Case Study - Meadow
Creek
Design a restoration
scheme for a channel component of a wetland mitigation project. The
existing channel is a straightened reach through a broad valley used for cattle
grazing and farming. This “impacted reach” is spring-fed and has become
entrenched in a sandy soil. It looks like a gully in many locations.
The restoration scheme selected for the wetland includes raising the channel bed
into a slightly more gravely layer of soil while lifting the localized water
table to increase support of aquatic plants and wetland habitat. A small,
spring-fed, E4 reference reach was observed in a farm field a few miles from the
project site. Use this reference reach to help design a restored,
meandering reach in the Meadow Creek wetland project.
Case Study -
Meadow Creek: Solution
1.
Setting
up the RIVERMorph database and project file
2.
Define the
Impacted Reach Cross-Section Data
3.
Add the Profile
data to the Impacted Reach and Reference Reach
4.
Add the
Sediment Data to the Impacted Reach and Reference Reach
5.
Classify the
Impacted Reach and Reference Reach
6.
Perform the
Natural Channel Design Calculations
7.
Layout the
Channel in a “Natural” Pattern
1.
Setting
up the RIVERMorph database and project file
Open RIVERMorph
and create a new project. Right click in the data tree and use the popup
menu to create two river nodes (data sets). The impacted and design data
will be stored in the “Meadow Creek” set and the reference reach will be stored
in “Wolsey Branch Spring”. Rename the two nodes as shown.
Create
three reaches under the “Meadow Creek” river node. The first reach is
called “Impacted” and will store the existing conditions survey and the design
calculations for a tributary of Meadow Creek through the wetland mitigation
project. The second reach is “Historical” and stores planform data
collected from historical mapping of Meadow Creek for reference. “Meadow
Creek”, the last reach, contains data for the main stem below the project
reach. These reaches are in the Meadow Creek watershed. Rename the
reach nodes as shown.
Create one reach in the “Wolsey Branch
Spring” data set named “Reference Reach”. The reference reach is in a
separate watershed so it is useful to store it under a separate river node in
the database.
Case Study -
Meadow Creek: Solution
1.
Setting up the
RIVERMorph database and project file
2.
Define
the Impacted Reach Cross-Section Data
3.
Add the Profile
data to the Impacted Reach and Reference Reach
4.
Add the
Sediment Data to the Impacted Reach and Reference Reach
5.
Classify the
Impacted Reach and Reference Reach
6.
Perform the
Natural Channel Design Calculations
7.
Layout the
Channel in a “Natural” Pattern
2. Define the Impacted Reach Cross-Section
Data
The
impacted reach data set will include a surveyed riffle cross section; the
reference reach data set will include a pool and a riffle. We will
configure the RIVERMorph database to store and analyze this data.
Expand
the “Impacted” reach and cross section nodes under Meadow Creek in the
RIVERMorph data tree. Right click on the cross section nodes and use the
popup menu to add a cross section named “Riffle”.
Enter the first table of
survey data into this “Riffle” cross-section screen. Remember to check the
“Type” of cross section at the top of the screen, it should be set to
Riffle. Create the Reference Reach cross sections in Wolsey Branch the
same way.

Save your
data after entering each cross section.
Click the graph tab to view the cross
section. Could you guess where bankfull elevation falls by looking at the
graph without the bankfull indicators? It is very difficult in incised,
gully channels. The bankfull indicators correspond to annual flood
predictions and recent floodplain incision and depositional features.
Click the BKF tool button to align the bankfull elevation with the bankfull
indicators. The bankfull elevation should appear in the toolbar as
88.82. This number is displayed with greater precision than may be
necessary and will vary with the same error as the survey data. Save your
data.

