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Albuquerque, NM
Characterization and Evaluation of Riparian Buffers
on Sediment Load in Goodwin Creek Watershed
1
Henrique Momm
Joel Miranda
Department of Geosciences
Middle Tennessee State University
Ronald Bingner
Lindsey Yasarer
Robert Wells
Roger Kuhnle
USDA-ARS
National Sedimentation Laboratory
Albuquerque, NM
Riparian Vegetation
Albuquerque, NM
The primary function of riparian
buffers is to reduce overland flow
velocity, promote infiltration, and
sediment/chemical deposition
Characterization of Riparian Vegetation
Ponding of water upstream of
buffer, spreading of flow passing
through, and increased surface
roughness
A quantitative measure of the
sediment transport reduction by
riparian buffers
AGNPS-GIS Buffer Utility Feature (AGBUF)
Flow Buffer width
Local slope
One-dimensional representation (field scale)
Profile TE
Profile TE
Albuquerque, NM
Profile TE is aggregated to calculate
maximum TE (MTE) and catchment
area to riparian zone
Characterization of Riparian Vegetation (continued)
AnnAGNPS
Soil characteristics, sediment sizes, cell peak
flow, and peak flow to buffer
B
C
MTE = 90%
MTE = 47%
MTE = 97%
Actual TE
Sand
Actual TE
Small
Aggregates
Actual TE
Silt
MTE
“short-circuits” or concentrated flow path CFPs
Albuquerque, NM
Objective 1: Characterization and quantification of sediment trapping efficiency of natural
riparian vegetation at watershed scale
Goodwin Creek Watershed
Objective 2: The effect of concentrated flow paths to sediment yield and loads
Objective 3: Sediment loads of different particle sizes are contrasted by different
alternative scenarios with varying buffer width and concentrated flow paths assumptions
Topography: 1m DEM
2,271 cells (0.94ha)
911 reaches (170m)
Simulation: 1982-1991
Flow: 4 stream gauges
Sediment: 1 gauge
Two steps
calibration/validation
Albuquerque, NM
Channel Network
GCW Boundary
Buffer zone digitized
Goodwin Creek Watershed (continued)
10
100
1000
10000
100000
0 50 100 150 200 250 300 350 400 450 500 550 600
0
10
20
30
40
50
60
70
80
90
100
(a)
Frequency
Cumulativepercentage
Upstream contributing area, m
2
0
500
1000
1500
2000
2500
3000
0 10 20 30 40 50 60 70 80 90 100
0
10
20
30
40
50
60
70
80
90
100
(b)
Frequency
Cumulativepercentage
Flow path length, m
10
100
1000
10000
100000
0 50 100 150 200 250 300 350 400 450 500 550 600
0
10
20
30
40
50
60
70
80
90
100
(a)
Frequency
Cumulativepercentage
Upstream contributing area, m
2
3000
90
100
(b)
Albuquerque, NM
Goodwin Creek Watershed (continued)
Set ID
Riparian zone
layer
Buffer
width,
m and ft
CPFs
threshold,
ha
A Actual digitized 1985 variable none
B
0 digitized 1985 variable 0.0010
1 digitized 1985 variable 0.0025
2 digitized 1985 variable 0.0050
3 digitized 1985 variable 0.0100
4 digitized 1985 variable 0.0500
5 digitized 1985 variable 0.1000
6 digitized 1985 variable 0.5000
7 digitized 1985 variable 1.0000
C
8 GIS buffer analysis 2.29 7.5 none
9 GIS buffer analysis 4.57 15 none
10 GIS buffer analysis 9.14 30 none
11 GIS buffer analysis 15.24 50 none
12 GIS buffer analysis 30.48 100 none
D
13 GIS buffer analysis 30.48 100 0.0010
14 GIS buffer analysis 30.48 100 0.0025
15 GIS buffer analysis 30.48 100 0.0050
16 GIS buffer analysis 30.48 100 0.0100
17 GIS buffer analysis 30.48 100 0.0500
18 GIS buffer analysis 30.48 100 0.1000
19 GIS buffer analysis 30.48 100 0.5000
