2018
DOI: 10.1016/j.ecolind.2017.05.015
|View full text |Cite
|
Sign up to set email alerts
|

A simplified method for estimating the longitudinal dispersion coefficient in ecological channels with vegetation

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
4
1

Citation Types

0
11
0

Year Published

2018
2018
2022
2022

Publication Types

Select...
9

Relationship

0
9

Authors

Journals

citations
Cited by 29 publications
(12 citation statements)
references
References 27 publications
0
11
0
Order By: Relevance
“…The study of pollutant and contaminant transport in the natural streams is important in several aspects such as quality management, pollution control of the chemical and biological processes, hydro-ecological studies and environmental impact assessments [1,2]. Hazardous pollutants and effluents, when discharged to the streams, in the mixing process, dispersed transversely, vertically, and longitudinally by advective and dispersive processes.…”
Section: Introductionmentioning
confidence: 99%
“…The study of pollutant and contaminant transport in the natural streams is important in several aspects such as quality management, pollution control of the chemical and biological processes, hydro-ecological studies and environmental impact assessments [1,2]. Hazardous pollutants and effluents, when discharged to the streams, in the mixing process, dispersed transversely, vertically, and longitudinally by advective and dispersive processes.…”
Section: Introductionmentioning
confidence: 99%
“…Consequently, estimation of the longitudinal dispersion coefficient could be useful in the management of water quality in rivers and optimal pollution control strategies [19], [20]. Seo and Cheong [11] stated that the K x is affected by three groups of factors, including hydraulic river features, vegetation, fluid properties and geometric patterns of river reach [21], [22]. The longitudinal dispersion coefficient measurements showed that the most effective parameters are channel width (B), flow depth (H ), bed shear velocity (U * ) and cross-sectional average flow velocity (U ) [23].…”
Section: Introductionmentioning
confidence: 99%
“…(a) Technical limitations and high cost (material, manpower, and time) in characterizing in detail real‐world aquifer (or stream) flow conditions and the evolutions of the condition. For example, the ideal pre‐estimation method of D in a field application has not been well established, although some preliminary tests have been done (Huai, Shi, Song, & Ni, 2018; Nofuentes & Polo, 2012; Shen, Niu, Anderson, & Phanikumar, 2010; Wang & Huai, 2016). (b) The explicit relationship between flow field characteristics and parameters of FADEs is unclear.…”
Section: Challenges and Suggestions For Future Workmentioning
confidence: 99%