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dc.contributor.authorAlley, Marcus M.en_US
dc.date.accessioned2014-03-14T21:11:44Z
dc.date.available2014-03-14T21:11:44Z
dc.date.issued1975-03-07en_US
dc.identifier.otheretd-06022010-020404en_US
dc.identifier.urihttp://hdl.handle.net/10919/37937
dc.description.abstract

The research was undertaken to provide basic information on Mn in Virginia soils and to evaluate rates and methods of Mn application to correct Mn deficiency in soybeans. Soil profile samples were analyzed from catenas representing the Appalachian, Piedmont, and Coastal Plain regions. The exchangeable, easily reducible, and total Mn contents were higher in the Appalachian soils than in the Piedmont or Coastal Plain soils. The total Mn content of the well-drained soil was higher than the poorly-drained soil in the Appalachian catena. No other differences were found between soils varying in drainage. Parent material and time appear to be the soil forming factors that exert the largest influence on total soil Mn. Further research is necessary to fully characterize soil Mn in these broad physiographic regions.

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dc.format.mediumBTDen_US
dc.publisherVirginia Techen_US
dc.relation.haspartLD5655.V856_1975.A447.pdfen_US
dc.subjectVirginia physiographic regionsen_US
dc.subject.lccLD5655.V856 1975.A447en_US
dc.titleManganese in Virginia soils and correction of manganese deficiency in soybeans (Glycine max L.)en_US
dc.typeDissertationen_US
dc.contributor.departmentAgronomyen_US
dc.description.degreePh. D.en_US
thesis.degree.namePh. D.en_US
thesis.degree.leveldoctoralen_US
thesis.degree.grantorVirginia Polytechnic Institute and State Universityen_US
thesis.degree.disciplineAgronomyen_US
dc.contributor.committeechairRich, Charles I.en_US
dc.contributor.committeememberMartens, David C.en_US
dc.contributor.committeememberMoore, Laurence D.en_US
dc.contributor.committeememberHutcheson, Thomas B. Jr.en_US
dc.contributor.committeememberWightman, James P.en_US
dc.identifier.sourceurlhttp://scholar.lib.vt.edu/theses/available/etd-06022010-020404/en_US
dc.date.sdate2010-06-02en_US
dc.date.rdate2010-06-02
dc.date.adate2010-06-02en_US


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