/do
cs/nwr/biofilters.pdf
Source: J. Davis
Submerged Gravel Wetland
http://www.neiwpcc.org/neiwpcc_docs/GravelWetlandNutrientCyclingFinalReport3-31-10.pdf
Rational Equation for Peak
Discharge:
Q = ciA
Where,
Q = peak discharge [cfs]
c = runoff coefficient
i = rainfall intensity [in/d]
A = area [acres]
Five year design storm:
Q = (0.8)(4.73in/d)(4.15ac)
Q = 293GPM
Sustainability Measures
● Economical
○ Feasibility
○ Maintenance
○ Location
● Ecological
○ Improving Stream Health
● Social
○ Educational
■ Foundation in Clemson’s
Will
■ Biosystems Engineering
● Ethical Considerations
○ Solving the problem without
damage to downstream http://cantov.deviantart.com/art/Clemson-University-Still-Water-145243984
Time Line
References
Jurries, Dennis, P.E. “Biofilters For Storm Water Discharge Pollution Removal”. Department of Environmental Quality. State of Oregon. 2003. PDF.
<.http://www.deq.state.or.us/wq/stormwater/docs/nwr/biofilters.pdf> Accessed 7 August 2015.
Mey, Gerald Vander. et. al. “Riparian Corridor Master Plan”. Campus Planning Services. Clemson University. December 2006. PDF.
<http://www.clemson.edu/public/hunnicutt/documents/riparian_corridor_master_plan.pdf>
Google Maps. Accessed 13 August 2015.
Ruhlman, Melanie. President, Save Our Saluda. Personal communication. 12 August 2015.
Murphree, Brian Frank, P.E. et. al. MS 4 Outfall Inspections and Evaluation, Clemson University. Project No. 1505. Design South Professionals, Inc. July 2015.
Dorren, Luuk, and Freddy Rey. "A Review of the Effect of Terracing on Erosion." SCAPE: Soil Conseveration and Protection for Europe (n.d.): 97-108. Web. 15 Oct. 2015.
Widomski, Marcin K. "Terracing as a Measure of Soil Erosion Control and Its Effect on Improvement of Infiltration in Eroded Environment." Ed. Danilo Godone. Soil Erosion
Issues in Agriculture (2011): 315-34. InTech. Web. 15 Oct. 2015. <http://www.intechopen.com/books/soil-erosion-issues-inagriculture/ terracing-as-a-measure-of-soil-
erosion-control-and-its-effect-on-improvement-of-infiltration-in-erod>.
Watershed Hydrology and Small Catchments, BE3220. Owino, T, PhD. Clemson University. Spring 2015.
http://www.erosionpollution.com/support-files/coir_geotextiles_specification.pdf
http://water.epa.gov/scitech/wastetech/upload/2002_06_28_mtb_wetdtnpn.pdf
http://www.unh.edu/unhsc/sites/unh.edu.unhsc/files/pubs_specs_info/unhsc_gravel_wetland_specs_6_09.pdf
http://www.unh.edu/unhsc/sites/unh.edu.unhsc/files/presentations/NJASLA%20subsurface%20gravel%20wetland.pdf
http://sfrc.ifas.ufl.edu/urbanforestry/Resources/PDF%20downloads/Rushton_2001.pdf

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Kite Hill Stormwater Management Design

  • 1. Kite Hill Stormwater Management C. Bury, J. Davis, A. Hough, R. Middlewarth, J. Ossorio Clemson University - Biosystems Engineering BE 4750 Fall 2015 Senior Design Presentation November 23, 2015
  • 3. Recognition of Problem Stormwater runoff from Kite Hill and Kite Hill parking lot resulting in: ● Erosion ● Pollution transportation ● Destruction of downstream ecology of Hunnicutt Creek watershed
  • 4. Photo Credit: Conor Bury, 2015
  • 5. Photo Credit: Conor Bury, 2015
  • 6. Photo Credit: Conor Bury, 2015
  • 7. Photo Credit: Conor Bury, 2015
  • 8. Define Problem Lack of infiltration Pollution runoff Damage to Hunnicutt Creek
  • 9. Goals of the Project The goal of this project is to biologically treat stormwater runoff, and increase infiltration back into the ground to improve the water quality of the downstream watershed of Hunnicutt Creek. ● Reduce peak flow rates ● Slow velocity ● Improving quality ○ Reducing soil erosion ○ Treating pollution ■ Microbiological and Phytological processes ■ Physical mechanical filtration and ionic exchange capacity within the soil layers itself