Click the
summary tab to view an analysis of the cross section data. The screen will
display the anticipated stream classification A or G. The profile in the
impacted reach shows that the bankfull hydraulic slope is Sbkf =
0.004. With this slope, the stream classification will likely be a G
stream type.
We will
use this riffle cross section to estimate the bankfull discharge and other
design parameters so take care not to change the surveyed values. You can
copy the data from this screen using the toolbar and paste it into another cross
section to make changes to bankfull elevation or other parameters if you want to
preserve the original data.
Additional cross sections are
supplied to the database and analyzed in the same way. Typically pools,
riffles, runs and glides, if available, are measured in the impacted
reach. You can experiment with the cross section tools by adding other
cross sections to this reach node. Remember to set the type (riffle, pool,
etc.) each time you add a cross section.
Case Study -
Meadow Creek: Solution
1.
Setting up the
RIVERMorph database and project file
2.
Define the
Impacted Reach Cross-Section Data
3.
Add the
Profile data to the Reference Reach
4.
Add the
Sediment Data to the Impacted Reach and Reference Reach
5.
Classify the
Impacted Reach and Reference Reach
6.
Perform the
Natural Channel Design Calculations
7.
Layout the
Channel in a “Natural” Pattern
3. Add
the Profile data to the Reference Reach
We will
now add the surveyed longitudinal profile data to the Reference Reach to help
develop dimensionless ratios needed for natural channel design. Expand the
“Wolsey Branch Springs” River node and the “Reference Reach” Reach node.
Right-click on the “Profiles” node and add a profile. Before you enter
data, be sure the “rod” and “water as depth” state buttons are depressed in the
toolbar. Enter the following survey information in the blank Profile data
grid:
|
DIST |
CH |
WS |
BKF |
|
0 |
9.18 |
0.2 |
|
|
2 |
9.52 |
0.3 |
8.35 |
|
5 |
9.61 |
0.23 |
|
|
10 |
9.65 |
0.26 |
|
|
14 |
9.62 |
0.1 |
|
|
18 |
9.77 |
0.1 |
8 |
|
24 |
9.83 |
0.2 |
|
|
30 |
9.96 |
0.3 |
|
|
36 |
10.08 |
0.4 |
|
|
40 |
10.08 |
0.4 |
|
|
45 |
10.06 |
0.4 |
8.41 |
|
48 |
9.87 |
0.2 |
|
|
52 |
10 |
0.1 |
|
|
55 |
10.3 |
0.4 |
|
|
59 |
10.38 |
0.5 |
9.1 |
|
63 |
10.24 |
0.3 |
|
|
67 |
10.31 |
0.33 |
|
|
72 |
10.45 |
0.47 |
|
|
76 |
10.27 |
0.3 |
|
|
81 |
10.24 |
0.2 |
|
|
87 |
10.19 |
0.1 |
9.29 |
|
90 |
10.22 |
0.1 |
|
|
93 |
10.39 |
0.2 |
|
|
98 |
10.51 |
0.3 |
|
|
104 |
10.69 |
0.4 |
|
|
108 |
10.73 |
0.4 |
|
|
113 |
10.67 |
0.3 |
|
|
118 |
10.62 |
0.1 |
|
|
123 |
10.85 |
0.1 |
|
|
127 |
11 |
0.12 |
9.91 |
|
133 |
11.01 |
0.1 |
|
|
139 |
11.04 |
0.1 |
|
|
143 |
11.17 |
0.2 |
|
|
147 |
11.19 |
0.2 |
|
|
150 |
11.3 |
0.3 |
|
|
153 |
11.2 |
0.1 |
|
|
153.3 |
11.39 |
0.1 |
|
|
156 |
11.59 |
0.2 |
|
|
158 |
11.68 |
0.3 |
|
|
160 |
11.75 |
0.4 |
|
|
164 |
11.66 |
0.3 |
|
|
169 |
11.66 |
0.3 |
10.41 |
|
176 |
11.79 |
0.28 |
|
|
179 |
11.61 |
0.06 |
|
|
183 |
11.68 |
0.1 |
|
|
186 |
11.86 |
0.1 |
|
|
188 |
11.96 |
0.1 |
|
|
192 |
12.27 |
0.4 |
|
|
198 |
12.31 |
0.4 |
|
|
203 |
12.34 |
0.4 |
|
Since the cross sections have already been input,
you can place them along the profile by specifying their profile station at the
bottom of the data screen. The riffle cross section is located at profile
station 93 and the pool at 160. Enter this data into the grid.
Select the “Turning Points”
tab. Set the bench mark elevation to 880 and the backsite rod reading to 0
in the toolbar. Now you can return to the “Profile Data” tab and click the
“Elev” state button to view your data in real elevations. Data entry for
this profile is now complete.
To
measure slopes and depths, proceed to the “Measurements” tab and click the
“Graph” button. This will open a new window with the longitudinal profile
graph…which should look like this:

