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STUDY OF THE ROUGHNESS CHARACTERISTICS OF
PLANT SPECIES IN
CALIFORNIA RIVERS
By
U.C.Davis J.Amorocho Hydraulics Laboratory
The objectives of this study:
1. to determine the hydraulic roughness (Manning’s n) associated with each of California native plant species under various flow conditions (from low to high flows),
2. to compare these roughness values to bare soil roughness conditions that may be present on the floodplains in river reaches where these plants occur,
3. to quantify the response of stems of known density, diameter and height of various native plant species under different flow conditions;
Flume Setup for Roughness Study
H
Depth Control Weir
x =49'
31'
x =60'
V
2’
Flume tail tank
x =0'
x =66'
Pumps
x =17'
17' 32'
6’
80'9'
Head
Tank
Bare Soil Sample Layout
4 ft bin Width
Flume width 5 ft
8 ft
6 ft
2 ft
Flume Body Cross-section
Partial Plan View
8 bins with a total distance of 32 ft
bin length 4 ft
4 ft
STREAMBED BARE SOIL SAMPLE
PREPARATION
Measurement Instrument
1) SonTek ADV 3-D Velocimeter
Velocity profiles at various locations
2) Point Gages with Stilling Tube
Hydraulic head
3) Ultrasound Flow Meter:
Total Discharge
4) Digital Floater
Water surface wave
Hydraulic Measurements
For each individual experimental setup for a plant species, three different depths (three different hydraulic radii)
are taken, where depths depend upon the species being studied.
For each depth, three different cross-sectional average velocities are considered
(within the range of 0.5 – 5 ft/second).
Therefore, for each experimental setup, nine different depth – velocity combinations are considered.
Each experimental setup for a particular plant species is repeated three times, with new plant patches each time,
to obtain three independent replicates.
Velocity measurement locations in a cross-section
4 ft bin Width
Flume width 5 ft
8 ft
6 ft
2 ft
4 ft bin Width
Flume width 5 ft
8 ft
6 ft
2 ft
Water depth higher than 2 ft
Water depth lower than 2 ft
The velocity head profile is determined from the cross-sectionally-averaged velocity measurements at three specified locations in the plant patch section.
Hydraulic radius is directly measured (depth and width of flow) through the plant patch section.
The friction slope is determined from the measured total energy head (hydraulic head plus velocity head) gradient under each average depth – average velocity combination.
The hydraulic head gradient is determined from measuring three cross-sectionally-averaged water depths (water surface elevations) along the longitudinal direction of the flume within the plant patch section.
A Manning’s roughness coefficient that corresponds to the specified plant species and specified average hydraulic radius – average velocity condition is calculated.
PRELIMINARY EXPERIMENTAL RESULTS
BASED UPON
FIRST BARE SOIL REPLICATE
WHILE
STANDARDIZING THE EXPERIMENTAL PROCEDURES
Water Surface and Energy Gradient LineS61 (H=1 ft, V=1 ft/s)
1
1.005
1.01
1.015
1.02
15 20 25 30 35 40 45 50
x(ft)
ft
E= (H + hv)
H(Point Gage)
Water Surface and Energy Gradient LineS71(H=1 ft, V=2 ft/s)
0.98
1
1.02
1.04
1.06
1.08
15 20 25 30 35 40 45 50x(ft)
ft
E= (H + hv)
H(Point Gage)
Water Surface and Energy Gradient LineS51(H=2.5ft, V=5 ft/s)
2.50
2.60
2.70
2.80
2.90
3.00
15 20 25 30 35 40 45 50
x(ft)
ft
E= (H + hv)
H (Point Gage)
Water Surface and Energy Gradient LineS21 (H=5ft,V=2ft/s)
5.155.165.175.185.195.205.215.225.23
15 20 25 30 35 40 45 50
x(ft)
ft
E= (H + hv)
H (Point Gage)
Water Surface and Energy Gradient LineS41(H=2.5,V=2ft/s)
2.542.552.562.572.582.592.6
2.612.62
15 20 25 30 35 40 45 50
x(ft)
ft
E= (H + hv)
H(Point Gage)
Measured Water Surface and Energy Gradient Lines
0.0100
0.0120
0.0140
0.0160
0.0180
0.0200
0.0220
0.0240
0.0260
0.0280
0 100,000 200,000 300,000 400,000 500,000
Reynolds Number
Ma
nn
ing
's R
ou
gh
ne
ss
Co
eff
icie
nt
y = 0.0199x + 0.0121
R2 = 0.8703
0.0100
0.0120
0.0140
0.0160
0.0180
0.0200
0.0220
0.0240
0.0260
0.0280
0.000 0.200 0.400 0.600 0.800
Froude Number
Ma
nn
ing
's R
ou
gh
ne
ss
Co
eff
icie
nt