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contributor authorSreenivas Kota
contributor authorMorton A. Barlaz
contributor authorRobert C. Borden
date accessioned2017-05-08T21:29:54Z
date available2017-05-08T21:29:54Z
date copyrightApril 2004
date issued2004
identifier other%28asce%291090-025x%282004%298%3A2%2889%29.pdf
identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/53760
description abstractThe availability of Fe(III) for microbial reduction was measured in macrocosms containing contaminated aquifer sediment with benzaldehyde as the organic substrate. Repeated benzaldehyde additions initially resulted in an increase in Fe(II) and decrease in Fe(III). However, after ∼400 h total Fe(II) and Fe(III) stabilized and both ethanol and benzylalcohol began to accumulate, indicating a shift in microbial processes from iron reduction to fermentation. Addition of Fe(III) as amorphous–oxyhydroxide, goethite, and hematite to the Fe(III) depleted sediment stimulated ethanol and benzylalcohol degradation. Washing the sediment with
publisherAmerican Society of Civil Engineers
titleInfluence of Solid Phase Fe(II) on Fe(III) Bioavailability in Aquifer Sediment
typeJournal Paper
journal volume8
journal issue2
journal titlePractice Periodical of Hazardous, Toxic, and Radioactive Waste Management
identifier doi10.1061/(ASCE)1090-025X(2004)8:2(89)
treePractice Periodical of Hazardous, Toxic, and Radioactive Waste Management:;2004:;Volume ( 008 ):;issue: 002
contenttypeFulltext


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