000904472 001__ 904472
000904472 005__ 20220126162542.0
000904472 0247_ $$2doi$$a10.1111/ejss.13034
000904472 0247_ $$2ISSN$$a0022-4588
000904472 0247_ $$2ISSN$$a1351-0754
000904472 0247_ $$2ISSN$$a1365-2389
000904472 0247_ $$2ISSN$$a2056-5240
000904472 0247_ $$2altmetric$$aaltmetric:93669852
000904472 0247_ $$2WOS$$aWOS:000580992700001
000904472 037__ $$aFZJ-2021-06042
000904472 082__ $$a550
000904472 1001_ $$00000-0001-6375-617X$$aKuang, Xingxing$$b0$$eCorresponding author
000904472 245__ $$aA modification to the van Genuchten model for improved prediction of relative hydraulic conductivity of unsaturated soils
000904472 260__ $$aOxford [u.a.]$$bWiley-Blackwell$$c2021
000904472 3367_ $$2DRIVER$$aarticle
000904472 3367_ $$2DataCite$$aOutput Types/Journal article
000904472 3367_ $$0PUB:(DE-HGF)16$$2PUB:(DE-HGF)$$aJournal Article$$bjournal$$mjournal$$s1641285836_24212
000904472 3367_ $$2BibTeX$$aARTICLE
000904472 3367_ $$2ORCID$$aJOURNAL_ARTICLE
000904472 3367_ $$00$$2EndNote$$aJournal Article
000904472 500__ $$aKein Postprint vorhanden
000904472 520__ $$aModelling of flow and transport in unsaturated soils requires information on two fundamental hydraulic properties: the soil water retention curve and relative hydraulic conductivity. A soil's relative hydraulic conductivity is frequently predicted from the soil water retention curve. The most widely used combination is the van Genuchten model for the soil water retention curve and the Mualem model for relative hydraulic conductivity (VGM). Previous studies show that the VGM model underestimates measured relative hydraulic conductivity for soils with fine textures; a sharp drop in relative hydraulic conductivity can be seen near saturation. A new modification of the van Genuchten soil water retention model is proposed with the aim of improving the agreement between predicted and measured relative hydraulic conductivity. The Brooks and Corey-Burdine model is used to predict relative hydraulic conductivity from the modified van Genuchten soil water retention curve (MVG-BCB). The modified model assumes independent m and n in the van Genuchten model but with constraints n > 2 and 0 < m < 1. The MVG-BCB model is evaluated by comparing calculated and measured data for 59 soils that have widely varying soil textures, ranging from sandstone to clay. The MVG-BCB model improves the agreement between calculated and measured data for both the soil water retention curve and relative hydraulic conductivity. The MVG-BCB model is closer to measured relative hydraulic conductivity data for most of the selected soils and the sharp drop near saturation is eliminated. Both the modified soil water retention curve and relative hydraulic conductivity functions are smooth curves and can easily be incorporated into vadose zone flow and transport modellings.
000904472 536__ $$0G:(DE-HGF)POF4-2173$$a2173 - Agro-biogeosystems: controls, feedbacks and impact (POF4-217)$$cPOF4-217$$fPOF IV$$x0
000904472 588__ $$aDataset connected to CrossRef, Journals: juser.fz-juelich.de
000904472 7001_ $$0P:(DE-HGF)0$$aJiao, Jiu Jimmy$$b1
000904472 7001_ $$0P:(DE-HGF)0$$aShan, Jipeng$$b2
000904472 7001_ $$0P:(DE-Juel1)174587$$aYang, Zhenlei$$b3
000904472 773__ $$0PERI:(DE-600)2020243-X$$a10.1111/ejss.13034$$gVol. 72, no. 3, p. 1354 - 1372$$n3$$p1354 - 1372$$tEuropean journal of soil science$$v72$$x0022-4588$$y2021
000904472 8564_ $$uhttps://juser.fz-juelich.de/record/904472/files/European%20J%20Soil%20Science%20-%202020%20-%20Kuang%20-%20A%20modification%20to%20the%20van%20Genuchten%20model%20for%20improved%20prediction%20of%20relative.pdf$$yRestricted
000904472 909CO $$ooai:juser.fz-juelich.de:904472$$pVDB
000904472 9101_ $$0I:(DE-588b)5008462-8$$6P:(DE-Juel1)174587$$aForschungszentrum Jülich$$b3$$kFZJ
000904472 9131_ $$0G:(DE-HGF)POF4-217$$1G:(DE-HGF)POF4-210$$2G:(DE-HGF)POF4-200$$3G:(DE-HGF)POF4$$4G:(DE-HGF)POF$$9G:(DE-HGF)POF4-2173$$aDE-HGF$$bForschungsbereich Erde und Umwelt$$lErde im Wandel – Unsere Zukunft nachhaltig gestalten$$vFür eine nachhaltige Bio-Ökonomie – von Ressourcen zu Produkten$$x0
000904472 9141_ $$y2021
000904472 915__ $$0StatID:(DE-HGF)0420$$2StatID$$aNationallizenz$$d2021-01-27$$wger
000904472 915__ $$0StatID:(DE-HGF)3001$$2StatID$$aDEAL Wiley$$d2021-01-27$$wger
000904472 915__ $$0StatID:(DE-HGF)0200$$2StatID$$aDBCoverage$$bSCOPUS$$d2021-01-27
000904472 915__ $$0StatID:(DE-HGF)0300$$2StatID$$aDBCoverage$$bMedline$$d2021-01-27
000904472 915__ $$0StatID:(DE-HGF)0199$$2StatID$$aDBCoverage$$bClarivate Analytics Master Journal List$$d2021-01-27
000904472 915__ $$0StatID:(DE-HGF)0160$$2StatID$$aDBCoverage$$bEssential Science Indicators$$d2021-01-27
000904472 915__ $$0StatID:(DE-HGF)1050$$2StatID$$aDBCoverage$$bBIOSIS Previews$$d2021-01-27
000904472 915__ $$0StatID:(DE-HGF)1060$$2StatID$$aDBCoverage$$bCurrent Contents - Agriculture, Biology and Environmental Sciences$$d2021-01-27
000904472 915__ $$0StatID:(DE-HGF)1190$$2StatID$$aDBCoverage$$bBiological Abstracts$$d2021-01-27
000904472 915__ $$0StatID:(DE-HGF)0113$$2StatID$$aWoS$$bScience Citation Index Expanded$$d2021-01-27
000904472 915__ $$0StatID:(DE-HGF)0150$$2StatID$$aDBCoverage$$bWeb of Science Core Collection$$d2021-01-27
000904472 915__ $$0StatID:(DE-HGF)0100$$2StatID$$aJCR$$bEUR J SOIL SCI : 2019$$d2021-01-27
000904472 915__ $$0StatID:(DE-HGF)0600$$2StatID$$aDBCoverage$$bEbsco Academic Search$$d2021-01-27
000904472 915__ $$0StatID:(DE-HGF)0030$$2StatID$$aPeer Review$$bASC$$d2021-01-27
000904472 915__ $$0StatID:(DE-HGF)9900$$2StatID$$aIF < 5$$d2021-01-27
000904472 9201_ $$0I:(DE-Juel1)IBG-3-20101118$$kIBG-3$$lAgrosphäre$$x0
000904472 980__ $$ajournal
000904472 980__ $$aVDB
000904472 980__ $$aI:(DE-Juel1)IBG-3-20101118
000904472 980__ $$aUNRESTRICTED