4. Background
● USDA issued project proposal
● Francis Marion National Forest
● 18th and 19th century irrigation
canals and watering cattle
● 20th and 21st century timber and
ecological research
7. Rationale
● Degraded hydrology
○ Channelization drained watershed
○ Bottomland hardwood forest
○ Hardwood flat
● Loss of natural habitat
○ Disrupted ecosystem
○ Destroyed habitat of native species
8. Objectives
The objectives of this project are to
(1) develop engineering systems for soil and water management to
restore wetlands of the Francis Marion National Forest,
(2) design hydraulic structures for open channel flow, and
(3) evaluate designs based on their effectiveness, cost, and
environmental impacts in order to recommend a final design that
meets the standards for the best management practices outlined
by the US Army Corps of Engineers
9. Approaches
Task 1. Conduct a preliminary site survey in order to determine the project
boundaries and take measurements of the channel
Task 2. Collect and analyze soil samples for soil physical and chemical
characterizations
Task 3. Perform hydraulic and hydrologic measurements for surface and
groundwater characterizations
Task 4. Determine U.S. Army Corps of Engineers proposed action
guidelines
Task 5. Model hydrology of the area to identify the best course of action for
channels and wetlands
Task 6. Evaluate cost analysis and environmental impacts for proposed
solutions
12. Wetland Restoration
Wetland restoration involves returning one or more of these three
characteristics to a degraded site:
● Hydrology
● Hydric soil
● Wetland vegetation
Restoration project sites can vary due to:
● Ditched, tiled and leveed areas for agricultural purposes
● Degradation from excessive logging
● Uncontrolled cattle grazing
● Unrestricted off-road vehicle use
13. Bottom Contouring
● Cut and fill method
● Modified by removal (cut) or addition (fill)
● Surface sediment
● Sediment fill can raise the water table in
flat wetlands that have:
○ Channels
○ Ditches
○ Streams
● Equal cut and fill
○ No export or import of
sediment
14. Cut and Fill Case Study
● Location: Kissimmee River
○ Central Florida
● Problem: River became
compartmentalized
○ Altered hydrology of surrounding
areas
● Solution: Cut and fill
○ Increased the water table
○ Restored wetland habitats for
native species
15. Water Control Structures
● Bring water into the wetland, and maintain a desired water level
● Inlet and Outlet Structures
○ Water will arrive to the wetland by gravity from surface streams
○ Outlet structures are designed to be the primary control on water level and
maintain flow distribution
● Ease of operation and ability to set the desired water level.
○ Outlets devices should have enough capacity to accommodate for peak storm
events within the design range
16. Weirs
● A structure built across a river or stream and
provides a constriction that regulates flow and raises
the level of water upstream
● Can become blocked by ice or floating debris
● In small wetlands, flashboards or adjustable weir
gates are common
○ Flashboard structures are made from stacked
dimensioned lumber and water level is adjusted
through the addition or removal of logs
17. Low Water Crossings
● Stable roadway used to cross streams
● Allows for the natural passage of water and sediment over a road with little to no
maintenance
● Constructed of crushed aggregate, concrete, concrete planks and/or brick tiles
● Vented or Unvented
18. Vented Low Water Crossing Case Study
● Location: Indian Creek
○ North Carolina
● Problem: Recreational fishing and high
flow rate
● Solution: Vented Low Water Crossing
○ Easy access for fish
○ Protects crossing from damage
Vents
19. Unvented Low Water Crossing Case Study
● Location: Cienega Creek
○ Arizona
● Problem: Need for natural passage of flow
because of seasonal flooding
● Solution: Unvented Low Water Crossing
○ Traffic passes with or without seasonal
flooding
20. Berms
● Earthen embankments constructed to
contain water
● Require maintenance
● Sometimes created through scrapes
● Conjunction with water control structures