20 GIS buffer analysis 30.48 100 1.0000
Development of alternative scenarios
CFPs on actual conditions
Buffer width on managed
buffers
CFPs on managed buffers
Albuquerque, NM
Goodwin Creek Watershed (continued)
Development of alternative scenarios
Albuquerque, NM
RESULTS – Field Scale
0 25 5012.5
Meters
Reaches
Flow Accumulation
raster grid cells
High : 10773
Low : 0
CELL 7442 CELL 1912
Albuquerque, NM
RESULTS – Field Scale (continued)
0
20
40
60
80
100
120
140
1982 1983 1984 1985 1986 1987 1988 1989 1990 1991 1992
AnnAGNPS Cell: 7442
SedimentTrapped-Silt[Mg]
2.29m(7.5ft)
4.57m(15ft)
9.14m(30ft)
15.24m(50ft)
30.48m(100t)
0
20
40
60
80
100
120
140
1982 1983 1984 1985 1986 1987 1988 1989 1990 1991 1992
AnnAGNPS Cell: 1912
SedimentTrapped-Silt[Mg]
0
20
40
60
80
100
120
140
1982 1983 1984 1985 1986 1987 1988 1989 1990 1991 1992
AnnAGNPS Cell: 7442
SedimentTrapped-Silt[Mg]
0.001 ha
0.005 ha
0.050 ha
0.500 ha
1.000 ha
0
20
40
60
80
100
120
140
1982 1983 1984 1985 1986 1987 1988 1989 1990 1991 1992
AnnAGNPS Cell: 1912
SedimentTrapped-Silt[Mg]
57
74
95
131
Considering 30.48m (100ft):
• Cell 7442 ->
• 65% of cell area drains into buffer
• MTE: 99%
• Cell 1992 ->
• 77% of cell area drains into buffer
• MTE: 88%
Shape of catchment,
flow path patterns
topography
Albuquerque, NM
RESULTS – Field Scale (continued)
0
20
40
60
80
100
120
140
1982 1983 1984 1985 1986 1987 1988 1989 1990 1991 1992
AnnAGNPS Cell: 7442
SedimentTrapped-Silt[Mg]
0.001 ha
0.005 ha
0.050 ha
0.500 ha
1.000 ha
0
20
40
60
80
100
120
140
1982 1983 1984 1985 1986 1987 1988 1989 1990 1991 1992
AnnAGNPS Cell: 1912
SedimentTrapped-Silt[Mg]
Considering 30.48m (100ft) with DA
threshold of 0.05ha and 0.5ha:
• Cell 1992 ->
• Same results
• Cell 7442 ->
• Significant difference in sediment
trapping efficiency
One flow path that drains 62% of total cell area (0.7ha)
0 25 5012.5
Meters
Reaches
Flow Accumulation
raster grid cells
High : 10773
Low : 0
Albuquerque, NM
RESULTS – Watershed scale
Station 14 Comparing observed versus simulated
1985 buffer with varying assumptions of CFPs
Real condition between no buffer and buffer with no CFPS
• No buffer not realistic -> locations with several meters of forest
• No CFPs not realistic -> not managed
0.35
0.40
0.45
0.50
0.55
0.60
0.65
0.70
0.75
0 1 2 3 4 5 6 7
Nash-Sutcliffe
Alternative Scenarios
Small
Sand
Total
Actual-Small
Actual-Sand
Actual-Total
0.00
5.00
10.00
15.00
20.00
25.00
30.00
0 1 2 3 4 5 6 7
PBIAS
Alternative Scenarios
Small
Sand
Total
Actual-Small
Actual-Sand
Actual-Total
Less CFPs Less CFPs
Albuquerque, NM
RESULTS – Watershed scale
OUTLET – Constructed buffers
Optimum width
Spatial configuration
Complex interaction
between CFPs and
buffer width
0.65
0.70
0.75
0.80
0.85
0.90
0.95
0 5 10 15 20 25 30 35
y=-0.5771 *x-0.3958
+ 1.079
Adjusted R2
: 0.9998
(a)
AverageTE,%
Riparian buffer width, m
Constructed
0.10
0.20
0.30
0.40
0.50
0.60
0.70
0.80
0.90
1.00
1.10
0 5 10 15 20 25 30 35
y=2.098 *x
-0.2934
- 0.5851
Adjusted R
2
: 0.9979
y=0.1288 *x-0.3037
+ 0.1776
Adjusted R2
: 0.9988
(b)
Sedimentyield,Mg/ha/yr
Riparian buffer width, m
Clay Silt
0.30
0.40
0.50
0.60
0.70
0.80
0.90
0.001 0.01 0.1 1
y=0.7798 *x0.1498
+ 0.0976
Adjusted R
2
: 0.9934
y=0.4179 *x0.1324
+ 0.2766
Adjusted R2
: 0.9977
(c)
AverageTE,%
Threshold drainage contributing area, ha
Constructed Natural
0.20
0.40
0.60
0.80
1.00
1.20
1.40
