{"id":2859,"date":"2015-03-06T11:18:18","date_gmt":"2015-03-06T09:18:18","guid":{"rendered":"http:\/\/www.geology.com.ua\/?page_id=2859"},"modified":"2015-04-09T13:03:31","modified_gmt":"2015-04-09T11:03:31","slug":"2859-2","status":"publish","type":"page","link":"http:\/\/www.geology.com.ua\/en\/2859-2\/","title":{"rendered":""},"content":{"rendered":"<p>Geoinformatika 2011; 1 : 22-31<\/p>\n<h4>PRACTICAL PROBLEMS OF NEAR-SURFACE GEOPHYSICS AND THEIR OPERATIVE SOLVING: FROM THE NON-CLASSICAL GEOELECTRIC METHODS TO THE NEW PARADIGM OF GEOPHYSICAL RESEARCH<\/h4>\n<h5><em>Levashov S.P., Yakymchuk N.A., Korchagin\u00a0I.N.<\/em><\/h5>\n<p style=\"text-align: justify;\">Many years of practical application of non-classical geoelectric methods of forming a short-pulsed field (FSPEF) and vertical electric-resonance sounding (VERS) in the near-surface geophysics problem solving have demonstrated their high efficiency in searching and delineating subsurface water flows and aquifers. The results of our study indicate that the zone of rocks moistening, underground water streams of natural and man-caused origin and aquifers are detected and mapped operatively by areal survey with FSPEF method. The depth of lying and thicknesses of water-saturated horizons are determined with a high accuracy by VERS sounding. Field works of such type are often executed very quickly and easily. The FSPEF and VERS methods make a significant contribution into emergence of a new paradigm of geophysical research, which includes the &#8220;direct&#8221; searching for a specific physical substance: gas, oil, gas hydrates, water, ore minerals and rocks (gold, platinum, silver, zinc, uranium, diamonds, kimberlites, etc.). The effectiveness of these geophysical methods based on the paradigm principles is much higher than that of traditional ones.<\/p>\n<p style=\"text-align: justify;\"><strong>Keywords:<\/strong> geoelectric survey, electric-resonance sounding, deposit type anomaly, zone of moistening, aquifer, water flow, well, landslide zone.<\/p>\n<p style=\"text-align: justify;\"><a href=\"http:\/\/www.geology.com.ua\/wp-content\/uploads\/2014\/09\/02_Levashov5.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 : 22-31 PRACTICAL PROBLEMS OF NEAR-SURFACE GEOPHYSICS AND THEIR OPERATIVE SOLVING: FROM THE NON-CLASSICAL GEOELECTRIC METHODS TO THE NEW PARADIGM OF GEOPHYSICAL RESEARCH Levashov S.P., Yakymchuk N.A., Korchagin\u00a0I.N. Many years of practical application of non-classical geoelectric methods of forming a short-pulsed field (FSPEF) and vertical electric-resonance sounding (VERS) in the near-surface geophysics problem solving have demonstrated their high efficiency in searching and delineating subsurface water flows and aquifers. The results of our study indicate that the zone of rocks moistening, underground water streams of natural and man-caused origin and aquifers are detected and mapped operatively by areal survey with FSPEF method. The depth of lying and thicknesses of water-saturated horizons are determined with a high accuracy by VERS sounding. Field works of such type are often executed very quickly and easily. The FSPEF and VERS methods make a significant contribution into emergence of a new paradigm of geophysical research, which includes the &#8220;direct&#8221; searching for a specific physical substance: gas, oil, gas hydrates, water, ore minerals and rocks (gold, platinum, silver, zinc, uranium, diamonds, kimberlites, etc.). The effectiveness of these geophysical methods based on the paradigm principles is much higher than that of traditional ones. Keywords: geoelectric survey, electric-resonance sounding, deposit type anomaly, zone of moistening, aquifer, water flow, well, landslide zone.