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Journal ArticleDOI

Indirect Environmental Effects of Dikes on Estuarine Tidal Channels: Thinking Outside of the Dike for Habitat Restoration and Monitoring

W. Gregory Hood
- 01 Apr 2004 - 
- Vol. 27, Iss: 2, pp 273-282
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TLDR
In this article, the authors analyzed historical photos of the Skagit River delta marshes (Washington, U.S.) and compared changes in estuarine marsh and tidal channel surface area from 1956-2000 in the Wiley Slough area of the South Fork Skagits delta, and from 1937-2000 on the North Fork delta.
Abstract
While the most obvious effects of dike construction and marsh conversion are those affecting the con- verted land (direct or intended effects), less immediately apparent effects also occur seaward of dikes (indirect or unintended effects). I analyzed historical photos of the Skagit River delta marshes (Washington, U.S.) and compared changes in estuarine marsh and tidal channel surface area from 1956-2000 in the Wiley Slough area of the South Fork Skagit delta, and from 1937-2000 in the North Fork delta. Dike construction in the late 1950s caused the loss of 80 ha of estuarine marsh and 6.7 ha of tidal channel landward of the Wiley Slough dikes. A greater amount of tidal channel surface area, 9.6 ha, was lost seaward of the dikes. Similar losses were observed for two smaller North Fork tidal channel systems. Tidal channels far from dikes did not show comparable changes in channel surface area. These results are consistent with hydraulic geometry theory, which predicts that diking reduces tidal flushing in the undiked channel remnants and this results in sedimentation. Dikes may have significant seaward effects on plants and animals associated with tidal channel habitat. Another likely indirect dike effect is decreased sinuosity in a distributary channel of the South Fork Skagit River adjacent to and downstream of the Wiley Slough dikes, compared to distributary channels upstream or distant from the dikes. Loss of floodplain area to diking and marsh conversion prevents flood energy dissipation over the marsh surface. The distributary channel has responded to greater flood energy by increasing mean channel width and decreasing sinuosity. Restoration of diked areas should consider historic habitat loss seaward of dikes, as well as possible benefits to these areas from dike breaching or removal. Habitat restoration by breaching or removal of dikes should be monitored in areas directly affected by dikes, areas indirectly affected, and distinct reference areas.

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Citations
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References
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Journal ArticleDOI

Salt Marsh Diking and Restoration: Biogeochemical Implications of Altered Wetland Hydrology.

TL;DR: Results indicate that seawater restoration should proceed cautiously to avoid nutrient loading of surface waters in drained sites or sulfide toxicity in diked–waterlogged marshes.
Journal ArticleDOI

Effects of historic tidal restrictions on salt marsh sediment chemistry

TL;DR: In this paper, the effects of diking on salt marsh biogeochemistry were analyzed by comparing the hydrology, porewater chemistry and solid phase composition of both seasonally flooded and drained diked marshes with adjacent natural salt marshes on Cape Cod,Massachusetts.
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On size and scale in geomorphology

TL;DR: In this paper, the authors examine some of these formal relations in terms of the information that they indicate must be included in geomorphological theories, and the constraints imposed by the requirements of sound mechanical theories.
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Stability shear stress and equilibrium cross-sectional geometry of sheltered tidal channels

TL;DR: In this paper, the stability shear stress (tau sub(S) is assumed to be sufficient to maintain a zero gradient in net along-channel sediment transport, which is consistent with this concept.
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Rehabilitation of impounded estuarine wetlands by hydrologic reconnection to the Indian River Lagoon, Florida (USA)

TL;DR: In the Indian River Lagoon, Florida, most of the salt marshes (over 16.200 ha) were impounded by the early 1970s to control mosquito production as mentioned in this paper.
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