Source, composition, and biodegradability of dissolved organic matter in the Parlung Zangbo river in southern Tibet, China

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dc.contributor Andrus, Fred
dc.contributor Tick, Geoffrey
dc.contributor Kuang, Xingxing
dc.contributor.advisor Lu, Yuehan
dc.contributor.advisor Zheng, Chunmiao
dc.contributor.author Warren, Olivia Marie
dc.date.accessioned 2020-01-16T15:03:36Z
dc.date.available 2020-01-16T15:03:36Z
dc.date.issued 2019
dc.identifier.other u0015_0000001_0003402
dc.identifier.other Warren_alatus_0004M_13882
dc.identifier.uri http://ir.ua.edu/handle/123456789/6459
dc.description Electronic Thesis or Dissertation
dc.description.abstract Regions of the Tibetan Plateau are experiencing increasing temperatures and decreasing glacial mass at a faster rate than the global average. Our study area, the Parlung Zangbo River basin, is within the southeastern region of the Tibetan Plateau which is experiencing the greatest degree of glacial mass loss. Glacial loss could mobilize organic matter from the terrestrial landscape to lakes and rivers and thereby influence watershed carbon cycles, water quality, and aquatic ecological functioning. However, the present-day dissolved organic matter (DOM) pool of the river, which could serve as a baseline for future predictions, has not been characterized. This project will characterize spatial distribution of the amount, source, and biodegradability of DOM exported from the Parlung Zangbo River basin. Samples were collected along the main stem of the river over 170 km, nearby tributaries, and a headwater lake and analyzed for DOC concentration and DOM quality based on absorbance and fluorescence properties. The excitation emission matrix coupled with parallel factor analysis (EEM-PARAFAC) yielded three humic-like fluorophores and two protein-like fluorophores. A subset of samples analyzed with Fourier Transform Ion Cyclotron Resonance Mass Spectrometry (FT-ICR-MS) analysis showed that the DOM pool was dominated by lignins. Incubation experiments showed microbial utilization of DOM increased with increasing temperature up to an optimum temperature (between 17°C and 25°C) before declining. Lake samples showed characteristics indicative of glacial contribution, including greater proportions of Nitrogen-rich DOM and microbially-derived DOM, as well as higher β:α values that suggest lower degrees of diagenesis and higher bioreactivity. Our results suggest that increasing glacial loss in the future may shift the composition and increase the bioreactivity of DOM pool in Tibetan rivers. Consequently, these shifts in the DOM pool will contribute to global warming through a positive feedback loop.
dc.format.extent 81 p.
dc.format.medium electronic
dc.format.mimetype application/pdf
dc.language English
dc.language.iso en_US
dc.publisher University of Alabama Libraries
dc.relation.ispartof The University of Alabama Electronic Theses and Dissertations
dc.relation.ispartof The University of Alabama Libraries Digital Collections
dc.relation.hasversion born digital
dc.rights All rights reserved by the author unless otherwise indicated.
dc.subject.other Geochemistry
dc.subject.other Hydrologic sciences
dc.subject.other Environmental science
dc.title Source, composition, and biodegradability of dissolved organic matter in the Parlung Zangbo river in southern Tibet, China
dc.type thesis
dc.type text
etdms.degree.department University of Alabama. Department of Geological Sciencess
etdms.degree.discipline Geology
etdms.degree.grantor The University of Alabama
etdms.degree.level master's
etdms.degree.name M.S.


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