001     57171
005     20180211190807.0
024 7 _ |2 pmid
|a pmid:17337313
024 7 _ |2 DOI
|a 10.1016/j.jconhyd.2007.01.009
024 7 _ |2 WOS
|a WOS:000248292400006
037 _ _ |a PreJuSER-57171
041 _ _ |a eng
082 _ _ |a 550
084 _ _ |2 WoS
|a Environmental Sciences
084 _ _ |2 WoS
|a Geosciences, Multidisciplinary
084 _ _ |2 WoS
|a Water Resources
100 1 _ |a Gargiulo, G.
|b 0
|0 P:(DE-HGF)0
245 _ _ |a Bacteria transport and deposition under unsaturated conditions: the role of the matrix grain size and the bacteria surface protein
260 _ _ |a Amsterdam [u.a.]
|b Elsevier Science
|c 2007
300 _ _ |a
336 7 _ |a Journal Article
|0 PUB:(DE-HGF)16
|2 PUB:(DE-HGF)
336 7 _ |a Output Types/Journal article
|2 DataCite
336 7 _ |a Journal Article
|0 0
|2 EndNote
336 7 _ |a ARTICLE
|2 BibTeX
336 7 _ |a JOURNAL_ARTICLE
|2 ORCID
336 7 _ |a article
|2 DRIVER
440 _ 0 |a Journal of Contaminant Hydrology
|x 0169-7722
|0 3225
|y 3
|v 92
500 _ _ |a Record converted from VDB: 12.11.2012
520 _ _ |a Unsaturated (80% water saturated) packed column experiments were conducted to investigate the influence of grain size distribution and bacteria surface macromolecules on bacteria (Rhodococcus rhodochrous) transport and deposition mechanisms. Three sizes of silica sands were used in these transport experiments, and their median grain sizes were 607, 567, and 330 microm. The amount of retained bacteria increased with decreasing sand size, and most of the deposited bacteria were found adjacent to the column inlet. The deposition profiles were not consistent with predictions based on classical filtration theory. The experimental data could be accurately characterized using a mathematical model that accounted for first-order attachment, detachment, and time and depth-dependent straining processes. Visual observations of the bacteria deposition as well as mathematical modelling indicated that straining was the dominant mechanism of deposition in these sands (78-99.6% of the deposited bacteria), which may have been enhanced due to the tendency of this bacterium to form aggregates. An additional unsaturated experiment was conducted to better deduce the role of bacteria surface macromolecules on attachment and straining processes. In this case, the bacteria surface was treated using a proteolitic enzyme. This technique was assessed by examining the Fourier-transform infrared spectrum and hydrophobicity of untreated and enzyme treated cells. Both of these analytical procedures demonstrated that this enzymatic treatment removed the surface proteins and/or associated macromolecules. Transport and modelling studies conducted with the enzyme treated bacteria, revealed a decrease in attachment, but that straining was not significantly affected by this treatment.
536 _ _ |a Terrestrische Umwelt
|c P24
|2 G:(DE-HGF)
|0 G:(DE-Juel1)FUEK407
|x 0
588 _ _ |a Dataset connected to Web of Science, Pubmed
650 _ 2 |2 MeSH
|a Bacteria: chemistry
650 _ 2 |2 MeSH
|a Bacteria: metabolism
650 _ 2 |2 MeSH
|a Bacterial Adhesion
650 _ 2 |2 MeSH
|a Bacterial Proteins: chemistry
650 _ 2 |2 MeSH
|a Bacterial Proteins: metabolism
650 _ 2 |2 MeSH
|a Membrane Proteins: chemistry
650 _ 2 |2 MeSH
|a Membrane Proteins: metabolism
650 _ 2 |2 MeSH
|a Particle Size
650 _ 2 |2 MeSH
|a Porosity
650 _ 2 |2 MeSH
|a Silicon Dioxide: chemistry
650 _ 2 |2 MeSH
|a Surface Properties
650 _ 7 |0 0
|2 NLM Chemicals
|a Bacterial Proteins
650 _ 7 |0 0
|2 NLM Chemicals
|a Membrane Proteins
650 _ 7 |0 7631-86-9
|2 NLM Chemicals
|a Silicon Dioxide
650 _ 7 |a J
|2 WoSType
653 2 0 |2 Author
|a bacteria transport
653 2 0 |2 Author
|a classical filtration theory
653 2 0 |2 Author
|a unsaturated flow
653 2 0 |2 Author
|a Rhodococcus rhodochrous
700 1 _ |a Bradford, S.
|b 1
|0 P:(DE-HGF)0
700 1 _ |a Simunek, J.
|b 2
|0 P:(DE-HGF)0
700 1 _ |a Ustohal, P.
|b 3
|0 P:(DE-HGF)0
700 1 _ |a Vereecken, H.
|b 4
|u FZJ
|0 P:(DE-Juel1)129549
700 1 _ |a Klumpp, E.
|b 5
|u FZJ
|0 P:(DE-Juel1)129484
773 _ _ |a 10.1016/j.jconhyd.2007.01.009
|g Vol. 92
|q 92
|0 PERI:(DE-600)1494766-3
|t Journal of contaminant hydrology
|v 92
|y 2007
|x 0169-7722
856 7 _ |u http://dx.doi.org/10.1016/j.jconhyd.2007.01.009
909 C O |o oai:juser.fz-juelich.de:57171
|p VDB
913 1 _ |k P24
|v Terrestrische Umwelt
|l Terrestrische Umwelt
|b Erde und Umwelt
|0 G:(DE-Juel1)FUEK407
|x 0
914 1 _ |a
|y 2007
915 _ _ |0 StatID:(DE-HGF)0010
|a JCR/ISI refereed
920 1 _ |d 31.10.2010
|g ICG
|k ICG-4
|l Agrosphäre
|0 I:(DE-Juel1)VDB793
|x 1
920 1 _ |0 I:(DE-82)080011_20140620
|k JARA-ENERGY
|l Jülich-Aachen Research Alliance - Energy
|g JARA
|x 2
920 1 _ |0 I:(DE-Juel1)VDB1045
|k JARA-SIM
|l Jülich-Aachen Research Alliance - Simulation Sciences
|g JARA
|x 3
970 _ _ |a VDB:(DE-Juel1)89924
980 _ _ |a VDB
980 _ _ |a ConvertedRecord
980 _ _ |a journal
980 _ _ |a I:(DE-Juel1)IBG-3-20101118
980 _ _ |a I:(DE-82)080011_20140620
980 _ _ |a I:(DE-Juel1)VDB1045
980 _ _ |a UNRESTRICTED
981 _ _ |a I:(DE-Juel1)IBG-3-20101118
981 _ _ |a I:(DE-Juel1)VDB1045
981 _ _ |a I:(DE-Juel1)VDB1047


LibraryCollectionCLSMajorCLSMinorLanguageAuthor
Marc 21