2011
DOI: 10.1002/etc.745
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Changes in liquid water alter nutrient bioavailability and gas diffusion in frozen antarctic soils contaminated with petroleum hydrocarbons

Abstract: Bioremediation has been used to remediate petroleum hydrocarbon (PHC)-contaminated sites in polar regions; however, limited knowledge exists in understanding how frozen conditions influence factors that regulate microbial activity. We hypothesized that increased liquid water (θ(liquid) ) would affect nutrient supply rates (NSR) and gas diffusion under frozen conditions. If true, management practices that increase θ(liquid) should also increase bioremediation in polar soils by reducing nutrient and oxygen limit… Show more

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Cited by 6 publications
(2 citation statements)
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“…Although NH 4 + and PO 4 3− availability were higher in injected treatments, there was no consistency between locations. This could result from local differences in soil properties between Iqaluit and Whitehorse, such as θ liquid and the initial amount of PHC contamination (Supplemental Table S2), both of which can affect NH 4 + (Harvey et al, 2012) and PO 4 3− (Mouat and Nes, 1985) availability.…”
Section: Resultsmentioning
confidence: 99%
“…Although NH 4 + and PO 4 3− availability were higher in injected treatments, there was no consistency between locations. This could result from local differences in soil properties between Iqaluit and Whitehorse, such as θ liquid and the initial amount of PHC contamination (Supplemental Table S2), both of which can affect NH 4 + (Harvey et al, 2012) and PO 4 3− (Mouat and Nes, 1985) availability.…”
Section: Resultsmentioning
confidence: 99%
“…Previous bioremediation experiments indicate that the presence of unfrozen water is critical for extending hydrocarbon biodegradation in frozen contaminated soil. , However, the relationship between the manipulation of unfrozen water retention via controllable soil factors and the enhancement of petroleum hydrocarbon biodegradation is not understood. Unfrozen water content, influenced by a variety of factors, gradually decreases as soils undergo seasonal freezing, before stabilizing at a minimum threshold in deeply frozen soil .…”
Section: Introductionmentioning
confidence: 99%