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Legacy Sediment Problems in Pennsylvania
  What to do about those dammed eroding
                streams?

                 Pennsylvania
                  Department of Environmental Protection


         Pennsylvania Legacy Sediment Workgroup

                        Jeffrey Hartranft
          Bureau of Waterways Engineering and Wetlands
         Division of Wetlands Encroachments and Training
Presentation Outline
• Legacy Sediment Examples and Definition


• A New Best Management Practice to Address the Problem


• Big Spring Run Demonstration Project


• Aquatic Resource Restoration Potential
Big Beaver Creek – Lancaster County, PA
                                Photos Courtesy Franklin & Marshall College
Conoy Creek – Lancaster County, PA
Mountain Creek - Cumberland County, PA
Seneca Creek, Maryland


   Photo Courtesy Franklin & Marshall College
Impact of Water-Powered Mills
     on Sediment Storage




              New dam




                        Courtesy Franklin & Marshall College
Typical Mill Dam and Valley Cross Section

                                            Riparian Zone


                                                   Time 2
                                                   Time 1




Upland                                                                                                                                Upland
                                                  Modern Substrate
 Soil                                                                                                                                  Soil
  Colluvium
                                           Legacy Sediment
                                                                                                                                 Colluvium
                   Natural Wetland Soils                                                   Natural Wetland Soils
                                 Gravel                                           Gravel
                                                         r   Gr
                                                     ate          oun
         Bedrock                              oun
                                                  dw                 dw
                                                                       a te
                                                                                                            Bedrock
                                           Gr                                 r




                                                                                                                   DEPARTMENT OF ENVIRONMENTAL
                                                                                                                           PROTECTION
Typical Valley Cross Section Evolution
                                           Riparian Zone
                                         Time 1
                                 Time 2 - Dam Breached
                                 Time 3 - Dam Breached




Upland                                               Modern Substrates                                                         Upland
 Soil         Legacy Sediment                                                          Legacy Sediment                          Soil
  Colluvium
                                                                                                                          Colluvium
                   Natural Wetland Soils                                              Natural Wetland Soils
                                 Gravel                                           Gravel
                                                         r   Gr
                                                     ate          oun
         Bedrock                              oun
                                                  dw                 dw
                                                                       a te
                                                                                                         Bedrock
                                           Gr                                 r




                                                                                                              DEPARTMENT OF ENVIRONMENTAL
                                                                                                                      PROTECTION
Mill density map based on the 1840 US Census and county boundaries.




More than 65,000 waterpowered mills existed along U.S. streams in the year 1840.
  The greatest density of mills occurred in the Piedmont and Ridge and Valley
                            physiographic province.

                    http://www.depweb.state.pa.us/chesapeake
Dam Locations from 1860-1870 Era Atlases




     http://www.depweb.state.pa.us/chesapeake
Photos Courtesy Franklin & Marshall College
http://www.depweb.state.pa.us/chesapeake
Natural Streams and the
 Legacy of Water-Powered
           Mills
   January 18, 2008 pp. 299-304
Robert C. Walter and Dorothy J. Merritts

    Franklin & Marshall
          College
            Lancaster, PA
Riparian Zones With Incised Channels

                                                 Riparian Zone

  Rural              • Bank Trampling                                                                • Stormwater                            Sub-
    &                                                                                                                                       Urban
                     • Upland Soil Erosion                                                           • Impervious surfaces                    &
Agriculture          • Few Trees / Shrubs                                                            • Few Trees / Shrubs                   Urban
                     • Manure                                                                        • Wastewater discharges




                                                                      Flood Flow
                                                                                                 Legacy Sediment
                      Legacy Sediment
   Gro
       und
          w   ater                                                                                                                    ter
                                                                                                                                  dwa
                        Natural Wetland Soils               Base Flow                          Natural Wetland Soils     Gro
                                                                                                                             un

                                      Gravel                                                Gravel
                                                                  r    Gr
                                                            ate             oun
                                                         dw
                          Bedrock               Gr
                                                   o   un                      dw
                                                                                 a te
                                                                                        r
                                                                                                         Bedrock