21. Ditch Plugs
● The filling of a section of a drainage path
with an earthen wall
● Slow flow through a drainage path and
increasing water retention
● Emergency spillways can protect the
structure from damage. An orifice may be
used to allow flow through the ditch plug
22. Ditch Plugs Case Study
● Location: Seney, MI
● Problem: Need to restore land back to its
original environment, a wetland
○ 2002 USDA began restoration
project
● Solution: Ditch Plugs
○ 9 Plugs
○ Colonization of wetland species
and rise of water table
Ditch Plug
23. Tile Breaks
● Removal or breaking of an underground clay or
perforated plastic drain tile
● Buried at a depth of two to six feet, drain tile is often
removed by a contractor
● Tile breaks restore wetland hydrology, vegetation and
wildlife back to its original ecosystem
24. Tile Breaks Case Study
● Location: Ozaukee County
○ Wisconsin
● Problem: Drain tiles dried out the soil
○ Agricultural fields had been made out of
wetlands
○ 1989 USDA proposed wetland restoration
● Solution: Tile Breaks
○ water table levels began to rise and wetland
vegetation was making a come back
25. Venturi Flumes
● Channel that transports water through the
use of gravity
● A constriction in a standard flume forces the
flow upstream of the constriction to be
subcritical, and downstream to become
supercritical
● Flumes allow unimpaired passage through
the structure, however, do not form a stilling
basin upstream
● Examples of constricted flumes are the H-
Type and the Parshall flume
26. Vegetation Establishment
● Restored wetlands place considerable
emphasis on vegetative diversity
● Competitive die-out continuously changes
plant communities
● Assisted Natural Selection
● Altering the water table, the top layer of the
zone of saturation, can have a impact on
the prosperity of certain plant species in an
area
28. Our Project Site
● Our site:
○ Hardwood Flat
○ A 1500 ft section of Nicholson
Creek Watershed, most of
which has been channelized
○ The watershed is approximately
500 ac
○ Surface elevations varying from
3.5 to 6.5 ft
○ Less than 1 % slope
Stream
restoration sites
---- Project site
29. Hardwood flat
dendrology
(6) Dwarf palmetto
Sabal minor
(7) Swamp chestnut oak
Quercus michauxii
Bottomland hardwood
forest dendrology
(1) American holly
Ilex opaca
(2) American beech
Fagus grandifolia
Dendrology found
in both
(3) Loblolly pine
Pinus taeda
(4) American sweetgum
Liquidambar styraciflua
(5) Red maple
Acer rubrum
(1) (2) (3) (4) (5) (6) (7)
30. Soil Conditions
● Hydric soil is soil that is permanently or temporarily
saturated with water. Soil can take years to reach hydric
conditions
● An indicator of hydric mineral soil is called gleying
○ Gleying is a lack of oxygen in soil which turns the
soil a blue or grey
● The sediment beneath the topsoil of this project area is
grey supporting that the watershed already contains
appropriate soil for wetland restoration to be viable
without the need for hydric soil conditions to develop or
the import of hydric soil
31. Climate Conditions
● This project site experiences 44-49 in of rainfall per year
● During the fall it experiences less than 2 in of rainfall per month
● In the summer the area experiences 6-8 in per month due to
intense hurricanes and thunderstorms
● These rainfall periods can cause inundation of the watershed
during this time of the year
● This gives us an adequate amount of water to raise the water table
with the proper wetland restoration technique
32. Topographic Surveying
● Digital Elevation Model (DEM)
map
○ 1 meter resolution
○ Provides specific topographic data
such as flood bank levels
33. Channel Survey
● Flood Bank Level
○ Channel dimensions
○ Total station
● Channel
○ Open channel cross-section found
with range finder
○ Control structure dimensions
34. Soil Collection and Analyses
● Soil was collected at several key points along and in
the channel using a manual auger
○ Soil analyses
○ Soil type
○ Soil physico-chemical properties
35. Groundwater Monitoring
● A well was installed in the channel to
monitor the water table height in 15 minute
