2009
DOI: 10.1139/x09-017
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The influence of riparian vegetation on leaf litter inputs to Boreal Shield streams: implications for partial-harvest logging in riparian reserves

Abstract: Litter inputs to headwater streams were measured to characterize and describe input patterns to the streams and to quantify the relationships between leaf litter inputs and surrounding riparian characteristics in Boreal Shield forests. Our goal was to provide information on litter inputs to streams in the Boreal Shield to determine if partial-harvest logging of commercial trees within riparian reserves has the potential to cause significant changes to litter inputs. Total leaf litter comprised 87% deciduous le… Show more

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Cited by 16 publications
(3 citation statements)
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“…The particular importance of riparian trees is witnessed by the fact that sometimes riparian buffers are expressed in terms of tree height (Forest Ecosystem Management Assessment Team [FEMAT], 1993;Ilhardt et al, 2000;Young, 2000). A width of one tree height -ranging from 30 m in eastern North America to 50 m in the west -is estimated to provide most of the coarse woody debris and litter to the watercourse, enough shade to prevent significant warming of its water, and the root system necessary to stabilize its banks (FEMAT, 1993;Reid & Hilton, 1998;Young, 2000;Moore, Spittlehouse, & Story, 2005;Muto, Kreutzweiser, & Sibley, 2009) (Figure 2a). One tree height is consistent with reviews indicating that treed buffers on the order of 30 m are responsible for the majority of these riparian functions (Broadmeadow & Nisbet, 2004;Lee et al, 2004;Groom, Dent, Madsen, & Fleuret, 2011).…”
Section: Riparian Area Influence On the Watercoursementioning
confidence: 99%
“…The particular importance of riparian trees is witnessed by the fact that sometimes riparian buffers are expressed in terms of tree height (Forest Ecosystem Management Assessment Team [FEMAT], 1993;Ilhardt et al, 2000;Young, 2000). A width of one tree height -ranging from 30 m in eastern North America to 50 m in the west -is estimated to provide most of the coarse woody debris and litter to the watercourse, enough shade to prevent significant warming of its water, and the root system necessary to stabilize its banks (FEMAT, 1993;Reid & Hilton, 1998;Young, 2000;Moore, Spittlehouse, & Story, 2005;Muto, Kreutzweiser, & Sibley, 2009) (Figure 2a). One tree height is consistent with reviews indicating that treed buffers on the order of 30 m are responsible for the majority of these riparian functions (Broadmeadow & Nisbet, 2004;Lee et al, 2004;Groom, Dent, Madsen, & Fleuret, 2011).…”
Section: Riparian Area Influence On the Watercoursementioning
confidence: 99%
“…Indeed, selective logging to promote broadleaved trees in mixed species buffer zones may actually improve ecological values as suggested by Lidman et al (2017b). Leaf litter inputs to headwater streams have been shown to correlate well with the basal area of broadleaved trees in the buffer zone (Muto et al 2009). Selective logging of conifer trees in mixed stands has the potential to increase the broadleaved basal area over time.…”
Section: Introductionmentioning
confidence: 96%
“…Non‐woody debris can decay more rapidly in running water than in forests (Graça et al, 2015), and its decomposition rate increases with increasing temperature (Taylor & Chauvet, 2014), introducing more dissolved carbon and nitrogen into streams. As non‐woody debris enters a stream, it is often retained locally or is transported over a short distance until it is trapped around obstacles (Muto et al, 2009; Osei et al, 2015; Webster et al, 1999), such as root masses, instream wood or other woody debris. Hence, non‐woody debris is drawn into the water by flow and then submerged and accumulated around woody debris (Turowski et al, 2016) or buried within the streambed by sediment movement and flooding (Cornut et al, 2012), thus extending the residence time of the non‐woody debris and promoting the transformation of dissolved organic matter.…”
Section: Introductionmentioning
confidence: 99%