Please use this identifier to cite or link to this item: https://hdl.handle.net/2440/27251
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dc.contributor.authorSmernik, R.-
dc.contributor.authorOades, J.-
dc.date.issued2001-
dc.identifier.citationSolid State Nuclear Magnetic Resonance, 2001; 20(1-2):74-84-
dc.identifier.issn0926-2040-
dc.identifier.issn1527-3326-
dc.identifier.urihttp://hdl.handle.net/2440/27251-
dc.description.abstract13C background signal, obtained for an empty rotor, was shown by spin counting experiments to be equivalent to 1 mg of observable carbon for cross-polarization (CP) spectra and 69 mg of observable C for Bloch decay (BD) spectra. The BD background was mainly due to Kel-F in the stator. with minimal signal detected from the Kel-F end-caps. The CP background was attributed to non-Kel-F components of the stator, probe, or probe supports. The BD background signal was eliminated by using a modified dipolar dephasing pulse sequence in which the absence of 19F decoupling (rather than the absence of 1H decoupling) causes selective elimination of the Kel-F signal.-
dc.description.statementofresponsibilityRonald J. Smernik and J. Malcolm Oades-
dc.description.urihttp://www.elsevier.com/wps/find/journaldescription.cws_home/622947/description#description-
dc.language.isoen-
dc.publisherElsevier Science BV-
dc.rightsCopyright © 2001 Academic Press. All rights reserved.-
dc.source.urihttp://dx.doi.org/10.1006/snmr.2001.0031-
dc.subjectCarbon Isotopes-
dc.subjectSoil-
dc.subjectMagnetic Resonance Spectroscopy-
dc.titleBackground signal in solid state 13C NMR spectra of soil organic matter (SOM) - quantification and minimization-
dc.typeJournal article-
dc.identifier.doi10.1006/snmr.2001.0031-
pubs.publication-statusPublished-
dc.identifier.orcidSmernik, R. [0000-0001-6033-5855]-
Appears in Collections:Aurora harvest 2
Soil and Land Systems publications

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