{"id":2893,"date":"2015-03-10T10:54:02","date_gmt":"2015-03-10T08:54:02","guid":{"rendered":"http:\/\/www.geology.com.ua\/?page_id=2893"},"modified":"2015-04-09T13:05:49","modified_gmt":"2015-04-09T11:05:49","slug":"2011-1-66-71","status":"publish","type":"page","link":"http:\/\/www.geology.com.ua\/en\/2011-1-66-71\/","title":{"rendered":"2011; 1 : 66-71"},"content":{"rendered":"<p>Geoinformatika 2011; 1 : 66-71<\/p>\n<h4>RESEARCH RESULTS OF THE TOTAL SUSPENDED MATTER (TSM) FIELD STRUCTURE FOR THE AZOV AND BLACK SEA COASTS APPOSITIVELY TO THE TASKS OF MARINE GEOLOGY AND ECOLOGY<\/h4>\n<h5><em>Lomakin P.D., Chepyzhenko A.I., Chepyzhenko A.A.<\/em><\/h5>\n<p style=\"text-align: justify;\">The paper shows the possibility of operative survey of a 3-demensional field concentration of the TSM in water with the help of sounder turbidimeter. An analysis of the data allows to value the kinematic particularities of suspension currents, reveal the sources of the TSM distribution, find out the areas of coastal and bottom erosion, as well as the zones of TSM accumulation. Presented in the article are the results of naval research that demonstrate these characteristics for different areas of the Azov and Black Sea coasts. The paper gives expediency and efficiency of the information use of a 3-dimensional field of the TSM to solve a wide range of applied problems including marine geology and ecology.<\/p>\n<p style=\"text-align: justify;\"><strong>Keywords:<\/strong> the Azov and Black Sea coasts, total suspended matter (TSM), kinematic particularities of suspension currents, ways of the TSM distribution.<\/p>\n<p style=\"text-align: justify;\">\u00a0<a href=\"http:\/\/www.geology.com.ua\/wp-content\/uploads\/2014\/09\/10_Lomakin.pdf\"><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-790 alignleft\" src=\"http:\/\/www.geology.com.ua\/wp-content\/uploads\/2013\/09\/pdf.jpg\" alt=\"pdf\" width=\"48\" height=\"48\" srcset=\"http:\/\/www.geology.com.ua\/wp-content\/uploads\/2013\/09\/pdf.jpg 128w, http:\/\/www.geology.com.ua\/wp-content\/uploads\/2013\/09\/pdf-150x150.jpg 150w\" sizes=\"auto, (max-width: 48px) 100vw, 48px\" \/><\/a><\/p>\n<p><\/p>","protected":false},"excerpt":{"rendered":"<p>Geoinformatika 2011; 1 : 66-71 RESEARCH RESULTS OF THE TOTAL SUSPENDED MATTER (TSM) FIELD STRUCTURE FOR THE AZOV AND BLACK SEA COASTS APPOSITIVELY TO THE TASKS OF MARINE GEOLOGY AND ECOLOGY Lomakin P.D., Chepyzhenko A.I., Chepyzhenko A.A. The paper shows the possibility of operative survey of a 3-demensional field concentration of the TSM in water with the help of sounder turbidimeter. An analysis of the data allows to value the kinematic particularities of suspension currents, reveal the sources of the TSM distribution, find out the areas of coastal and bottom erosion, as well as the zones of TSM accumulation. Presented in the article are the results of naval research that demonstrate these characteristics for different areas of the Azov and Black Sea coasts. The paper gives expediency and efficiency of the information use of a 3-dimensional field of the TSM to solve a wide range of applied problems including marine geology and ecology. Keywords: the Azov and Black Sea coasts, total suspended matter (TSM), kinematic particularities of suspension currents, ways of the TSM distribution. \u00a0<\/p>\n","protected":false},"author":2,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"open","ping_status":"open","template":"","meta":{"footnotes":""},"class_list":["post-2893","page","type-page","status-publish","hentry"],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v27.5 - https:\/\/yoast.com\/product\/yoast-seo-wordpress\/ -->\n<title>2011; 1 : 66-71 - \u0421\u0430\u0439\u0442 \u0436\u0443\u0440\u043d\u0430\u043b\u0443 \u00ab\u0413\u0435\u043e\u0456\u043d\u0444\u043e\u0440\u043c\u0430\u0442\u0438\u043a\u0430\u00bb<\/title>\n<meta name=\"robots\" content=\"index, follow, max-snippet:-1, max-image-preview:large, max-video-preview:-1\" \/>\n<link rel=\"canonical\" href=\"http:\/\/www.geology.com.ua\/en\/2011-1-66-71\/\" \/>\n<meta property=\"og:locale\" content=\"en_US\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"2011; 1 : 66-71 - \u0421\u0430\u0439\u0442 \u0436\u0443\u0440\u043d\u0430\u043b\u0443 \u00ab\u0413\u0435\u043e\u0456\u043d\u0444\u043e\u0440\u043c\u0430\u0442\u0438\u043a\u0430\u00bb\" \/>\n<meta property=\"og:description\" content=\"Geoinformatika 2011; 1 : 66-71 RESEARCH RESULTS OF THE TOTAL SUSPENDED MATTER (TSM) FIELD STRUCTURE FOR THE AZOV AND BLACK SEA COASTS APPOSITIVELY TO THE TASKS OF MARINE GEOLOGY AND ECOLOGY Lomakin P.D., Chepyzhenko A.I., Chepyzhenko A.A. The paper shows the possibility of operative survey of a 3-demensional field concentration of the TSM in water with the help of sounder turbidimeter. An analysis of the data allows to value the kinematic particularities of suspension currents, reveal the sources of the TSM distribution, find out the areas of coastal and bottom erosion, as well as the zones of TSM accumulation. Presented in the article are the results of naval research that demonstrate these characteristics for different areas of the Azov and Black Sea coasts. The paper gives expediency and efficiency of the information use of a 3-dimensional field of the TSM to solve a wide range of applied problems including marine geology and ecology. Keywords: the Azov and Black Sea coasts, total suspended matter (TSM), kinematic particularities of suspension currents, ways of the TSM distribution. \u00a0\" \/>\n<meta property=\"og:url\" content=\"http:\/\/www.geology.com.ua\/en\/2011-1-66-71\/\" \/>\n<meta property=\"og:site_name\" content=\"\u0421\u0430\u0439\u0442 \u0436\u0443\u0440\u043d\u0430\u043b\u0443 \u00ab\u0413\u0435\u043e\u0456\u043d\u0444\u043e\u0440\u043c\u0430\u0442\u0438\u043a\u0430\u00bb\" \/>\n<meta property=\"article:modified_time\" content=\"2015-04-09T11:05:49+00:00\" \/>\n<meta property=\"og:image\" content=\"http:\/\/www.geology.com.ua\/wp-content\/uploads\/2013\/09\/pdf.jpg\" \/>\n<meta name=\"twitter:label1\" content=\"Est. reading time\" \/>\n\t<meta name=\"twitter:data1\" content=\"1 minute\" \/>\n<script type=\"application\/ld+json\" class=\"yoast-schema-graph\">{\"@context\":\"https:\\\/\\\/schema.org\",\"@graph\":[{\"@type\":\"WebPage\",\"@id\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/2011-1-66-71\\\/\",\"url\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/2011-1-66-71\\\/\",\"name\":\"2011; 1 : 66-71 - \u0421\u0430\u0439\u0442 \u0436\u0443\u0440\u043d\u0430\u043b\u0443 \u00ab\u0413\u0435\u043e\u0456\u043d\u0444\u043e\u0440\u043c\u0430\u0442\u0438\u043a\u0430\u00bb\",\"isPartOf\":{\"@id\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/#website\"},\"primaryImageOfPage\":{\"@id\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/2011-1-66-71\\\/#primaryimage\"},\"image\":{\"@id\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/2011-1-66-71\\\/#primaryimage\"},\"thumbnailUrl\":\"http:\\\/\\\/www.geology.com.ua\\\/wp-content\\\/uploads\\\/2013\\\/09\\\/pdf.jpg\",\"datePublished\":\"2015-03-10T08:54:02+00:00\",\"dateModified\":\"2015-04-09T11:05:49+00:00\",\"breadcrumb\":{\"@id\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/2011-1-66-71\\\/#breadcrumb\"},\"inLanguage\":\"en-US\",\"potentialAction\":[{\"@type\":\"ReadAction\",