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What Makes a Stream Healthy? ,[object Object]
Sediment transport balance
In-stream habitat & flow diversity
Bank stability (native plant roots)
Riparian buffer (streamside forest)
Active floodplain,[object Object]
Riffle/Pool sequences in alluvial streams
Step/Pool sequences in high-gradient streamsPhoto Credit: Eve Brantley, Auburn University
Sediment Transport Balance ,[object Object]
Alluvial bars and benches
Sufficient stream power to avoid aggradation,[object Object]
Bank Stability ,[object Object]
Low banks with low stress,[object Object]
Food and shade,[object Object]
Riparian wetlands
Stormwater retention & treatment,[object Object]
Lane’s Stream Balance Relationship
Causes of Instability ,[object Object]
Increase slope
Changes in sediment load
Loss of riparian buffer
Floodplain filling
Instream modification,[object Object]
10% 50% Development Impacts on the Water Cycle 55% 15% Courtesy NEMO, Univ. of CT
Impervious Surfaces Across the Landscape Center for Watershed Protection Sidewalks Roads Parking Driveways Buildings
More Runoff Arriving Faster NEMO The Science of Stormwater…
Hydrologic Responses to Urbanization Increased discharge Increased peak discharge Increased velocities Shorter time to peak flow More frequent bankfull events Increased flooding Lower baseflow Less ground water recharge
Increase Slope ,[object Object]
Lower Reservoir Water Surface
Dam Break
Geologic Uplift,[object Object]
Head Cut
I I I I I I I II II I I III III IV I III Original Nickpoint IV V I VI
G4c Alabama
Changes in Sediment Load ,[object Object]
Agriculture
Bank Erosion
Impoundments,[object Object]
Aggradation
Mid-channel bar and transverse bar directing flow into a high bank causing erosion and slumping
Debris Occurrence ,[object Object]
Depends on Riparian Stability
Beaver Dams,[object Object]
Impoundments Upstream: ,[object Object]
Deposition of fine material
Loss of habitatDownstream: ,[object Object]
Change in flow,[object Object]
Density
Potential,[object Object]
Streamside Forests (also known as riparian buffers) ,[object Object]
Buffers are the first line of defense against the impacts of polluted runoff
natural vegetation buffers are especially critical in urban areas,[object Object]
Altered States Due to Disturbance ,[object Object]
Straightening
Levees
Hardening
Mining,[object Object]
Stability Assessment http://www.epa.gov/warsss/index.htm
Entrenchment Ratio
Lateral Stability ,[object Object]
Bank Erosion (BEHI),[object Object]
Stream Channel Succession (WARSSS)
Stream Channel Succession (WARSSS) http://www.epa.gov/WARSSS/sedsource/successn.htm
Stability Assessment http://www.epa.gov/warsss/index.htm
Entrenchment Ratio
Lateral Stability ,[object Object]
Bank Erosion (BEHI),[object Object]
Bank ErosionMonitoring
Bank Erosion Hazard Index (BEHI)
Bank Erosion Hazard Index (BEHI)
Bank Erosion Hazard Index (BEHI)
Bankfull Stage:  Water fills the active channel and begins to spread onto the floodplain Stream Corridor Restoration: Principles, Processes, and Practices. 1998. Federal Interagency Stream Restoration Working Group.
Bank Height RatioVery Low
Bank Height RatioModerate
Bank Height RatioVery High
Root Depth RatioVery Low BEHI

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