1.60
1.80
2.00
2.20
0.001 0.01 0.1 1
y=-1.864 *x
0.3359
+ 2.261
Adjusted R
2
: 0.9909
y=-0.1089 *x
0.3788
+ 0.3474
Adjusted R2
: 0.9958
(d)
Sedimentyield,Mg/ha/yr
Threshold drainage contributing area, ha
Clay Silt
Albuquerque, NM
Take Home
• Natural riparian vegetation contributes to sediment TE
• Sediment yield – CLAY 0.51 Mg/ha/yr (no buffer) vs. 0.32 Mg/ha/yr (buffer)
• Sediment yield – SILT 3.73 Mg/ha/yr (no buffer) vs. 1.43 Mg/ha/yr (buffer)
• Sediment yield – SAND 0.14 Mg/ha/yr (no buffer) vs. 0.04 Mg/ha/yr (buffer)
No Buffer Buffer no CFPs
Actual conditions
• Importance of buffer maintenance
• Significant impact of CFPs to reduce the TE of riparian vegetation
• Potential similar TE of well maintained narrower buffer than wider with CFPs
• Less land removed from production
Albuquerque, NM
Take Home (continued)
• There isn’t a “one size fits all” solution
• Shape of field catchment in relation to stream
• Flow path pattern (berms, topographic swales, furrows, etc.)
• Sediment size and/or chemical in study site
• Future Studies
• Evaluation of modeling technology with field-based measurements of
riparian vegetation in the field
• Methods for optimal location and configuration (where and how wide)
• Integration with other conservation practices (wetlands, grassed waterways,
cover crops, etc).
Albuquerque, NM
Thank you
Questions??
Albuquerque, NM
Goodwin Creek Watershed (continued)
Albuquerque, NM
RESULTS – Watershed scale
OUTLET – Constructed buffers
(A) (B)
(C) (D)
Cell load per unit of area
Mg/ha/yr
< 0.013
0.013 - 0.625
0.625 - 1.476
> 1.476001
0 2 41
Kilometers

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Characterization and evaluation of riparian buffers on sediment load

  • 1. Albuquerque, NM Characterization and Evaluation of Riparian Buffers on Sediment Load in Goodwin Creek Watershed 1 Henrique Momm Joel Miranda Department of Geosciences Middle Tennessee State University Ronald Bingner Lindsey Yasarer Robert Wells Roger Kuhnle USDA-ARS National Sedimentation Laboratory
  • 3. Albuquerque, NM The primary function of riparian buffers is to reduce overland flow velocity, promote infiltration, and sediment/chemical deposition Characterization of Riparian Vegetation Ponding of water upstream of buffer, spreading of flow passing through, and increased surface roughness A quantitative measure of the sediment transport reduction by riparian buffers AGNPS-GIS Buffer Utility Feature (AGBUF) Flow Buffer width Local slope One-dimensional representation (field scale) Profile TE Profile TE
  • 4. Albuquerque, NM Profile TE is aggregated to calculate maximum TE (MTE) and catchment area to riparian zone Characterization of Riparian Vegetation (continued) AnnAGNPS Soil characteristics, sediment sizes, cell peak flow, and peak flow to buffer B C MTE = 90% MTE = 47% MTE = 97% Actual TE Sand Actual TE Small Aggregates Actual TE Silt MTE “short-circuits” or concentrated flow path CFPs
  • 5. Albuquerque, NM Objective 1: Characterization and quantification of sediment trapping efficiency of natural riparian vegetation at watershed scale Goodwin Creek Watershed Objective 2: The effect of concentrated flow paths to sediment yield and loads Objective 3: Sediment loads of different particle sizes are contrasted by different alternative scenarios with varying buffer width and concentrated flow paths assumptions Topography: 1m DEM 2,271 cells (0.94ha) 911 reaches (170m) Simulation: 1982-1991 Flow: 4 stream gauges Sediment: 1 gauge Two steps calibration/validation
