001     45074
005     20180210124246.0
024 7 _ |2 pmid
|a pmid:15792662
024 7 _ |2 DOI
|a 10.1016/j.chemosphere.2004.10.027
024 7 _ |2 WOS
|a WOS:000228890400007
037 _ _ |a PreJuSER-45074
041 _ _ |a eng
082 _ _ |a 333.7
084 _ _ |2 WoS
|a Environmental Sciences
100 1 _ |a Berns, A.
|b 0
|u FZJ
|0 P:(DE-Juel1)129438
245 _ _ |a Use of 15N-depleted artificial compost in bound residue studies
260 _ _ |a Amsterdam [u.a.]
|b Elsevier Science
|c 2005
300 _ _ |a 649 - 658
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 Chemosphere
|x 0045-6535
|0 1228
|v 59
500 _ _ |a Record converted from VDB: 12.11.2012
520 _ _ |a Association of bound residues to soil humic matter may be accomplished by different binding mechanisms such as sequestration in hydrophobic interiors of the organic material or covalent linkage to the organic matter. The structures and chemical environments of compounds can be observed by NMR spectroscopy. We applied 15N-NMR spectroscopy to study the soil-bound residues of 15N-labeled simazine. As the 15N-isotope has a low sensitivity and natural abundance 15N-NMR experiments require long measurement times and often result in low signal-to-noise (S/N) ratios. Therefore, in addition to the use of 15N-labeled simazine, 15N-depleted compost was used to reduce the amount of background signal and enhance the sensitivity. The compost was produced from maize and wheat plants grown on sand with 15N-depleted NH4NO3 as sole nitrogen source. The plants were freeze-dried, ground and mixed with sand for composting. After a composting period of 224 days analysis of the compost revealed a 15N-content of 267 ppm as opposed to a natural abundance of 3650 ppm. Characterization of this artificial compost produced parameter values similar to those of a natural compost. The 13C-NMR-spectra of the humic and fulvic acids during different stages of maturity showed that there was a shift from single-bond functional groups to more complex double-bond and aromatic structures. Experiments with this compost showed an increased signal intensity. The improved sensitivity made it possible to obtain interpretable NMR signals in contrast to experiments with 15N-simazine on native soil where no signals were detectable. The data indicated that the bound residues of simazine are composed of metabolites resulting from N-dealkylation and triazine ring destruction. Silylation of the bound residues showed a very strong binding of the residues to the matrix as only a small fraction could be solubilized.
536 _ _ |a Chemie und Dynamik der Geo-Biosphäre
|c U01
|2 G:(DE-HGF)
|0 G:(DE-Juel1)FUEK257
|x 0
588 _ _ |a Dataset connected to Web of Science, Pubmed
650 _ 2 |2 MeSH
|a Chromatography, Gel
650 _ 2 |2 MeSH
|a Humic Substances: analysis
650 _ 2 |2 MeSH
|a Magnetic Resonance Spectroscopy: methods
650 _ 2 |2 MeSH
|a Nitrogen Isotopes
650 _ 2 |2 MeSH
|a Pesticide Residues: chemistry
650 _ 2 |2 MeSH
|a Simazine: chemistry
650 _ 2 |2 MeSH
|a Soil: analysis
650 _ 2 |2 MeSH
|a Trimethylsilyl Compounds
650 _ 7 |0 0
|2 NLM Chemicals
|a Humic Substances
650 _ 7 |0 0
|2 NLM Chemicals
|a Nitrogen Isotopes
650 _ 7 |0 0
|2 NLM Chemicals
|a Pesticide Residues
650 _ 7 |0 0
|2 NLM Chemicals
|a Soil
650 _ 7 |0 0
|2 NLM Chemicals
|a Trimethylsilyl Compounds
650 _ 7 |0 122-34-9
|2 NLM Chemicals
|a Simazine
650 _ 7 |0 75-77-4
|2 NLM Chemicals
|a trimethylchlorosilane
650 _ 7 |a J
|2 WoSType
653 2 0 |2 Author
|a N-15-depleted compost
653 2 0 |2 Author
|a bound residues
653 2 0 |2 Author
|a N-15-CPMAS spectroscopy
653 2 0 |2 Author
|a N-15-labeled simazine
653 2 0 |2 Author
|a silylation
700 1 _ |a Vinken, R.
|b 1
|u FZJ
|0 P:(DE-Juel1)VDB21718
700 1 _ |a Bertmer, M.
|b 2
|u FZJ
|0 P:(DE-Juel1)VDB21719
700 1 _ |a Breitschwerdt, A.
|b 3
|u FZJ
|0 P:(DE-Juel1)VDB21720
700 1 _ |a Schäffer, A.
|b 4
|u FZJ
|0 P:(DE-Juel1)VDB1399
773 _ _ |a 10.1016/j.chemosphere.2004.10.027
|g Vol. 59, p. 649 - 658
|p 649 - 658
|q 59<649 - 658
|0 PERI:(DE-600)1496851-4
|t Chemosphere
|v 59
|y 2005
|x 0045-6535
856 7 _ |u http://dx.doi.org/10.1016/j.chemosphere.2004.10.027
909 C O |o oai:juser.fz-juelich.de:45074
|p VDB
913 1 _ |k U01
|v Chemie und Dynamik der Geo-Biosphäre
|l Chemie und Dynamik der Geo-Biosphäre
|b Environment (Umwelt)
|0 G:(DE-Juel1)FUEK257
|x 0
914 1 _ |y 2005
915 _ _ |0 StatID:(DE-HGF)0010
|a JCR/ISI refereed
920 1 _ |k ICG-IV
|l Agrosphäre
|d 31.12.2006
|g ICG
|0 I:(DE-Juel1)VDB50
|x 0
970 _ _ |a VDB:(DE-Juel1)67306
980 _ _ |a VDB
980 _ _ |a ConvertedRecord
980 _ _ |a journal
980 _ _ |a I:(DE-Juel1)IBG-3-20101118
980 _ _ |a UNRESTRICTED
981 _ _ |a I:(DE-Juel1)IBG-3-20101118


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