2008
DOI: 10.1016/j.foreco.2008.01.051
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Spatial distribution and influence of large woody debris in an old-growth forest river system, New Zealand

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Cited by 44 publications
(39 citation statements)
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“…Major structural factors that may influence SW function are piece diameter, presence of rootwads and branches, decay state, form, and piece species. Elements of the SW relationship with a stream channel include wood length/channel width ratio, how it rests within the channel (position), degree of anchoring, and horizontal orientation (Braudrick and Grant, 2000;Chen et al, 2008;Cordova et al, 2007;Baillie et al, 2008;Magilligan et al, 2008;Jones et al, 2011). In an earlier study, we documented that burned wood recruited to streams following a fire generally was thicker, had less structural complexity, and was more decayed than wood that was not burned .…”
Section: Introductionmentioning
confidence: 92%
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“…Major structural factors that may influence SW function are piece diameter, presence of rootwads and branches, decay state, form, and piece species. Elements of the SW relationship with a stream channel include wood length/channel width ratio, how it rests within the channel (position), degree of anchoring, and horizontal orientation (Braudrick and Grant, 2000;Chen et al, 2008;Cordova et al, 2007;Baillie et al, 2008;Magilligan et al, 2008;Jones et al, 2011). In an earlier study, we documented that burned wood recruited to streams following a fire generally was thicker, had less structural complexity, and was more decayed than wood that was not burned .…”
Section: Introductionmentioning
confidence: 92%
“…We suggest that these characteristics are relevant for a broad spectrum of SW functions, including their well-established role on the probability of pool formation and as primary controls on the stability of SW (Beechie and Sibley, 1997;Grant, 2000, 2001;Martin and Benda, 2001;Baillie et al, 2008;Magilligan et al, 2008). Piece diameter and the presence of rootwads (raising the center of mass of a piece) strongly influence the depth of flow required to entrain and transport logs (e.g.…”
Section: What Wood Structure Favors Function Within Streams?mentioning
confidence: 99%
“…Natural wood loading in streams ranged from ϳ10 m 3 ·m −2 of channel area in deciduous-softwoods (willows) to well over 1000 m 3 ·m −2 in conifer forests (Gurnell 2003). Examples include low loadings of 0.021-222 m 3 ·m −2 in high-elevation and drier environments (Berg et al 1998;Dunkerley 2014;Hering et al 2000;Lester et al 2006), moderate loadings of 227-638 m 3 ·m −2 in dense forests (e.g., Baillie et al 2008;Carlson et al 1990), and high loadings of over 1000 m 3 ·m −2 in California redwood forests (MacDonald et al 1982).…”
Section: Wood Mobilitymentioning
confidence: 99%
“…Volume of wood per unit area is often lower in larger rivers because they can transport more wood than smaller streams (Gurnell 2003;Naiman et al 2002;Seo et al 2010), even though total wood abundance per unit length of channel can be much higher (Baillie et al 2008). In some densely forested areas, large logjams (spanning the full channel and more than 1 km long) may have created very high wood abundances per unit of channel area, though exact values have not been calculated (Collins et al 2002).…”
Section: Wood Loadingmentioning
confidence: 99%
“…La distribución de las orientaciones fue similar a la encontrada por Baillie et al (2008) en el río Whirinaki en Nueva Zelandia. Andreoli et al (2008) reportan que en el río Toro, Chile, las piezas no estaban distribuidas aleatoriamente, pero en este caso los elementos dispuestos ortogonalmente a la corriente representan un 51 %.…”
Section: Discussionunclassified