Use the
graph measurement tool to populate all of the fields on the “Measurements”
tab. When you have measured all of the facets, you should have results
similar to the following:

Once this
grid is complete, save your data. You are now finished with the profile
portion of the reference reach data set.
Case Study -
Meadow Creek: Solution
1.
Setting up the
RIVERMorph database and project file
2.
Define the
Impacted Reach Cross-Section Data
3.
Add the Profile
data to the Reference Reach
4.
Add the
Sediment Data to the Impacted Reach and Reference Reach
5.
Classify the
Impacted Reach and Reference Reach
6.
Perform the
Natural Channel Design Calculations
7.
Layout the
Channel in a “Natural” Pattern
4. Add the Sediment Data to
the Impacted Reach and Reference Reach
Create a
new pebble count data set in the reference reach named “Reach” for
reach-average. Add the following pebble count data:
.jpg)
Be sure
to set the sample type as “Reach” in the pebble count toolbar.
This
completes sediment data in the reference reach. The impacted reach will
have three particle data sets: “Reach Average” (pebble count), “Riffle” (pebble
count), and “Bar Sample” (sieves). Create these three data sets with the
following data:

Particle size data is now complete, RIVERMorph does
all of the analysis necessary to derive the sediment sizes used for sediment
transport competency analysis later on in the natural channel design
module. Be sure to save your data!
Case Study -
Meadow Creek: Solution
1.
Setting up the
RIVERMorph database and project file
2.
Define the
Impacted Reach Cross-Section Data
3.
Add the Profile
data to the Reference Reach
4.
Add the
Sediment Data to the Impacted Reach and Reference Reach
5.
Classify
the Impacted Reach and Reference Reach
6.
Perform the
Natural Channel Design Calculations
7.
Layout the
Channel in a “Natural” Pattern
5. Classify the Impacted
Reach and Reference Reach
Let’s start
with the Impacted Reach. Select the “Classification” node in the tree view
under the Impacted Reach. RIVERMorph will display the classification
screen.
1. Select
a pebble count from the list at the top of the screen to load the D50.
2. Enter
the Valley Morphology data.
3. Enter
the Location and Date of Survey.
4. Enter
the bankfull data as shown below. RIVERMorph will classify the data as it
is entered and you can always force a calculation by clicking a button on the
toolbar. The impacted reach is a G5c stream type, which means that it has
gully characteristics at low slope. Refer to Rosgen 1996 for a complete
description of this stream type. This stream type is not unexpected for
the impacted reach, it is what remains from a straightened or “ditched” channel
that is incising and becoming entrenched. Compare the classification to
the valley type you recorded near the top of the screen.

Now for the reference reach. This time we are going to
use the cross section and profile information already entered (refer to part 3
of this example) to help populate most of the fields in the classification
screen. We do this by activating the “Ratios” node, which is a “child” of
the “Classification” node. Expand the tree view in the reference reach,
expand the classification node and click “Ratios”. You will see a screen
similar to the one shown below.
The “Ratios” screen is used to record/view dimensionless
ratios that are properties of the active reach. RIVERMorph will load all
of your cross sections and profiles with the same reach identification.
On the “Dimension” tab, select the riffle cross section by
checking the box next to its name. Some data will be extracted from the
cross section and placed into the blank fields on this screen as shown
below. Next select the pool cross section to see which values are
updated.

Select the “Pattern” tab and enter the values shown
below. If you had used RIVERMorph’s GIS to measure this data it would
appear automatically.

Next select the “Profile” tab and then select a profile data
set from the Profile List. All of the saved values will populate the blank
cells. Click the “Update Dimensions Tab” button to copy the max. depth
values to the “Dimensions” tab, if you prefer.

The last page of the “Ratios” screen is for saving hydraulics
information. Complete the information as shown below.

Save your data. Close this window and refresh the
classification screen. RIVERMorph will populate the classification screen
with the average values you saved in the dimensionless ratios table.

