001     6838
005     20180208195022.0
024 7 _ |2 DOI
|a 10.1016/j.pce.2009.02.002
024 7 _ |2 WOS
|a WOS:000267959300005
037 _ _ |a PreJuSER-6838
041 _ _ |a eng
082 _ _ |a 550
084 _ _ |2 WoS
|a Geosciences, Multidisciplinary
084 _ _ |2 WoS
|a Meteorology & Atmospheric Sciences
084 _ _ |2 WoS
|a Water Resources
100 1 _ |a Tetzlaff, B.
|b 0
|u FZJ
|0 P:(DE-Juel1)129578
245 _ _ |a Aerial photograph-based delineation of artificially drained areas and their relevance for water balance and nutrient modeling in large river basins
260 _ _ |a Amsterdam [u.a.]
|b Elsevier Science
|c 2009
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 Physics and Chemistry of the Earth
|x 0079-1946
|0 9941
|y 8
|v 34
500 _ _ |a Record converted from VDB: 12.11.2012
520 _ _ |a Intensive agriculture in lowland river catchments is unthinkable without artificial drainage, but these drainage installations represent also an important pathway for diffuse nutrient inputs to surface waters.Efficient tackling of eutrophication requires distributed nutrient modelling with special emphasis on phosphorus inputs, because of their limitative role in freshwater ecosystems. General decision-making aims at the regional scale, but usually only little information exists about the location of drainage installations within meso- and macro-scale river basins. This lead to the development of an approach, how artificially drained lands can be identified by interpreting aerial photographs, and how these findings can be extrapolated by combining land use and soil information in GIS. The approach results in a map of artificially drained areas, which is presented here for the River Ems basin (12,940 km(2)), located in north-western Germany. This map provides the basis for distributed modelling of drainage runoff and diffuse phosphorus inputs. From the model results, it can be found, that about 69% of all P-inputs into surface waters are discharged via artificial drainages.Just under 30% of the diffuse P-inputs arise from less than 4% of the catchment area. These subareas consist of drained raised bogs used as grassland. Due to the favourable ratio of input level to area they are now at the focus of mitigation measures. With respect to the implementation of the European Water Framework Directive, the importance of model-supported analyses of nutrient inputs is increasing. (C) 2009 Elsevier Ltd. 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 Artificial drainage
653 2 0 |2 Author
|a Water balance modelling
653 2 0 |2 Author
|a Nutrient modelling
653 2 0 |2 Author
|a Phosphorus
653 2 0 |2 Author
|a Eutrophication
653 2 0 |2 Author
|a River Ems
700 1 _ |a Kuhr, P.
|b 1
|u FZJ
|0 P:(DE-Juel1)VDB72524
700 1 _ |a Vereecken, H.
|b 2
|u FZJ
|0 P:(DE-Juel1)129549
700 1 _ |a Wendland, F.
|b 3
|u FZJ
|0 P:(DE-Juel1)VDB4997
773 _ _ |a 10.1016/j.pce.2009.02.002
|g Vol. 34
|q 34
|0 PERI:(DE-600)1500664-5
|t Physics and chemistry of the earth
|v 34
|y 2009
|x 0079-1946
856 7 _ |u http://dx.doi.org/10.1016/j.pce.2009.02.002
909 C O |o oai:juser.fz-juelich.de:6838
|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 2009
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)115251
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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