{"id":3107,"date":"2015-03-23T12:56:56","date_gmt":"2015-03-23T10:56:56","guid":{"rendered":"http:\/\/www.geology.com.ua\/?page_id=3107"},"modified":"2015-03-23T12:56:56","modified_gmt":"2015-03-23T10:56:56","slug":"2014-452-61-67","status":"publish","type":"page","link":"http:\/\/www.geology.com.ua\/en\/2014-452-61-67\/","title":{"rendered":"2014; 4(52) : 61-67"},"content":{"rendered":"<p>Geoinformatika 2014; 4(52) :\u00a061-67<\/p>\n<h4>CHARACTERISTICS OF SUSPENSION IN THE KERCH SOUND ACCORDING TO CONTACT AND SENSING MEASUREMENTS<\/h4>\n<h5><em>Kushnir V.M., Berdnikov S.V.<\/em><\/h5>\n<p style=\"text-align: justify;\">Suspension characteristics in the Kerch strait were studied on the basis of remote sensing measurements of the optical characteristics by MODIS scanners in the red and IR spectrum as well as on the basis of the contact measurements of the suspension concentration in separate points. Functional dependence of this parameter on the colour index for waves of 0,645 and 0,8585 microns is received. This dependence is used for definition of concentration of the small (0,01 \u2264\u00a0<i>r<\/i>\u00a0\u2264 1\u00a0microns) and large (1 \u2264\u00a0<i>r<\/i>\u00a0\u2264 10 microns) particles of the suspension, parametres of the probability distributions and number of these particles in volume unit. Comparison of the received optical parametres with the characteristic data for the Azov \u2013 Black Sea basin has shown satisfactory conformity of these values.<\/p>\n<p><strong>Keywords: <\/strong>suspension, sensing measurements, color index.<\/p>\n<p><a href=\"http:\/\/www.geology.com.ua\/wp-content\/uploads\/2014\/09\/08_Kushnir.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>","protected":false},"excerpt":{"rendered":"<p>Geoinformatika 2014; 4(52) :\u00a061-67 CHARACTERISTICS OF SUSPENSION IN THE KERCH SOUND ACCORDING TO CONTACT AND SENSING MEASUREMENTS Kushnir V.M., Berdnikov S.V. Suspension characteristics in the Kerch strait were studied on the basis of remote sensing measurements of the optical characteristics by MODIS scanners in the red and IR spectrum as well as on the basis of the contact measurements of the suspension concentration in separate points. Functional dependence of this parameter on the colour index for waves of 0,645 and 0,8585 microns is received. This dependence is used for definition of concentration of the small (0,01 \u2264\u00a0r\u00a0\u2264 1\u00a0microns) and large (1 \u2264\u00a0r\u00a0\u2264 10 microns) particles of the suspension, parametres of the probability distributions and number of these particles in volume unit. Comparison of the received optical parametres with the characteristic data for the Azov \u2013 Black Sea basin has shown satisfactory conformity of these values. Keywords: suspension, sensing measurements, color index.<\/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-3107","page","type-page","status-publish","hentry"],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v27.6 - https:\/\/yoast.com\/product\/yoast-seo-wordpress\/ -->\n<title>2014; 4(52) : 61-67 - \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\/2014-452-61-67\/\" \/>\n<meta property=\"og:locale\" content=\"en_US\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"2014; 4(52) : 61-67 - \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 2014; 4(52) :\u00a061-67 CHARACTERISTICS OF SUSPENSION IN THE KERCH SOUND ACCORDING TO CONTACT AND SENSING MEASUREMENTS Kushnir V.M., Berdnikov S.V. Suspension characteristics in the Kerch strait were studied on the basis of remote sensing measurements of the optical characteristics by MODIS scanners in the red and IR spectrum as well as on the basis of the contact measurements of the suspension concentration in separate points. Functional dependence of this parameter on the colour index for waves of 0,645 and 0,8585 microns is received. This dependence is used for definition of concentration of the small (0,01 \u2264\u00a0r\u00a0\u2264 1\u00a0microns) and large (1 \u2264\u00a0r\u00a0\u2264 10 microns) particles of the suspension, parametres of the probability distributions and number of these particles in volume unit. Comparison of the received optical parametres with the characteristic data for the Azov \u2013 Black Sea basin has shown satisfactory conformity of these values. 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Suspension characteristics in the Kerch strait were studied on the basis of remote sensing measurements of the optical characteristics by MODIS scanners in the red and IR spectrum as well as on the basis of the contact measurements of the suspension concentration in separate points. Functional dependence of this parameter on the colour index for waves of 0,645 and 0,8585 microns is received. This dependence is used for definition of concentration of the small (0,01 \u2264\u00a0r\u00a0\u2264 1\u00a0microns) and large (1 \u2264\u00a0r\u00a0\u2264 10 microns) particles of the suspension, parametres of the probability distributions and number of these particles in volume unit. Comparison of the received optical parametres with the characteristic data for the Azov \u2013 Black Sea basin has shown satisfactory conformity of these values. 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