{"id":2399,"date":"2015-02-09T12:14:01","date_gmt":"2015-02-09T10:14:01","guid":{"rendered":"http:\/\/www.geology.com.ua\/?page_id=2399"},"modified":"2015-03-31T16:06:46","modified_gmt":"2015-03-31T14:06:46","slug":"2399-2","status":"publish","type":"page","link":"http:\/\/www.geology.com.ua\/en\/2399-2\/","title":{"rendered":""},"content":{"rendered":"

Geoinformatika 2013; 2(46) : 69-75<\/p>\n

ATMOSPHERIC-ELECTRIC AND HYDROGEN-RADON TECHNOLOGY FOR STUDYING LANDSLIDE STRESS STATE<\/h4>\n

V.N. Shuleikin<\/h5>\n

A method is developed to monitor a landslide stress state on relative gas\u2013permeability rated on the maximum value concentration of hydrogen of soil. The same parameter is calculated as a function of soil radon and radon of the atmosphere, as soil radon and polar conductivity of atmospheric air and as soil radon and the inverse value of the atmospheric electric field. The maximum one relative gas permeability is a stretching zone; the minimum is a compression zone. The technique was successfully tested in 9 observations cycles on the landslide slope.<\/p>\n

Keywords:<\/strong> slope, landslide, stress state, hydrogen, radon, polar conductivity, atmospheric electric field.<\/p>\n

\"pdf\"<\/a><\/p>\n

<\/p>","protected":false},"excerpt":{"rendered":"

Geoinformatika 2013; 2(46) : 69-75 ATMOSPHERIC-ELECTRIC AND HYDROGEN-RADON TECHNOLOGY FOR STUDYING LANDSLIDE STRESS STATE V.N. Shuleikin A method is developed to monitor a landslide stress state on relative gas\u2013permeability rated on the maximum value concentration of hydrogen of soil. The same parameter is calculated as a function of soil radon and radon of the atmosphere, as soil radon and polar conductivity of atmospheric air and as soil radon and the inverse value of the atmospheric electric field. The maximum one relative gas permeability is a stretching zone; the minimum is a compression zone. The technique was successfully tested in 9 observations cycles on the landslide slope. Keywords: slope, landslide, stress state, hydrogen, radon, polar conductivity, atmospheric electric field.<\/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-2399","page","type-page","status-publish","hentry"],"yoast_head":"\n- \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\/2399-2\/\" \/>\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 2013; 2(46) : 69-75 ATMOSPHERIC-ELECTRIC AND HYDROGEN-RADON TECHNOLOGY FOR STUDYING LANDSLIDE STRESS STATE V.N. Shuleikin A method is developed to monitor a landslide stress state on relative gas\u2013permeability rated on the maximum value concentration of hydrogen of soil. The same parameter is calculated as a function of soil radon and radon of the atmosphere, as soil radon and polar conductivity of atmospheric air and as soil radon and the inverse value of the atmospheric electric field. The maximum one relative gas permeability is a stretching zone; the minimum is a compression zone. The technique was successfully tested in 9 observations cycles on the landslide slope. Keywords: slope, landslide, stress state, hydrogen, radon, polar conductivity, atmospheric electric field.\" \/>\n<meta property=\"og:url\" content=\"http:\/\/www.geology.com.ua\/en\/2399-2\/\" \/>\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=\"2015-03-31T14:06:46+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\\\/2399-2\\\/\",\"url\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/2399-2\\\/\",\"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\\\/2399-2\\\/#primaryimage\"},\"image\":{\"@id\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/2399-2\\\/#primaryimage\"},\"thumbnailUrl\":\"http:\\\/\\\/www.geology.com.ua\\\/wp-content\\\/uploads\\\/2013\\\/09\\\/pdf.jpg\",\"datePublished\":\"2015-02-09T10:14:01+00:00\",\"dateModified\":\"2015-03-31T14:06:46+00:00\",\"inLanguage\":\"en-US\",\"potentialAction\":[{\"@type\":\"ReadAction\",\"target\":[[\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/2399-2\\\/\"]]}]},{\"@type\":\"ImageObject\",\"inLanguage\":\"en-US\",\"@id\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/2399-2\\\/#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\/2399-2\/","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 2013; 2(46) : 69-75 ATMOSPHERIC-ELECTRIC AND HYDROGEN-RADON TECHNOLOGY FOR STUDYING LANDSLIDE STRESS STATE V.N. Shuleikin A method is developed to monitor a landslide stress state on relative gas\u2013permeability rated on the maximum value concentration of hydrogen of soil. The same parameter is calculated as a function of soil radon and radon of the atmosphere, as soil radon and polar conductivity of atmospheric air and as soil radon and the inverse value of the atmospheric electric field. The maximum one relative gas permeability is a stretching zone; the minimum is a compression zone. The technique was successfully tested in 9 observations cycles on the landslide slope. Keywords: slope, landslide, stress state, hydrogen, radon, polar conductivity, atmospheric electric field.","og_url":"http:\/\/www.geology.com.ua\/en\/2399-2\/","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":"2015-03-31T14:06:46+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\/2399-2\/","url":"http:\/\/www.geology.com.ua\/en\/2399-2\/","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\/2399-2\/#primaryimage"},"image":{"@id":"http:\/\/www.geology.com.ua\/en\/2399-2\/#primaryimage"},"thumbnailUrl":"http:\/\/www.geology.com.ua\/wp-content\/uploads\/2013\/09\/pdf.jpg","datePublished":"2015-02-09T10:14:01+00:00","dateModified":"2015-03-31T14:06:46+00:00","inLanguage":"en-US","potentialAction":[{"@type":"ReadAction","target":[["http:\/\/www.geology.com.ua\/en\/2399-2\/"]]}]},{"@type":"ImageObject","inLanguage":"en-US","@id":"http:\/\/www.geology.com.ua\/en\/2399-2\/#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"}]}},"_links":{"self":[{"href":"http:\/\/www.geology.com.ua\/en\/wp-json\/wp\/v2\/pages\/2399","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=2399"}],"version-history":[{"count":3,"href":"http:\/\/www.geology.com.ua\/en\/wp-json\/wp\/v2\/pages\/2399\/revisions"}],"predecessor-version":[{"id":3438,"href":"http:\/\/www.geology.com.ua\/en\/wp-json\/wp\/v2\/pages\/2399\/revisions\/3438"}],"wp:attachment":[{"href":"http:\/\/www.geology.com.ua\/en\/wp-json\/wp\/v2\/media?parent=2399"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}