2000
DOI: 10.1016/s1093-0191(00)00026-5
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Geochemical and microbial reactions affecting the long-term performance of in situ ‘iron barriers’

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Cited by 123 publications
(90 citation statements)
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“…Given Fe(III)'s low solubility, considerable attention has been paid to Fe(III) sensing and acquisition by bacteria, and much is understood about these processes (43,53,59,67). Less is understood about Fe(II) sensing and uptake despite the facts that many environments contain Fe(II) (2,29) and that increased solubility of Fe(II) renders it more bioavailable than Fe(III) (35). In particular, Fe(II) is known to be important in acidic and/or reducing environments (35,38,57), and such conditions can easily arise at the microscale in diverse habitats (28,46), including biofilms (21).…”
mentioning
confidence: 99%
“…Given Fe(III)'s low solubility, considerable attention has been paid to Fe(III) sensing and acquisition by bacteria, and much is understood about these processes (43,53,59,67). Less is understood about Fe(II) sensing and uptake despite the facts that many environments contain Fe(II) (2,29) and that increased solubility of Fe(II) renders it more bioavailable than Fe(III) (35). In particular, Fe(II) is known to be important in acidic and/or reducing environments (35,38,57), and such conditions can easily arise at the microscale in diverse habitats (28,46), including biofilms (21).…”
mentioning
confidence: 99%
“…DCE and VC are co-contaminants with the parent compounds TCE and PCE at most sites where any degree of microbe-driven natural attenuation is occurring. In addition to the CVOCs, native inorganic parameters (e.g., calcium, magnesium, and alkalinity) are present in the groundwater and react with the ZVI to form precipitates that could potentially deposit on and passivate the ZVI surfaces (Liang et al, 2000). However, these changes typically are expected to take place over several years and this is the reason why the PRB needs to be monitored over the long term.…”
Section: Tce Plume In Groundwater At Moffett Fieldmentioning
confidence: 99%
“…Similarly, biological activity at the same barrier studied by O'Hannesin and Gillham (1998) remained low after two years (Matheson 1994) while some laboratory (Gu et al 1999) and pilot studies (Liang et al 1997) did observe significant increases in biological activity with time. These varying results can be related to differences in groundwater geochemistry, as recently reviewed by Liang et al (2000). In general, when the groundwater is more highly buffered, that is, when alkalinity and sulfate are high, the pH change within the iron is moderated, and both precipitation and microbial activity are enhanced.…”
Section: Effects Of Groundwater Chemistry On Barrier Longevitymentioning
confidence: 99%