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dc.contributor.authorBridgestock, Luke
dc.contributor.authorHenderson, Gideon M
dc.contributor.authorHoldship, Phil
dc.contributor.authorKhaing, Aung Myo
dc.contributor.authorNaing, Tin Tin
dc.contributor.authorMyint, Tin Aung
dc.contributor.authorHtun, Wint Wint
dc.contributor.authorKhant, Win
dc.contributor.authorThu, Win Myo
dc.contributor.authorChi, Mo Aung Nay
dc.contributor.authorBaronas, J Jotautas
dc.contributor.authorTipper, Edward
dc.contributor.authorChapman, Hazel
dc.contributor.authorBickle, Mike
dc.date.accessioned2022-06-27T23:30:57Z
dc.date.available2022-06-27T23:30:57Z
dc.date.issued2022-10-01
dc.identifier.issn0048-9697
dc.identifier.urihttps://www.repository.cam.ac.uk/handle/1810/338384
dc.description.abstractThe Irrawaddy (Ayeyarwaddy) and Salween (Thanlwin) globally rank among the largest rivers for supplying dissolved and particulate material to the ocean. Along with the Sittaung and Kaladan rivers they have societal importance to Myanmar in terms water sources and food production. Despite their importance for global biogeochemical cycles and the ~50 million people who live in their catchments, the chemistry of these rivers is poorly known. This study presents a comprehensive survey of dissolved (<0.22 μm) trace element concentrations (Sr, Fe, Al, Ba, Mn, V, Rb, Cu, Zn, As, Li, Ni, Mo, Cr, U, Pb, Sb, Co, Cs, Tl and Cd) at 38 locations within these river catchments, spanning a period of 2 years. The results highlight the global importance of the Irrawaddy and Salween rivers for trace element global biogeochemical cycles; contributing between 1 and 17 % of global dissolved riverine fluxes to the land-ocean interface for the studied elements. Area normalized dissolved fluxes in these catchments are ~2 to 10 times higher than global average values for most elements, consistent with high rates of chemical weathering. In general, anthropogenic activities have yet to significantly perturb dissolved trace element fluxes in these river systems. The presented dataset should therefore serve as a useful 'natural' baseline, against which future perturbations driven by climate change and/or the development of Myanmar's mining industry could be assessed. Exceptions to this include As in the Sittaung River and Sb, Zn, Pb and As in the Salween River, which may already be significantly impacted by anthropogenic inputs. The former represents a water quality issue of concern for public health, and so constraining the exact sources of As in the Sittaung River should be considered a priority for future research.
dc.format.mediumPrint-Electronic
dc.publisherElsevier BV
dc.rightsAttribution 4.0 International
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/
dc.subjectGlobal trace element cycles
dc.subjectRiverine trace element fluxes
dc.subjectTrace element pollution
dc.subjectWater quality
dc.titleDissolved trace element concentrations and fluxes in the Irrawaddy, Salween, Sittaung and Kaladan Rivers.
dc.typeArticle
dc.publisher.departmentDepartment of Earth Sciences
dc.date.updated2022-06-26T13:51:55Z
prism.number156756
prism.publicationDate2022
prism.publicationNameSci Total Environ
prism.startingPage156756
prism.volume841
dc.identifier.doi10.17863/CAM.85796
dcterms.dateAccepted2022-06-13
rioxxterms.versionofrecord10.1016/j.scitotenv.2022.156756
rioxxterms.versionVoR
dc.contributor.orcidBridgestock, Luke [0000-0001-7636-6090]
dc.identifier.eissn1879-1026
rioxxterms.typeJournal Article/Review
cam.issuedOnline2022-06-17
cam.depositDate2022-06-26
pubs.licence-identifierapollo-deposit-licence-2-1
pubs.licence-display-nameApollo Repository Deposit Licence Agreement


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Attribution 4.0 International
Except where otherwise noted, this item's licence is described as Attribution 4.0 International