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dc.contributor.advisorPost, Donald F.en_US
dc.contributor.authorCederstrom, Myriam Ransenberg, 1955-
dc.creatorCederstrom, Myriam Ransenberg, 1955-en_US
dc.date.accessioned2013-04-03T13:17:34Z
dc.date.available2013-04-03T13:17:34Z
dc.date.issued1992en_US
dc.identifier.urihttp://hdl.handle.net/10150/278235
dc.description.abstractSurface soil samples from a climosequence were studied with the purpose of relating color, reflectance variations and texture to contents of organic carbon and free iron oxides. Information on the physicochemical properties of the soils were obtained with a fine resolution spectroradiometer, a chromameter and by laboratory analyses. The effect of soil organic carbon and free iron oxides is shown by the varying shape of the soil spectral curves. Both the chromameter and the spectroradiometer detected the varying amounts of organic carbon and free iron oxides in soil. Silt had a positive, highly significant relationship with organic carbon. Clay and silt had a positive highly significant relationship with free iron oxides.
dc.language.isoen_USen_US
dc.publisherThe University of Arizona.en_US
dc.rightsCopyright © is held by the author. Digital access to this material is made possible by the University Libraries, University of Arizona. Further transmission, reproduction or presentation (such as public display or performance) of protected items is prohibited except with permission of the author.en_US
dc.subjectAgriculture, Agronomy.en_US
dc.subjectEngineering, Agricultural.en_US
dc.subjectChemistry, Agricultural.en_US
dc.titleSpectroradiometric and color analysis of soil organic carbon and free iron oxides along a climosequenceen_US
dc.typetexten_US
dc.typeThesis-Reproduction (electronic)en_US
thesis.degree.grantorUniversity of Arizonaen_US
thesis.degree.levelmastersen_US
dc.identifier.proquest1351313en_US
thesis.degree.disciplineGraduate Collegeen_US
thesis.degree.nameM.S.en_US
dc.identifier.bibrecord.b27149742en_US
refterms.dateFOA2018-04-25T17:03:05Z
html.description.abstractSurface soil samples from a climosequence were studied with the purpose of relating color, reflectance variations and texture to contents of organic carbon and free iron oxides. Information on the physicochemical properties of the soils were obtained with a fine resolution spectroradiometer, a chromameter and by laboratory analyses. The effect of soil organic carbon and free iron oxides is shown by the varying shape of the soil spectral curves. Both the chromameter and the spectroradiometer detected the varying amounts of organic carbon and free iron oxides in soil. Silt had a positive, highly significant relationship with organic carbon. Clay and silt had a positive highly significant relationship with free iron oxides.


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