{"id":242,"date":"2020-04-21T00:53:34","date_gmt":"2020-04-20T21:53:34","guid":{"rendered":"https:\/\/hydro-chemistry-ecology.knu.ua\/?page_id=242"},"modified":"2020-08-26T09:31:23","modified_gmt":"2020-08-26T06:31:23","slug":"%d1%96%d0%b3%d0%bd%d0%b0%d1%82%d0%b5%d0%bd%d0%ba%d0%be-%d1%96-%d1%96-%d1%84%d0%be%d1%80%d0%bc%d0%b8-%d0%bc%d1%96%d0%b3%d1%80%d0%b0%d1%86%d1%96%d1%97-%d0%bc%d0%be%d0%bb%d1%96%d0%b1%d0%b4%d0%b5%d0%bd","status":"publish","type":"page","link":"https:\/\/hydro-chemistry-ecology.knu.ua\/en\/%d1%96%d0%b3%d0%bd%d0%b0%d1%82%d0%b5%d0%bd%d0%ba%d0%be-%d1%96-%d1%96-%d1%84%d0%be%d1%80%d0%bc%d0%b8-%d0%bc%d1%96%d0%b3%d1%80%d0%b0%d1%86%d1%96%d1%97-%d0%bc%d0%be%d0%bb%d1%96%d0%b1%d0%b4%d0%b5%d0%bd\/","title":{"rendered":"IGNATENKO I.I. THE MOLYBDENUM FORM MIGRATION IN THE LYBID RIVER WATER, FLOWING THROUGH THE CITY OF KIYV"},"content":{"rendered":"\n<p><strong>DOI: <a href=\"https:\/\/doi.org\/10.17721\/2306-5680.2019.4.7\">https:\/\/doi.org\/10.17721\/2306-5680.2019.4.7<\/a><\/strong><\/p>\n\n\n\n<p><a href=\"https:\/\/hydro-chemistry-ecology.knu.ua\/en\/issn2306-5680-%d0%b3%d1%96%d0%b4%d1%80%d0%be%d0%bb%d0%be%d0%b3%d1%96%d1%8f-%d0%b3%d1%96%d0%b4%d1%80%d0%be%d1%85%d1%96%d0%bc%d1%96%d1%8f-%d1%96-%d0%b3%d1%96%d0%b4%d1%80%d0%be%d0%b5%d0%ba%d0%be%d0%bb\/\">Hidrolohii\u0430, hidrokhimii\u0430 i hidroekolohii\u0430. 2019. \u2116 4 (55)<br><\/a><strong>Publication language: <\/strong>Ukrainian<br><strong>Authors:<br><\/strong>Ignatenko I.I.,&nbsp;Institute of Hydrobiology of the National Academy of Sciences of Ukraine,<\/p>\n\n\n\n<p><em>The research results of molybdenum form migration in the water of the Lybid river. The total molybdenum content was 5,8\u201335,0 \u03bcg\/dm3, which is much higher than in the water of the Kaniv reservoir \u2013&nbsp; 2,7\u20138,0 \u03bcg\/dm3. The ratio of dissolved and suspended molybdenum forms was 80,8\u201398,5 and 1,5\u201319,2 %, respectively.&nbsp; The peculiarity of the Lybid river was the presence of molybdate-ions in all sections of the river. This caused a high concentration of dissolved molybdenum form and is an indication of anthropogenic pollution. Molybdate-ions are detected throughout the entire length of the river. They comprised of 5,6\u201323,2 \u03bcg\/dm3 and always exceeded the maximum permissible concentration for fishery reservoirs (1,2 \u03bcg\/dm3). The molybdate-ion concentration was 15 and 18 times higher in the two sections of the Lybid river.&nbsp; Due to their high concentration this can be dangerous for the development of hydrobiota, because the MoO42-\u2013ions are toxins to living organisms.<br>In conclustion, the molybdate-ions in the water of the Lybid river were partly connected to complexes of dissolved organic matters (DOM). The main groups of which are carbohydrates and protein, humic substances. As a result of the processes of water dilution and complexation with DOM,&nbsp; in the water of the Kaniv reservoir, the MoO42- -ions weren\u2019t detected. The humic substances played the primary role in the complexation of molybdate-ions.<\/em><\/p>\n\n\n\n<p><strong><em>Keywords<\/em><\/strong><strong>: <\/strong><em>river runoff, researches, climate change, hydrological models.