001     9702
005     20180208220116.0
024 7 _ |2 pmid
|a pmid:20176838
024 7 _ |2 DOI
|a 10.2134/jeq2009.0001
024 7 _ |2 WOS
|a WOS:000275383600022
037 _ _ |a PreJuSER-9702
041 _ _ |a eng
082 _ _ |a 333.7
084 _ _ |2 WoS
|a Environmental Sciences
100 1 _ |a Wehrhan, A.
|b 0
|u FZJ
|0 P:(DE-Juel1)VDB36636
245 _ _ |a Long-Term Sorption and Desorption of Sulfadiazine in Soil: Experiments and Modeling
260 _ _ |a Madison, Wis.
|b ASA [u.a.]
|c 2010
300 _ _ |a 654 - 666
336 7 _ |a Journal Article
|0 PUB:(DE-HGF)16
|2 PUB:(DE-HGF)
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336 7 _ |a ARTICLE
|2 BibTeX
336 7 _ |a JOURNAL_ARTICLE
|2 ORCID
336 7 _ |a article
|2 DRIVER
440 _ 0 |a Journal of Environmental Quality
|x 0047-2425
|0 3300
|y 2
|v 39
500 _ _ |a Record converted from VDB: 12.11.2012
520 _ _ |a Antibiotics, such as sulfadiazine (SDZ), may enter arable soil by spreading of manure of medicated husbandry or directly by the excrement of grazing animals. Knowledge of the fate of antibiotics in soils is crucial for assessing the environmental risk of these compounds, including possible transport to ground water. Kinetic sorption of (14)C-labeled SDZ (4-amino-N-pyrimidin-2-yl-benzenesulfonamide) was investigated using the batch technique. The batch sorption-desorption experiments were conducted at various concentration levels (0.044-13 mg L(-1) initial solute concentration) and time scales (0.75-272 d). Sorption of (14)C-SDZ in the investigated silty loam was time dependent and strongly nonlinear in the solution phase concentration. The time to reach an apparent sorption equilibrium was about 20 d. However, desorption was very slow, and 41 d were insufficient to reach the desorption equilibrium. An inverse modeling technique was used to identify relevant sorption processes of (14)C-SDZ during the batch experiments. Among the investigated two- and three-domain sorption models, adsorption and desorption of (14)C-SDZ were best described with a new model defining two sorption domains and four parameters. Whereas sorption in the first sorption domain was nonlinear and instantaneous, solute uptake in the second sorption domain was rate limited following first-order kinetics. Desorption followed the same rate law until an equilibrium distribution was reached. After that, desorption was assumed to be impossible due to partly irreversible sorption. Although the proposed model needs further validation, it contributes to the discussion on complex sorption processes of organic chemicals in soils.
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 Adsorption
650 _ 2 |2 MeSH
|a Anti-Infective Agents: chemistry
650 _ 2 |2 MeSH
|a Models, Chemical
650 _ 2 |2 MeSH
|a Soil: analysis
650 _ 2 |2 MeSH
|a Sulfadiazine: chemistry
650 _ 7 |0 0
|2 NLM Chemicals
|a Anti-Infective Agents
650 _ 7 |0 0
|2 NLM Chemicals
|a Soil
650 _ 7 |0 68-35-9
|2 NLM Chemicals
|a Sulfadiazine
650 _ 7 |a J
|2 WoSType
700 1 _ |a Streck, T.
|b 1
|0 P:(DE-HGF)0
700 1 _ |a Groeneweg, J.
|b 2
|u FZJ
|0 P:(DE-Juel1)129462
700 1 _ |a Vereecken, H.
|b 3
|u FZJ
|0 P:(DE-Juel1)129549
700 1 _ |a Kasteel, R.
|b 4
|u FZJ
|0 P:(DE-Juel1)VDB724
773 _ _ |a 10.2134/jeq2009.0001
|g Vol. 39, p. 654 - 666
|p 654 - 666
|q 39<654 - 666
|0 PERI:(DE-600)2050469-X
|t Journal of environmental quality
|v 39
|y 2010
|x 0047-2425
856 7 _ |u http://dx.doi.org/10.2134/jeq2009.0001
909 C O |o oai:juser.fz-juelich.de:9702
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913 1 _ |k P24
|v Terrestrische Umwelt
|l Terrestrische Umwelt
|b Erde und Umwelt
|0 G:(DE-Juel1)FUEK407
|x 0
914 1 _ |y 2010
915 _ _ |0 StatID:(DE-HGF)0010
|a JCR/ISI refereed
920 1 _ |d 31.10.2010
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920 1 _ |0 I:(DE-82)080011_20140620
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|l Jülich Aachen Research Alliance - High-Performance Computing
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980 _ _ |a UNRESTRICTED
981 _ _ |a I:(DE-Juel1)IBG-3-20101118
981 _ _ |a I:(DE-Juel1)VDB1047
981 _ _ |a I:(DE-Juel1)VDB1346


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