                           Conventional wisdom                                                                             DEPARTMENT OF ENVIRONMENTAL
                                                                                                                                   PROTECTION
Typical Existing Condition




                                                Flood
                                                Flow
       1850 AD (210PB)    Existing Root
                          Zone
                                             Bank-full   Flow   Legacy Sediment
~300 - ~10,000 BP (14C)
                           Hydric Paleosol     Base Flow        Hydric Soils
                                                    Gravel
                                                   Bedrock      Modern, inset bar


 •   Legacy sediment stored in valley bottoms predominantly was established by the combined
 effect of increased sediment supply from uplands and sediment trapping behind ubiquitous
 dams in many watersheds of the mid-Atlantic Region. (Walter and Merritts, 2008)
 •  Conceptual models linking channel condition and sediment yield exclusively with modern
 upland landuses are incomplete for valleys impacted by mill dams (Merritts, et al. 2011)

 •  Streambanks represent a significant sediment and nutrient source in watersheds where
 channels have incised through legacy sediment. (Walter, Merritts, Rahnis, 2007; 2010)
Big Spring Run - Type Section




                    Courtesy Franklin & Marshall College
Ecological Restoration Guiding Principles

Address ongoing causes of degradation.
   • Restoration efforts are likely to fail if the sources
       of degradation persist.
   • It is essential to correctly identify the causes of
   degradation and eliminate or remediate them.
   • Understanding a stream’s evolutionary trajectory is
   relevant to correctly diagnosing the problem, as well as
   to developing restoration approaches that are likely to
   be sustainable.

    “… understanding the legacy sediment problem is the
          first step in proposing a fix.”
       Bay Journal, March, 2007. Alliance for the Chesapeake Bay.
Natural Floodplain, Stream and Riparian Wetland
            Restoration Best Management Practice
                                              Conceptual Design

 Typical Existing Conditions                                 Proposed Restoration




                      Flood
                      Flow
Existing Root                                                                           Flood Flow
Zone
                   Bank-full   Flow   Legacy Sediment                                Bank-full     Flow
                                                          Restored Hydric Paleosol      Base Flow         Root Zone
 Hydric Paleosol     Base Flow        Hydric Soils
                          Gravel                                                         Gravel

                         Bedrock      Modern, inset bar
                                                                                         Bedrock



                                                              Natural Valley Morphology
Typical Existing Conditions                              Restoration
          9/13/2011                                            9/23/2011




                                                           Natural Valley
                                                            Morphology
                      Photos Courtesy Franklin & Marshall College
Flow Direction
2007 Banta Restoration Site, Lititz Run – Lancaster Co.




                                 Photo Courtesy Franklin & Marshall College
2007 Banta Restoration Site, Lititz Run – Lancaster Co.




                                 Photo Courtesy Franklin & Marshall College
2007 Banta Restoration Site, Lititz Run – Lancaster Co.
2011 Banta Restoration Site, Lititz Run – Lancaster Co.
Big Spring Run Natural Floodplain, Stream and
        Riparian Wetland Restoration Project




     We have assembled a multidisciplinary team of biologists,
ecologists, engineers, geomorphologists, geochemists, landowners,
 restoration practitioners, and construction experts (Hartranft et al,
USGS 015765195 Big Spring Run near Mylin Corners, PA
Funding Partners
PA Department of Environmental Protection
       Franklin & Marshall College
   US Environmental Protection Agency
          US Geological Survey
           Joseph V. Sweeney
      Chesapeake Bay Commission
 Foundation for Pennsylvania Watersheds
      PA Fish and Boat Commission
        Lancaster Farmland Trust




        Big Spring Run ca. 1930
                           Photo Courtesy Franklin & Marshall College
Monitoring and Research Partners
             Franklin and Marshall College
                US Geological Survey
 US Environmental Protection Agency (ORD & Region III)
      PA Department of Environmental Protection
             PA Fish and Boat Commission
               Johns Hopkins University
                Elizabethtown College
                 Penn State University




