{"id":13116,"date":"2024-11-14T11:15:52","date_gmt":"2024-11-14T11:15:52","guid":{"rendered":"https:\/\/blog.geostru.eu\/?p=13116"},"modified":"2024-11-14T11:15:54","modified_gmt":"2024-11-14T11:15:54","slug":"strat-lenticular-cum-sa-il-introduceti-in-geostru-slope","status":"publish","type":"post","link":"https:\/\/blog.geostru.eu\/ro\/strat-lenticular-cum-sa-il-introduceti-in-geostru-slope\/","title":{"rendered":"Strat lenticular: cum s\u0103 \u00eel introduce\u021bi \u00een GeoStru Slope"},"content":{"rendered":"<div class=\"wpb-content-wrapper\"><p>[vc_row][vc_column][vc_column_text css=&#8221;&#8221;]<\/p>\n<p style=\"text-align: justify\">\u00cen geologie, un <strong>strat lenticular<\/strong> este un corp de mineral, roc\u0103 sau depozit, de obicei mai gros \u00een centru \u0219i sub\u021bire la margini, asem\u0103n\u0103tor cu o lentil\u0103 convex\u0103 \u00een sec\u021biunea sa transversal\u0103. O lentil\u0103 poate face referire \u0219i la o forma\u021biune de form\u0103 neregulat\u0103, constituit\u0103 dintr-un depozit poros, sedimentar, permeabil, \u00eenconjurat de roc\u0103 impermeabil\u0103.<\/p>\n<p style=\"text-align: justify\">\u00cen acest articol vom vedea cum s\u0103 introducem \u0219i s\u0103 lu\u0103m \u00een considerare un strat lenticular \u00een cadrul software-ului <a href=\"https:\/\/www.geostru.eu\/ro\/shop\/software-ro\/geotehnica-si-geologie\/stabilitatea-taluzurilor-slope\/\">GeoStru Stabilitatea versan\u021bilor \u2013 Slope.<\/a><\/p>\n<p>[\/vc_column_text][\/vc_column][\/vc_row][vc_row][vc_column][vc_column_text css=&#8221;&#8221;]<\/p>\n<h3 style=\"text-align: justify\">Construc\u021bia sec\u021biunii f\u0103r\u0103 strat lenticular<\/h3>\n<p style=\"text-align: justify\">Primul pas este s\u0103 definim sec\u021biunea noastr\u0103 \u00een cadrul software-ului, f\u0103r\u0103 a lua \u00een considerare stratul lentifcular. Astfel, pe l\u00e2ng\u0103 desenarea manual\u0103 sau introducerea numeric\u0103 a coordonatelor diverselor straturi, Slope permite diferite metode de importare a sec\u021biunii geotehnice, cum ar fi:<\/p>\n<ul>\n<li style=\"text-align: justify\">Import din modelul 3D;<\/li>\n<li style=\"text-align: justify\">Importa\u021bi sec\u021biuni din alte programe GeoStru;<\/li>\n<li style=\"text-align: justify\">Import din fi\u0219ier DXF;<\/li>\n<li style=\"text-align: justify\">Import din Penetrometrie;<\/li>\n<li style=\"text-align: justify\">Import din <a href=\"https:\/\/www.geostru.eu\/ro\/shop\/software-ro\/geotehnica-si-geologie\/capacitatea-portanta-si-tasari-fundatii\/\"><strong>GeoStru Loadcap<\/strong><\/a>;<\/li>\n<li style=\"text-align: justify\"><a href=\"https:\/\/www.youtube.com\/watch?v=VeEa4dUM8S8\"><strong>Vectorizarea rasterului prin inteligen\u021b\u0103 artificial\u0103.<\/strong><\/a><\/li>\n<\/ul>\n<p>[\/vc_column_text][\/vc_column][\/vc_row][vc_row][vc_column][vc_single_image image=&#8221;13118&#8243; img_size=&#8221;full&#8221; alignment=&#8221;center&#8221; onclick=&#8221;link_image&#8221; css=&#8221;&#8221;][\/vc_column][\/vc_row][vc_row][vc_column][vc_column_text css=&#8221;&#8221;]<\/p>\n<h3 style=\"text-align: justify\">Introducerea stratului lenticular se poate face folosind instrumentul poligon<\/h3>\n<p style=\"text-align: justify\">Dup\u0103 ce sec\u021biunea a fost construit\u0103 f\u0103r\u0103 <strong>\u201elentil\u0103\u201d<\/strong>, aceasta trebuie ad\u0103ugat\u0103. Merg\u00e2nd la Instrumente \u0219i apoi la Poligon, se poate trasa o form\u0103 geometric\u0103 \u00een sec\u021biune, iar odat\u0103 completat\u0103 va ap\u0103rea fereastra de propriet\u0103\u021bi a poligonului. Aici, pe l\u00e2ng\u0103 toate op\u021biunile legate de stil \u0219i coordonatele v\u00e2rfurilor, se g\u0103se\u0219te op\u021biunea \u201e<strong>Trata\u021bi acest poligon ca un material<\/strong>\u201d. Odat\u0103 bifat\u0103, software-ul va trata regiunea nou creat\u0103 ca un material, iar caracteristicile geotehnice vor putea fi introduse, cum ar fi: greutatea volumic\u0103, coeziunea, unghiul de frecare.