  • 10. Constraints and Considerations Constraints Existing Infrastructure Future Construction Theoretical data/ Experimental Data Multiple advisors Budget http://fisheyestudios.com/gallery-categories/aerial/ Considerations Safety Entering for maintenance Safety around the area Prohibiting pollution to groundwater Sustainability Self-sustaining Biological Filtration Possible Implementation MS4 Regulations Riparian Corridor Master Plan Aesthetics
  • 11. 3 Questions User - Clemson University 1. Is this going to limit where people can park on campus? 2. How much maintenance is required? What does this entail? 3. Will the design be aesthetically pleasing? 4. What reduction of runoff can be expected? Client - Clemson University Facilities, Subcontractor/Developer, Stormwater Project Team 1. Can the design system elements be implemented at different times? 2. What is the approximate cost of the design and installation of the project? 3. What is the expected lifetime of the structures and systems being proposed? Designer - Stormwater Project Team 1. What regulations must we work within? 2. Is the design system resilient? 3. What funding is available for this project? What requirements would need to be met for this design to be implemented? http://nypost.com/2014/09/24/frat-activities-banned-at-clemson-university/
  • 12. Source: Basemap: Google Maps; Highlighted Areas: J. Davis
  • 13. Elements of Design ● Kite Hill Erosion Control ● Parking Lot Median BMPs ● Enhanced Swale ● End of Pipe BMPs Basemap: Google Maps; Highlighted Areas: J. Davis
  • 14. Sub-Goals of Hill Redesign 1.Reduce Erosion from Kite Hill by 75% per yr 2.Reduce Runoff Volume by 50 % for a 25 yr- 24 hr storm 3.Safe Driving Option: Gameday parking
  • 15. Area Section Area of Section (m2) Slope Percent 1 394 14 % 2 272 20 % 3 560 12 % 4 828 11.5 % 5 1052 9.5 % 6 479 19 % 7 1101 8.2 % 8 642 17 % 9 423 5 % 10 290 18 % Source: Basemap: Google Maps; Area Analysis: J. Ossorio Area of Interest Defined
  • 16. Universal Soil Loss Equation T= R*K*LS*C*P R- Rain factor = 250 (Pickens, SC) K- Soil Erodibility Factor = 0.17 (Web Soil Survey) C- Cropping Factor = 0.01 (For complete Meadow) P- Conservation Practice = 1 (Assume not preventive practice) LS- Length Slope Factor = (Calculated separately for each area) Area Section Length Slope Factor 1 2.5 2 2.7 3 2.2 4 2.5 5 1.3 Estimated Soil Loss T=(250)*(.17)*(.01)*(1)*(22.6) = 9.5625 tons/ acre/ year 9.5625 tons/ acre/ yr *1.54 acres = 14.726 tons = 13.36 metric tonnes of SOIL LOSS per year Area Section Length Slope Factor 6 3 7 1.1 8 3.5 9 0.7 10 3.1 Photo Credit: Conor Bury, 2015
  • 17. Runoff Volume Estimates Soil-Cover Complex Method CN- Curve Number= 61 (Urban Area Grass Cover Open Area, HSG B, <75% grass cover) P- Rainfall for 25 yr -24 hr storm = 6.77 in (Rain Data obtained from Tony Putnam) S- Surface Storage Q- Runoff Vr- Volume of Runoff S = (1000/CN)-10 = 6.39 in Q= (P - 0.2S)2/(P + 0.8S) = 2.538 in of runoff Vr = 2.538 in * (1.54 acres) = 21,850 ft3 = 618.7 m3 of Runoff during a 25 yr - 24 hr storm Photo Credit: Conor Bury, 2015
  • 18. Runoff Flow Rate Estimates Peak Runoff Rate Qp = qp*A*Q Q = 2.538 in S = 6.39 in tL= L0.8(S +1) 0.7/(1900γ0.5) tc = tL/0.6 Area Section Flow Length (ft) Slope (%) tC (min) qp (cfs/acre-in) qp *A (cfs/in) 1 256 14 4.8 1.8 0.18 2 155 20 2.7 2 0.2 3 282 12 5.6 1.6 0.224 4 325 11.5 6.4 1.5 0.30 5 360 9.5 7.7 1.4 0.364 Area Section Flow Length (ft) Slope (%) tC (min) qp (cfs/acre-in) qp *A (cfs/in) 6 252 19 4.1 1.85 0.222 7 450 8.2 9.8 1.3 0.351 8 330 17 5.6 1.6 0.256 9 411 5 11.8 0.8 0.08 10 375 18 5.8 1.6 0.16 Weighted qp = 1.517 (cfs/ac-in) Qp= (1.517 cfs/ac-in *2.538 in *1.54 ac = 5.93 cfs = 0.168 m3/s is the FLOW RATE of Runoff during a 25 yr -24 hr Storm
  • 19. Design Option 1: Terracing with Existing Driveway at Recycling Center SDR- Soil Delivery Ratio = 14 % LS for 60 ft - 13% = 3 LS for 15 ft - 13% = 1 3 = 9.5625 ton/ac/yr 1 = (⅓) * 9.5625 ton = 3.1875 tons per terrace Source: Basemap: Google Maps; Area Analysis: J. Ossorio 3 - 15 ft Terraces have the potential to reduce Soil Loss per year from 9.5625 ton/ ac to 0.518 ton/ac, a 95 % reduction in erosion.
