000837570 001__ 837570
000837570 005__ 20210129231356.0
000837570 0247_ $$2doi$$a10.1080/02626667.2017.1313979
000837570 0247_ $$2ISSN$$a0020-6024
000837570 0247_ $$2ISSN$$a0262-6667
000837570 0247_ $$2ISSN$$a0303-6936
000837570 0247_ $$2ISSN$$a2150-3435
000837570 0247_ $$2WOS$$aWOS:000403800000005
000837570 0247_ $$2altmetric$$aaltmetric:23226377
000837570 037__ $$aFZJ-2017-06458
000837570 082__ $$a550
000837570 1001_ $$0P:(DE-HGF)0$$aEludoyin, Adebayo O.$$b0$$eCorresponding author
000837570 245__ $$aAn evaluation of the hysteresis in chemical concentration–discharge ( C – Q ) relationships from drained, intensively managed grasslands in southwest England
000837570 260__ $$aWallingford$$bIAHS Press$$c2017
000837570 3367_ $$2DRIVER$$aarticle
000837570 3367_ $$2DataCite$$aOutput Types/Journal article
000837570 3367_ $$0PUB:(DE-HGF)16$$2PUB:(DE-HGF)$$aJournal Article$$bjournal$$mjournal$$s1504860100_17820
000837570 3367_ $$2BibTeX$$aARTICLE
000837570 3367_ $$2ORCID$$aJOURNAL_ARTICLE
000837570 3367_ $$00$$2EndNote$$aJournal Article
000837570 520__ $$aThis study examined the hysteresis exhibited in concentration–discharge (C–Q) relationships in the runoff from four hydrologically separated fields (catchments) at an intensively managed grassland. The objectives were to examine C–Q relationships constructed from high-resolution time series of flow, temperature, pH, conductivity, nitrate and turbidity, and their implications for hydrological processes. High-resolution datasets from the quality assured records of the Rothamsted Research North Wyke Farm Platform in the UK were examined using a graphical method and cross-correlation statistics. The study found that storm events based C–Q hysteresis reflects the cross-correlation that is generally hidden in time series analysis of large datasets, and that although Q and water quality variables can be effectively influenced by catchment size, the C–Q relationship is less significantly influenced. The dominant C–Q relationships of the water variables in the study area reflect that saturated overland flow was prevalent during the study period in the catchments, while the CCF results indicate coupled transfer of sediments and solute in the area at lag ≥ 0.
000837570 536__ $$0G:(DE-HGF)POF3-255$$a255 - Terrestrial Systems: From Observation to Prediction (POF3-255)$$cPOF3-255$$fPOF III$$x0
000837570 588__ $$aDataset connected to CrossRef
000837570 7001_ $$0P:(DE-HGF)0$$aGriffith, Bruce$$b1
000837570 7001_ $$0P:(DE-HGF)0$$aOrr, Robert J.$$b2
000837570 7001_ $$0P:(DE-Juel1)145865$$aBol, Roland$$b3
000837570 7001_ $$0P:(DE-HGF)0$$aQuine, Timothy A.$$b4
000837570 7001_ $$0P:(DE-HGF)0$$aBrazier, Richard E.$$b5
000837570 773__ $$0PERI:(DE-600)2180448-5$$a10.1080/02626667.2017.1313979$$gVol. 62, no. 8, p. 1243 - 1254$$n8$$p1243 - 1254$$tHydrological sciences journal$$v62$$x2150-3435$$y2017
000837570 909CO $$ooai:juser.fz-juelich.de:837570$$pVDB:Earth_Environment$$pVDB
000837570 9101_ $$0I:(DE-588b)5008462-8$$6P:(DE-Juel1)145865$$aForschungszentrum Jülich$$b3$$kFZJ
000837570 9131_ $$0G:(DE-HGF)POF3-255$$1G:(DE-HGF)POF3-250$$2G:(DE-HGF)POF3-200$$3G:(DE-HGF)POF3$$4G:(DE-HGF)POF$$aDE-HGF$$bErde und Umwelt$$lTerrestrische Umwelt$$vTerrestrial Systems: From Observation to Prediction$$x0
000837570 9141_ $$y2017
000837570 915__ $$0StatID:(DE-HGF)0200$$2StatID$$aDBCoverage$$bSCOPUS
000837570 915__ $$0StatID:(DE-HGF)0100$$2StatID$$aJCR$$bHYDROLOG SCI J : 2015
000837570 915__ $$0StatID:(DE-HGF)0600$$2StatID$$aDBCoverage$$bEbsco Academic Search
000837570 915__ $$0StatID:(DE-HGF)0030$$2StatID$$aPeer Review$$bASC
000837570 915__ $$0StatID:(DE-HGF)0199$$2StatID$$aDBCoverage$$bThomson Reuters Master Journal List
000837570 915__ $$0StatID:(DE-HGF)0111$$2StatID$$aWoS$$bScience Citation Index Expanded
000837570 915__ $$0StatID:(DE-HGF)0150$$2StatID$$aDBCoverage$$bWeb of Science Core Collection
000837570 915__ $$0StatID:(DE-HGF)1060$$2StatID$$aDBCoverage$$bCurrent Contents - Agriculture, Biology and Environmental Sciences
000837570 915__ $$0StatID:(DE-HGF)9900$$2StatID$$aIF < 5
000837570 9201_ $$0I:(DE-Juel1)IBG-3-20101118$$kIBG-3$$lAgrosphäre$$x0
000837570 980__ $$ajournal
000837570 980__ $$aVDB
000837570 980__ $$aI:(DE-Juel1)IBG-3-20101118
000837570 980__ $$aUNRESTRICTED