Title: Wind and Water Erosion under Alternate Land Uses: Insights from Ongoing Research
1 Wind and Water Erosion under Alternate Land Uses
Insights from Ongoing Research at the Santa Rita
Experimental Range
David D. Breshears1,2 Jason P. Field1,, Chris B.
Zou1 and
Jeffrey J. Whicker3
1 School of Natural Resources, University of
Arizona 2 Institute for the Study of Planet
Earth Department of Ecology and Evolutionary
Biology, University of Arizona 3 Health Physics
Measurements Group Health, Safety, and Radiation
Protection Division, Los Alamos National
Laboratory
2The Importance of Wind Erosion
Wind Erosion
3The Importance of Wind Erosion
Wind Erosion
4The Importance of Wind Erosion
Wind Erosion
5The Importance of Wind Erosion
Wind Erosion
Peters et al. 2006 BioScience
6On Saturday, this area of Texas had a dust storm
pass through. The sky turned brown, but there was
not much deposition of the fine material.Surface
winds had gusts well into the 30 mph range. It
was sort of a nice teaser for your talk.
7Competing contaminant transport mechanisms?
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10Conceptual Framework
Canopy
Intercanopy
Ecosystem Properties Dynamics
11Conceptual Framework
Canopy
Intercanopy
Ecosystem Properties Dynamics
Climate Variation Change
Land Use Management
12Contaminant Transport and Risk
Vegetation Dynamics and Biogeochemistry
Geomorphology
13Time Scales
Paleo
Annual
Disturbance Event
Event
Water Erosion
14Time Scales
Paleo
Annual
Disturbance Event
Event
Water Erosion
Wind Erosion
15Dryland Ecosystems
Barren / Disturbed
Agricultural
Grassland
Shrubland
Woodland
Forest
Water Erosion
16Dryland Ecosystems
Barren / Disturbed
Agricultural
Grassland
Shrubland
Woodland
Forest
Water Erosion
Wind Erosion
17Big Spring Number Eight (BSNE) Dust Samplers
18Breshears et al. Geomorphology in review
19Breshears et al. Geomorphology in review
20Breshears et al. Geomorphology in review
21Breshears et al. Geomorphology in review
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23Breshears et al. Geomorphology in review
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25Dimensions
- Water erosion
- Horizontal Fluxes
26Dimensions
- Water erosion
- Horizontal Fluxes
- Wind erosion
- Vertical and Horizontal Fluxes
27Footprint
Water erosion Often bordered
28Footprint
Water erosion Often bordered
Wind erosion Usually not bordered
29Common Erosional Processes
Detachment
Suspension
Transport
EROSION
30Common Erosional Processes
Detachment
Suspension
Transport
EROSION
Loss
31Common Erosional Processes
Detachment
Suspension
Transport
EROSION
Loss
32Erosion
Wind Erosion
Water Erosion
1-m wide gate
33Horizontal Transport
Gate rotates opening into wind
Wind-driven transport
Water-driven transport
1-m wide gate
34Study Sites
Shrubland
Grassland
Forest
Chiuahuan Desert Shrubland
Ponderosa Pine Forest
Shortgrass Steppe
Precipitation (mm)
300
370
500
Ground cover ()
66 (80)
79 (72)
98 (50)
Soil texture
Sand
Silt loam
Clay
35Soil Erosion Drivers
36- Problems
- Both contribute to total erosion rates
- No simultaneous field measures
- Relative magnitudes importance?
?
37- Problems
- Both contribute to total erosion rates
- No simultaneous field measures
- Relative magnitudes importance?
?