  • 20. Terrace Designs that encourage more infiltration and velocity reductions Design Option 1: Terracing with Existing Driveway at Recycling Center Source: Basemap: Google Maps; Area Analysis: J. Ossorio www. intechopen.com Driveway already exists, but the proposal is to allow access to this entrance after hours by changing Recycling Center enclosure
  • 21. Design Option 2: Create an entrance driveway to Kite Hill Driveway allows for safe maneuvering on and off of Kite Hill The Paved Area should mimic current runoff behaviors Permeable Surface Storage (S) 6.39 in/ac and Q = 2. 538 in 25 yr- 24 hr to avoid runoff increase Asphalt Has Surface Storage (S) of 0.204 in [CN = 98] and Q = 6.538 in Need to decrease curve number of other areas to compensate Overall Runoff increased from 2.54 in to 2.94 in Source: Basemap: Google Maps; Area Analysis: J. Ossorio
  • 22. Design Option 2: Create an entrance driveway to Kite Hill Erosion Control (Goal: Reduce by 75%) Universal Soil Loss T=R*K*LS*C*P P: The addition of a Conversation practice like contouring can reduce on a slope of 9-12 % P factor will decrease from 1 to 0.60 for that area LS: The factor will decrease because the slope % will need to be cut down to 12% or less a safe drive C: Heavier vegetation (erosion control covers) can be added on sides to allow for less erosion Runoff Velocity and Volume (Reduce Volume by 50%) Soil-Cover Complex Method CN: By implementing different land cover with lower Curve Numbers can reduce the volume and velocity Peak Runoff Rate S: To implement the driveway the % slope will be decreased, which will help slow velocities
  • 23. Kite Hill Erosion Reduction Design Comparison Option 1 Pros -Reduce erosion significantly -Preserve green space of Kite Hill -Potential to slow velocity and reduce runoff -Discourages driving up side of Kite Hill Cons -Expensive Soil Conservation Practice -Construction and Maintenance of terraces -Failure to maintain terraces can result in degradation of bench (possible landslide) -Adds heavy traffic volume at the Recycling Center Option 2 Pros -Allows for two entrances for heavy traffic -Reduce Erosion with implementations -Allows for safer travel up side of Kite Hill Cons -Driveways require slope % of 12 % or less for safety -Require extensive cut and fill into the Hill -If driveway is permeable, extra maintenance to prevent clogging of the pores -Reinforce permeable pavement -May increase runoff velocity
  • 24. Flow Diversion Techniques Flow Diversion Options: Concrete cut with apron & stabilization Grated Trench Drain Flow Diverting Speed Bumps Must handle QR=0.168 m3/s Photo Credit: Conor Bury, 2015 Source: Basemap: Google Maps; Area Analysis: R. Middleswarth
  • 25. Curb Cut with Apron Divert flow into swale Must set stabilizers and apron Concrete GCL Erosion Mat May disturb swale function Source: www.lastreetblog.org Photo Credit: Conor Bury, 2015
  • 26. Grated Trench Drain Q=(k*A*R2/3*S1/2)/n Q- volumetric flowrate A- cross sectional area of drain R - Hydraulic Radius S- Slope n - coefficient of friction Source: www.trenchdrainsupply.com Source: www.lastreetblog.org
  • 27. Enhanced Swale Design 500ft stretch options: Grassy Swale Riprap Swale Check Dam Swale Source: Basemap: Google Maps; Area Analysis: R. Middleswarth
  • 28. Trapezoidal Swale Used for unlined channels because of side slope stability Easy to cut grass and maintain Large surface area for infiltration
