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dc.contributor.authorCawley, K. M.
dc.contributor.authorMcKnight, Diane M.
dc.contributor.authorPenney, P. M.
dc.contributor.authorCory, R. M.
dc.contributor.authorFimmen, R. L.
dc.contributor.authorGuerard, J.
dc.contributor.authorDieser, Markus
dc.contributor.authorJaros, C.
dc.contributor.authorChin, Yu-Ping
dc.contributor.authorForeman, Christine M.
dc.date.accessioned2017-01-24T18:56:37Z
dc.date.available2017-01-24T18:56:37Z
dc.date.issued2013-10
dc.identifier.citationCawley KM, McKnight DM, Penney Miller P, Cory R, Fimmen RL, Guerard J, Dieser M, Jaros C, Chin Y-P, Foreman C, "Characterization of fulvic acid fractions of dissolved organic matter during ice-out in a hyper-eutrophic, coastal pond in Antarctica," Environmental Research Letters, 2013 8:4. 045015 (10pp).en_US
dc.identifier.issn1748-9326
dc.identifier.urihttps://scholarworks.montana.edu/xmlui/handle/1/12434
dc.description.abstractDissolved humic material (HDOM) is ubiquitous to all natural waters and its source material influences its chemical structure, reactivity, and bioavailability. While terrestrially derived HDOM reference materials distributed by the International Humic Substances Society (IHSS) have been readily available to engineering and scientific communities, a microbially derived reference HDOM was not, despite the well-characterized differences in the chemistry and reactivity of HDOM derived from terrestrial versus microbial sources. To address this gap, we collected a microbial reference fulvic acid from Pony Lake (PLFA) for distribution through the IHSS. Pony Lake is a saline coastal pond on Ross Island, Antarctica, where the landscape is devoid of terrestrial plants. Sample collection occurred over a 17-day period in the summer season at Pony Lake. During this time, the dissolved organic carbon (DOC) concentrations increased nearly two-fold, and the fulvic acid fraction (collected using the XAD-8 method) accounted for 14.6% of the DOC. During the re-concentration and desalting procedures we isolated two other chemically distinct fulvic acid fractions: (1) PLFA-2, which was high in carbohydrates and (2) PLFA-CER, which was high in nitrogen. The chemical characteristics (elemental analysis, optical characterization with UV–vis and fluorescence spectroscopy, and 13C NMR spectroscopy) of the three fulvic acid fractions helped to explain their behavior during isolation.en_US
dc.rightsCC BY 4.0en_US
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/legalcodeen_US
dc.titleCharacterization of fulvic acid fractions of dissolved organic matter during ice-out in a hyper-eutrophic, coastal pond in Antarcticaen_US
dc.typeArticleen_US
mus.citation.extentfirstpage45015en_US
mus.citation.issue4en_US
mus.citation.journaltitleEnvironmental Research Lettersen_US
mus.citation.volume8en_US
mus.identifier.categoryChemical & Material Sciencesen_US
mus.identifier.categoryEngineering & Computer Scienceen_US
mus.identifier.categoryLife Sciences & Earth Sciencesen_US
mus.identifier.doi10.1088/1748-9326/8/4/045015en_US
mus.relation.collegeCollege of Agricultureen_US
mus.relation.collegeCollege of Engineeringen_US
mus.relation.collegeCollege of Letters & Scienceen_US
mus.relation.departmentCenter for Biofilm Engineering.en_US
mus.relation.departmentChemical & Biological Engineering.en_US
mus.relation.departmentChemistry & Biochemistry.en_US
mus.relation.departmentMicrobiology & Immunology.en_US
mus.relation.universityMontana State University - Bozemanen_US
mus.relation.researchgroupCenter for Biofilm Engineering.en_US
mus.data.thumbpage4en_US
mus.contributor.orcidForeman, Christine M.|0000-0003-0230-4692en_US


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