Physicochemical Kinetics and Transport at Biointerfaces 2004
DOI: 10.1002/0470094044.ch9
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Mobilisation of Organic Compounds and Iron by Microorganisms

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Cited by 6 publications
(2 citation statements)
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“…It is well‐established, that in the subsurface environment, petroleum hydrocarbons accumulate in the solid or nonaqueous liquid phase (NAPL) of soil, which is attributed to the sorption by soil components, dissolution in NAPL, and sequestration in soil micropores. This is because most of the hydrocarbons are scarcely water‐soluble and, therefore, have the tendency to interact with natural organic matter and other soil constituents—processes which render them poorly mobile and restrict their accessibility for microorganisms (Harms & Wick, 2004; Wick et al, 2001).…”
Section: Introductionmentioning
confidence: 99%
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“…It is well‐established, that in the subsurface environment, petroleum hydrocarbons accumulate in the solid or nonaqueous liquid phase (NAPL) of soil, which is attributed to the sorption by soil components, dissolution in NAPL, and sequestration in soil micropores. This is because most of the hydrocarbons are scarcely water‐soluble and, therefore, have the tendency to interact with natural organic matter and other soil constituents—processes which render them poorly mobile and restrict their accessibility for microorganisms (Harms & Wick, 2004; Wick et al, 2001).…”
Section: Introductionmentioning
confidence: 99%
“…The vadose zone water occurs as a thin film on the surface of soil particles and in the smallest interstices between soil particles. The life functions of most microorganisms rely on the water phase and they remain in contact with the aqueous phase (Harms & Wick, 2004). The balance of the pore space is filled with air.…”
Section: Introductionmentioning
confidence: 99%