  • 29. Enhanced Grassy and Rocky Swale Q=(k*A*R2/3*S1/2)/n Q- volumetric flowrate A- cross sectional area of drain R - Hydraulic Radius S- Slope n - coefficient of friction For soil group B reduction - TSS = 60% - TP = 32% - TN = 36% Source: www.bae.ncsu.edu Source: www.bae.ncsu.edu
  • 30. Enhanced Grass Swale V=Q/A V - velocity (m/s) Q - Peak Flow rate (m3/s) A - Cross-sectional area (m2) Factors affecting velocity include: - Manning’s coefficient n - Cross-sectional area - Slope - designed hydraulic radius Source: www.bae.ncsu.edu
  • 31. Enhanced Rock Swale Rip-rap lined swales have varying n values Source: www.bae.ncsu.edu
  • 32. Check Dam Design Primary Design Benefits: Soil Erosion Sediment Control Total Suspended Solids (TSS) Flow Attenuation Secondary Benefits: Runoff Volume Reduction Phosphorous Nitrogen Heavy Metals Floatables BOD Source: www.riverlink.org
  • 33. Check Dam Design 33 ft intervals @ 6% slope ⅓ - ⅔ of the swale depth ~66% slope on upstream side of dam Acts as terracing to reduce sedimentation and velocity Flow Through a dam Q = h1.5/(L/D + 2.5 + L2)0.5 L = (ss)*(2d - h) Q- flow rate exiting check dam h - flow depth L - length of flow D - average stone diameter in feet ss - check dam side slope (maximum 2:1) d = height of dam
  • 34. McMillan Road Enhanced Swale Design Comparison Check Dams Pros - Inexpensive - Reduces erosion and sediment transport - Allows infiltration - May discourage illegal parking Cons - Requires periodic repair and sediment removal - Allows infiltration - Doesn’t treat oils Grassy / Riprap Swale (dry) Pros - Simple Installation - Easy Maintenance - Aesthetically Pleasing Cons - May form rills - Higher velocity - Less treatment and infiltration than other methods
  • 36. Sub-Goals of Median Redesign 1.Reduce the Velocity of Runoff 2.Allow Infiltration into Medians 3.Prevent Sediment Loss
  • 37. Area of Interest Defined Parking Lot Medians 123 4 5 6 7 Area (m2) Slope (%) H. Slope (%) V. 1 385.11 10.8 1.0 2 613.41 4.2 0.9 3 923.9 6.7 0.8 4 929.79 6.1 1.0 5 735.48 6.4 1.2 6 695.93 5.9 1.4 7 601.01 5.0 1.6 Source: Google Maps
  • 38. Design 1 - Vegetated Filter Strip Manning’s Equation V = (k/n)*Rh (⅔)*So (½) k: coefficient to convert units k = 1.486 (US Customary Units) n: Gauckler-Manning’s coefficient short vegetation - 2 to 6 inches: 0.04 tall vegetation - 12 to 24 inches: 0.08 Rh: hydraulic radius - Rh = areaCS/wetted perimeter So: slope of channel length bed Parabolic Channel Design Slope V (short veg 12”) f/s V (short veg 6”) f/s V (tall veg 12”) f/s V (tall veg 6”) f/s 1 0.01 0.330 0.083 0.165 0.041 2 0.009 0.297 0.074 0.149 0.037 3 0.008 0.264 0.066 0.132 0.033 4 0.01 0.330 0.826 0.165 0.041 5 0.012 0.396 0.099 0.198 0.49 6 0.014 0.462 0116 0.231 0.058 7 0.016 0.528 0.132 0.264 0.066
  • 39. Design 1: Vegetated Filter Strip Excavation - cut and fill using paversCurb cuts versus curb stops http://www.lowes.com/Outdoors/Pavers-Retaining-Walls/_/N- 1z0wgaf/pl http://www.publicdomainpictures.net/view- image.php?image=3409&picture=parking-lot http://www.estuarypartnership.org/sites/default/files/fieldguide/e xamples/swale.htm http://www.hrwc.net/stormwat erbmps.htm
  • 40. Vegetated Filter Strip Soil - gravel layer Plants http://www.clemson.edu/psapublishing/pa ges/HORT/IL87.PDF http://www.watershedmanagement.vt.gov/stormwater/htm/sw_gi_bmp_bioretention.htm http://www.emuseum.org/alcoa-foundation-outdoor-classroom