Once the remainder of your data has been entered you should
have a classification screen that looks similar to the one shown above.
Important – check the Reference Reach box at the bottom of the
screen. Be sure to save your data.
This example has illustrated some techniques for measuring
and classifying your streams. This impacted reach is a G stream type,
which is a very unstable gully. The reference reach is a stable E stream
type with low width to depth ratio and some bedrock control. Next time
we’ll use this information to help design improvements for the impacted
reach.
Case Study -
Meadow Creek: Solution
1.
Setting up the
RIVERMorph database and project file
2.
Define the
Impacted Reach Cross-Section Data
3.
Add the Profile
data to the Reference Reach
4.
Add the
Sediment Data to the Impacted Reach and Reference Reach
5.
Classify the
Impacted Reach and Reference Reach
6.
Perform
the Natural Channel Design Calculations
7.
Layout the
Channel in a “Natural” Pattern
6. Perform the Natural Channel Design Calculations
This part of the example will illustrate the input and output
of a natural channel design using the reference reach approach and sediment
transport validation.
Expand the Impacted Reach, Designs node and click NCD in the
tree view. RIVERMorph will display the first screen, shown below, of a
step-by-step process that will walk you through the design sequence.

The list on this tab will contain all of the reference
reaches available in the database. This database only contains the one we
entered in the last part of this example. Select Wolsey Branch Springs
from the list (or whatever you named your reference reach). The
description will display some of the key parameters of this reach. Reach
condition and biological assessment refer to Pfankuch and SVAP results (see
Help).
After selecting a reference reach, proceed to the second tab
to enter the Boundary Conditions.
.jpg)
The Boundary Conditions screen contains all of the additional
input parameters. Change the valley slope to 0.002. This means that
earthwork will have to be performed to change elevations in the
floodplain. Change the Dmax Bar to 12. Field reviews have indicated
that the original bar sample contained large particles being deposited by local
bank erosion in the gully. A more precise estimate of the largest portion
of the bedload (characterized by deposits) is 12 mm. Select the options
shown above and click the Go Design! button.

The initial solution is shown on the Results tab. If
you are using sediment transport competency validation, then tweak the design
until you get a Green light in the Sediment Transport Competency portion of the
screen (shown above). Select a channel pattern that will match the riffle
geometry and the depth required to transport the sediment. This design is
valid for one meander wavelength of the new channel. You can link meanders
together to form chains, or vary the design from one to the other by selecting
different input parameters or by varying the solution.
Save your design. View the suggested meander pattern
and longitudinal profile on the Plan View and Long Pro tabs. Click the
Typical Sections tab to create riffle, pool and other cross sections.
.jpg)
The “rubber-band” cross section can be edited to produce a
variety of shapes that have the required bankfull parameters. Use
the reference reach cross sections as templates (see Help\Cross
Sections\Overlays). You can create a cross section node out of one of
these templates by clicking the “XS Exp” button.
Next, use the RIVERMorph output to layout your design on
paper. Generate a report of your meander wavelength calculations, which
can be sent to your CADD department for assistance in laying out the channel
plan form geometry. Similarly, generate reports for your NCD profile and
cross sectional analyses. If at any time you need to rework your plan
form, profile of cross sectional geometry during final plan preparation, you can
quickly check the impact of these changes on your design using RIVERMorph.
RIVERMORPH Example
113: Solution
1.
Setting up the RIVERMorph database
2.
Add the Cross Section data to the Impacted Reach and Reference
Reach
3.
Add the Profile data to the Reference Reach
4.
Add the Sediment Data to the Impacted Reach and Reference
Reach
5.
Classify the Impacted Reach and Reference Reach
6.
Perform the Natural Channel Design Calculations
7.
Layout the Channel in a “Natural” Pattern
7. Layout the Channel in a “Natural” Pattern
After
the design is complete, use the meander wavelength, radius of curvature, belt
width and sinuosity information from the natural channel design to layout the
pattern. RIVERMorph calculates the pattern on a "meander wavelength
scale". Coordinates of the pattern you have developed can be generated by
clicking on the report icon on the pattern tab, which can be given to your
drafting department. Remember to vary the pattern. Streams are naturally
variable and should not be designed with one constant pattern. With RIVERMorph
you can quickly iterate to find a number of patterns that yield acceptable
solutions. To vary the pattern, you can develop 4 or 5 acceptable "meander
wavelength scale" plan forms and then switch between these patterns in a random
order.