2014
DOI: 10.1016/j.geomorph.2013.10.009
|View full text |Cite
|
Sign up to set email alerts
|

Influence of four run-of-river dams on channel morphology and sediment characteristics in Illinois, USA

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1
1
1

Citation Types

3
54
2
1

Year Published

2015
2015
2022
2022

Publication Types

Select...
10

Relationship

0
10

Authors

Journals

citations
Cited by 104 publications
(65 citation statements)
references
References 46 publications
3
54
2
1
Order By: Relevance
“…We obtained similar results with finer substratum and higher bottom organic matter in the upstream reach and coarser substratum downstream. However, changes in size substratum and depth around dams depend on many local factors, such as, spatial patterns of channel morphology and sedimentation can decrease because suspended sediment levels in the water decrease because of the presence of aquatic plants that accumulate sediment (Bond 2004;Skalak et al, 2009;Csiki & Rhoads, 2014). Despite it was expected a decrease in the number of taxa downstream of the weir, we did not found significant differences in richness between upstream and downstream reaches.…”
Section: Discussioncontrasting
confidence: 62%
“…We obtained similar results with finer substratum and higher bottom organic matter in the upstream reach and coarser substratum downstream. However, changes in size substratum and depth around dams depend on many local factors, such as, spatial patterns of channel morphology and sedimentation can decrease because suspended sediment levels in the water decrease because of the presence of aquatic plants that accumulate sediment (Bond 2004;Skalak et al, 2009;Csiki & Rhoads, 2014). Despite it was expected a decrease in the number of taxa downstream of the weir, we did not found significant differences in richness between upstream and downstream reaches.…”
Section: Discussioncontrasting
confidence: 62%
“…In the sediments, there was a decreasing trend of percentage sand content and increasing trend of percentage clay, silt and total organic carbon content from upstream to downstream areas. This can be due to the reduced flow rate and increased amount of sediment load carried by the stream as it flows downstream as reported for lotic wetlands in many regions of the world (Bravard et al 2014;Csiki and Rhoads 2014;Yang et al 2014). All the annelids recorded in the present study were of Class Oligochaeta which is considered as pollution tolerant class (Sarang and Sharma 2009).…”
Section: Discussionsupporting
confidence: 57%
“…Based on their modelling results, Baker et al (2011) also concluded that small, low-gradient streams with smaller-sized substrate were more susceptible to fine-sediment accumulation than large streams. However, RoR dams that are regularly overtopped at high flows are expected to experience fewer discontinuities in the morphological and sediment size distribution of stream channels (Kondolf 1997;Csiki and Rhoads 2013;Kibler and Tullos 2013). The proportion of flow diverted is also of importance for the transport of sediments.…”
Section: Pathway 2: the Presence Of Low-head Damsmentioning
confidence: 99%