  • 41. Design 2 - Erosion Mat Coconut Fiber Mat Vegetation Live stakes T= R*K*LS*C*P R- Rain factor = 250 (Pickens, SC) K- Soil Erodibility Factor = 0.17 (Web Soil Survey) C- Cropping Factor = 0.01 (For complete Meadow) P- Conservation Practice = 1 (Assume not preventive practice) LS- Length Slope Factor - For the steepest slope - Control Mat 40 (Granite Environmental) - 80% efficiency of sediment removal http://www.in.gov/legislative/iac/20120404-IR-312120154NRA.xml.html
  • 42. Erosion Mat Permeable Pavement Miscanthus Grass http://www.in.gov/legislative/iac/20120404-IR- 312120154NRA.xml.html http://www.vwrrc.vt.edu/swc/NonPBMPSpecsMarch11/VASWMBMPSpec7PERME ABLEPAVEMENT.html http://www.hgtvgardens.com/flowers-and-plants/maiden-grass- miscanthus-sinensis-morning-light
  • 43. Medians Design Comparison Option 1 Pros -Reduce sediment, pollutants and velocity of stormwater -Allow more time for infiltration of stormwater -Adds more green area to Kite Hill (aesthetically pleasing) Cons -Steep slope adds more complex issue -Maintenance -Failure of pavers Option 2 Pros -Allows for more infiltration -Reduce erosion with vegetated mat Cons -Failure of permeable pavement -Sediment clogging -Anaerobic issues -4 to 6 year life span -Pollutant removal -Maintenance
  • 44. End of Pipe “Solutions” ● Upstream reductions are not enough ● Most common designs are: ○Detention Basin ○ Retention basin ■ Submerged gravel wetland
  • 45. Detention Pond ● Reduce peak flows ● Little filtration ● Little to no pollutant conversion Source: https://stormwater.files.wordpress.com/2009/05/img_4745.jpg?w=640
  • 47. Settling Velocities Stokes Law for settling velocities: where, VS: settling velocity VP: volume of particle ρP: density of particle CD: drag coefficient ρ: density of fluid AP: surface area of particle g: gravitational constant
  • 48. Settling Velocities cont. To get the VP and AP, Approximated particle geometry as sphere Found mean particle diameter (d50) for Cecil Sandy Loam (low: 0.2 cm, high: 7.4 cm; Source: Web Soils Survey) Low end value used to determine minimum settling velocity Calculated mean particle volume (4/3·𝜋·r3) and surface area (4·𝜋·r2) VPmin = 0.004189 cm3 APmin = 0.125664 cm2
  • 49. Settling Velocities cont. To get the ρP, ρ, and CD, An average soil particle density value: 2.66 g/cm3 Assuming pure water at 4oC and 1 atm: 1 g/cm3 CD can be determined experimentally or using representative values Unfortunately this value can change dramatically depending on the number of particles falling the true particle geometry aggregate particles vs single particles turbulence generated by mass particles falling
  • 50. Settling Velocities cont. Given the high level of variability, SCDOT Stormwater Manual Reports Cecil as d15 = 0.0066 ~ 0.0043 mm If d15 < 0.01 mm, use simplified Stokes, Vs = 2.81·d2 where, d = particle diameter in mm Vs = settling velocity in ft/s
  • 51. Settling Velocities cont. SCDOT Stormwater Manual Reports Cecil ranging in particle sizes as 0.001 ~ 1.4 mm, Vs = 2.81·(0.001)2 ≈ 2.81·10-6 ft/s ≈ 8.56·10-7 m/s Vs = 2.81·(1.4)2 ≈ 5.51 ft/s ≈ 1.68 m/s Sizing a basin is not enough. Vegetation, microbial, and aggregate filtration necessary.
  • 54.
  • 55. Rational Equation for Peak Discharge: Q = ciA Where, Q = peak discharge [cfs] c = runoff coefficient i = rainfall intensity [in/d] A = area [acres] Five year design storm: Q = (0.8)(4.73in/d)(4.15ac) Q = 293GPM
  • 56.
