000000367 001__ 367
000000367 005__ 20210811125345.0
000000367 0247_ $$2DOI$$a10.1111/j.1365-2389.2008.01044.x
000000367 0247_ $$2WOS$$aWOS:000255917300019
000000367 037__ $$aPreJuSER-367
000000367 041__ $$aENG
000000367 082__ $$a630
000000367 084__ $$2WoS$$aSoil Science
000000367 1001_ $$0P:(DE-Juel1)VDB9230$$aSéquaris, J.-M.$$b0$$uFZJ
000000367 245__ $$aEffects of mineral surface iron on the CPMAS C-13-NMR spectroscopic detection of organic matter from soil fractions in an agricultural topsoil with different amendments
000000367 260__ $$aOxford [u.a.]$$bWiley-Blackwell$$c2008
000000367 300__ $$a592 - 599
000000367 3367_ $$0PUB:(DE-HGF)16$$2PUB:(DE-HGF)$$aJournal Article
000000367 3367_ $$2DataCite$$aOutput Types/Journal article
000000367 3367_ $$00$$2EndNote$$aJournal Article
000000367 3367_ $$2BibTeX$$aARTICLE
000000367 3367_ $$2ORCID$$aJOURNAL_ARTICLE
000000367 3367_ $$2DRIVER$$aarticle
000000367 440_0 $$01973$$aEuropean Journal of Soil Science$$v59$$x1351-0754$$y3
000000367 500__ $$aRecord converted from VDB: 12.11.2012
000000367 520__ $$aThe decrease of NMR visibility of the C signal in soil samples due to the association between organic carbon (OC) and the topsoil mineral surface was investigated. CPMAS 13C-NMR spectra were obtained for soil particle-size fractions (< 2 μm, 2–20 μm, > 20 μm) and bulk soils from an agricultural topsoil (Chernozem) that had received three different amendments (no fertilization, mineral fertilization (NPK), mineral (NPK) and organic (cattle manure) fertilizations) at Bad Lauchstädt, Germany. The soil organic carbon content of the three soils depended on the degree of soil fertilization. There was no constant relationship between the total NMR signal intensity and the total amount of organic carbon (TOC) for all size fractions. Indeed, a key role played in the C signal intensity by the paramagnetic ferric ion from the clay content in soil fractions and bulk soils was confirmed. Thus, we describe the variations of C signal intensity by taking into account the distribution of clay-associated OC and non-associated OC pools. Depending on the amendment, the C signal visibility was weakened by a factor of 2–4 for the clay-associated OC. This estimation was rendered possible by combining mineral specific surface area (SSA) measurements with the N2 gas adsorption method (BET method) and determination of TOC and iron concentrations. This approach contributes to the quantitative evaluation of the CPMAS 13C-NMR detection.
000000367 536__ $$0G:(DE-Juel1)FUEK407$$2G:(DE-HGF)$$aTerrestrische Umwelt$$cP24$$x0
000000367 588__ $$aDataset connected to Web of Science, Pubmed
000000367 7001_ $$0P:(DE-Juel1)VDB2349$$aPhilipp, H.$$b1$$uFZJ
000000367 7001_ $$0P:(DE-Juel1)VDB9232$$aNarres, H. D.$$b2$$uFZJ
000000367 7001_ $$0P:(DE-Juel1)129549$$aVereecken, H.$$b3$$uFZJ
000000367 773__ $$0PERI:(DE-600)2020243-X$$a10.1111/j.1365-2389.2008.01044.x$$gVol. 59, p. 592 - 599$$p592 - 599$$q59<592 - 599$$tEuropean journal of soil science$$v59$$x1351-0754$$y2008
000000367 8567_ $$uhttp://dx.doi.org/10.1111/j.1365-2389.2008.01044.x
000000367 909CO $$ooai:juser.fz-juelich.de:367$$pVDB
000000367 915__ $$0StatID:(DE-HGF)0010$$aJCR/ISI refereed
000000367 9141_ $$y2008
000000367 9131_ $$0G:(DE-Juel1)FUEK407$$bErde und Umwelt$$kP24$$lTerrestrische Umwelt$$vTerrestrische Umwelt$$x0
000000367 9201_ $$0I:(DE-Juel1)VDB793$$d31.10.2010$$gICG$$kICG-4$$lAgrosphäre$$x1
000000367 9201_ $$0I:(DE-82)080011_20140620$$gJARA$$kJARA-ENERGY$$lJülich-Aachen Research Alliance - Energy$$x2
000000367 9201_ $$0I:(DE-Juel1)VDB1045$$gJARA$$kJARA-SIM$$lJülich-Aachen Research Alliance - Simulation Sciences$$x3
000000367 970__ $$aVDB:(DE-Juel1)100695
000000367 980__ $$aVDB
000000367 980__ $$aConvertedRecord
000000367 980__ $$ajournal
000000367 980__ $$aI:(DE-Juel1)IBG-3-20101118
000000367 980__ $$aI:(DE-82)080011_20140620
000000367 980__ $$aI:(DE-Juel1)VDB1045
000000367 980__ $$aUNRESTRICTED
000000367 981__ $$aI:(DE-Juel1)IBG-3-20101118
000000367 981__ $$aI:(DE-Juel1)VDB1045
000000367 981__ $$aI:(DE-Juel1)VDB1047