- Objectives
- Measure wind water erosion simultaneously
- Compare temporal dynamics of both processes
- Evaluate resource redistribution potential
38Measurements vs. Models
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40Wind-associated Measurements
Transport
Bagnold samplers- Horizontal flux
Weather stations
Erosion
1 and 3 m TSP samplers- Vertical flux
41Water-associated Measurements
-3m x 10m plots -Rainfall simulation of 60
mm/hr - measure runoff and sediment yield -3
replicate plots per site
42Transport
Erosion
Water
Wind
43Wind Erosion Temporal variation
44Wind Transport Spatial variation
45Event-based annual projections
Field Data
46Event-based annual projections
Field Data
Define erosion event threshold
47Event-based annual projections
Field Data
Define erosion event threshold
Determine events during sampling and multi-year
periods
48Event-based annual projections
Field Data
Define erosion event threshold
Determine events during sampling and multi-year
periods
Scale flux measurements
49Annual Erosion Projections
Water Erosion
Sediment yield (kg m-2 mm-1)
Rainfall rate gt infiltration rate
Rainfall amount per year greater than
threshold from multiyear data
ERwaterSYwater x rain/yr gt threshold
50Annual Erosion Projections
Water Erosion
Wind Erosion
Sediment yield (kg m-2 mm-1)
Soil flux (g/d/m2)
Rainfall rate gt infiltration rate
7 m/s
measurements gt 7 m/s during sampling and
from multiyear data
Rainfall amount per year greater than
threshold from multiyear data
gt 7 m/s(multiyear)
SFwind x
ERwind
ERwaterSYwater x rain/yr gt threshold
gt 7 m/s(sampling)
51Erosion
52Erosion
53Annual Transport Projections
Water Transport
Wind Transport
Sediment yield (kg m-1 mm-1)
Soil flux (g/d/m1)
Rainfall rate gt infiltration rate
7 m/s
measurements gt 7 m/s during sampling and
from multiyear data
Rainfall amount per year greater than
threshold from multiyear data
gt 7 m/s(multiyear)
SFwind x
TRwind
TRwaterSYwater x rain/yr gt threshold
gt 7 m/s(sampling)
54Transport
55Transport
56Shrubland
Grassland
Forest
Hypotheses
Wind
Water
Precipitation L M H
Near-surface wind velocity M H L
Ground Cover L M H
Mean bare patch size H M L
Soil clay content L H M
57Shrubland
Grassland
Forest
Hypotheses
Erosion Linear Scale
Wind
Water
Precipitation L M H
Near-surface wind velocity M H L
Ground Cover L M H
Mean bare patch size H M L
Soil clay content L H M
58Shrubland
Grassland
Forest
Hypotheses
Erosion Linear Scale
Wind
Water
Precipitation L M H
Near-surface wind velocity M H L
Ground Cover L M H
Mean bare patch size H M L
Soil clay content L H M
59Shrubland
Grassland
Forest
Hypotheses
Erosion Linear Scale
Wind
Water
Transport Log Scale
Precipitation L M H
Near-surface wind velocity M H L
Ground Cover L M H
Mean bare patch size H M L
Soil clay content L H M
60Shrubland
Grassland
Forest
Hypotheses
Erosion Linear Scale
Wind
Water
Transport Log Scale
Precipitation L M H
Near-surface wind velocity M H L
Ground Cover L M H
Mean bare patch size H M L
Soil clay content L H M
61Shrubland
Grassland
Forest
Hypotheses
Erosion Linear Scale
Wind
Water
Transport Log Scale
Precipitation L M H
Near-surface wind velocity M H L
Ground Cover L M H
Mean bare patch size H M L
Soil clay content L H M
62Shrubland
Grassland
Forest
Hypotheses
Erosion Linear Scale
Wind
Water
Transport Log Scale
Precipitation L M H
Near-surface wind velocity M H L
Ground Cover L M H
Mean bare patch size H M L
Soil clay content L H M
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64Sediment Check Dam
- Three undisturbed plots
(50 x 50 m) - Each plot contains
- Six self-orienting dust samplers
- A pair of sediment check dams
(bordered 3 x 10 m and unbordered)
- Sediment collection
- Sample collection every 7 14 days
- Sediment oven-dried at 60ÂșC
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67Summer monsoon
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72WIND vs. WATER Other Dryland Ecosystems?
WIND
WATER
Shrubland Grassland Forest
Breshears et al. 2003
73Soil Erosion Issues and Uncertainties
74Soil Erosion Issues and Uncertainties
Hydrological Bias?
75Soil Erosion Issues and Uncertainties
Hydrological Bias?
Disturbance?
76Soil Erosion Issues and Uncertainties
Hydrological Bias?
Disturbance?
Climate Change?
Walker and Steffen 1997
77- WIND erosion can dominate WATER erosion
in semiarid systems - Wind erosion appears to be more important
than suggested in the literature
78- WIND erosion can dominate WATER erosion
in semiarid systems - Wind erosion appears to be more important
than suggested in the literature - Simultaneous measures of both processes are
needed to - Improve model predictions
- Determine relative magnitudes and importance
- Address potential ecological implications
79Wind Erosion Graze Small increase Fire Large
increase
Field et al. - in prep
80Wind Erosion Graze Small increase Fire Large
increase
Water Erosion Graze Small increase Fire Large
increase
Field et al. - in prep
81Field et al. - in prep
82Variation with woody plant cover and percent bare
soil
83Variation with woody plant cover and percent bare
soil Wind erosion can exceed water erosion
84Variation with woody plant cover and percent bare
soil Wind erosion can exceed water
erosion Ecologically important process?
85Redistribution
Runoff from bare patches becomes runon to
herbaceous patches
Runon ( mm )
Precipitation ( mm)
Reid et al. 1999 Soil Sci. Soc. J. Am.
86Experimental Design
R
R
R
R
87Drought-induced Changes
Forest Cover
Allen Breshears 1998 - PNAS
88Post-fire erosion
Johansen et al. 2001 - Hydro. Proc.
89Post-fire erosion
Johansen et al. 2001 - Hydro. Proc.
90Post-fire erosion
Johansen et al. 2001 - Hydro. Proc.
91Applications
Contaminant Transport and Risk
Vegetation Dynamics and Biogeochemistry
Geomorphology