  • 57. Sustainability Measures ● Economical ○ Feasibility ○ Maintenance ○ Location ● Ecological ○ Improving Stream Health ● Social ○ Educational ■ Foundation in Clemson’s Will ■ Biosystems Engineering ● Ethical Considerations ○ Solving the problem without damage to downstream http://cantov.deviantart.com/art/Clemson-University-Still-Water-145243984
  • 59. References Jurries, Dennis, P.E. “Biofilters For Storm Water Discharge Pollution Removal”. Department of Environmental Quality. State of Oregon. 2003. PDF. <.http://www.deq.state.or.us/wq/stormwater/docs/nwr/biofilters.pdf> Accessed 7 August 2015. Mey, Gerald Vander. et. al. “Riparian Corridor Master Plan”. Campus Planning Services. Clemson University. December 2006. PDF. <http://www.clemson.edu/public/hunnicutt/documents/riparian_corridor_master_plan.pdf> Google Maps. Accessed 13 August 2015. Ruhlman, Melanie. President, Save Our Saluda. Personal communication. 12 August 2015. Murphree, Brian Frank, P.E. et. al. MS 4 Outfall Inspections and Evaluation, Clemson University. Project No. 1505. Design South Professionals, Inc. July 2015. Dorren, Luuk, and Freddy Rey. "A Review of the Effect of Terracing on Erosion." SCAPE: Soil Conseveration and Protection for Europe (n.d.): 97-108. Web. 15 Oct. 2015. Widomski, Marcin K. "Terracing as a Measure of Soil Erosion Control and Its Effect on Improvement of Infiltration in Eroded Environment." Ed. Danilo Godone. Soil Erosion Issues in Agriculture (2011): 315-34. InTech. Web. 15 Oct. 2015. <http://www.intechopen.com/books/soil-erosion-issues-inagriculture/ terracing-as-a-measure-of-soil- erosion-control-and-its-effect-on-improvement-of-infiltration-in-erod>. Watershed Hydrology and Small Catchments, BE3220. Owino, T, PhD. Clemson University. Spring 2015. http://www.erosionpollution.com/support-files/coir_geotextiles_specification.pdf http://water.epa.gov/scitech/wastetech/upload/2002_06_28_mtb_wetdtnpn.pdf http://www.unh.edu/unhsc/sites/unh.edu.unhsc/files/pubs_specs_info/unhsc_gravel_wetland_specs_6_09.pdf http://www.unh.edu/unhsc/sites/unh.edu.unhsc/files/presentations/NJASLA%20subsurface%20gravel%20wetland.pdf http://sfrc.ifas.ufl.edu/urbanforestry/Resources/PDF%20downloads/Rushton_2001.pdf

Editor's Notes

  1. Conor Image of Clemson University Watershed Hunnicutt Creek is primary drainage basin for the university About ⅔ of all campus storm drains drain to Hunnicutt Creek Water from Hunnicutt Creek is pumped into Lake Hartwell *Red circle is the Stream Restoration Reach Riparian Corridor Master Plan (2006) In-depth research on problems, and unique challenges associated with improvements Focuses on conservation, restoration, stabilization Clemson hopes the restoration projects and research on Hunnicut Creek will provide starting blocks for future projects and education resources for students, faculty and visitors Highlight the location of design then proceed
  2. Conor
  3. Conor
  4. Conor
  5. Conor
  6. Rainwater is not able to infiltrate into ground due to impervious surfaces and steep slopes Sediment and parking lot pollution is transported by runoff Excessive, improperly managed stormwater is damaging downstream portions of Hunnicutt Creek
  7. J
  8. Ash Existing Infrastructure - busy street, parking area, cars park on grass on game day, so we have to account for that when choosing location and materials Future Construction- avoid areas that will be disturbed by new development Theoretical Data - There requires a lot of field examination to see where the runoff is coming from and where it is actually going instead of just modeling what we think will happen Also we will need to take some water samples to see what are pollutants coming off the parking lot Multiple Advisors - There are a lot of people within Clemson Facilities and Hunnicutt Creek and Future Development that we should consult with to help us create a design that Clemson could implement Budget- Our design should be able to fit into a budget that Clemson would be willing to pay for, there is about $150,000 set aside for a solution to reduced the runoff in the Kite Hill Area so that will be a guiding factor for our design
  9. Jeannie
  10. J Brief Description of Where this is Parking Area Kite Hill Further problems persist downstream, but those are not within the scope of this project. However, our design is expected to reduce problems downstream
  11. J Filtration: Biological - phyto- (sedges), micro- (soil-borne bacteria, bacteria native to sedge root structures) Mechanical: sand filtration, soil filtration Chemical: exchange capacity (charge of soil), redox (from organic material), pH
