2016
DOI: 10.1016/j.rsma.2016.02.002
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Plymouth — A World Harbour through the ages

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Cited by 23 publications
(12 citation statements)
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“…5). At a larger scale, seawall design and location can affect benthic colonisation (Jackson 2014). For instance, slope differences can affect the susceptibility of seawalls to extreme surface temperatures, with sloping seawalls absorbing more solar radiation compared to vertical ones (Zhao et al 2019).…”
Section: Discussionmentioning
confidence: 99%
“…5). At a larger scale, seawall design and location can affect benthic colonisation (Jackson 2014). For instance, slope differences can affect the susceptibility of seawalls to extreme surface temperatures, with sloping seawalls absorbing more solar radiation compared to vertical ones (Zhao et al 2019).…”
Section: Discussionmentioning
confidence: 99%
“…Vulnerable, degraded and culturally valuable artificial structures on which manipulations are not permitted Some artificial structures are degraded or have cultural or heritage value, which can make it challenging to obtain permissions for retrofitting eco-engineering interventions, especially interventions that involve drilling or attaching heavy materials. For example, Plymouth Breakwater, built between 1812 and 1841, is a 1.6 km long structure (Southward and Orton 1954;Hawkins et al 1983) that is considered a historic monument (Knights et al 2016) and that is not permitted to be manipulated. As the original structure has become undermined over the years, sacrificial concrete wave-breaker blocks (100 t) are systematically placed on the seaward side of the breakwater as an additional form of protection from wave action.…”
Section: Vertical and Sloping Seawalls (Supplementary Information Tabmentioning
confidence: 99%
“…The study was carried out at Mount Batten, Plymouth, UK (Figure 1) between September and December 2014. Mount Batten is a headland of limestone protruding into Plymouth Sound (see Knights et al ., 2016 for description of the area). Two sites on the shore were identified and defined as limestone rock surfaces of similar aspect, gradient, tidal exposure and orientation (~ south-west facing; see Figure 1 and for more information) where Semibalanus balanoides and Chthamalus montagui are locally abundant and coexist in the mid-shore.…”
Section: Methodsmentioning
confidence: 99%