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Testing the downwash of atmospherically deposited metals in peat and the influence of rainfall intensity
Umeå University, Faculty of Science and Technology, Department of Ecology and Environmental Sciences.
Umeå University, Faculty of Science and Technology, Department of Ecology and Environmental Sciences.
Umeå University, Faculty of Science and Technology, Department of Ecology and Environmental Sciences.
(English)Article in journal (Refereed) Submitted
National Category
Geochemistry
Identifiers
URN: urn:nbn:se:umu:diva-84159OAI: oai:DiVA.org:umu-84159DiVA: diva2:679737
Available from: 2013-12-16 Created: 2013-12-16 Last updated: 2013-12-16Bibliographically approved
In thesis
1. Incorporation and preservation of geochemical fingerprints in peat archives
Open this publication in new window or tab >>Incorporation and preservation of geochemical fingerprints in peat archives
2013 (English)Doctoral thesis, comprehensive summary (Other academic)
Abstract [en]

The present status of the environment, including environmental problems such as heavy metal accumulation in aquatic and terrestrial ecosystems, is in part the consequence of long-term changes. Cores from peatlands and other natural archives provide us with the potential to study aspects of the atmospheric cycling of elements, such as metal pollutants, on timescales much longer than the decade or two available to us with atmospheric deposition monitoring programs. The past decade especially has seen a rapid increase in interest in the biogeochemical record preserved in peat, particularly as it relates to environmental changes (e.g. climate and pollution). Importantly, recent studies have shown that carbon dynamics, i.e., organic matter decomposition, may influence the record of atmospherically derived elements such as halogens and mercury. Other studies have shown that under certain conditions some downward movement of atmospherically deposited elements may also occur, which adds complexity to establishing reliable chronologies as well as inherent problems of estimating accurate accumulation rates of peat and past metal deposition. Thus, we still lack a complete understanding of the basic biogeochemical processes and their effects on trace element distributions. While many studies have validated the general temporal patterns of peat records, there has been a limited critical examination of accumulation records in quantitative terms. To be certain that we extract not only a qualitative record from peat, it is important that we establish a quantitative link between the archive and the few to several decades of data that are available from contemporary monitoring and research. The main objective of this doctoral thesis was to focus on improving the link between the long-term paleorecord and the contemporary monitoring data available from biomonitoring and direct deposition observations. The main research questions have therefore been: Are peat archives an absolute or relative record? And how are geochemical signals, including dating, incorporated in the peat archive? What temporal resolution is realistic to interpret by using peat cores?

Place, publisher, year, edition, pages
Umeå: Umeå Universitet, 2013. 36 p.
Keyword
Peat, Beryllium, bulk density, C/N-ratio, decomposition, deposition, downwash, elemental mobility, geochemistry, humification, lead, light transmission, mercury, peat accumulation, precipitation
National Category
Environmental Sciences
Research subject
biology, Environmental Science
Identifiers
urn:nbn:se:umu:diva-84161 (URN)978-91-7459-779-0 (ISBN)
Public defence
2014-01-24, KB3A9, KBC, Umeå University, Umeå, 10:00 (English)
Opponent
Supervisors
Available from: 2013-12-17 Created: 2013-12-16 Last updated: 2013-12-17Bibliographically approved

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