intervals since implementation
● allows for a comparison with watershed 80
which has historical flow and climate data
36. Bottom Contouring
● Use the soil that is currently on
the channel banks to fill in the
bottom of the channel
● Large horizontal:vertical side
slope increases wetted
perimeter, decreasing flowrate
37. Culvert Removal
● Two culverts at intersection of main
channel and Tanner Road
● This site is a potential location for a low
water crossing
● Stormwater flow does not currently rise
to a high enough elevation to overflow
the road
● Removing this culvert reduces flow in
the drainage channel
38. ● Auto Computer Aided Design version 2018
○ Modeled channel dimensions to show cut and fill
■ Design equal cut and fill
○ Model a weir addition
○ Model the creation of a low water crossing
Modeling Channel Dimensions and Hydraulic
Structures with AutoCAD
39. Flow Modeling
● Hydrologic Engineering Center River
Analysis System (HEC-RAS)
● Inputs
○ geometry of site
○ Manning’s numbers (n)
○ Rainfall and Climate Data
○ Historic data, DHEC Stormwater
Management Handbook
○ Site specific rainfall and climate
data compiled by USDA FS
40. HEC-RAS Flow Model
● Uses the one-dimensional energy equation (1) to solve for flow
● Manning’s equation (2): used to find velocity
● Gives an output of flow area at each cross sectional area of the channel
(1)
(2)
41. Soil Modeling
Inputs:
● Geometry of the site
○ Same variables as those used in flooding calculations
● Quasi-Unsteady Flow of the channel
○ Flow of the channel over time
○ Temperature of the area during the simulation time
● Sediment
○ Create a bed gradation: state the composition of the soil as
percentiles of soil textures
○ Fall velocity- how the sediment types fall in the stream beds
○ Maximum depth
42. ● HEC-RAS uses the Exner continuity equation to state that the difference
between sediment entering and leaving an area must be either stored or
removed from storage
HEC-RAS Soil Model
Sediment entering - sediment leaving = change in storage in the control volume
(between cross-sections) (by erosion / deposition of sediment)
Active layer
porosity Transported
sediment load
Channel elevation
44. Soil Data: Soil Texture
● Soil samples were collected along the channel and analyzed for their soil type
and grain size
○ The results showed the composition included an average of 71.88%
sand, 15.86% silt and 12.26% clay
45. Soil Data: Chemical Composition
● Further analysis identified the chemical qualities of the soil
○ Including and average pH of 5.97, average Buffer pH of 7.68, and key
nutrients in pounds per acre
○ These results provide a basis for analyzing what plant species are able to
thrive in the soil
Sample
ID
Soil pH Buffer
pH
P
lbs/A
K
lbs/A
Ca
lbs/A
Mg
lbs/A
Zn
lbs/A
Mn
lbs/A
Cu
lbs/A
B
lbs/A
Na
lbs/A
SS1 5.3 7.4 9 60 2038 172 1.4 25 0.2 0.8 21
SS2 6.4 7.95 61 27 1085 48 2.7 11 0.4 0.2 21
SSwell 6.2 7.70 458 78 3775 185 0.8 66 0.5 0.5 50
46. Rainfall and corresponding water table
● Records the groundwater table height with respect to the bottom of the
channel
● Shows the reaction of the water table from rainfall in 15 minute intervals since
implementation
● If the channel bed is raised, the water table change would also be monitored
47. About Water – Groundwater Data
●Need to have Groundwater data
51. Pre-Development – Flooding Data
Predevelopment Velocity
(ft/s)
Cross
sectional
area (ft2)
top width
(ft)
Average Upstream 0.33 11.24 73.17
Average downstream 0.43 10.75 66.02
Overall Average 0.41 10.86 67.51
Velocity
● A high water velocity could damage any
present water control structure
● Keeping the velocity low allows for structure to
withstand more intense flooding conditions
Cross Sectional Area
● This is the area of the cross sections that is
below water when running the simulation
● A higher cross sectional area means a greater
water depth
Top Width
● The top width is the width of the water’s
surface
● The wider the water's surface, the higher the
storage area for flooding
52. Pre-Development – Soil erosion conditions
● HEC-RAS soil transfer
