2011
DOI: 10.1016/j.watres.2011.02.018
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Fate of N-nitrosomorpholine in an anaerobic aquifer used for managed aquifer recharge: A column study

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Cited by 18 publications
(11 citation statements)
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“…Two stainless steel columns (1 m length, 0.1 m internal diameter) were constructed following the design of Pitoi et al with 10 sample ports located along the length (Figure S1; additional details in SI). Sample ports consisted of stainless steel needles with Teflon Luer-lock hubs that extended 0.05 m to the center of the column.…”
Section: Materials and Methodsmentioning
confidence: 99%
“…Two stainless steel columns (1 m length, 0.1 m internal diameter) were constructed following the design of Pitoi et al with 10 sample ports located along the length (Figure S1; additional details in SI). Sample ports consisted of stainless steel needles with Teflon Luer-lock hubs that extended 0.05 m to the center of the column.…”
Section: Materials and Methodsmentioning
confidence: 99%
“…Achromobacter spp. could be mediating the biodegradation of disinfection byproducts N-nitrosodimethylamine in the Leederville aquifer and N-nitrosomorpholine and N-nitrosodimethylamine in column experiments carried out utilizing Leederville aquifer sediment and recycled water (Pitoi et al, 2011;Patterson et al, 2012).…”
Section: Minor Biogeochemical Reactionsmentioning
confidence: 99%
“…During simulated MAR at the laboratory-scale, the majority of TOrC show enhanced removal under oxic redox conditions (Burke et al 2014;Regnery et al 2015a). Although anoxic to anaerobic subsurface conditions are beneficial for the removal of nitrate (Rivett et al 2008) or certain substance groups such as certain disinfection-byproducts (Pitoi et al 2011), iron, manganese, and other inorganic trace elements are mobilized under reducing subsurface conditions and usually require post-treatment of the recovered groundwater. Main driving factors for redox zonation in MAR systems are the availability of oxidizing agents such as oxygen and nitrate, of reducing agents (organic matter, reduced mineral phases), nutrients, the biological activity of the soil microbial community, and subsurface travel time (Grützmacher and Reuleaux 2011;Regnery et al 2013).…”
Section: Introductionmentioning
confidence: 99%