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dc.contributor.advisorConklin, Martha H.en
dc.contributor.authorMarble, Justin Carl
dc.creatorMarble, Justin Carlen
dc.date.accessioned2018-02-26T18:40:54Z
dc.date.available2018-02-26T18:40:54Z
dc.date.issued1998
dc.identifier.urihttp://hdl.handle.net/10150/626813
dc.description.abstractIt is hypothesized that biotic factors are playing a large role in the formation of manganese oxide deposits in Pinal Creek. To test this hypothesis, a series of batch experiments were run to characterize the key processes that could control biotic and abiotic processes. It was determined that biotic systems remove manganese by at least a magnitude faster than abiotic systems, 0.00161 hr-1 compared to 0.00043 hr-1. Increasing pH augmented the rate constant; 0.05080 hr-1 for pH 7.8 to 0.00157 hr-1 for pH 6.0. Initial Mn concentration influenced manganese removal with the net rate of re1noval described by Michaelis-Menton kinetics. Mn oxides on sediments also influenced increased rates. There are many factors that control the removal and oxidation of manganese from Pinal Creek. Understanding the key variables are important in promoting naturally remediating systems.
dc.language.isoen_USen
dc.publisherThe University of Arizona.en
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
dc.titleBiotic contribution of Mn(Il) removal at Pinal Creek, Globe, Arizonaen_US
dc.typetexten
dc.typeThesis-Reproduction (electronic)en
thesis.degree.grantorUniversity of Arizonaen
thesis.degree.levelmastersen
dc.contributor.committeememberConklin, Martha H.en
thesis.degree.disciplineGraduate Collegeen
thesis.degree.disciplineHydrology and Water Resourcesen
thesis.degree.nameM.S.en
dc.description.noteDigitized from paper copies provided by the Department of Hydrology & Atmospheric Sciences.en
refterms.dateFOA2018-08-13T19:13:32Z
html.description.abstractIt is hypothesized that biotic factors are playing a large role in the formation of manganese oxide deposits in Pinal Creek. To test this hypothesis, a series of batch experiments were run to characterize the key processes that could control biotic and abiotic processes. It was determined that biotic systems remove manganese by at least a magnitude faster than abiotic systems, 0.00161 hr-1 compared to 0.00043 hr-1. Increasing pH augmented the rate constant; 0.05080 hr-1 for pH 7.8 to 0.00157 hr-1 for pH 6.0. Initial Mn concentration influenced manganese removal with the net rate of re1noval described by Michaelis-Menton kinetics. Mn oxides on sediments also influenced increased rates. There are many factors that control the removal and oxidation of manganese from Pinal Creek. Understanding the key variables are important in promoting naturally remediating systems.


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