2022
DOI: 10.1016/j.gca.2022.06.040
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Impact of submarine groundwater discharge on biogeochemistry and microbial communities in pockmarks

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Cited by 17 publications
(8 citation statements)
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“…However, the key controls of surface-charge driven mechanisms and the specific effects on contaminant transport should be thoroughly explored beyond the assumptions and limitations of the current study, such as steady state flow, dimensionality, and the lack of reactive processes. Therefore, it would be of interest to investigate the effects of dynamic water flow conditions (e.g., Haberer et al 2012;Qi et al 2020), fully 3-D domains involving anisotropy and complex flow topology (e.g., Chiogna et al 2014;Ye et al 2015b), presence of other charged minerals (e.g., Prigiobbe and Bryant 2014;McNeece and Hesse 2017;Stolze et al 2019;Cogorno et al 2022), biogeochemical (e.g., Bauer et al 2009Purkamo et al 2022) and mineral dissolution/precipitation reactions (e.g., Tartakovsky et al 2008;Poonoosamy et al 2016;Soltanian et al 2015;Fakhreddine et al 2016;Battistel et al 2019;Pieretti et al 2022), multiphase flow and transport (e.g., Ahmadi et al 2022;. Further extension of this approach is also envisioned in synergy with hydrogeophysical exploration (e.g., ERT, DCIP), as well as in the context of engineered remediation involving electrokinetic transport (e.g., Wu et al 2012;Martens et al 2021;Alizadeh et al 2019;Sprocati et al 2020;Lo ´pez-Vizcaı ´no et al 2022).…”
Section: Discussionmentioning
confidence: 99%
“…However, the key controls of surface-charge driven mechanisms and the specific effects on contaminant transport should be thoroughly explored beyond the assumptions and limitations of the current study, such as steady state flow, dimensionality, and the lack of reactive processes. Therefore, it would be of interest to investigate the effects of dynamic water flow conditions (e.g., Haberer et al 2012;Qi et al 2020), fully 3-D domains involving anisotropy and complex flow topology (e.g., Chiogna et al 2014;Ye et al 2015b), presence of other charged minerals (e.g., Prigiobbe and Bryant 2014;McNeece and Hesse 2017;Stolze et al 2019;Cogorno et al 2022), biogeochemical (e.g., Bauer et al 2009Purkamo et al 2022) and mineral dissolution/precipitation reactions (e.g., Tartakovsky et al 2008;Poonoosamy et al 2016;Soltanian et al 2015;Fakhreddine et al 2016;Battistel et al 2019;Pieretti et al 2022), multiphase flow and transport (e.g., Ahmadi et al 2022;. Further extension of this approach is also envisioned in synergy with hydrogeophysical exploration (e.g., ERT, DCIP), as well as in the context of engineered remediation involving electrokinetic transport (e.g., Wu et al 2012;Martens et al 2021;Alizadeh et al 2019;Sprocati et al 2020;Lo ´pez-Vizcaı ´no et al 2022).…”
Section: Discussionmentioning
confidence: 99%
“…Because of the influence of domestic wastewater, rivers, and coral reefs, it is possible that groundwater that previously seeped into the subsurface may be upwelling from the coastal seafloor (Umezawa et al, 2002). Submarine groundwater discharge has been observed along the world's coasts, and it has been reported that as groundwater passes through sediments, it entrains and discharges reducing substances such as methane, hydrogen sulfide, and ammonia, which are rarely distributed in seawater (Lecher et al, 2016;Purkamo et al, 2022;Brankovits et al, 2017;Lecher, 2017;Lecher and Mackey, 2018;Sadat-Noori et al, 2018). Such an inflow of land water, such as groundwater or river water, could be observed using anomalies in the T-S diagram.…”
Section: Unidentified Methane Sources In the Shelf Areamentioning
confidence: 99%
“…Contrary to the relatively stable conditions maintained in inland aquifers, coastal aquifers entail rapid fluctuations and steep physiochemical gradients to which STE microbes need to quickly adapt. This results in a highly diverse microbial community composition along the hydrological continuum of SGD sites, reflecting a mixture of seawater‐ and groundwater‐associated taxa (Adyasari et al., 2019; Chen et al., 2020; Degenhardt et al., 2020), as well as microbial functional groups that follow redox gradients (McAllister et al., 2015; Purkamo et al., 2022). Therefore, diverse prokaryotic groups in coastal ecosystems potentially affect bacterioplankton communities upon discharge into the marine environment (Lee et al., 2017; Ruiz‐González et al., 2021).…”
Section: Introductionmentioning
confidence: 99%