2016
DOI: 10.1007/s10021-016-0080-1
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Riparian Soil Development Linked to Forest Succession Above and Below Dams Along the Elwha River, Washington, USA

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Cited by 9 publications
(13 citation statements)
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“…The changes in plant community composition across landforms were correlated with flood‐associated environmental variables. Bar plots had relatively more sand and gravel, and larger particle sizes, whereas terrace plots had finer soil texture, more litter, and higher total exchange capacity, consistent with previous findings along the Elwha River (Perry et al, 2017).…”
Section: Discussionsupporting
confidence: 89%
“…The changes in plant community composition across landforms were correlated with flood‐associated environmental variables. Bar plots had relatively more sand and gravel, and larger particle sizes, whereas terrace plots had finer soil texture, more litter, and higher total exchange capacity, consistent with previous findings along the Elwha River (Perry et al, 2017).…”
Section: Discussionsupporting
confidence: 89%
“…However, plantavailable inorganic N pools and N transformation rates measured in soil during the peak growing season immediately prior to the annual return of salmon were largely unaffected by salmon enhancement. Indeed, the 20 yr of cumulative salmon N additions in the zone near the stream in our study (~6690 kg N/ha) greatly exceeded typical riparian surface soil N pools (500-2500 kg N/ha; Walker 1989, Morris and Stanford 2011, Perry et al 2017, suggesting that even partial retention of salmon N inputs in soils should have increased soil [N org ]. Given numerous conventional long-term fertilization experiments worldwide have shown a consistent pattern of elevated soil inorganic N pools and N transformations (H€ ogberg et al 2006(H€ ogberg et al , Lu et al 2010, it was surprising that 20 yr of MDN inputs did not clearly accelerate soil N cycling in our study.…”
Section: Discussionmentioning
confidence: 65%
“…Soils are the dominant (>70%) sink for added N in forests worldwide (Templer et al 2012), and tree growth in high-latitude conifer forests is often strongly N-limited (Nordin et al 2001), both of which should have fostered retention of salmon N inputs to our site. Indeed, the 20 yr of cumulative salmon N additions in the zone near the stream in our study (~6690 kg N/ha) greatly exceeded typical riparian surface soil N pools (500-2500 kg N/ha; Walker 1989, Morris and Stanford 2011, Perry et al 2017), suggesting that even partial retention of salmon N inputs in soils should have increased soil [N org ]. The lack of increase in soil [N org ] due to salmon that we observed is consistent with the lack of increase in N availability, because soil [N org ] fuels long-term , Table 1) for ½NH þ 4 and ½NO À 3 , net mineralization and nitrification, [N org ], and gravimetric water content for both the salmon-enhanced and the salmon-depleted banks of Hansen Creek at 1, 3, 6, 10, and 20 m from the edge of the creek bed with 95% confidence intervals (dashed line) for predicted values.…”
Section: Discussionmentioning
confidence: 67%
“…Overstory Thuja also occurred in 20% of plots, mainly in stands >90 years old but sometimes in relatively young stands 34–55 years old, unlike the findings of Stolnack and Naiman (), because they did not examine forests along the lower segment where almost all of the Thuja we observed were located. Higher soil calcium and magnesium in the lower segment may have contributed to higher Thuja abundance (Hawkins and Robbins ; Perry et al., in press).…”
Section: Discussionmentioning
confidence: 99%