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024 7 _ |2 DOI
|a 10.1016/j.geoderma.2006.08.033
024 7 _ |2 WOS
|a WOS:000243842700011
037 _ _ |a PreJuSER-55349
041 _ _ |a eng
082 _ _ |a 550
084 _ _ |2 WoS
|a Soil Science
100 1 _ |a Kasteel, R.
|b 0
|u FZJ
|0 P:(DE-Juel1)VDB724
245 _ _ |a Dye tracer infiltration in the plough layer after straw incorporation
260 _ _ |a Amsterdam [u.a.]
|b Elsevier Science
|c 2007
300 _ _ |a 360 - 369
336 7 _ |a Journal Article
|0 PUB:(DE-HGF)16
|2 PUB:(DE-HGF)
336 7 _ |a Output Types/Journal article
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336 7 _ |a Journal Article
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336 7 _ |a ARTICLE
|2 BibTeX
336 7 _ |a JOURNAL_ARTICLE
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336 7 _ |a article
|2 DRIVER
440 _ 0 |a Geoderma
|x 0016-7061
|0 8464
|v 137
500 _ _ |a Record converted from VDB: 12.11.2012
520 _ _ |a Straw residues may be accumulated in isolated zones in the plough layer after mouldboard ploughing. This may limit straw decomposition because of limited nitrogen availability depending on the prevalent water flow pathways induced by tillage. In this study, we used the food dye Brilliant Blue FCF (Color Index 42090) to make visible the flow pathways in the plough layer of a loamy soil after incorporation of 10 tonne of dry mass ha(-1), and to get a qualitative and quantitative interpretation of the small-scale flow behaviour. Approximately 1.3 L of a 4 g L-1 Brilliant Blue solution was applied at a matric head of -1 cm with an infiltrometer, equipped with a 25 cm-diameter disk. Horizontal cross-sections of 50 x 50 cm were photographed at 1.5 to 3.5 cm depth intervals. High-resolution spatial maps of Brilliant Blue concentration were derived from the scanned photographs, using separate calibration relationships between the measured Brilliant Blue concentrations and the color spectra and depth for the soil and the straw. Pronounced lateral dye movement was observed through the soil matrix owing to soil sorptivity. In cases of high sorptivity, the dye barely reached the depth of straw incorporation. Otherwise, enhanced preferential dye transport directed towards the incorporated straw was made visible and the stained water eventually ponded on the plough pan which induced lateral redistribution. Although the straw inclusions contributed to dye transport, they did not retain a substantial part of the applied dye mass, owing to the low density and surface area of straw. However, these inclusions may enhance the fast migration of potential pollutants such as nitrate or pesticides out of the tilled layer where much of the transformation occurs due to biological activity. (c) 2006 Elsevier B.V. All rights reserved.
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
650 _ 7 |a J
|2 WoSType
653 2 0 |2 Author
|a straw
653 2 0 |2 Author
|a mouldboard ploughing
653 2 0 |2 Author
|a dye tracers
653 2 0 |2 Author
|a image analysis
653 2 0 |2 Author
|a infiltrometer
653 2 0 |2 Author
|a plough layer
700 1 _ |a Garnier, P.
|b 1
|0 P:(DE-HGF)0
700 1 _ |a Vachier, P.
|b 2
|0 P:(DE-HGF)0
700 1 _ |a Coquet, Y.
|b 3
|0 P:(DE-HGF)0
773 _ _ |a 10.1016/j.geoderma.2006.08.033
|g Vol. 137, p. 360 - 369
|p 360 - 369
|q 137<360 - 369
|0 PERI:(DE-600)2001729-7
|t Geoderma
|v 137
|y 2007
|x 0016-7061
856 7 _ |u http://dx.doi.org/10.1016/j.geoderma.2006.08.033
909 C O |o oai:juser.fz-juelich.de:55349
|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 _ |y 2007
915 _ _ |0 StatID:(DE-HGF)0010
|a JCR/ISI refereed
920 1 _ |k ICG-4
|l Agrosphäre
|d 31.10.2010
|g ICG
|0 I:(DE-Juel1)VDB793
|x 1
970 _ _ |a VDB:(DE-Juel1)86305
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980 _ _ |a journal
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980 _ _ |a UNRESTRICTED
981 _ _ |a I:(DE-Juel1)IBG-3-20101118


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