DSpace Repository

Sedimentation in created freshwater riverine wetlands: 15 years of succession and contrast of methods

Show simple item record

dc.contributor.author Mitsch, William J. en
dc.contributor.author Nedrich, Sara M. en
dc.contributor.author Harter, Sarah K. en
dc.contributor.author Anderson, Christopher en
dc.contributor.author Nahlik, Amanda M. en
dc.contributor.author Bernal, Blanca en
dc.date.accessioned 2015-03-03T15:54:40Z
dc.date.available 2015-03-03T15:54:40Z
dc.date.issued 2014
dc.identifier.citation Mitsch, William J., Nedrich, Sara M., Harter, Sarah K., Anderson, Christopher, Nahlik, Amanda M., and Bernal, Blanca. 2014. "<a href="https://repository.si.edu/handle/10088/24698">Sedimentation in created freshwater riverine wetlands: 15 years of succession and contrast of methods</a>." <em>Ecological Engineering</em>. 72:25&ndash;34. <a href="https://doi.org/10.1016/j.ecoleng.2014.09.116">https://doi.org/10.1016/j.ecoleng.2014.09.116</a> en
dc.identifier.issn 0925-8574
dc.identifier.uri http://hdl.handle.net/10088/24698
dc.description.abstract This study summarizes five separate sedimentation studies spanning 15 years (years 3 17 following wetland creation in 1994) of two 1 ha experimental flow-through wetlands. Included are methods and analyses of the most recent (2009 2010) comparative study that attempted to quantify both erosion and bioturbation processes. Depending on techniques used, two distinct types of sedimentation rates were estimated gross and net sedimentation. Gross sedimentation in 2004 2005 (years 11 and 12) using sediment trap bottles was 45 kg m-2 for 4 months during and after spring flood pulsing conditions in 2004 and 39 kg m-2 for the same 4 months during and after steady flow conditions in 2005. Annual sediment accretion using feldspar and other horizon markers was 31.7 ± 4.4 kg m-2 yr-1 (4.2 ± 0.6 cm yr-1) in 1996 (year 3 after wetland creation) and 34.4 ± 4.5 kg m-2 yr-1 (5.5 ± 0.8 cm yr-1) in 2009 (year 16 after wetland creation). Net sedimentation using soil cores to estimate accumulation of sediments over antecedent soil horizon layers was 4.7 ± 0.3 kg m-2 yr-1 (0.9 ± 0.07 cm yr-1) in 2004 (year 11) and 6.0 ± 0.4 kg m-2 yr-1 (0.9 ± 0.06 cm yr-1) in 2009 (year 16). Net sedimentation, using estimates of sedimentation and erosion with the sediment erosion table (SET) method in 2009 2010 (years 16 17) was 3.9 ± 6.1 9.0 kg m-2 yr-1 (1.3 ± 0.8 1.4 cm yr-1). Bioturbation by macrofauna significantly decreased sedimentation rates during the 2009 (year 16) study. Spatial patterns, consistent among horizon marker and net sedimentation studies, showed that deep, open-water areas had higher rates of sedimentation than shallow areas with emergent vegetation, and that sedimentation rates were higher when closer to the inflow than at the outflow of these flow-through wetlands. Net sedimentation of these created riverine wetlands ranged from 1.2 cm/yr to 1.4 cm/yr, suggesting that these wetlands will accumulate about 30 cm of sediments in a little more than two decades. en
dc.relation.ispartof Ecological Engineering en
dc.title Sedimentation in created freshwater riverine wetlands: 15 years of succession and contrast of methods en
dc.type Journal Article en
dc.identifier.srbnumber 130171
dc.identifier.doi 10.1016/j.ecoleng.2014.09.116
rft.jtitle Ecological Engineering
rft.volume 72
rft.spage 25
rft.epage 34
dc.description.SIUnit SERC en
dc.description.SIUnit Peer-reviewed en
dc.citation.spage 25
dc.citation.epage 34


Files in this item

This item appears in the following Collection(s)

Show simple item record

Search DSpace


Browse

My Account