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Ecosystem Tradeoffs<br />

Associated with Tidal Marsh<br />

Sills<br />

Karen Duhring<br />

Marine Scientist<br />

Virginia Institute of Marine Science<br />

International Submerged Lands Management Conference<br />

October 29, 2007


<strong>Presentation</strong> Outline<br />

Typical erosion protection projects in<br />

Virginia’s portion of Chesapeake Bay<br />

Preferred approaches from an ecosystem<br />

perspective<br />

Marsh sill case studies<br />

Summary of ecosystem tradeoffs<br />

associated with marsh sills


Typical Erosion Protection Projects<br />

on Virginia’s s Tidal Shorelines<br />

Revetments<br />

Bulkheads<br />

Bank Grading & Structures


Northumberland Co.<br />

County<br />

Lancaster Co.<br />

Permit site<br />

Potomac<br />

River<br />

Chesapeake<br />

Bay<br />

Tidal Shoreline Permit<br />

Sites<br />

Lower Northern Neck,<br />

VA<br />

1999-2007<br />

Widespread<br />

distribution<br />

regardless of energy<br />

Middlesex<br />

Co.<br />

Rappahannock River<br />

Cumulative impacts<br />

throughout<br />

watersheds


Cumulative Impact of<br />

Shoreline Hardening<br />

Cumulative length new<br />

structures permitted<br />

each year<br />

18.2 miles / yr average<br />

Cumulative length<br />

permitted 1993-2006<br />

255.5 miles<br />

Direct loss & isolation<br />

of tidal wetlands<br />

Source:<br />

VIMS Tidal Shoreline Permit Database


Order of Preferred Approaches<br />

for Shoreline Protection<br />

1. No Action<br />

Leave shoreline in<br />

natural condition or<br />

restore habitats<br />

Reduce risk through land<br />

use changes<br />

2. Non-Structural<br />

Maximize vegetation<br />

cover


Order of Preferred Approaches<br />

for Shoreline Protection<br />

1. No Action<br />

Leave shoreline in<br />

natural condition or<br />

restore habitats<br />

Reduce risk through land<br />

use changes<br />

2. Non-Structural<br />

Maximize vegetation<br />

cover<br />

3.“Hybrid”<br />

Use structures to support<br />

natural erosion buffers<br />

(e.g. tidal marshes,<br />

beaches)<br />

4. Revetments<br />

5. Bulkheads


Preferred Approaches<br />

that may affect public submerged lands<br />

Tidal marsh enhancement or creation<br />

Beach nourishment in sand-limited system<br />

Bank grading with cut and fill to create or enhance<br />

tidal marsh<br />

Offshore breakwater systems for high-energy beach<br />

shorelines<br />

Tidal marsh sills for low to medium energy shorelines


Gapped sills with backfill from<br />

graded bank<br />

Marsh Sill<br />

with Planted Marsh<br />

Low profile revetment<br />

backfilled with sand to<br />

create or enhance tidal<br />

marsh<br />

Imported sediment from<br />

upland source or suitable<br />

bank grading material<br />

Offensive approach<br />

structures built in sand transport<br />

region to address impinging waves<br />

before they reach upland areas


Typical Sill Cross-Section<br />

Planted tidal marsh<br />

Height near mean high<br />

water elevation<br />

Average 20-30 feet<br />

Source: Jefferson Patterson Park project, Maryland


Marsh Toe Revetment<br />

Natural Marsh Edge Stabilization<br />

Low profile<br />

revetment placed<br />

along the eroding<br />

edge of existing<br />

tidal marsh


VIMS Study<br />

36 marsh structures in 2004-2005<br />

2005<br />

A Survey of the Effectiveness of<br />

Existing Marsh Toe Protection<br />

Structures in Virginia<br />

July 2006<br />

K.A. Duhring, T.A. Barnard &<br />

C.S. Hardaway, Jr.


