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dc.contributor.authorPaul, Eldor A.
dc.contributor.authorSmucker, Alvin J. M.
dc.date.accessioned2007-01-03T07:17:15Z
dc.date.available2007-01-03T07:17:15Z
dc.date.issued1998-08
dc.descriptionWorkshop given at the 16th World Congress of Soil Science, Montpellier, France 20-26 August, 1998.
dc.descriptionScientific registration: 2742, Workshop: D, Presentation: oral.
dc.description.abstractSoil aggregation dynamics directly control agricultural production and reduce environmental contamination by convection-dispersion sequestrations of most ions. Greater containment and longer residence times of most plant nutrients, pesticides, and water would better sustain most agricultural production systems without polluting nearby groundwater supplies. In short, the large surface areas associated with the plethora of porosities within each natural soil aggregate provide dynamically interactive areas for chemical sequestration. Once known, it is these active/inactive centers which can be modified to improve plant productivity and water quality.
dc.format.mediumborn digital
dc.format.mediumarticles
dc.identifier.bibliographicCitationSmucker, Alvin J. M. and Eldor A. Paul, Analytical Determination of Concentric Carbon Gradients within Stable Soil Aggregates = Détermination analytique de gradients concentriques de carbone au sein d’agrégats stables de sol. 16th World Congress of Soil Science: 1 p. [Montpelier, France]: ISSS-AISS-IBG-SICS, 1998.
dc.identifier.urihttp://hdl.handle.net/10217/85960
dc.languageEnglish
dc.publisherColorado State University. Libraries
dc.publisher.original[ISSS-AISS-IBG-SICS]
dc.relation.ispartofFaculty Publications - Natural Resource Ecology Laboratory (NREL)
dc.subjectmicrogradients
dc.subjectdelta 13C
dc.subjectmass spectroscopy
dc.titleAnalytical determination of concentric carbon gradients within stable soil aggregates = Détermination analytique de gradients concentriques de carbone au sein d’agrégats stables de sol
dc.title.alternativeDétermination analytique de gradients concentriques de carbone au sein d’agrégats stables de sol
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