River Flow 2014 2014
DOI: 10.1201/b17133-333
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Wood density assessment to improve understanding of large wood buoyancy in rivers

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Cited by 4 publications
(2 citation statements)
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“…However, the hypothesized < 1,000 km explanations for the natural arrival of X. darwini to the Galápagos, and X. clarionensis to the Revillagigedo Islands could be possible (Hurd 1958a). In ocean currents, some driftwood is capable of travelling great distances (e.g., Eggertsson 1993) provided it does not lose buoyancy, which typically can occur with 6 months to 1.5 years (Häggblom 1982), with logs of lesser volume (Eggertsson 1993) or greater density (Ruiz-Villanueva et al 2014) with decreased buoyancy. For many animals, total travel time is likely the main issue for successful natural dispersal in oceans over great distances (see de Queiroz 2014).…”
Section: Discussionmentioning
confidence: 99%
“…However, the hypothesized < 1,000 km explanations for the natural arrival of X. darwini to the Galápagos, and X. clarionensis to the Revillagigedo Islands could be possible (Hurd 1958a). In ocean currents, some driftwood is capable of travelling great distances (e.g., Eggertsson 1993) provided it does not lose buoyancy, which typically can occur with 6 months to 1.5 years (Häggblom 1982), with logs of lesser volume (Eggertsson 1993) or greater density (Ruiz-Villanueva et al 2014) with decreased buoyancy. For many animals, total travel time is likely the main issue for successful natural dispersal in oceans over great distances (see de Queiroz 2014).…”
Section: Discussionmentioning
confidence: 99%
“…Some pieces of wood can be transported over very long distances during a single flood (Gurnell et al, 2002;Gurnell, 2012;Comiti et al, 2016;. Moreover, the amount of wood can be documented at multi-annual and annual time intervals over long time periods by historical data (Seo et al, 2008;Seo and Nakamura, 2009;Ruiz-Villanueva et al, 2014b). Based on this long time scale, however, it is not possible to record continuous series and study wood transport processes during shorter but critical hydrological events such as floods, exceptional wind events, and landslides, which are known to drive wood fluxes in rivers (Lassettre and Kondolf, 2012;Ruiz Villanueva et al, 2014a).…”
Section: Introductionmentioning
confidence: 99%