Marsh Sill at VIMS<br />

Marsh Sill at VIMS<br />

since 1983<br />

Salt Bushes<br />

Saltmarsh Cordgrass<br />

Stone Sill


Before<br />

After 1 year<br />

High, vertical, sandy bank<br />

Undercutting erosion at bank toe<br />

Narrow, patchy fringe marsh + 5 ft wide<br />

Tidal creek with regular boat wakes<br />

Graded bank now stable<br />

Suitable material used for backfill<br />

Planted tidal marsh + 25 ft wide<br />

Gapped sills (3)


Combination Approach<br />

Graded Bank with cut & fill + Planted Tidal Marsh + Gapped Sills<br />

Tidal opening<br />

Saltmeadow hay<br />

Spartina patens<br />

Smooth<br />

cordgrass<br />

Spartina<br />

alterniflora<br />

Approx. mean high water<br />

+ 25 feet


Before<br />

After 1 year<br />

Regular high<br />

tides<br />

Remnant tidal marsh at high<br />

energy setting<br />

Extensive beds of submerged<br />

aquatic vegetation (SAV)<br />

Existing revetment stabilizing<br />

bank<br />

Desire to protect 1 oak tree from<br />

saltwater intrusion<br />

“Perched” marsh not<br />

accessible to marine organisms


Tidal Openings<br />

Straight<br />

Offset<br />

gapped<br />

Offset end at<br />

upland revetment


Before<br />

After 10 years<br />

Non-vegetated sand/mud,<br />

narrow intertidal zone<br />

Open water (before sill)<br />

Sediment movement<br />

Nutrient cycling by infaunal<br />

community<br />

Eroding upland bank (not<br />

visible)<br />

Stone sill & wide vegetated intertidal area<br />

Less open water area<br />

Sediment trapping<br />

Nutrient cycling by marsh plants and infaunal<br />

community<br />

Stable upland bank with dense vegetation (not<br />

visible)


Aerial habitat<br />

Polychaete worms, crustaceans, molluscs<br />

Bivalves – clams, oysters, mussels<br />

Essential prey for blue crab, benthic<br />

feeding fish (e.g. spot, croaker)<br />

Habitat Diversity<br />

Comparison<br />

spiders, insects, wading birds, waterfowl,<br />

mammals<br />

Marsh surface & belowground<br />

microbial fungi and bacteria, algae,<br />

meiofauna (nematodes, copepods, rotifers,<br />

protozoa)<br />

Foraging invertebrates (polychaetes,<br />

gastropod mollusks, fiddler crab, blue crab,<br />

amphipods)<br />

Filter feeders (ribbed mussel, oyster)<br />

Aquatic pools and channels<br />

Small & juvenile fish, shrimp, blue crab


Habitat in Riprap<br />

Reefs<br />

Lower diversity &<br />

abundance than marshes<br />

& oyster reefs<br />

May support similar or<br />

higher nekton abundance<br />

than bare sediment


Potentially Negative Effects of<br />

Marsh Sills<br />

Covering shallow water benthic infauna<br />

Hydrodynamic changes - altering tidal<br />

exchange, wave height and wave direction<br />

Construction access & maintenance<br />

impacts<br />

Altering sediment transport <br />

Altering habitat use at marsh edge


Potentially Positive Effects<br />

Wave attenuation including boat wakes<br />

Sediment stabilization<br />

Vegetation stabilization<br />

Allows for efficient nutrient cycling, complex habitat<br />

structure<br />

Tidal marsh creation and restoration<br />

Protection and restoration of salt marsh habitats may be essential<br />

to the maintenance of high benthic production and consumer<br />

biomass in estuarine ecosystems (Seitz et al 2006)<br />

Habitat diversity & complexity<br />

For terrestrial, wetland and aquatic organisms


Current Guidelines for Marsh Sills<br />

Use only if action is required and nonstructural<br />

methods are not sufficient<br />

Minimize channelward encroachment<br />

Make structure as porous & low as possible<br />

Minimize / restore construction access<br />

impacts<br />

Periodic maintenance required<br />

Pruning overhanging branches, removing excess<br />

tidal debris, replacing scattered stone, additional<br />

planting


Main Conclusions about<br />

Tradeoffs<br />

Marsh sills are better choice for erosion protection<br />

in low & medium energy settings than bulkheads<br />

Not as appropriate at high energy settings or where<br />

significant aquatic resources would be impacted<br />

(e.g. SAV, unique shellfish areas)<br />

Tidal marsh creation & restoration at the land-water<br />

interface is beneficial for public trust resources<br />

More research is needed & underway to compare<br />

actual productivity before and after sill construction,<br />

evaluate effects of tidal gaps


Any Questions About Marsh Sills

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