  • 6. Albuquerque, NM Channel Network GCW Boundary Buffer zone digitized Goodwin Creek Watershed (continued) 10 100 1000 10000 100000 0 50 100 150 200 250 300 350 400 450 500 550 600 0 10 20 30 40 50 60 70 80 90 100 (a) Frequency Cumulativepercentage Upstream contributing area, m 2 0 500 1000 1500 2000 2500 3000 0 10 20 30 40 50 60 70 80 90 100 0 10 20 30 40 50 60 70 80 90 100 (b) Frequency Cumulativepercentage Flow path length, m 10 100 1000 10000 100000 0 50 100 150 200 250 300 350 400 450 500 550 600 0 10 20 30 40 50 60 70 80 90 100 (a) Frequency Cumulativepercentage Upstream contributing area, m 2 3000 90 100 (b)
  • 7. Albuquerque, NM Goodwin Creek Watershed (continued) Set ID Riparian zone layer Buffer width, m and ft CPFs threshold, ha A Actual digitized 1985 variable none B 0 digitized 1985 variable 0.0010 1 digitized 1985 variable 0.0025 2 digitized 1985 variable 0.0050 3 digitized 1985 variable 0.0100 4 digitized 1985 variable 0.0500 5 digitized 1985 variable 0.1000 6 digitized 1985 variable 0.5000 7 digitized 1985 variable 1.0000 C 8 GIS buffer analysis 2.29 7.5 none 9 GIS buffer analysis 4.57 15 none 10 GIS buffer analysis 9.14 30 none 11 GIS buffer analysis 15.24 50 none 12 GIS buffer analysis 30.48 100 none D 13 GIS buffer analysis 30.48 100 0.0010 14 GIS buffer analysis 30.48 100 0.0025 15 GIS buffer analysis 30.48 100 0.0050 16 GIS buffer analysis 30.48 100 0.0100 17 GIS buffer analysis 30.48 100 0.0500 18 GIS buffer analysis 30.48 100 0.1000 19 GIS buffer analysis 30.48 100 0.5000 20 GIS buffer analysis 30.48 100 1.0000 Development of alternative scenarios CFPs on actual conditions Buffer width on managed buffers CFPs on managed buffers
  • 8. Albuquerque, NM Goodwin Creek Watershed (continued) Development of alternative scenarios
  • 9. Albuquerque, NM RESULTS – Field Scale 0 25 5012.5 Meters Reaches Flow Accumulation raster grid cells High : 10773 Low : 0 CELL 7442 CELL 1912
  • 10. Albuquerque, NM RESULTS – Field Scale (continued) 0 20 40 60 80 100 120 140 1982 1983 1984 1985 1986 1987 1988 1989 1990 1991 1992 AnnAGNPS Cell: 7442 SedimentTrapped-Silt[Mg] 2.29m(7.5ft) 4.57m(15ft) 9.14m(30ft) 15.24m(50ft) 30.48m(100t) 0 20 40 60 80 100 120 140 1982 1983 1984 1985 1986 1987 1988 1989 1990 1991 1992 AnnAGNPS Cell: 1912 SedimentTrapped-Silt[Mg] 0 20 40 60 80 100 120 140 1982 1983 1984 1985 1986 1987 1988 1989 1990 1991 1992 AnnAGNPS Cell: 7442 SedimentTrapped-Silt[Mg] 0.001 ha 0.005 ha 0.050 ha 0.500 ha 1.000 ha 0 20 40 60 80 100 120 140 1982 1983 1984 1985 1986 1987 1988 1989 1990 1991 1992 AnnAGNPS Cell: 1912 SedimentTrapped-Silt[Mg] 57 74 95 131 Considering 30.48m (100ft): • Cell 7442 -> • 65% of cell area drains into buffer • MTE: 99% • Cell 1992 -> • 77% of cell area drains into buffer • MTE: 88% Shape of catchment, flow path patterns topography
  • 11. Albuquerque, NM RESULTS – Field Scale (continued) 0 20 40 60 80 100 120 140 1982 1983 1984 1985 1986 1987 1988 1989 1990 1991 1992 AnnAGNPS Cell: 7442 SedimentTrapped-Silt[Mg] 0.001 ha 0.005 ha 0.050 ha 0.500 ha 1.000 ha 0 20 40 60 80 100 120 140 1982 1983 1984 1985 1986 1987 1988 1989 1990 1991 1992 AnnAGNPS Cell: 1912 SedimentTrapped-Silt[Mg] Considering 30.48m (100ft) with DA threshold of 0.05ha and 0.5ha: • Cell 1992 -> • Same results • Cell 7442 -> • Significant difference in sediment trapping efficiency One flow path that drains 62% of total cell area (0.7ha) 0 25 5012.5 Meters Reaches Flow Accumulation raster grid cells High : 10773 Low : 0