simulations are able to show
soil build up across the
different reaches of a river
● The build up is most easily
identified when observing the
Profile plot which shows a
difference between the
channel bed and the build up
of soils
63. Culvert Removal Cross Sections
Predevelopment Cross Section Post development Cross Section
64. Culvert Removal
Velocity
(ft/s)
Cross
sectional
area (ft2)
Top
Width (ft)
Average Upstream 0.34 10.80 72.28
Average
Downstream
0.43 10.75 66.02
Overall Average 0.41 10.77 67.32
Culvert Removal Analysis
Predevelopment
Velocity
(ft/s)
Cross
Sectional
Area (ft2)
Top
Width (ft)
Average Upstream 0.33 11.24 73.17
Average
Downstream
0.43 10.75 66.02
Overall Average 0.41 10.86 67.51
65. Culvert Removal Cost Analysis
Component Name Price ($/unit) Quantity Cost ($)
Compacted Earthfill $5.75 per yd3 3 yd3 $17.25
Hydraulic Excavator $117.15 per hour 18 hr $2,108.70
Heavy Equipment
Operators
$33.69 per hour 18 hr $606.42
Aggregate, Gravel $35.73 per yd3 14 yd3 $500.22
Low Water Crossing
Planks
$30 per plank 30 planks $9,000.00
Mobilization $262.64 per item 1 excavator $262.64
Total Cost $12,495.23
66. Flooding Solution Caparison
Average Velocity
(ft/s)
Average Cross
Sectional Area (ft2)
Average Top Width
(ft)
Predevelopment 0.41 10.86 67.51
Channel Filling 0.31 37.16 70.25
Weir Installment 0.0571 118.2 100.1
Culvert Removal 0.41 10.77 67.32
67. Cost Comparison
Restoration
Technique
Final Cost
Channel Filling $8,361.59
Weir Installment $3,598.73
Culvert Removal $12,495.23
● When compared the weir
was concluded to be the
most cost-effective option
● Installing a weir requires less
time for installment as well
as lower material costs
68. Weir Installation Test for a Major Storm Event
● Modeled after Hurricane Matthew (category 5)
● 1,000 year storm event
● Peak flowrate at reference watershed: 1000 ft3/s
69. Major Storm Event Data
● Desired approaching velocity for a weir is 0.5 ft/s
● Flood simulation resulted in an approaching velocity of 1.86 ft/s
○ The resulting velocity is high and may damage the weir if placed similarly
to the model
73. Take Home Messages
● In its current state, the Francis Marion National Forest hydrology is
compartmentalized due to previous agricultural practices
● Case studies and further research show methods such as ditch plugs, culvert
removal, tile breaks, and channel filling have proven to minimize the effects of
channelization
● Using modeling programs such as HEC-RAS allow for different solutions to
be simulated leading to making the best possible choice for a solution
74. Our Recommendation
● By analyzing a low level storm event in HEC-RAS, it was determined that the
addition of a cement weir with a soil berm would be the most effective at
reducing flowrates and increasing top width flooding to maximize the area of
the hydric soil
● Using preliminary cost analysis, this is also the most cost-effective design
option
● The berm will limit sediment transportation and seedbank dispersion for
promoting the growth of wetland vegetation
75.
76. Acknowledgements
USDA Staff
Dr. Carl C. Trettin, Team Leader & Suprv. Research Soil Scientist
Mrs. Julie A. Arnold, Forestry Technician
USACE Wetland Specialist
Mrs. Andrea Hughes
USACE Wetland Regulatory Deputy
Mrs. Robin Socha
Clemson University Staff
Dr. Christophe Darnault, Ingénieur, Ph.D.
Remove
By, put names in row
capstone design BE 4750
Midterm presentation
Sponsored by
Dr. Carl trettin (separate slide afterwards, towards the end ie. acknowledgement)
Add date, location
Figure too large, change picture (satellite image)
Bullet points
Font too small
Remove abstract
Approach instead of tasks
Remove comprehensive
Remove inputs, models, outputs, place themes of results (flooding, erosions, post design)
Discussion and Conclusion -> take home messages
Remove References
Thank you
In the 18th and 19th century this project site was channelized for irrigation of cash crops and watering livestock such as cattle.
`
This is a satellite image of our project site and as you can see there is highlighted straight channel that was dug out.
