Establishment of vegetation for shoreline stabilization in Galveston Bay / by J.D. Dodd and J.W. Webb.

Dodd, John D.; Webb, John W.

doi:10.5962/bhl.title.47477

Cited by 15 publications

(23 citation statements)

References 2 publications

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“…Successful vegetative stabilization was achieved in a variety of intertidal environments at a fraction of the cost required for comparable structural protection (Woodhouae, Seneca, and Broome, 1972, 1974, 1976. Based upon this work, shoreline stabilization studies were initiated in Chesapeake Bay (Garbisch, et al, 1973;Garbisch, Woller, and McCallum, 1975), Calveston Bay (Dodd and Webb, 1975;Webb and Dodd, 1976), and San Francisco Bay (Knutson, 1975;U.S. Army Engineer District, San Francisco, 1976;Knutson, 1976;Newcombe, et al, 1979).…”

Section: Army Corps Of Engineers Coastal Engineering Research Centementioning

confidence: 99%

National survey of planted salt marshes (Vegetative stabilization and wave stress)

et al. 1981

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There have been many recent attempts to establish salt marshes in the coastal United States. Plantings are generally made for the purpose of shore protection, dredged material stabilization, or habitat development. During 1980 a survey was made of recent and historic salt marsh planting projects. Data were collected in 104 planted marshes in 12 coastal states. The relative stability of these plantings was compared to physical indicators of wave climate severity (fetch, shore slope, offshore depth, shore configuration, sediment grain size, orientation with respect to prevailing and storm winds, and proximity to boat traffic).Fetch, shore configuration, and sediment grain size were found to be related to planting stability. Using these parameters, a system was developed for evaluating potential marsh development sites.

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Section: Army Corps Of Engineers Coastal Engineering Research Centementioning

confidence: 99%

National survey of planted salt marshes (Vegetative stabilization and wave stress)

et al. 1981

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“…These theories have been applied to explain the hottearing behavior of binary and certain multicomponent alloys. [9][10][11][12][13][14][15][16] Because hot-tearing defects are caused by a number of complex interrelated variables, evaluation of the principal factors is very difficult.…”

Section: A Theories Of Hot Tearingmentioning

confidence: 99%

In-Situ Investigation of Hot Tearing in Aluminum Alloy AA1050 via Acoustic Emission and Cooling Curve Analysis

Pekguleryuz

Aliravci

2009

Metall Mater Trans A

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Hot tearing in the AA1050 alloy was investigated in real time and in situ using acoustic emission (AE) and cooling curve analysis techniques and a ring mold. Activities involving AE have been detected in three zones of the solidification curve. The characteristic signals for hot tearing were an AE energy of over 600 e.u. and an average frequency of~125 ± 15 kHz in zone II. For hot cracking, the AE energy was over 650 e.u. and the average frequency was~128 ± 17 kHz in zone III. The hot-tear start temperature ranged from 636°C to 653°C; the nonequilibrium solidus T¢ S , from 556°C to 614°C; the fraction solid at hot-tear onset from 0.71 to 0.99; and the Clyne-Davis hot-tear susceptibility coefficient (HSC) from 0.25 to 0.81. The HSC correlated inversely with a total energy of solidification cracking (E total ) HSC ffi 167 E total ð Þ À0:8 : A hot-tear susceptibility factor (HSF) = (pct Fe)AE(cooling rate (CR)) 2 was related to the HSC and T¢ S as HSC = 0.002 HSF + 0.3 and T¢ S = À0.3 HSF + 617.

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“…Based upon these studies , shoreline stabilization research was initiated in the Chesapeake Bay (G~bisch Woller, and McCallum, 1975) Galveston Bay (Dodd and Webb ~ 1975;Webh and Dodd ~ 1976), and San Francisco Bay (Knutson, 1976 ;Newcombe et al, ~979).…”

Section: Introductionmentioning

confidence: 99%

Vegetative erosion control in an oligohaline environment Currituck Sound, North Carolina

Benner¹,

Knutson²,

Brochu³

et al. 1982

Wetlands

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Research on erosion control with vegetation by the Coastal EngineeringResearch Center (CERC) demonstrated that salt marsh plantings help dissipate wave energy causing deposition of sediments. These processes can convert eroding environments into depositional environments producing shore advancement.To evaluate the impact of shoreline plantings in oligohaline coastal environments, a 30 meter segment of a planting was monitored over an eight-year period.Within five years, erosion ceased, and at least 20 additional species of plants had invaded the study site.

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Establishment of vegetation for shoreline stabilization in Galveston Bay / by J.D. Dodd and J.W. Webb.

Cited by 15 publications

References 2 publications

National survey of planted salt marshes (Vegetative stabilization and wave stress)

National survey of planted salt marshes (Vegetative stabilization and wave stress)

In-Situ Investigation of Hot Tearing in Aluminum Alloy AA1050 via Acoustic Emission and Cooling Curve Analysis

Vegetative erosion control in an oligohaline environment Currituck Sound, North Carolina

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