000003843 001__ 3843
000003843 005__ 20180208225030.0
000003843 0247_ $$2DOI$$a10.2136/vzj2008.0062
000003843 0247_ $$2WOS$$aWOS:000263915100009
000003843 037__ $$aPreJuSER-3843
000003843 041__ $$aeng
000003843 082__ $$a550
000003843 084__ $$2WoS$$aEnvironmental Sciences
000003843 084__ $$2WoS$$aSoil Science
000003843 084__ $$2WoS$$aWater Resources
000003843 1001_ $$0P:(DE-HGF)0$$aWeynants, M.$$b0
000003843 245__ $$aRevisting Vereecken Pedotransfer Functions: Introducing a Closed-Form Hydraulic Model
000003843 260__ $$aMadison, Wis.$$bSSSA$$c2009
000003843 300__ $$a86 - 95
000003843 3367_ $$0PUB:(DE-HGF)16$$2PUB:(DE-HGF)$$aJournal Article
000003843 3367_ $$2DataCite$$aOutput Types/Journal article
000003843 3367_ $$00$$2EndNote$$aJournal Article
000003843 3367_ $$2BibTeX$$aARTICLE
000003843 3367_ $$2ORCID$$aJOURNAL_ARTICLE
000003843 3367_ $$2DRIVER$$aarticle
000003843 440_0 $$010301$$aVadose Zone Journal$$v8$$x1539-1663$$y1
000003843 500__ $$aRecord converted from VDB: 12.11.2012
000003843 520__ $$aWe revisited the Vereecken database, which has been used to derive pedotransfer functions (PTFs) to estimate the soil hydraulic parameters of Belgian soils. We developed new PTFs based on the Mualem-van Genuchten model, constraining m = 1-1/n and using fewer parameters. The goodness-of-fit was similar to the one originally obtained by Vereecken. We used a one-step procedure that allows direct quantification of the correlation matrix and the uncertainties of the estimated parameter values. The coefficients of the new PTFs were estimated using a global search algorithm and they were validated against independent data. The PTFs have a wider range of applicability since: (i) they allow the use of the closed-form solution of the unsaturated hydraulic conductivity in the Mualem-van Genuchten model; and (ii) they consider the effect of macroporosity. We determined that the hydraulic conductivity measured close to saturation could not be estimated based on the available estimators; however, the hydraulic conductivity in the matrix domain was predicted with high accuracy.
000003843 536__ $$0G:(DE-Juel1)FUEK407$$2G:(DE-HGF)$$aTerrestrische Umwelt$$cP24$$x0
000003843 588__ $$aDataset connected to Web of Science
000003843 650_7 $$2WoSType$$aJ
000003843 7001_ $$0P:(DE-Juel1)129549$$aVereecken, H.$$b1$$uFZJ
000003843 7001_ $$0P:(DE-Juel1)129477$$aJavaux, M.$$b2$$uFZJ
000003843 773__ $$0PERI:(DE-600)2088189-7$$a10.2136/vzj2008.0062$$gVol. 8, p. 86 - 95$$p86 - 95$$q8<86 - 95$$tVadose zone journal$$v8$$x1539-1663$$y2009
000003843 8567_ $$uhttp://dx.doi.org/10.2136/vzj2008.0062
000003843 909CO $$ooai:juser.fz-juelich.de:3843$$pVDB
000003843 9131_ $$0G:(DE-Juel1)FUEK407$$bErde und Umwelt$$kP24$$lTerrestrische Umwelt$$vTerrestrische Umwelt$$x0
000003843 9141_ $$y2009
000003843 915__ $$0StatID:(DE-HGF)0010$$aJCR/ISI refereed
000003843 9201_ $$0I:(DE-Juel1)VDB793$$d31.10.2010$$gICG$$kICG-4$$lAgrosphäre$$x1
000003843 9201_ $$0I:(DE-82)080012_20140620$$gJARA$$kJARA-HPC$$lJülich Aachen Research Alliance - High-Performance Computing$$x2
000003843 970__ $$aVDB:(DE-Juel1)110359
000003843 980__ $$aVDB
000003843 980__ $$aConvertedRecord
000003843 980__ $$ajournal
000003843 980__ $$aI:(DE-Juel1)IBG-3-20101118
000003843 980__ $$aI:(DE-82)080012_20140620
000003843 980__ $$aUNRESTRICTED
000003843 981__ $$aI:(DE-Juel1)IBG-3-20101118
000003843 981__ $$aI:(DE-Juel1)VDB1346