dc.contributor.author | Mochizuki, Akihito | |
dc.contributor.author | Murata, Takahiro | |
dc.contributor.author | Hosoda, Ko | |
dc.contributor.author | Dulmaa, Ayuriin | |
dc.contributor.author | Ayushsuren, Chananbaatar | |
dc.contributor.author | Ganchimeg, Darmaa | |
dc.contributor.author | Drucker, Valentin V. | |
dc.contributor.author | Fialkov, Vladimir A. | |
dc.contributor.author | Depci, Tolga | |
dc.contributor.author | Üner, Tijen | |
dc.contributor.author | Oğhan, Fatih | |
dc.contributor.author | Sugiyama, Masahito | |
dc.date.accessioned | 12.07.201910:50:10 | |
dc.date.accessioned | 2019-07-12T22:06:12Z | |
dc.date.available | 12.07.201910:50:10 | |
dc.date.available | 2019-07-12T22:06:12Z | |
dc.date.issued | 2018 | |
dc.identifier.citation | Mochizuki, A., Murata, T., Hosoda, K., Dulmaa, A., Ayushsuren, C., Ganchimeg, D., Drucker, V.V.,
Fialkov, V.A., Depci, T., Üner, T., Oğhan, F., Sugiyama, M. (2018). Distribution of trace elements and the influence of major-ion water chemistry in saline lakes. Limnology and Oceanography, 63 (3), pp. 1253-1263.
https://doi.org/10.1002/lno.10770 | en_US |
dc.identifier.issn | 0024-3590 | |
dc.identifier.issn | 1939-5590 | |
dc.identifier.uri | https://doi.org/10.1002/lno.10770 | |
dc.identifier.uri | https://hdl.handle.net/20.500.12508/663 | |
dc.description | WOS: 000432019600015 | en_US |
dc.description.abstract | Although the water chemistry in saline lakes can differ drastically due to subtle differences in inflowing water conditions, the concentrations, distributions, and geochemical behaviors of trace elements in such environments are poorly understood. In this study, the influence of major-ion chemistry on the trace element distribution in saline lakes is examined based on major and trace element concentrations and geochemical modeling in three carbonate-rich saline lakes located in Mongolia and Turkey. The results are compared to data reported from other carbonate-rich and carbonate-depleted lakes. The concentrations of U and oxyanions (V, Mo, and W) in carbonate-rich saline lakes are several orders of magnitude higher than their contributing rivers and seawater. By contrast, their concentrations in carbonate-depleted saline lakes are lower than those in rivers and oceans. The high U concentrations in carbonate-rich saline lakes are possibly attributed to the formation of (magnesium-)uranyl-carbonate complexes, and the high oxyanion concentrations are likely a result of the high pH of lake water preventing them from being adsorbed onto solid phases such as suspended particulate matter and sediment. Strontium and Ba concentrations are lower in carbonate-rich saline lakes than in river water and seawater, but relatively higher in carbonate-depleted lakes. Incorporation into aragonite and/or calcite, adsorption onto solid phases, and formation of carbonate minerals are possible mechanisms that may account for the lower concentrations of these elements in carbonate-rich lakes. These results help elucidate the influence of water chemistry on trace element distribution in saline lakes. | en_US |
dc.description.sponsorship | Japan Society for the Promotion of Science KAKENHI [15H05114, 21255002] | en_US |
dc.description.sponsorship | We are grateful to Prof. Y. Sohrin of Kyoto University for providing the inductively coupled plasma mass spectrometry facilities. We are also grateful to the two anonymous reviewers for their constructive comments and invaluable suggestions. This work was partly supported by Japan Society for the Promotion of Science KAKENHI grant numbers 21255002 and 15H05114. | en_US |
dc.language.iso | eng | en_US |
dc.publisher | Wiley | en_US |
dc.relation.isversionof | 10.1002/lno.10770 | en_US |
dc.rights | info:eu-repo/semantics/closedAccess | en_US |
dc.subject.classification | Limnology | en_US |
dc.subject.classification | Oceanography | en_US |
dc.subject.classification | Neodymium Isotope | Ferro-Manganese Alloy | Rare Earth Element | en_US |
dc.subject.other | Dead-sea | en_US |
dc.subject.other | Uranium concentration | en_US |
dc.subject.other | Surface waters | en_US |
dc.subject.other | Mono-lake | en_US |
dc.subject.other | Adsorption | en_US |
dc.subject.other | Ph | en_US |
dc.subject.other | Carbonate | en_US |
dc.subject.other | Vanadium | en_US |
dc.subject.other | Uranyl | en_US |
dc.subject.other | Brine | en_US |
dc.subject.other | Adsorption | en_US |
dc.subject.other | Aragonite | en_US |
dc.subject.other | Carbonate | en_US |
dc.subject.other | Concentration (composition) | en_US |
dc.subject.other | Geochemical method | en_US |
dc.subject.other | Ion | en_US |
dc.subject.other | Lake water | en_US |
dc.subject.other | Particulate matter | en_US |
dc.subject.other | River water | en_US |
dc.subject.other | Saline lake | en_US |
dc.subject.other | Seawater | en_US |
dc.subject.other | Suspended particulate matter | en_US |
dc.subject.other | Trace element | en_US |
dc.subject.other | Water chemistry | en_US |
dc.subject.other | Mongolia | en_US |
dc.subject.other | Turkey | en_US |
dc.title | Distribution of trace elements and the influence of major-ion water chemistry in saline lakes | en_US |
dc.type | article | en_US |
dc.relation.journal | Limnology and Oceanography | en_US |
dc.contributor.department | Mühendislik ve Doğa Bilimleri Fakültesi -- Petrol ve Doğalgaz Mühendisliği Bölümü | en_US |
dc.identifier.volume | 63 | en_US |
dc.identifier.issue | 3 | en_US |
dc.identifier.startpage | 1253 | en_US |
dc.identifier.endpage | 1263 | en_US |
dc.relation.publicationcategory | Makale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanı | en_US |
dc.contributor.isteauthor | Depci, Tolga | en_US |
dc.relation.index | Web of Science - Scopus | en_US |
dc.relation.index | Web of Science Core Collection - Science Citation Index Expanded | en_US |