  • 12. Albuquerque, NM RESULTS – Watershed scale Station 14 Comparing observed versus simulated 1985 buffer with varying assumptions of CFPs Real condition between no buffer and buffer with no CFPS • No buffer not realistic -> locations with several meters of forest • No CFPs not realistic -> not managed 0.35 0.40 0.45 0.50 0.55 0.60 0.65 0.70 0.75 0 1 2 3 4 5 6 7 Nash-Sutcliffe Alternative Scenarios Small Sand Total Actual-Small Actual-Sand Actual-Total 0.00 5.00 10.00 15.00 20.00 25.00 30.00 0 1 2 3 4 5 6 7 PBIAS Alternative Scenarios Small Sand Total Actual-Small Actual-Sand Actual-Total Less CFPs Less CFPs
  • 13. Albuquerque, NM RESULTS – Watershed scale OUTLET – Constructed buffers Optimum width Spatial configuration Complex interaction between CFPs and buffer width 0.65 0.70 0.75 0.80 0.85 0.90 0.95 0 5 10 15 20 25 30 35 y=-0.5771 *x-0.3958 + 1.079 Adjusted R2 : 0.9998 (a) AverageTE,% Riparian buffer width, m Constructed 0.10 0.20 0.30 0.40 0.50 0.60 0.70 0.80 0.90 1.00 1.10 0 5 10 15 20 25 30 35 y=2.098 *x -0.2934 - 0.5851 Adjusted R 2 : 0.9979 y=0.1288 *x-0.3037 + 0.1776 Adjusted R2 : 0.9988 (b) Sedimentyield,Mg/ha/yr Riparian buffer width, m Clay Silt 0.30 0.40 0.50 0.60 0.70 0.80 0.90 0.001 0.01 0.1 1 y=0.7798 *x0.1498 + 0.0976 Adjusted R 2 : 0.9934 y=0.4179 *x0.1324 + 0.2766 Adjusted R2 : 0.9977 (c) AverageTE,% Threshold drainage contributing area, ha Constructed Natural 0.20 0.40 0.60 0.80 1.00 1.20 1.40 1.60 1.80 2.00 2.20 0.001 0.01 0.1 1 y=-1.864 *x 0.3359 + 2.261 Adjusted R 2 : 0.9909 y=-0.1089 *x 0.3788 + 0.3474 Adjusted R2 : 0.9958 (d) Sedimentyield,Mg/ha/yr Threshold drainage contributing area, ha Clay Silt
  • 14. Albuquerque, NM Take Home • Natural riparian vegetation contributes to sediment TE • Sediment yield – CLAY 0.51 Mg/ha/yr (no buffer) vs. 0.32 Mg/ha/yr (buffer) • Sediment yield – SILT 3.73 Mg/ha/yr (no buffer) vs. 1.43 Mg/ha/yr (buffer) • Sediment yield – SAND 0.14 Mg/ha/yr (no buffer) vs. 0.04 Mg/ha/yr (buffer) No Buffer Buffer no CFPs Actual conditions • Importance of buffer maintenance • Significant impact of CFPs to reduce the TE of riparian vegetation • Potential similar TE of well maintained narrower buffer than wider with CFPs • Less land removed from production
  • 15. Albuquerque, NM Take Home (continued) • There isn’t a “one size fits all” solution • Shape of field catchment in relation to stream • Flow path pattern (berms, topographic swales, furrows, etc.) • Sediment size and/or chemical in study site • Future Studies • Evaluation of modeling technology with field-based measurements of riparian vegetation in the field • Methods for optimal location and configuration (where and how wide) • Integration with other conservation practices (wetlands, grassed waterways, cover crops, etc).
  • 17. Albuquerque, NM Goodwin Creek Watershed (continued)
  • 18. Albuquerque, NM RESULTS – Watershed scale OUTLET – Constructed buffers (A) (B) (C) (D) Cell load per unit of area Mg/ha/yr < 0.013 0.013 - 0.625 0.625 - 1.476 > 1.476001 0 2 41 Kilometers

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