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    Mechanisms of Fouling in Fine‐Pore Diffuser Aeration

    Source: Journal of Environmental Engineering:;1993:;Volume ( 119 ):;issue: 006
    Author:
    Yeong‐Kwan Kim
    ,
    William C. Boyle
    DOI: 10.1061/(ASCE)0733-9372(1993)119:6(1119)
    Publisher: American Society of Civil Engineers
    Abstract: Diffuser fouling is classified as one of three types, A, B, and C, based on the nature of the foulant. The accumulation of inorganic foulants, such as fine particles and precipitates, characterize type A fouling, and the formation of biomass‐characterize type B fouling. Type C fouling is characterized by the formation of biofilm, fortified by the entrapment of inorganic particles within the biomass. Hypotheses were developed to describe the mechanisms of dynamic change in diffuser operating performance as a result of the three different types of diffuser fouling. The hypotheses specific to each type were evaluated by testing the appropriate hypothetical equations using the data produced in this study. Results indicate that the physical properties of the biofilm are important factors in fouling, causing a significant change in diffuser characteristics. Entrapment of inorganic particles, such as sands, within the biofilm, significantly increase the dynamic wet pressure (DWP) and alter the bubble size. The association between DWP and bubble size could be quantitatively described by a hypothetical fouling equation for the three different types of fouling in these laboratory studies.
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      Mechanisms of Fouling in Fine‐Pore Diffuser Aeration

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    http://yetl.yabesh.ir/yetl1/handle/yetl/41843
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    • Journal of Environmental Engineering

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    contributor authorYeong‐Kwan Kim
    contributor authorWilliam C. Boyle
    date accessioned2017-05-08T21:11:00Z
    date available2017-05-08T21:11:00Z
    date copyrightNovember 1993
    date issued1993
    identifier other%28asce%290733-9372%281993%29119%3A6%281119%29.pdf
    identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/41843
    description abstractDiffuser fouling is classified as one of three types, A, B, and C, based on the nature of the foulant. The accumulation of inorganic foulants, such as fine particles and precipitates, characterize type A fouling, and the formation of biomass‐characterize type B fouling. Type C fouling is characterized by the formation of biofilm, fortified by the entrapment of inorganic particles within the biomass. Hypotheses were developed to describe the mechanisms of dynamic change in diffuser operating performance as a result of the three different types of diffuser fouling. The hypotheses specific to each type were evaluated by testing the appropriate hypothetical equations using the data produced in this study. Results indicate that the physical properties of the biofilm are important factors in fouling, causing a significant change in diffuser characteristics. Entrapment of inorganic particles, such as sands, within the biofilm, significantly increase the dynamic wet pressure (DWP) and alter the bubble size. The association between DWP and bubble size could be quantitatively described by a hypothetical fouling equation for the three different types of fouling in these laboratory studies.
    publisherAmerican Society of Civil Engineers
    titleMechanisms of Fouling in Fine‐Pore Diffuser Aeration
    typeJournal Paper
    journal volume119
    journal issue6
    journal titleJournal of Environmental Engineering
    identifier doi10.1061/(ASCE)0733-9372(1993)119:6(1119)
    treeJournal of Environmental Engineering:;1993:;Volume ( 119 ):;issue: 006
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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