Week 12 - Physical (Flap Gates and LWD) and Chemical in Estuaries Flashcards
Tidal Gates - Salinity Gradient
Changes to estuary channel form will change salinity gradient
Additional salinity impacts due to tidal flap gates, primarily installed for agriculture, also flood control
Tidal Flap Gates - Traditional
Tide gates are doors or flaps mounted on the downstream end of culverts in dikes or under roads, that allow upstream waters to drain while preventing inflows from tidal surges or flooding
Flap opens with positive hydraulic head
Flap closed most of the time
Fish passage?
Salinity/fluvial gradients?
Tidal Flap Gates - Upgrade Options
The critical issue is fish passage. The secondary issue is circulation and restoring fluvial/salinity
gradient.
Tide gate has buoyant door which floats on the incoming tide and remains open until the water elevation reaches the floats, which closes the door.
The door is open most of the time
Columbia River - Salmon Recovery
Example of jetty (levee) breach and removal of flap gate to restore fluvial/tidal gradients and connectivity to off-channel marsh habitat
Evaluation Criteria -
1, Opportunity/Access for salmon
2. Capacity/Complexity
3. Certainty of Success (self- maintaining, proven, subjective)
Pitt-Addington Marsh
Four tidal gates, entirely diked marsh
Former floodplain of the Pitt River
Upper chinook (COSEWIC)
Widgeon Sockeye (endemic)
Incredible restoration opportunity!
LWD in Estuaries - Where does it come from?
LWD is transported from the upper watershed to the estuary/ocean
Then ‘recycled’ by the actions of tides, wind and currents
The ocean is another source of wood
Winter storms blow wood into river mouths and onto
coastal beaches
Where did all the LWD go?
Snags and driftwood presented obstacles for river traffic, fishers, etc.
US Army Corps of Engineers during the late 1800’s removed wood to improve and maintain the navigability of rivers
Snags removed from rivers by US Army Corps of Engineers, 1891-1917
Woody debris in Restoration - Ecological functions
release organic carbon
provide habitat for fish and invertebrates
sediment accumulation
Estuary Wood Dynamics
Wood-boring crustacea (gribbles)
Bivalve mollucs
Marine fungi
Bacteria
Wood recycling - isopods
Wood-boring isopod crustacea (gribbles) of the genus Limnoria are major reducers of wood Pacific Northwest estuaries
Two species involved, L. lignorum, the endemic northern species, and L. tripunctata, the introduced species that is predominantly southern in distribution
Wood Recycling - Wood-Boring mollucs
Other than gribbles, the only shallow-water, wood-boring animals in the Pacific Northwest are two species of shipworms.
The most important reducers of wood in estuarine and shallow marine waters of PN region
Bankia setacea
most common species of shipworm, a coldwater native
the major marine, wood destroying animal in open ocean, embayments and estuaries
Terado nevalis - a smaller introduced warm water species of restricted distribution in PNW
Wood Recycling - Fungi
Marine fungi degrade cellulosic materials, but their ability to rapidly or extensively degrade large pieces of wood appears to be much less than that of terrestrial fungi
Wood Recycling - Bacteria
The role of cellulose-degrading bacteria in the sea is obscure, but many species of marine bacteria have been identified as active degraders of cellulose
Log Booms in the Fraser Estuary
Legacy of historical forestry practices - convenient, slow decomposition
Regulations prohibit boom grounding, but no enforcement
Significant damage to marsh habitat from repeated grounding with mixed tidal cycle
Will require a govt policy shift and bold, courageous action to force industry change