               Big Spring Run ca. 1930
                                  Photo Courtesy Franklin & Marshall College
Legacy Sediment Workgroup Collaborator
     Organizations and Individuals
 PA Department of Environmental Protection
 PA Fish and Boat Commission
 PA Department of Transportation
 US Environmental Protection Agency
 US Geological Survey
 Chesapeake Bay Commission
 Pennsylvania Environmental Council
 Franklin and Marshall College
 Penn State University
 Lafayette College
 Landstudies Inc.
 Rettew and Associates
 CDM
 Chesapeake Bay Foundation
 PA Farm Bureau
 American Rivers
 PA State Association of Township Supervisors
 Joseph Sweeney

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Land Conservation Strategies- Jeff Hartranft

  • 1. Legacy Sediment Problems in Pennsylvania What to do about those dammed eroding streams? Pennsylvania Department of Environmental Protection Pennsylvania Legacy Sediment Workgroup Jeffrey Hartranft Bureau of Waterways Engineering and Wetlands Division of Wetlands Encroachments and Training
  • 2. Presentation Outline • Legacy Sediment Examples and Definition • A New Best Management Practice to Address the Problem • Big Spring Run Demonstration Project • Aquatic Resource Restoration Potential
  • 3. Big Beaver Creek – Lancaster County, PA Photos Courtesy Franklin & Marshall College
  • 4. Conoy Creek – Lancaster County, PA
  • 5. Mountain Creek - Cumberland County, PA
  • 6. Seneca Creek, Maryland Photo Courtesy Franklin & Marshall College
  • 7. Impact of Water-Powered Mills on Sediment Storage New dam Courtesy Franklin & Marshall College
  • 8. Typical Mill Dam and Valley Cross Section Riparian Zone Time 2 Time 1 Upland Upland Modern Substrate Soil Soil Colluvium Legacy Sediment Colluvium Natural Wetland Soils Natural Wetland Soils Gravel Gravel r Gr ate oun Bedrock oun dw dw a te Bedrock Gr r DEPARTMENT OF ENVIRONMENTAL PROTECTION
  • 9. Typical Valley Cross Section Evolution Riparian Zone Time 1 Time 2 - Dam Breached Time 3 - Dam Breached Upland Modern Substrates Upland Soil Legacy Sediment Legacy Sediment Soil Colluvium Colluvium Natural Wetland Soils Natural Wetland Soils Gravel Gravel r Gr ate oun Bedrock oun dw dw a te Bedrock Gr r DEPARTMENT OF ENVIRONMENTAL PROTECTION
  • 10. Mill density map based on the 1840 US Census and county boundaries. More than 65,000 waterpowered mills existed along U.S. streams in the year 1840. The greatest density of mills occurred in the Piedmont and Ridge and Valley physiographic province. http://www.depweb.state.pa.us/chesapeake
  • 11. Dam Locations from 1860-1870 Era Atlases http://www.depweb.state.pa.us/chesapeake
  • 12. Photos Courtesy Franklin & Marshall College
  • 14. Natural Streams and the Legacy of Water-Powered Mills January 18, 2008 pp. 299-304 Robert C. Walter and Dorothy J. Merritts Franklin & Marshall College Lancaster, PA
  • 15. Riparian Zones With Incised Channels Riparian Zone Rural • Bank Trampling • Stormwater Sub- & Urban • Upland Soil Erosion • Impervious surfaces & Agriculture • Few Trees / Shrubs • Few Trees / Shrubs Urban • Manure • Wastewater discharges Flood Flow Legacy Sediment Legacy Sediment Gro und w ater ter dwa Natural Wetland Soils Base Flow Natural Wetland Soils Gro un Gravel Gravel r Gr ate oun dw Bedrock Gr o un dw a te r Bedrock Conventional wisdom DEPARTMENT OF ENVIRONMENTAL PROTECTION
  • 16. Typical Existing Condition Flood Flow 1850 AD (210PB) Existing Root Zone Bank-full Flow Legacy Sediment ~300 - ~10,000 BP (14C) Hydric Paleosol Base Flow Hydric Soils Gravel Bedrock Modern, inset bar • Legacy sediment stored in valley bottoms predominantly was established by the combined effect of increased sediment supply from uplands and sediment trapping behind ubiquitous dams in many watersheds of the mid-Atlantic Region. (Walter and Merritts, 2008) • Conceptual models linking channel condition and sediment yield exclusively with modern upland landuses are incomplete for valleys impacted by mill dams (Merritts, et al. 2011) • Streambanks represent a significant sediment and nutrient source in watersheds where channels have incised through legacy sediment. (Walter, Merritts, Rahnis, 2007; 2010)
