000001092 001__ 1092
000001092 005__ 20200423202345.0
000001092 0247_ $$2DOI$$a10.1029/2007WR006425
000001092 0247_ $$2WOS$$aWOS:000260389400002
000001092 0247_ $$2Handle$$a2128/19795
000001092 037__ $$aPreJuSER-1092
000001092 041__ $$aeng
000001092 082__ $$a550
000001092 084__ $$2WoS$$aEnvironmental Sciences
000001092 084__ $$2WoS$$aLimnology
000001092 084__ $$2WoS$$aWater Resources
000001092 1001_ $$0P:(DE-HGF)0$$aBloem, E.$$b0
000001092 245__ $$aLeaching surfaces to characterize transport in a heterogeneous aquifer: Comparison between flux concentrations, resident concentrations, and flux concentrations estimated from temporal moment analysis
000001092 260__ $$aWashington, DC$$bAGU$$c2008
000001092 300__ $$aW10412
000001092 3367_ $$0PUB:(DE-HGF)16$$2PUB:(DE-HGF)$$aJournal Article
000001092 3367_ $$2DataCite$$aOutput Types/Journal article
000001092 3367_ $$00$$2EndNote$$aJournal Article
000001092 3367_ $$2BibTeX$$aARTICLE
000001092 3367_ $$2ORCID$$aJOURNAL_ARTICLE
000001092 3367_ $$2DRIVER$$aarticle
000001092 440_0 $$05958$$aWater Resources Research$$v44$$x0043-1397
000001092 500__ $$aThis research is supported by the Research Council for Earth and Life Sciences (ALW) with financial aid from the Netherlands Organization for Scientific Research (NWO).
000001092 520__ $$aFor subsurface solute transport, flux concentrations are key, while usually resident concentrations are measured. Flux concentrations are frequently estimated from resident concentrations by temporal moment analysis. We tested this approach by simulating transport of an injected tracer during steady flow in an aquifer with a heterogeneous saturated hydraulic conductivity. We constructed grid cell-scale breakthrough curves (BTCs) from flux concentrations and approximated BTCs from resident concentrations and estimated flux concentrations. We assembled these BTCs into spatiotemporal leaching surfaces at various aquifer cross sections for subsequent analysis. Resident concentrations were unsuitable to assess solute movement in the aquifer. Temporal moment analysis worked well when the entire aquifer cross section was considered but performed poorer at the grid cell scale because it approximates the local velocity by the trajectory average. The leaching surfaces served as valuable tools to demonstrate and quantify the limitations of temporal moment analysis.
000001092 536__ $$0G:(DE-Juel1)FUEK407$$2G:(DE-HGF)$$aTerrestrische Umwelt$$cP24$$x0
000001092 588__ $$aDataset connected to Web of Science
000001092 650_7 $$2WoSType$$aJ
000001092 7001_ $$0P:(DE-Juel1)129548$$aVanderborght, J.$$b1$$uFZJ
000001092 7001_ $$0P:(DE-HGF)0$$ade Rooij, G. H.$$b2
000001092 773__ $$0PERI:(DE-600)2029553-4$$a10.1029/2007WR006425$$gVol. 44, p. W10412$$pW10412$$q44<W10412$$tWater resources research$$v44$$x0043-1397$$y2008
000001092 8567_ $$uhttp://dx.doi.org/10.1029/2007WR006425
000001092 8564_ $$uhttps://juser.fz-juelich.de/record/1092/files/Bloem_et_al-2008-Water_Resources_Research.pdf$$yOpenAccess
000001092 8564_ $$uhttps://juser.fz-juelich.de/record/1092/files/Bloem_et_al-2008-Water_Resources_Research.gif?subformat=icon$$xicon$$yOpenAccess
000001092 8564_ $$uhttps://juser.fz-juelich.de/record/1092/files/Bloem_et_al-2008-Water_Resources_Research.jpg?subformat=icon-180$$xicon-180$$yOpenAccess
000001092 8564_ $$uhttps://juser.fz-juelich.de/record/1092/files/Bloem_et_al-2008-Water_Resources_Research.jpg?subformat=icon-700$$xicon-700$$yOpenAccess
000001092 8564_ $$uhttps://juser.fz-juelich.de/record/1092/files/Bloem_et_al-2008-Water_Resources_Research.pdf?subformat=pdfa$$xpdfa$$yOpenAccess
000001092 909CO $$ooai:juser.fz-juelich.de:1092$$pdnbdelivery$$pdriver$$pVDB$$popen_access$$popenaire
000001092 9131_ $$0G:(DE-Juel1)FUEK407$$bErde und Umwelt$$kP24$$lTerrestrische Umwelt$$vTerrestrische Umwelt$$x0
000001092 9141_ $$y2008
000001092 915__ $$0StatID:(DE-HGF)0510$$2StatID$$aOpenAccess
000001092 915__ $$0StatID:(DE-HGF)0010$$aJCR/ISI refereed
000001092 915__ $$0StatID:(DE-HGF)0030$$2StatID$$aPeer review
000001092 9201_ $$0I:(DE-Juel1)VDB793$$d31.10.2010$$gICG$$kICG-4$$lAgrosphäre$$x1
000001092 970__ $$aVDB:(DE-Juel1)101982
000001092 980__ $$aVDB
000001092 980__ $$aConvertedRecord
000001092 980__ $$ajournal
000001092 980__ $$aI:(DE-Juel1)IBG-3-20101118
000001092 980__ $$aUNRESTRICTED
000001092 9801_ $$aFullTexts
000001092 981__ $$aI:(DE-Juel1)IBG-3-20101118