000857180 001__ 857180
000857180 005__ 20210129235520.0
000857180 0247_ $$2doi$$a10.1111/ejss.12504
000857180 0247_ $$2ISSN$$a0022-4588
000857180 0247_ $$2ISSN$$a1351-0754
000857180 0247_ $$2ISSN$$a1365-2389
000857180 0247_ $$2ISSN$$a2056-5240
000857180 0247_ $$2WOS$$aWOS:000427881900009
000857180 037__ $$aFZJ-2018-06417
000857180 082__ $$a550
000857180 1001_ $$00000-0003-0259-4079$$aHarris, P.$$b0$$eCorresponding author
000857180 245__ $$aEffect of long-term drainage on plant community, soil carbon and nitrogen contents and stable isotopic ( δ 13 C, δ 15 N) composition of a permanent grassland
000857180 260__ $$aOxford [u.a.]$$bWiley-Blackwell$$c2018
000857180 3367_ $$2DRIVER$$aarticle
000857180 3367_ $$2DataCite$$aOutput Types/Journal article
000857180 3367_ $$0PUB:(DE-HGF)16$$2PUB:(DE-HGF)$$aJournal Article$$bjournal$$mjournal$$s1542203218_10165
000857180 3367_ $$2BibTeX$$aARTICLE
000857180 3367_ $$2ORCID$$aJOURNAL_ARTICLE
000857180 3367_ $$00$$2EndNote$$aJournal Article
000857180 520__ $$aThis study compares data statistically that were collected from both long‐term drained and undrained plots to test hypotheses concerning the effect of drainage on plant community, soil total nitrogen (TN), soil total carbon (TC) and stable isotopic (δ15N, δ13C) contents in a permanent grassland. In addition, the effects of soil depth, topography (elevation, slope, aspect and compound topographic index (CTI)) and spatial autocorrelation were taken into account. Data were collected in 2010 at Rowden Moor, North Wyke, Devon, UK, where, for the plots of this study, subsurface drainage was introduced in 1987. The results of a set of six linear mixed models showed that: (i) plant community did not depend on drainage, but on elevation and spatial effects, (ii) both TN and TC not only depended on drainage, but also topography and sample depth, (iii) the TC to TN ratio did not depend on drainage, but on elevation, CTI and sample depth only, (iv) δ15N values did not depend on drainage, but on topography and sample depth and (v) δ13C values depended on drainage together with topography and sample depth. Thus, drainage represented a significant effect for only TN, TC and δ13C. Furthermore, changes in soil physicochemical conditions, following the introduction of drainage in the clay soil 24 years previously, induced a shift in the plant community from a Lolium perenne L. dominated grassland with numerous patches of Juncus species, towards one with Lolium perenne and Trifolium repens L.
000857180 536__ $$0G:(DE-HGF)POF3-255$$a255 - Terrestrial Systems: From Observation to Prediction (POF3-255)$$cPOF3-255$$fPOF III$$x0
000857180 588__ $$aDataset connected to CrossRef
000857180 7001_ $$0P:(DE-Juel1)145865$$aBol, R.$$b1
000857180 7001_ $$0P:(DE-HGF)0$$aEvans, J.$$b2
000857180 7001_ $$0P:(DE-HGF)0$$aHawkins, J. M. B.$$b3
000857180 7001_ $$0P:(DE-HGF)0$$aDixon, E. R.$$b4
000857180 7001_ $$0P:(DE-HGF)0$$aWolf, K.$$b5
000857180 7001_ $$0P:(DE-HGF)0$$aDungait, J. A. J.$$b6
000857180 7001_ $$0P:(DE-HGF)0$$aGriffith, B.$$b7
000857180 7001_ $$0P:(DE-Juel1)129469$$aHerbst, Michael$$b8
000857180 7001_ $$0P:(DE-HGF)0$$aDhanoa, M. S.$$b9
000857180 7001_ $$0P:(DE-HGF)0$$aBeaumont, D. A.$$b10
000857180 7001_ $$0P:(DE-HGF)0$$aDunn, R. M.$$b11
000857180 7001_ $$0P:(DE-HGF)0$$aWiesenberg, G. L. B.$$b12
000857180 773__ $$0PERI:(DE-600)2020243-X$$a10.1111/ejss.12504$$gVol. 69, no. 1, p. 48 - 68$$n1$$p48 - 68$$tEuropean journal of soil science$$v69$$x1351-0754$$y2018
000857180 8564_ $$uhttps://juser.fz-juelich.de/record/857180/files/Harris_et_al-2018-European_Journal_of_Soil_Science.pdf$$yRestricted
000857180 8564_ $$uhttps://juser.fz-juelich.de/record/857180/files/Harris_et_al-2018-European_Journal_of_Soil_Science.pdf?subformat=pdfa$$xpdfa$$yRestricted
000857180 909CO $$ooai:juser.fz-juelich.de:857180$$pVDB:Earth_Environment$$pVDB
000857180 9101_ $$0I:(DE-588b)5008462-8$$6P:(DE-Juel1)145865$$aForschungszentrum Jülich$$b1$$kFZJ
000857180 9101_ $$0I:(DE-588b)5008462-8$$6P:(DE-Juel1)129469$$aForschungszentrum Jülich$$b8$$kFZJ
000857180 9131_ $$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$$x0
000857180 9141_ $$y2018
000857180 915__ $$0StatID:(DE-HGF)0420$$2StatID$$aNationallizenz
000857180 915__ $$0StatID:(DE-HGF)0200$$2StatID$$aDBCoverage$$bSCOPUS
000857180 915__ $$0StatID:(DE-HGF)0100$$2StatID$$aJCR$$bEUR J SOIL SCI : 2017
000857180 915__ $$0StatID:(DE-HGF)0300$$2StatID$$aDBCoverage$$bMedline
000857180 915__ $$0StatID:(DE-HGF)0600$$2StatID$$aDBCoverage$$bEbsco Academic Search
000857180 915__ $$0StatID:(DE-HGF)0030$$2StatID$$aPeer Review$$bASC
000857180 915__ $$0StatID:(DE-HGF)0199$$2StatID$$aDBCoverage$$bClarivate Analytics Master Journal List
000857180 915__ $$0StatID:(DE-HGF)0110$$2StatID$$aWoS$$bScience Citation Index
000857180 915__ $$0StatID:(DE-HGF)0150$$2StatID$$aDBCoverage$$bWeb of Science Core Collection
000857180 915__ $$0StatID:(DE-HGF)0111$$2StatID$$aWoS$$bScience Citation Index Expanded
000857180 915__ $$0StatID:(DE-HGF)1060$$2StatID$$aDBCoverage$$bCurrent Contents - Agriculture, Biology and Environmental Sciences
000857180 915__ $$0StatID:(DE-HGF)1050$$2StatID$$aDBCoverage$$bBIOSIS Previews
000857180 915__ $$0StatID:(DE-HGF)9900$$2StatID$$aIF < 5
000857180 9201_ $$0I:(DE-Juel1)IBG-3-20101118$$kIBG-3$$lAgrosphäre$$x0
000857180 980__ $$ajournal
000857180 980__ $$aVDB
000857180 980__ $$aI:(DE-Juel1)IBG-3-20101118
000857180 980__ $$aUNRESTRICTED