{"id":1422,"date":"2019-10-25T12:42:28","date_gmt":"2019-10-25T09:42:28","guid":{"rendered":"http:\/\/www.g-o-f.org.ua\/?page_id=1422"},"modified":"2020-01-20T20:50:08","modified_gmt":"2020-01-20T18:50:08","slug":"distribution-of-halogens","status":"publish","type":"page","link":"http:\/\/www.g-o-f.org.ua\/gb\/archive\/2012-2\/distribution-of-halogens\/","title":{"rendered":"Distribution of halogens in the first aquifer of the Central Dnieper-Donets Basin"},"content":{"rendered":"<p style=\"text-align: justify;\">Kryuchenko N.O., Kukhar M.V.<\/p>\n<p style=\"text-align: justify;\">Language: Ukrainian<br \/>\nGeochemistry and ore formation 2012, 31-32: 150-153<\/p>\n<p><a href=\"https:\/\/doi.org\/10.15407\/gof.2012.31.150\">https:\/\/doi.org\/10.15407\/gof.2012.31.150<\/a><\/p>\n<p><a href=\"http:\/\/www.g-o-f.org.ua\/wp-content\/uploads\/2012-31-32\/20_1.pdf\">Download (PDF)<\/a><\/p>\n<p style=\"text-align: justify;\">According to studies of first aquifer of the Central part of the Dnieper-Donets Basin (the area of Poltava and Sumy regions) maps of the spatial distribution of halogens (F, I, Cl, Br). The high content of I and Br in the northern part of the territory due to the presence of halogen formations and sedimentary rocks (mainly clay), rich in organic matter, the high content of fluorine in the central part of the plot indicates the presence of low calcium \u041d\u0421\u041e3-N\u0430 waters, which are favorable for the removal fluoride from rocks and their accumulation in itself, the high content of chlorine in wells near the center of the Poltava region indicates contamination of water bodies household sewage.<\/p>\n<p>References<br \/>\n1. Alekseenko V.A. Ekologicheskaya geohimiya, Logos, 2000, 626 p.<br \/>\n2. Dobrovolskij V.V. Osnovy biogeohimii : Uchebnik dlya stud. vyssh. ucheb, zavedenij.\u00a0 Izd. centr Akademiya, 2003, 400 p.<br \/>\n3. Zhovinskij E.Ya., Kuraeva I.V. Geohimiya ftora (prikladnoe znachenie). Nauk. dumka, 1987, 158 p.<br \/>\n4. Ivanov V.V. Ekologicheskaya geohimiya elementov: v 6-ti t. Ekologiya, 1997.<br \/>\n5. Rudenko F.A. Gidrogeologiya SSSR. Tom V. Ukrainskaya SSR. Nedra, 1971, 614 p.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Kryuchenko N.O., Kukhar M.V. Language: Ukrainian Geochemistry and ore formation 2012, 31-32: 150-153 https:\/\/doi.org\/10.15407\/gof.2012.31.150 Download (PDF) According to studies of first aquifer of the Central part of the Dnieper-Donets Basin (the area of Poltava and Sumy regions) maps of the spatial distribution of halogens (F, I, Cl, Br). The high content of I and Br &hellip; <a href=\"http:\/\/www.g-o-f.org.ua\/gb\/archive\/2012-2\/distribution-of-halogens\/\" class=\"more-link\">Continue reading<span class=\"screen-reader-text\"> &#8220;Distribution of halogens in the first aquifer of the Central Dnieper-Donets Basin&#8221;<\/span><\/a><\/p>\n","protected":false},"author":1,"featured_media":0,"parent":256,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"class_list":["post-1422","page","type-page","status-publish","hentry"],"translation":{"provider":"WPGlobus","version":"3.0.0","language":"gb","enabled_languages":["uk","gb"],"languages":{"uk":{"title":true,"content":true,"excerpt":false},"gb":{"title":true,"content":true,"excerpt":false}}},"jetpack_sharing_enabled":true,"jetpack_shortlink":"https:\/\/wp.me\/P9ghyZ-mW","jetpack_likes_enabled":true,"jetpack-related-posts":[{"id":1556,"url":"http:\/\/www.g-o-f.org.ua\/gb\/archive\/2019-40\/8-2\/","url_meta":{"origin":1422,"position":0},"title":"Isotop-Geochemistry properties of carbonate formations of Crimea","author":"admin","date":"28\/11\/2019","format":false,"excerpt":"{:uk}\u0412.\u041c. \u0417\u0430\u0433\u043d\u0456\u0442\u043a\u043e 1, \u0404.\u0412. \u041d\u0430\u0443\u043c\u0435\u043d\u043a\u043e 2, \u0412.\u0421. \u041c\u043e\u0440\u043e\u0437 3, \u041b.