2014
DOI: 10.1016/j.scitotenv.2014.06.145
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Reach specificity in sediment E. coli population turnover and interaction with waterborne populations

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Cited by 16 publications
(16 citation statements)
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References 57 publications
(89 reference statements)
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“…This indicates that other unidentified factors may influence the flux rate. Recently, it was shown that during baseflow there can exist a flux of E. coli from sediments to the water column (Grant et al, 2011; Piorkowski et al, 2014; Park et al, 2017, Pachepsky et al, 2017). Since sediment E. coli concentrations grew in some locations and decreased in others, the increase of the E. coli flux from the “growth” locations may not compensate for the decrease in the flux from the “decrease” locations.…”
Section: Discussionmentioning
confidence: 99%
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“…This indicates that other unidentified factors may influence the flux rate. Recently, it was shown that during baseflow there can exist a flux of E. coli from sediments to the water column (Grant et al, 2011; Piorkowski et al, 2014; Park et al, 2017, Pachepsky et al, 2017). Since sediment E. coli concentrations grew in some locations and decreased in others, the increase of the E. coli flux from the “growth” locations may not compensate for the decrease in the flux from the “decrease” locations.…”
Section: Discussionmentioning
confidence: 99%
“…Increasing content of fine particles and organic carbon in sediments has been reported to lead to lower E. coli inactivation rates and a lower sensitivity to inactivation due to temperature effects (Garzio‐Hadzick et al, 2010). Additionally, sediment organic carbon and median particle size diameter were reported to be important explanatory variables for the concentrations of E. coli in stream sediments during baseflow periods (Piorkowski et al, 2014). Our work seems to corroborate that of Brinkmeyer et al (2015), who concluded that the balance between sediment grain size or texture, water content, and organic matter appear to be the key for the better survival of fecal indicator bacteria in sediments.…”
Section: Discussionmentioning
confidence: 99%
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“…The physical mechanisms involved include entrainment and settling of particles mediated by shear stresses along the boundaries of flow, as well as loss of suspended pathogens infiltrating into the soil column or channel bed. Additionally, pathogens trapped in sediment or soil near the surface-subsurface interface may be re-mobilized during high flows independent from sediment suspension (Ghimire and Deng 2013, Yakirevich, et al 2013, Grant, et al 2011); however, this hyporheic transport process is rarely accounted for in fate and transport models (Piorkowski, et al 2014). …”
Section: Modeling Pathogen Transport During Floodsmentioning
confidence: 99%