2017
DOI: 10.1007/s11368-017-1893-z
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Comparison of direct benthic flux to ebullition-facilitated flux of polycyclic aromatic hydrocarbons and heavy metals measured in the field

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Cited by 7 publications
(4 citation statements)
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“…In such a scenario, OC would provide effective advective sequestration and the sand layer would contribute to geotechnical stability and as a thicker diffusive pathway. In addition, an OC layer placed in a geotextile mat may help reduce the potential for formation of preferential pathways due to gas ebullition that could facilitate breakthrough of contaminants through the cap (Kaliappan 2016;Viana et al 2017;Viana et al 2012), scouring of reactive material, biointrusion, and mixing of reactive material with sediments, and provides uniform distribution of reactive material.…”
Section: Discussionmentioning
confidence: 99%
“…In such a scenario, OC would provide effective advective sequestration and the sand layer would contribute to geotechnical stability and as a thicker diffusive pathway. In addition, an OC layer placed in a geotextile mat may help reduce the potential for formation of preferential pathways due to gas ebullition that could facilitate breakthrough of contaminants through the cap (Kaliappan 2016;Viana et al 2017;Viana et al 2012), scouring of reactive material, biointrusion, and mixing of reactive material with sediments, and provides uniform distribution of reactive material.…”
Section: Discussionmentioning
confidence: 99%
“…Consumption or release of water volume that can be monitored over time affects the measured metal concentration. A decrease in concentration occurs due to the consumption of water volume, whereas an increase in concentration occurs due to the volume of water released (Viana et al 2018). Important points in this method are the guaranteed cleanliness of the instrument and the required sample volume at discrete time intervals for subsequent shipboard or laboratory analyses (Homoky et al 2016).…”
Section: In Situ Benthic Incubationmentioning
confidence: 99%
“…A number of methods have been developed to measure the benthic flux of trace metals, such as a sedimentporewater profile using gradient concentration (Cheng et al 2019;Duan et al 2019;Kalnejais et al 2015;Ni et al 2017;Santos-Echeandia et al 2009), in situ benthic chamber (Frogner-Kockum et al 2020;Han et al 2016), moored sediment trap (Buesseler et al 2007;Pohl et al 2004), benthic boundary layer profile (Croot et al 2019), the 224 Th/ 228 Ra disequilibrium method (Shi et al 2018;Vieira et al 2019), and isotopic mass balance data (Little et al 2014). Gradient concentration and benthic chambers are the two most commonly used methods for measuring benthic fluxes of trace metals from the sediment to the overlying water, or vice versa (Viana et al 2018). Both methods have many advantages, although each still has limitations.…”
Section: Introductionmentioning
confidence: 99%
“…Heavy metals could also bind to sediment matrices due to the porous nature and absorptive ability of sediment or soil organic matter. The sediment pollution has persisted over time and poses a significant challenge for the restoration of these water bodies [ 2 , 3 ]. The Environmental Protection Agency (US, EPA) has estimated that there are 1.2 billion cubic meters of contaminated surficial sediments in the US that could pose a risk to surface water resources, pollutant transport, public exposure, and even the security of drinking water supply [ 4 , 5 ].…”
Section: Introductionmentioning
confidence: 99%