\u0406. \u041f\u0440\u043e\u0441\u043a\u0443\u0440\u043a\u0430 3 1 \u2014 \u041d\u041d\u0406 \u00ab\u0406\u043d\u0441\u0442\u0438\u0442\u0443\u0442 \u0433\u0435\u043e\u043b\u043e\u0433\u0456\u0457\u00bb, \u041a\u0438\u0457\u0432\u0441\u044c\u043a\u0438\u0439 \u043d\u0430\u0446\u0456\u043e\u043d\u0430\u043b\u044c\u043d\u0438\u0439 \u0443\u043d\u0456\u0432\u0435\u0440\u0441\u0438\u0442\u0435\u0442 \u0456\u043c\u0435\u043d\u0456 \u0422\u0430\u0440\u0430\u0441\u0430 \u0428\u0435\u0432\u0447\u0435\u043d\u043a\u0430 2 \u2014 \u041d\u0430\u0446\u0456\u043e\u043d\u0430\u043b\u044c\u043d\u0438\u0439 \u043d\u0430\u0443\u043a\u043e\u0432\u043e-\u043f\u0440\u0438\u0440\u043e\u0434\u043d\u0438\u0447\u0438\u0439 \u043c\u0443\u0437\u0435\u0439 \u041d\u0410\u041d \u0423\u043a\u0440\u0430\u0457\u043d\u0438 3 \u2014 \u0406\u043d\u0441\u0442\u0438\u0442\u0443\u0442 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post","link":""},"img":{"alt_text":"","src":"https:\/\/i0.wp.com\/www.g-o-f.org.ua\/wp-content\/uploads\/2020\/index.jpg?resize=350%2C200","width":350,"height":200},"classes":[]},{"id":2025,"url":"http:\/\/www.g-o-f.org.ua\/gb\/archive\/2022-43\/7-2\/","url_meta":{"origin":1422,"position":1},"title":"RARE-EARTH DEPOSITS OF A NON-TRADITIONAL TYPE IN THE AZOV PART OF THE UKRAINIAN SHIELD","author":"admin","date":"20\/12\/2022","format":false,"excerpt":"{:uk} \u041b.\u0414. \u0421\u0454\u0442\u0430\u044fE-mail: lasetaya@gmail.com, https:\/\/orcid.org\/0000-0002-2996-0289\u0406.\u042e. \u041d\u0456\u043a\u043e\u043b\u0430\u0454\u0432E-mail: oemidonetsk@gmail.com, https:\/\/orcid.org\/0000-0003-2208-0032\u0421.\u041c. \u0421\u0442\u0440\u0435\u043a\u043e\u0437\u043e\u0432E-mail: ssss21161@gmail.com, https:\/\/orcid.org\/0000-0002-1421-4910\u0406\u043d\u0441\u0442\u0438\u0442\u0443\u0442 \u0433\u0435\u043e\u0445\u0456\u043c\u0456\u0457, 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formation","author":"admin","date":"09\/10\/2017","format":false,"excerpt":"{:uk}{:uk}\u0413\u0435\u043e\u0445\u0456\u043c\u0456\u044f \u0442\u0430 \u0440\u0443\u0434\u043e\u0443\u0442\u0432\u043e\u0440\u0435\u043d\u043d\u044f: \u0437\u0431. \u043d\u0430\u0443\u043a. \u043f\u0440. \/ \u041d\u0430\u0446. \u0430\u043a\u0430\u0434. \u043d\u0430\u0443\u043a \u0423\u043a\u0440\u0430\u0457\u043d\u0438, \u0406\u043d-\u0442 \u0433\u0435\u043e\u0445\u0456\u043c\u0456\u0457, \u043c\u0456\u043d\u0435\u0440\u0430\u043b\u043e\u0433\u0456\u0457 \u0442\u0430 \u0440\u0443\u0434\u043e\u0443\u0442\u0432\u043e\u0440\u0435\u043d\u043d\u044f \u0456\u043c. \u041c. \u041f. \u0421\u0435\u043c\u0435\u043d\u0435\u043d\u043a\u0430. \u2013 \u041a\u0438\u0457\u0432: [\u0431. \u0432.], 1972. - \u041f\u0435\u0440\u0456\u043e\u0434\u0438\u0447\u043d\u0456\u0441\u0442\u044c: \u0434\u043e \u0434\u0432\u043e\u0445 \u0440\u0430\u0437\u0456\u0432 \u043d\u0430 \u0440\u0456\u043a. 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post","link":""},"img":{"alt_text":"","src":"","width":0,"height":0},"classes":[]},{"id":1766,"url":"http:\/\/www.g-o-f.org.ua\/gb\/archive\/2020-41\/6-2\/","url_meta":{"origin":1422,"position":4},"title":"Lead-zinc mineralization of fluoriton-bearing areas of the Middle Transnistria","author":"admin","date":"09\/12\/2020","format":false,"excerpt":"{:uk}\u041d.\u041e. \u041a\u0440\u044e\u0447\u0435\u043d\u043a\u043e 1 https:\/\/orcid.org\/0000-0001-8774-9089 \u0415.\u042f. \u0416\u043e\u0432\u0438\u043d\u0441\u044c\u043a\u0438\u0439 1 https:\/\/orcid.org\/0000-0003-1601-5998 \u041e.\u0410. \u0416\u0443\u043a 1 https:\/\/orcid.org\/0000-0002-5264-0750 \u041f.\u0421. \u041f\u0430\u043f\u0430\u0440\u0438\u0433\u0430 2 https:\/\/orcid.org\/0000-0002-4021-0809 \u041c.\u0412. \u041a\u0443\u0445\u0430\u0440 1 https:\/\/orcid.org\/0000-0003-3572-5194 \u041a.\u0415. \u0414\u043c\u0438\u0442\u0440\u0435\u043d\u043a\u043e 1 https:\/\/orcid.org\/0000-0003-1001-3457 \u0422.\u0410. 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