<\/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-2859","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>- \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\/2859-2\/\" \/>\n<meta property=\"og:locale\" content=\"en_US\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" 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=\"og:description\" content=\"Geoinformatika 2011; 1 : 22-31 PRACTICAL PROBLEMS OF NEAR-SURFACE GEOPHYSICS AND THEIR OPERATIVE SOLVING: FROM THE NON-CLASSICAL GEOELECTRIC METHODS TO THE NEW PARADIGM OF GEOPHYSICAL RESEARCH Levashov S.P., Yakymchuk N.A., Korchagin\u00a0I.N. Many years of practical application of non-classical geoelectric methods of forming a short-pulsed field (FSPEF) and vertical electric-resonance sounding (VERS) in the near-surface geophysics problem solving have demonstrated their high efficiency in searching and delineating subsurface water flows and aquifers. The results of our study indicate that the zone of rocks moistening, underground water streams of natural and man-caused origin and aquifers are detected and mapped operatively by areal survey with FSPEF method. The depth of lying and thicknesses of water-saturated horizons are determined with a high accuracy by VERS sounding. Field works of such type are often executed very quickly and easily. The FSPEF and VERS methods make a significant contribution into emergence of a new paradigm of geophysical research, which includes the &#8220;direct&#8221; searching for a specific physical substance: gas, oil, gas hydrates, water, ore minerals and rocks (gold, platinum, silver, zinc, uranium, diamonds, kimberlites, etc.). The effectiveness of these geophysical methods based on the paradigm principles is much higher than that of traditional ones. Keywords: geoelectric survey, electric-resonance sounding, deposit type anomaly, zone of moistening, aquifer, water flow, well, landslide zone.\" \/>\n<meta property=\"og:url\" content=\"http:\/\/www.geology.com.ua\/en\/2859-2\/\" \/>\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=\"2015-04-09T11:03:31+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\\\/2859-2\\\/\",\"url\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/2859-2\\\/\",\"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\",\"isPartOf\":{\"@id\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/#website\"},\"primaryImageOfPage\":{\"@id\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/2859-2\\\/#primaryimage\"},\"image\":{\"@id\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/2859-2\\\/#primaryimage\"},\"thumbnailUrl\":\"http:\\\/\\\/www.geology.com.ua\\\/wp-content\\\/uploads\\\/2013\\\/09\\\/pdf.jpg\",\"datePublished\":\"2015-03-06T09:18:18+00:00\",\"dateModified\":\"2015-04-09T11:03:31+00:00\",\"inLanguage\":\"en-US\",\"potentialAction\":[{\"@type\":\"ReadAction\",\"target\":[[\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/2859-2\\\/\"]]}]},{\"@type\":\"ImageObject\",\"inLanguage\":\"en-US\",\"@id\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/2859-2\\\/#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\":\"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":"- \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\/2859-2\/","og_locale":"en_US","og_type":"article","og_title":"- \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 : 22-31 PRACTICAL PROBLEMS OF NEAR-SURFACE GEOPHYSICS AND THEIR OPERATIVE SOLVING: FROM THE NON-CLASSICAL GEOELECTRIC METHODS TO THE NEW PARADIGM OF GEOPHYSICAL RESEARCH Levashov S.P., Yakymchuk N.A., Korchagin\u00a0I.N. Many years of practical application of non-classical geoelectric methods of forming a short-pulsed field (FSPEF) and vertical electric-resonance sounding (VERS) in the near-surface geophysics problem solving have demonstrated their high efficiency in searching and delineating subsurface water flows and aquifers. The results of our study indicate that the zone of rocks moistening, underground water streams of natural and man-caused origin and aquifers are detected and mapped operatively by areal survey with FSPEF method. The depth of lying and thicknesses of water-saturated horizons are determined with a high accuracy by VERS sounding. Field works of such type are often executed very quickly and easily. The FSPEF and VERS methods make a significant contribution into emergence of a new paradigm of geophysical research, which includes the &#8220;direct&#8221; searching for a specific physical substance: gas, oil, gas hydrates, water, ore minerals and rocks (gold, platinum, silver, zinc, uranium, diamonds, kimberlites, etc.). The effectiveness of these geophysical methods based on the paradigm principles is much higher than that of traditional ones. 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