Format is off for rationale slide, explain the problems channelization is causing and explain why need to restore;
Because of the problem (channelization) there is loss of surface water thus corrections would…
Degraded hydrology
Channelization has drained the
watershed and a loss of
surface water has changed the
bottomland hardwood forest to
a hardwood flat
Loss of natural habitat
Disrupting the ecosystem and destroying the habitat of native species such as the red-cockaded woodpecker
Remove indention
Pause and read this with enthusiasm
2 become 3
Develop engineering system for soil and water management for restoration of wetland; Engineer restoration of wetland area (somehow add the words soil and water)
2. Design hydraulic structure
3.
The objectives of this project are to
(1) develop engineering systems for soil and water management to restore wetlands of the Francis Marion National Forest,
(2) design hydraulic structures for open channel flow, and
(3) evaluate designs based on their effectiveness, cost, and environmental impacts in order to recommend a final design for submission that meets the standards for the best management practices outlined by the US Army Corps of Engineers
https://wrt.org.uk/barrier-removal/
Approaches
Conduct preliminary site survey
Collect and analyze soil samples for soil physical chemical properties characterizations
Perform hydraulic and hydrologic measurements for surface and groundwater characterizations
Delete task 3
Consistent with US
Create channel and wetland models of the restoration site
Evaluate cost analysis and environmental impact for proposed solutions
Remove 6 change 7 to recommendation
Wetland
Restoration
Site history-> background
Methods of restoration split to methods and hydraulic structure
Move autocad and HEC-RAS to materials and methods
Group remaining slides by the restoration req. And mention during presentation
Cut and fill is a method in which natural elevation of a surface is modified by the removal (cut) or addition (fill) of surface sediment
Sediment fill in channels, ditches, or streams, is a common procedure to raise the water table of areas, especially in flat wetlands
Equal cut and fill, where importing and exporting material from the site can be avoided, is the preferred option
Along the Kissimmee River, a dechannelization project backfilled sections of channelized floodplain. Water Tables in the areas increased and use of the restored sections by both birds and fish provided evidence of successful environmental restoration.
The Kissimmee River spans from the headwater lakes of the Kissimmee river to Lake Okeechobee in central Florida
In the past half century, the river had become compartmentalized which significantly altered the hydrology of surrounding areas such as the Everglades
The use of cut and fill increased the water table, and the wetland habitats for native birds and aquatic organisms were restored
Water Control Structures are needed to bring water into the wetland, and maintain a desired water level. Many options are available which differ by magnitude of flow to be managed. Devices applied to convey water into the wetland are considered inlet devices, while devices that maintain flow distribution or control water level are outlet devices.
For both agricultural and urban runoff marshes, point inlets are typically used. Water arrives to the wetland by gravity from surface streams, tile drain or stormwater collection systems. Inlet structures often are considered to be unnecessary.
Outlets devices generally operate at the downstream end of the wetland. Outlet designs range in complexity from perforated plastic drain tiles to remote operated motor-actuated weirs. Outlet structures are designed to be the primary control on water level. Selection of device should include ease of operation and ability to set the desired water level. Outlets devices should have enough capacity to accommodate for peak storm events within the design range.
Weir blades can take a variety of shapes including triangular, rectangular, and trapezoidal
, which can lead to inaccurate discharge calculations
A weir is a structure built across a river or stream used to regulate the flow of water and raise the water level of the area upstream. A weir creates a stilling basin upstream of the constriction. This constriction is known as a weir blade. Weir blades can take a variety of shapes including triangular, rectangular, and trapezoidal, however, the blade can also become blocked by ice or floating debris which could lead to inaccurate discharge calculations.
In small wetlands, flashboard and adjustable weir gates are common devices for outlet control. Flashboard structures are made from stacked dimensioned lumber and water level is adjusted through the addition or removal of logs, however, these devices have have rates of leakage. Adjustable weir gates offer the advantage of being continuously adjustable.
In large applications weir designs can become complicated, sometimes rely on electrical power, or combine with other flow measurement elements such as flumes.
