2013
DOI: 10.1016/j.apgeochem.2012.08.007
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CO2 leakage impacts on shallow groundwater: Field-scale reactive-transport simulations informed by observations at a natural analog site

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Cited by 68 publications
(40 citation statements)
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“…One site that has received particular attention is an area of active CO 2 degassing located near Chimayó, New Mexico (Keating et al, 2010;Keating et al, 2013a;Keating et al, 2013b;Viswanathan et al, 2013), where physical-chemical data from about 30 shallow (<60m) drinking water wells around the Robert's Fault have been studied and modelled. Initial work used major and trace element concentrations and associations, major ion ratios (e.g.…”
Section: Natural Systemsmentioning
confidence: 99%
“…One site that has received particular attention is an area of active CO 2 degassing located near Chimayó, New Mexico (Keating et al, 2010;Keating et al, 2013a;Keating et al, 2013b;Viswanathan et al, 2013), where physical-chemical data from about 30 shallow (<60m) drinking water wells around the Robert's Fault have been studied and modelled. Initial work used major and trace element concentrations and associations, major ion ratios (e.g.…”
Section: Natural Systemsmentioning
confidence: 99%
“…Mobilization of arsenic in a shallow groundwater aquifer due to CO 2 leakage has been investigated at one of the natural analog sites, Chimayó, New Mexico, where CO 2 -saturated brackish water was leaked into the shallow aquifer along the fault [7,13,24,25]. At this site, decreased pH and the resulting mobilization of trace metals, including arsenic, were observed.…”
Section: Geofluidsmentioning
confidence: 99%
“…Even if their adverse effects had been alleviated due to the high buffering capacity of the local groundwater aquifer, Keating et al [7] reported significantly elevated trace metal concentrations at a number of local wells due to the influx of brackish waters. Later, both Keating et al [13] and Viswanathan et al [24] integrated the field dataset into a multiphase reactive transport model to understand the behavior of arsenic, since some wells in Chimayó exceeded the maximum contamination level (MCL). In addition to studies targeting natural CO 2 release sites, several experiments have been conducted at field-scale CO 2 injection sites to determine secondary contamination caused by the injected CO 2 [11,[26][27][28].…”
Section: Geofluidsmentioning
confidence: 99%
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“…Given the relatively benign properties of CO 2 , inflows of brines and other displaced storage formation fluids could have a greater impact on freshwater aquifers than the CO 2 . In this scenario, migration allows the CO 2 and brines to eventually intersect minor faults and fractures, but the probability of leakage to the surface via such potential conduits is extremely low (IEAGHG 2007b;Oldenburg et al 2009;Stenhouse et al 2009;Keating et al 2013;Pawar et al 2014Pawar et al , 2015Birkholzer et al 2015).…”
Section: Risk Scenario Amentioning
confidence: 99%