  • 17. Big Spring Run - Type Section Courtesy Franklin & Marshall College
  • 18.
  • 19. Ecological Restoration Guiding Principles Address ongoing causes of degradation. • Restoration efforts are likely to fail if the sources of degradation persist. • It is essential to correctly identify the causes of degradation and eliminate or remediate them. • Understanding a stream’s evolutionary trajectory is relevant to correctly diagnosing the problem, as well as to developing restoration approaches that are likely to be sustainable. “… understanding the legacy sediment problem is the first step in proposing a fix.” Bay Journal, March, 2007. Alliance for the Chesapeake Bay.
  • 20. Natural Floodplain, Stream and Riparian Wetland Restoration Best Management Practice Conceptual Design Typical Existing Conditions Proposed Restoration Flood Flow Existing Root Flood Flow Zone Bank-full Flow Legacy Sediment Bank-full Flow Restored Hydric Paleosol Base Flow Root Zone Hydric Paleosol Base Flow Hydric Soils Gravel Gravel Bedrock Modern, inset bar Bedrock Natural Valley Morphology
  • 21. Typical Existing Conditions Restoration 9/13/2011 9/23/2011 Natural Valley Morphology Photos Courtesy Franklin & Marshall College
  • 23.
  • 24. 2007 Banta Restoration Site, Lititz Run – Lancaster Co. Photo Courtesy Franklin & Marshall College
  • 25. 2007 Banta Restoration Site, Lititz Run – Lancaster Co. Photo Courtesy Franklin & Marshall College
  • 26. 2007 Banta Restoration Site, Lititz Run – Lancaster Co.
  • 27. 2011 Banta Restoration Site, Lititz Run – Lancaster Co.
  • 28. Big Spring Run Natural Floodplain, Stream and Riparian Wetland Restoration Project We have assembled a multidisciplinary team of biologists, ecologists, engineers, geomorphologists, geochemists, landowners, restoration practitioners, and construction experts (Hartranft et al,
  • 29. USGS 015765195 Big Spring Run near Mylin Corners, PA
  • 30.
  • 31.
  • 32.
  • 33. Funding Partners PA Department of Environmental Protection Franklin & Marshall College US Environmental Protection Agency US Geological Survey Joseph V. Sweeney Chesapeake Bay Commission Foundation for Pennsylvania Watersheds PA Fish and Boat Commission Lancaster Farmland Trust Big Spring Run ca. 1930 Photo Courtesy Franklin & Marshall College
  • 34. Monitoring and Research Partners Franklin and Marshall College US Geological Survey US Environmental Protection Agency (ORD & Region III) PA Department of Environmental Protection PA Fish and Boat Commission Johns Hopkins University Elizabethtown College Penn State University Big Spring Run ca. 1930 Photo Courtesy Franklin & Marshall College
  • 35. Legacy Sediment Workgroup Collaborator Organizations and Individuals PA Department of Environmental Protection PA Fish and Boat Commission PA Department of Transportation US Environmental Protection Agency US Geological Survey Chesapeake Bay Commission Pennsylvania Environmental Council Franklin and Marshall College Penn State University Lafayette College Landstudies Inc. Rettew and Associates CDM Chesapeake Bay Foundation PA Farm Bureau American Rivers PA State Association of Township Supervisors Joseph Sweeney

Hinweis der Redaktion

  1. Illustration from:Mills on the Tsatsawassa: Techniques for Documenting Early 19th Century Water-Power Industry in Rural New York, by Philip L. Lord, Purple Mountain Press, Fleischmanns, New York, 1983.