Perennial creek
Rarely used gravel road that was constructed for timber management and sales
26 years after construction no maintenance has been needed and the road passes traffic with or without seasonal flooding
Berms often increase water levels in a wetland above historic levels to creat open water. They also can protect a neighboring property from flooding.
Berms require maintenance to control muskrat damage and to guard against erosion caused by heavy rains. Another issue with berms comes from elevated water levels inhibiting the germination of native vegetation where the seed bank is adapted to shallower water.
On suitable sites, topsoil is stripped away to expose sub-surface soils, which are removed to create a berm
A ditch plug is the filling of a section of a drainage path up to the natural ground level with an earthen wall to impound water. The blockage is typically made of clay subsoil
In large scale, an emergency spillway is incorporated to protect the structure from damage in times of high flow rate. An orifice may be used to allow flow through the ditch plug once it reaches a certain level
Ditch plugs improve hydrology for degraded wetlands by slowing flow through a drainage path and improving water retention
Wetlands around the town of Seney, MI were ditched out and drained in the early 1900’s for agricultural use
In 2002 the USDA attempted to restore this area back to its original environment by reducing the flow of water through a 4.5 km section of ditch with 9 ditch plugs
8 years later colonization of wetland species with the rise of the water table are indicators that the wetland is in the process of being restored in the area
in order to stop drainage from a desired wetland area
, 1.5 acres of agricultural fields had been made out of wetlands
This was done by the installation of clay drain tiles that dried out the soil
In 1989, the USDA proposed a wetland restoration of the area, and used the tile breaks in order to stop the drainage from the area
The Iowa conservation reserve enhancement program is a state, federal, local, and private partnership that provides incentives to landowners who voluntarily establish wetlands for water quality improvement in the tile-drained regions of iowa.
is the opposite of “select and plant” where
Plant pictures
Selected plantings rarely survive, and natural recruitment and c
With assisted natural selection no planting is needed, desired species of vegetation are brought in by wildlife and the environment is altered to better suit the prefered conditions for those species
This is background
Refine project site (watershed 80)
Consistency is good (2-14 m)
Add slide about surface elevation
Concerns
Pic 1: American holly
Pic 2: American Beech
Pic 3: Loblolly pine
Pic 4: sweetgum
Pic 5: red maple
Pic 6: dwarf palm
Pic 7: swamp chestnut oak
Have a bottomland flat, want a bottomland forest (or swamp)
What we can effect → promotion of growth
Current trees present can go into background, promoted species can go into take home?
Outline different to fit into the section → starting data table?
Int the background talk about hurricanes
This allows us to tie in the different sections
Make it about methods
Berkeley County DEM
1 m resolution
Materials and Methods one slide
Size down picture maybe add more pictures
Surverying
-topography land (total station)
- channel dimensions
Groundwater monitoring
-water table (data logger)
Modelling
-HEC-ras
-computer aid-design
-cut and fill
-weir design
Water table date from 2005 from watershed 80
Instead put what materials will be needed?
1ft Canal Filler
Original Imported Sediment Volume
13,207 ft3
Natural Sediment Volume
3,411 ft3
New Imported Sediment Volume
9,796 ft3
Soil topographic map
Need to show soil topo map of the site, Need to mark where is your watershed 80, where is the channel that is to be modified…
Superimpose this over a map decrease flow
Sum Flow Areas for each restoration technique/hydraulic structure
Talk about how the road is a focus for USDA
Sum Flow Areas for each restoration technique/hydraulic structure
Talk about how the road is a focus for USDA
Both of these cross sections are at the same point on the channel. This is Cross Section view of our predevelopment vs the cross section view upstream from the weir installation.
Compare pre vs weir design. Velocity of water is significantly lower and our floodplain has expanded tremendously causing the cross sectional area to increase as well
Eventually the culvert will have to be removed because its structure will wear overtime and eventually break and fail. So, we need to take that into consideration when we talk about implementing the low water crossing. It would have to be replaced due to the failure of the culvert.
By modeling a major storm event with the desired solution, we are able to confirm if the weir is able to withstand high flow conditions without blowing out