\"target\":[[\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/2011-1-66-71\\\/\"]]}]},{\"@type\":\"ImageObject\",\"inLanguage\":\"en-US\",\"@id\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/2011-1-66-71\\\/#primaryimage\",\"url\":\"http:\\\/\\\/www.geology.com.ua\\\/wp-content\\\/uploads\\\/2013\\\/09\\\/pdf.jpg\",\"contentUrl\":\"http:\\\/\\\/www.geology.com.ua\\\/wp-content\\\/uploads\\\/2013\\\/09\\\/pdf.jpg\"},{\"@type\":\"BreadcrumbList\",\"@id\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/2011-1-66-71\\\/#breadcrumb\",\"itemListElement\":[{\"@type\":\"ListItem\",\"position\":1,\"name\":\"Home\",\"item\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/\"},{\"@type\":\"ListItem\",\"position\":2,\"name\":\"2011; 1 : 66-71\"}]},{\"@type\":\"WebSite\",\"@id\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/#website\",\"url\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/\",\"name\":\"\u0421\u0430\u0439\u0442 \u0436\u0443\u0440\u043d\u0430\u043b\u0443 \u00ab\u0413\u0435\u043e\u0456\u043d\u0444\u043e\u0440\u043c\u0430\u0442\u0438\u043a\u0430\u00bb\",\"description\":\"\u0426\u0435\u043d\u0442\u0440 \u043c\u0435\u043d\u0435\u0434\u0436\u043c\u0435\u043d\u0442\u0443 \u0442\u0430 \u043c\u0430\u0440\u043a\u0435\u0442\u0438\u043d\u0433\u0443 \u0432 \u0433\u0430\u043b\u0443\u0437\u0456 \u043d\u0430\u0443\u043a \u043f\u0440\u043e \u0417\u0435\u043c\u043b\u044e\",\"potentialAction\":[{\"@type\":\"SearchAction\",\"target\":{\"@type\":\"EntryPoint\",\"urlTemplate\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/?s={search_term_string}\"},\"query-input\":{\"@type\":\"PropertyValueSpecification\",\"valueRequired\":true,\"valueName\":\"search_term_string\"}}],\"inLanguage\":\"en-US\"}]}<\/script>\n<!-- \/ Yoast SEO plugin. -->","yoast_head_json":{"title":"2011; 1 : 66-71 - \u0421\u0430\u0439\u0442 \u0436\u0443\u0440\u043d\u0430\u043b\u0443 \u00ab\u0413\u0435\u043e\u0456\u043d\u0444\u043e\u0440\u043c\u0430\u0442\u0438\u043a\u0430\u00bb","robots":{"index":"index","follow":"follow","max-snippet":"max-snippet:-1","max-image-preview":"max-image-preview:large","max-video-preview":"max-video-preview:-1"},"canonical":"http:\/\/www.geology.com.ua\/en\/2011-1-66-71\/","og_locale":"en_US","og_type":"article","og_title":"2011; 1 : 66-71 - \u0421\u0430\u0439\u0442 \u0436\u0443\u0440\u043d\u0430\u043b\u0443 \u00ab\u0413\u0435\u043e\u0456\u043d\u0444\u043e\u0440\u043c\u0430\u0442\u0438\u043a\u0430\u00bb","og_description":"Geoinformatika 2011; 1 : 66-71 RESEARCH RESULTS OF THE TOTAL SUSPENDED MATTER (TSM) FIELD STRUCTURE FOR THE AZOV AND BLACK SEA COASTS APPOSITIVELY TO THE TASKS OF MARINE GEOLOGY AND ECOLOGY Lomakin P.D., Chepyzhenko A.I., Chepyzhenko A.A. The paper shows the possibility of operative survey of a 3-demensional field concentration of the TSM in water with the help of sounder turbidimeter. An analysis of the data allows to value the kinematic particularities of suspension currents, reveal the sources of the TSM distribution, find out the areas of coastal and bottom erosion, as well as the zones of TSM accumulation. Presented in the article are the results of naval research that demonstrate these characteristics for different areas of the Azov and Black Sea coasts. The paper gives expediency and efficiency of the information use of a 3-dimensional field of the TSM to solve a wide range of applied problems including marine geology and ecology. Keywords: the Azov and Black Sea coasts, total suspended matter (TSM), kinematic particularities of suspension currents, ways of the TSM distribution. \u00a0","og_url":"http:\/\/www.geology.com.ua\/en\/2011-1-66-71\/","og_site_name":"\u0421\u0430\u0439\u0442 \u0436\u0443\u0440\u043d\u0430\u043b\u0443 \u00ab\u0413\u0435\u043e\u0456\u043d\u0444\u043e\u0440\u043c\u0430\u0442\u0438\u043a\u0430\u00bb","article_modified_time":"2015-04-09T11:05:49+00:00","og_image":[{"url":"http:\/\/www.geology.com.ua\/wp-content\/uploads\/2013\/09\/pdf.jpg","type":"","width":"","height":""}],"twitter_misc":{"Est. reading time":"1 minute"},"schema":{"@context":"https:\/\/schema.org","@graph":[{"@type":"WebPage","@id":"http:\/\/www.geology.com.ua\/en\/2011-1-66-71\/","url":"http:\/\/www.geology.com.ua\/en\/2011-1-66-71\/","name":"2011; 1 : 66-71 - \u0421\u0430\u0439\u0442 \u0436\u0443\u0440\u043d\u0430\u043b\u0443 \u00ab\u0413\u0435\u043e\u0456\u043d\u0444\u043e\u0440\u043c\u0430\u0442\u0438\u043a\u0430\u00bb","isPartOf":{"@id":"http:\/\/www.geology.com.ua\/en\/#website"},"primaryImageOfPage":{"@id":"http:\/\/www.geology.com.ua\/en\/2011-1-66-71\/#primaryimage"},"image":{"@id":"http:\/\/www.geology.com.ua\/en\/2011-1-66-71\/#primaryimage"},"thumbnailUrl":"http:\/\/www.geology.com.ua\/wp-content\/uploads\/2013\/09\/pdf.jpg","datePublished":"2015-03-10T08:54:02+00:00","dateModified":"2015-04-09T11:05:49+00:00","breadcrumb":{"@id":"http:\/\/www.geology.com.ua\/en\/2011-1-66-71\/#breadcrumb"},"inLanguage":"en-US","potentialAction":[{"@type":"ReadAction","target":[["http:\/\/www.geology.com.ua\/en\/2011-1-66-71\/"]]}]},{"@type":"ImageObject","inLanguage":"en-US","@id":"http:\/\/www.geology.com.ua\/en\/2011-1-66-71\/#primaryimage","url":"http:\/\/www.geology.com.ua\/wp-content\/uploads\/2013\/09\/pdf.jpg","contentUrl":"http:\/\/www.geology.com.ua\/wp-content\/uploads\/2013\/09\/pdf.jpg"},{"@type":"BreadcrumbList","@id":"http:\/\/www.geology.com.ua\/en\/2011-1-66-71\/#breadcrumb","itemListElement":[{"@type":"ListItem","position":1,"name":"Home","item":"http:\/\/www.geology.com.ua\/en\/"},{"@type":"ListItem","position":2,"name":"2011; 1 : 66-71"}]},{"@type":"WebSite","@id":"http:\/\/www.geology.com.ua\/en\/#website","url":"http:\/\/www.geology.com.ua\/en\/","name":"\u0421\u0430\u0439\u0442 \u0436\u0443\u0440\u043d\u0430\u043b\u0443 \u00ab\u0413\u0435\u043e\u0456\u043d\u0444\u043e\u0440\u043c\u0430\u0442\u0438\u043a\u0430\u00bb","description":"\u0426\u0435\u043d\u0442\u0440 \u043c\u0435\u043d\u0435\u0434\u0436\u043c\u0435\u043d\u0442\u0443 \u0442\u0430 \u043c\u0430\u0440\u043a\u0435\u0442\u0438\u043d\u0433\u0443 \u0432 \u0433\u0430\u043b\u0443\u0437\u0456 \u043d\u0430\u0443\u043a \u043f\u0440\u043e \u0417\u0435\u043c\u043b\u044e","potentialAction":[{"@type":"SearchAction","target":{"@type":"EntryPoint","urlTemplate":"http:\/\/www.geology.com.ua\/en\/?s={search_term_string}"},"query-input":{"@type":"PropertyValueSpecification","valueRequired":true,"valueName":"search_term_string"}}],"inLanguage":"en-US"}]}},"_links":{"self":[{"href":"http:\/\/www.geology.com.ua\/en\/wp-json\/wp\/v2\/pages\/2893","targetHints":{"allow":["GET"]}}],"collection":[{"href":"http:\/\/www.geology.com.ua\/en\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"http:\/\/www.geology.com.ua\/en\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"http:\/\/www.geology.com.ua\/en\/wp-json\/wp\/v2\/users\/2"}],"replies":[{"embeddable":true,"href":"http:\/\/www.geology.com.ua\/en\/wp-json\/wp\/v2\/comments?post=2893"}],"version-history":[{"count":2,"href":"http:\/\/www.geology.com.ua\/en\/wp-json\/wp\/v2\/pages\/2893\/revisions"}],"predecessor-version":[{"id":3705,"href":"http:\/\/www.geology.com.ua\/en\/wp-json\/wp\/v2\/pages\/2893\/revisions\/3705"}],"wp:attachment":[{"href":"http:\/\/www.geology.com.ua\/en\/wp-json\/wp\/v2\/media?parent=2893"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}