<\/em><em><\/em><\/p>\n\n\n\n<p><strong>References<\/strong>:<br>1. Vyshnevskiy V.I. Mali richky Kyeva. K. Interpres LTD, 2013. 84 s.<br>2. Kryzhanivskiy O.A. Istoryko-mistobudivniy ta ekoloho-heolohichniy analis terytorii baseyinu richky Lybid. \/\/ Suchasni problemy arhitektury ta mistobuduvannia. 2016. Vyp. 46. \u0421. 287\u2013292.<br>3. Lynnyk P.M., Ihnatenko I.I. Spivicnuyuchi phormy molibdenu v pryrodnyh vodah. \/\/ Hidrolohiia, hidrokhimiia I hidroekolohiia. \u041a., 2006. \u0422. 8. S. 92\u2013102.<br>4. Osnovy analiticheskoj himii. \/ V.I. Phadeeva, T.N. Shehovcova, V.M. Ivanov i dr. \/pod red. Ju.A. Solotova. \u041c.: Vyssh. shk., 2001. 463 s.<br>5.&nbsp; Perepelyzhya O.P. Ecohimia ta endoekolohia elementiv. \u041a.: NUHT: \u0415kohim., 2004. 736 s.<br>6. Linnik P.N., Ignatenko I.I. Molybdenum in Natural Surface Waters: Content and Forms of Occurrence \/\/ Hydrob. Journal. 2015. V.51. I.4. P. 80\u2013103.<\/p>\n\n\n\n<p><a rel=\"noreferrer noopener\" href=\"https:\/\/hydro-chemistry-ecology.knu.ua\/wp-content\/uploads\/2020\/03\/2019_\u2116455_9.pdf\" target=\"_blank\">READ THE FULL ARTICLE<\/a><\/p>\n\n\n\n<p>HOW TO CITE<\/p>\n\n\n\n<p>Ignatenko, I.I. (2019). The molybdenum form migration in the Lybid river water, flowing through the city of Kiyv. <em>Hidrolohiia, hidrokhimiia i hidroekolohiia<\/em> [Hydrology, Hydrochemistry and Hydroecology], 4(55), 88-94 (in Ukrainian, abstr. in English). https:\/\/doi.org\/10.17721\/2306-5680.2019.4.7.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>DOI: https:\/\/doi.org\/10.17721\/2306-5680.2019.4.7 Hidrolohii\u0430, hidrokhimii\u0430 i hidroekolohii\u0430. 2019. \u2116 4 (55)Publication language: UkrainianAuthors:Ignatenko I.I.,&nbsp;Institute of Hydrobiology of the National Academy of Sciences of Ukraine, The research results of molybdenum form migration in the water of the Lybid river. The total molybdenum [&hellip;]<\/p>\n","protected":false},"author":1,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"class_list":["post-242","page","type-page","status-publish","hentry"],"translation":{"provider":"WPGlobus","version":"3.0.0","language":"en","enabled_languages":["uk","en"],"languages":{"uk":{"title":true,"content":true,"excerpt":false},"en":{"title":true,"content":true,"excerpt":false}}},"_links":{"self":[{"href":"https:\/\/hydro-chemistry-ecology.knu.ua\/en\/wp-json\/wp\/v2\/pages\/242","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/hydro-chemistry-ecology.knu.ua\/en\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/hydro-chemistry-ecology.knu.ua\/en\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/hydro-chemistry-ecology.knu.ua\/en\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/hydro-chemistry-ecology.knu.ua\/en\/wp-json\/wp\/v2\/comments?post=242"}],"version-history":[{"count":4,"href":"https:\/\/hydro-chemistry-ecology.knu.ua\/en\/wp-json\/wp\/v2\/pages\/242\/revisions"}],"predecessor-version":[{"id":649,"href":"https:\/\/hydro-chemistry-ecology.knu.ua\/en\/wp-json\/wp\/v2\/pages\/242\/revisions\/649"}],"wp:attachment":[{"href":"https:\/\/hydro-chemistry-ecology.knu.ua\/en\/wp-json\/wp\/v2\/media?parent=242"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}