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Selenium redox-potential conditions

Anaerobic metabolism occnrs nnder conditions in which the diffusion rate is insufficient to meet the microbial demand, and alternative electron acceptors are needed. The type of anaerobic microbial reaction controls the redox potential (Eh), the denitrification process, reduction of Mu and SO , and the transformation of selenium and arsenate. Keeney (1983) emphasized that denitrification is the most significant anaerobic reaction occurring in the subsurface. Denitrification may be defined as the process in which N-oxides serve as terminal electron acceptors for respiratory electron transport (Firestone 1982), because nitrification and NOj" reduction to produce gaseous N-oxides. hi this case, a reduced electron-donating substrate enhances the formation of more N-oxides through numerous elechocarriers. Anaerobic conditions also lead to the transformation of organic toxic compounds (e.g., DDT) in many cases, these transformations are more rapid than under aerobic conditions. [Pg.305]

Figure 12.6 Potential distribution for an n-GaAs electrode in contact with a selenium redox couple with fast interfacial reactions curve a in the absence of illumination curve b at open circuit with 882 W/m illumination and curve c under illumination near the short-circuit condition (-23.1 mA/cm ). The Debye length in the electrolyte was 0.2 nm, and the Debye length in the semiconductor was 70 nm. (Taken from Orazem and Newman. Figure 12.6 Potential distribution for an n-GaAs electrode in contact with a selenium redox couple with fast interfacial reactions curve a in the absence of illumination curve b at open circuit with 882 W/m illumination and curve c under illumination near the short-circuit condition (-23.1 mA/cm ). The Debye length in the electrolyte was 0.2 nm, and the Debye length in the semiconductor was 70 nm. (Taken from Orazem and Newman.
Arsenic and selenium demonstrate many similarities in their behavior in the environment. Both are redox sensitive and occur in several oxidation states under different environmental conditions. Both partition preferentially into sulfide minerals and metal oxides and are concentrated naturally in areas of mineralization and geothermal activity. Both elements occur as oxyanions in solution and, depending on redox status, are potentially mobile in the near-neutral to alkaline pH conditions that typify many natural waters. However, there are also some major differences. Selenium is immobile under reducing conditions while the mobility of arsenic is less predictable and depends on a range of other factors. Selenium also appears to partition more strongly with organic matter than arsenic. [Pg.4600]


See other pages where Selenium redox-potential conditions is mentioned: [Pg.885]    [Pg.340]    [Pg.358]    [Pg.47]    [Pg.277]    [Pg.57]    [Pg.133]    [Pg.168]   
See also in sourсe #XX -- [ Pg.885 ]




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