  12. For low flows, check-dam geometry and swale width are actually more influential on flow than stone size. The average flow length through a check-dam as a function of flow depth can be determined by the following equation:
  13. changing the manning’s n - between short and tall vegetation changing the depth of the channel from 1 foot to 6 inches
  14. curb stops are for safety - curb cuts are very common
  15. drainage layer with sand, gravel, compost plant species that are drought and flood tolerant -native - sedges, daylillies cardnail flower, swamp sunflower - two native plants that are drought tolerant and easy to grow
  16. Made from a natural and biodegradable coconut fiber, these mats work to increase soil stabilization, effectively decreasing erosion and allowing vegetation to effectively take root (vegetation is optional). These mats are recommended for steep slopes such as stream bank erosion. - the top is buried about 6 inches underneath the top of the slope - should have seeding before mat is installed - 4 to 6 years will biodegrade naturally live stakes are dormant plant material - as they grow they will help anchor the mat - some type of tall iscantus no till - can use horticulture crops or hay and pasture overland flow - sheet flow (before mat) gives enough time for the grass to establish
  17. permeable pavement allows for the infiltration of water - it would only be the bottom side of each sloped median miscanthus grass can be used for live stakes
  18. J Retention Basins
  19. J Filtration: Biological - phyto- (sedges), micro- (soil-borne bacteria, bacteria native to sedge root structures) Mechanical: sand filtration, soil filtration Chemical: exchange capacity (charge of soil), redox (from organic material), pH
  20. J Filtration: Biological - phyto- (sedges), micro- (soil-borne bacteria, bacteria native to sedge root structures) Mechanical: sand filtration, soil filtration Chemical: exchange capacity (charge of soil), redox (from organic material), pH
  21. J Filtration: Biological - phyto- (sedges), micro- (soil-borne bacteria, bacteria native to sedge root structures) Mechanical: sand filtration, soil filtration Chemical: exchange capacity (charge of soil), redox (from organic material), pH
  22. J Filtration: Biological - phyto- (sedges), micro- (soil-borne bacteria, bacteria native to sedge root structures) Mechanical: sand filtration, soil filtration Chemical: exchange capacity (charge of soil), redox (from organic material), pH
  23. J Filtration: Biological - phyto- (sedges), micro- (soil-borne bacteria, bacteria native to sedge root structures) Mechanical: sand filtration, soil filtration Chemical: exchange capacity (charge of soil), redox (from organic material), pH
  24. J Filtration: Biological - phyto- (sedges), micro- (soil-borne bacteria, bacteria native to sedge root structures) Mechanical: sand filtration, soil filtration Chemical: exchange capacity (charge of soil), redox (from organic material), pH
  25. J Filtration: Biological - phyto- (sedges), micro- (soil-borne bacteria, bacteria native to sedge root structures) Mechanical: sand filtration, soil filtration Chemical: exchange capacity (charge of soil), redox (from organic material), pH
  26. J Filtration: Biological - phyto- (sedges), micro- (soil-borne bacteria, bacteria native to sedge root structures) Mechanical: sand filtration, soil filtration Chemical: exchange capacity (charge of soil), redox (from organic material), pH
  27. J Filtration: Biological - phyto- (sedges), micro- (soil-borne bacteria, bacteria native to sedge root structures) Mechanical: sand filtration, soil filtration Chemical: exchange capacity (charge of soil), redox (from organic material), pH
  28. Pathways to remove nitrogen: Assimilation - inorganic nitrogen is taken up by plant roots and temporarily stored as organic nitrogen in plant biomass Adsorption - positive ammonium ions attach to negatively charged soil particles. The soil particles settle out which prevents the nitrogen from leaving the system Denitrification - Nitrate is reduced under anaerobic conditions and in the presence of an electron donor to nitrogen gas, which is then released into the atmosphere TSS - Total Suspended Solids TPH-D - Total Petroleum Hydrocarbons as Diesel DIN - Dissolved Inorganic Nitrogen (sum of nitrate and ammonia) Zn - Zinc TP - Total Phosphorous
  29. Jeannie Economical - Low Maintenance Design that can reduce Ecological - Social - It promotes the importance of sustainability in design by finding a Ethical Considerations -
  30. R
  31. J