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River Dynamics and Erosion
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Transcript of River Dynamics and Erosion
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River Dynamics and Erosion
Presented to:Great Bay Siltation Commission
December 1, 2008
Steve CoutureNHDES Rivers Coordinator
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http://des.nh.gov/organization/divisions/water/wmb/rive
rs/documents/designated_rivers.pdf
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Fluvial GeomorphologyFluvial Geomorphology
Fluvial
Geo
Morphology
Water
Earth
Land Shape
Fluvial Geomorphology = The Interaction of Water and theLandscape through which it Works
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Streams Are Dynamic
• Streams are dynamic systems that
balance water flow and sedimenttransport
• A river’s energy must be in balance withthe size and volume of sediment carriedby the river.
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Source: Ontario Ministry of Natural Resources, 2001
Striving for Balance
Sediment Load Transport Capacity
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Source: Ontario Ministry of Natural Resources, 2001
Striving for Balance
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Source: Ontario Ministry of Natural Resources, 2001
Striving for Balance
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Striving for Balance
• When river channels are altered by
humans or nature, the river must readjustto reach its former balance.
• Adjustments to Dimension, Profile andPattern
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Striving for Balance
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Warren Brook –
NHDES Biomonitoring Station, AlsteadOctober 21, 2004 October 17, 2005
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Source: Rosgen, 1996
Striving for Balance
Channel pattern
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Understanding Erosion
• Erosion is an ongoing natural process
• The rate of erosion is affected by soil
type, slope, precipitation, and velocity
• Erosion can be slowed but not stopped
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When is Erosion a Problem?
• People forget that rivers are systems in
dynamic equilibrium• Structures are built too too close to
eroding banks• Riparian buffers aren’t maintained
• Other natural or human activitiesaccelerate the natural rate of erosion
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• Flood mitigation• Water supply• Water quality
• Sediment storage and transport• Habitat• Recreation
• Transportation• Aesthetic qualities
Functions/Values of Healthy Streams
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Channel Equilibrium
Lane (1955)
Transport CapacitySediment LoadWidth, Depth, RoughnessWidth, Depth, Roughness
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And...many streams are rapidly changing dueto:
• Greater land development insusceptible areas
•Channels are enlarging due tostormwater conveyance
• Potential global climateshifts or cycles
•Traditional river managementdon’t support natural hydrology
Exeter River Watershed,
Raymond, 2007
Results
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Source: Vermont ANR, River Management Program, 2008
Results..High flows result in high
erosive power kept in thechannel,
instead of allowing theenergy of the water to
flow onto floodplain
Channel adjustments during high water events can have
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Channel adjustments during high water events can havedevastating economic consequences
NH Flooding: May 2006, April 2007 $75.6 Million In Damages
Suncook River, Epsom, 2006Piscsataquog River Watershed
Exeter River Watershed,
Raymond, 2007
Riverine Erosion Hazards a National Concern
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Cold River Alstead, New Hampshire, 2005
Clark Fork River Sanders Co, Montana, 1997
Cimarron River Logan Co, Oklahoma, 1998
Chapel Hill, NC, 2000
Riverine Erosion Hazards - a National Concern• 1/3 of the Nation’s Streams Experience Severe Erosion
(National Research Council, 1999)
• Catastrophic Erosion Costs $595 Million/year (2008 dollars)
Cycle of Escalating Costs Risks
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Source: Vermont ANR, River Management Program, 2008
Cycle of Escalating Costs, Risks,and Ecosystem Degradation
Floods andProperty Damage
Dredge, Berm
and Armor
Encroachment
Roaring Branch, Bennington, 1987
H C W Miti t Th I t ?
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Cold River, Shrewsbury, 2000
Sucker Brook, Williston, VT 2005
Honey Brook, Barre, VT 2007
How Can We Mitigate These Impacts?
Warren Brook, Alstead 2005
Suncook River, Epsom 2006
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Exeter River Geomorphic Assessment:
Restoring and Maintaining Healthy River Conditions
Fordway Brook
G hi A t
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Source: Vermont ANR, River Management Program, 2008
• Transport Capacity• Bed and Bank Materials• Sediment Supply
• Reference Condition• Major Adjustment
• Stream Type Departure
Inherent Sensitivity + Adjustment Processes
Geomorphic Assessment
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Source: Vermont ANR, River Management Program, 2008
Fluvial Erosion Hazard Planning
Hazard Type
VH7 - Very High
Based on identification of degree & likelihood of fluvialadjustments; assigns a corresponding level of risk
to infrastructure & property within the river corridor
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Source: Vermont ANR, River Management Program, 2008
Six (6)
channel widths
Extreme
(EX)
Six (6)
channel widths
Very High
(VH)
Six (6)
channel widths
High
(HI)
Four (4)
channel widths
Moderate
(MD)
Reference
channel width
Low
(LW)
Referencechannel width
Very Low(VL)
Belt WidthsFEH Rating
FEH Corridors based on
Erosion Hazard Ratings and Belt width
Hazard Type
MD6 – Moderate
Four (4) Channel
Widths
Hazard Type
VH7 - Very High
Six (6) channel widths
Breaking the Cycle
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Source: Vermont ANR, River Management Program, 2008
Breaking the CycleThrough FEH-based Corridor Protection
• Avoids Land Use Constraints Which Prevent Maintenance or Achievement of the Equilibrium Condition
• Provides Low Cost Solution
• Enhances Public Safety• Minimizes Economic Losses• Manages towards Sustainable Healthy Stream Conditions
NH S t f FEH
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NH Support for FEH:
• NH Hazard Mitigation Plan (DOS,2007)http://www.nh.gov/safety/divisions/bem/HazardMitigation/haz_mit_plan.html
• Independent Evaluation of Recent Flooding in New Hampshire. FEMA July 2008.http://des.nh.gov/organization/divisions/water/dam/documents/flood_report_nh_flooding_analysis.pdf
• Comprehensive Flood Management Study Commission,New Hampshire House Bill 648 (Chapter 179 Laws of 2007), Final Report, September 2008.
http://gencourt.state.nh.us/statstudcomm/reports/1853.pdf
• LSR 2009-H-0207-R authorizing fluvial erosion hazardzoning
Sponsors: Prime –Rep. Gene Andersen
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NH FEH Applicability to Great Bay:
• Chesepeake Bay Approach
– Watershed-management plans that address the protection, conservation, and restoration of
stream corridors, riparian forest buffers, &
wetlands would be developed to meet theproposed goals.
(USGS, Water-Resources Investigations Report
03-4123)
Regional S pporting Data for
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Regional Supporting Data for
Floodplain Restoration
• Black Creek Floodplain Restoration(Bakersfield & Fairfield, VT)
• 200 acres of reconnected Floodplain
• Year 1 Data – 950 cubic yards of sediment
– 1.1 tons of phosphorus(VTDEC, Unpublished 2008)
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Questions?