<\/p>\n<p>[\/vc_column_text][\/vc_column][\/vc_row][vc_row][vc_column][vc_single_image image=&#8221;13122&#8243; img_size=&#8221;full&#8221; alignment=&#8221;center&#8221; onclick=&#8221;link_image&#8221; css=&#8221;&#8221;][\/vc_column][\/vc_row][vc_row][vc_column][vc_column_text css=&#8221;&#8221;]<\/p>\n<h3 style=\"text-align: justify\">Utilizarea unei imagini raster<\/h3>\n<p style=\"text-align: justify\">\u00cen cazul \u00een care coordonatele v\u00e2rfurilor stratului lentifcular nu sunt cunoscute, este posibil\u0103 construirea acestuia folosind o surs\u0103 precum o imagine care urmeaz\u0103 s\u0103 fie importat\u0103 \u00een GeoStru Slope. De asemenea, este posibil s\u0103 imprima\u021bi un DXF \u00een format imagine.<br \/>\n\u00cen Slope de la Tools, pur \u0219i simplu face\u021bi clic pe Insert Raster Image \u0219i selecta\u021bi imaginea. Apare fereastra de calibrare a rasterului \u0219i punctul de origine a inser\u021biei a v\u00e2rfului din st\u00e2nga jos, care pentru scopul nostru este irelevant; de fapt, pute\u021bi insera imaginea \u00een orice punct \u0219i cu orice dimensiune. Pute\u021bi apoi s\u0103 o muta\u021bi \u0219i s\u0103 o redimensiona\u021bi manual astfel \u00eenc\u00e2t rasterul, cu acest strat lenticular nou importat, s\u0103 corespund\u0103 sec\u021biunii create anterior \u00een Slope.<\/p>\n<p>[\/vc_column_text][\/vc_column][\/vc_row][vc_row][vc_column][vc_single_image image=&#8221;13126&#8243; img_size=&#8221;full&#8221; alignment=&#8221;center&#8221; onclick=&#8221;link_image&#8221; css=&#8221;&#8221;][\/vc_column][\/vc_row][vc_row][vc_column][vc_column_text css=&#8221;&#8221;]Acum tot ce trebuie s\u0103 face\u021bi este s\u0103 crea\u021bi poligonul, a\u0219a cum este descris mai sus, urm\u00e2nd imaginea pe care tocmai a\u021bi importat-o \u0219i redimensionat-o.<\/p>\n<p>[\/vc_column_text][\/vc_column][\/vc_row][vc_row][vc_column][vc_single_image image=&#8221;13131&#8243; img_size=&#8221;full&#8221; alignment=&#8221;center&#8221; onclick=&#8221;link_image&#8221; css=&#8221;&#8221;][\/vc_column][\/vc_row][vc_row 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data-phone-columns-num=\"1\" data-col-gap=\"10\" data-stage-padding=\"0\" data-speed=\"600\" data-autoplay=\"false\" data-autoplay_speed=\"6000\" data-arrows=\"true\" data-bullet=\"false\" data-next-icon=\"icon-ar-017-r\" data-prev-icon=\"icon-ar-017-l\" data-img-shadow-size=\"12px\" data-img-shadow-spread=\"3px\"><div data-post-id=\"12298\" data-date=\"2024-07-15T09:39:46+00:00\" data-name=\"slope 2024 en geostru\"><figure class=\"post\"><a href=\"https:\/\/blog.geostru.eu\/wp-content\/uploads\/sites\/9\/2024\/07\/slope-2024-en-geostru.png\" class=\"rollover dt-pswp-item layzr-bg\" data-large_image_width=\"1913\" data-large_image_height=\"1011\" data-dt-img-description=\"\" title=\"slope 2024 en geostru\"><img fetchpriority=\"high\" decoding=\"async\" class=\"preload-me owl-lazy-load aspect\" src=\"data:image\/svg+xml,%3Csvg%20xmlns%3D&#39;http%3A%2F%2Fwww.w3.org%2F2000%2Fsvg&#39;%20viewBox%3D&#39;0%200%201913%201011&#39;%2F%3E\" data-src=\"https:\/\/blog.geostru.eu\/wp-content\/uploads\/sites\/9\/2024\/07\/slope-2024-en-geostru.png\" data-srcset=\"https:\/\/blog.geostru.eu\/wp-content\/uploads\/sites\/9\/2024\/07\/slope-2024-en-geostru.png 1913w\" loading=\"eager\" style=\"--ratio: 1913 \/ 1011\" sizes=\"(max-width: 1913px) 100vw, 1913px\" alt=\"\" width=\"1913\" height=\"1011\"  \/><span class=\"gallery-rollover\"><span class=\"gallery-zoom-ico icomoon-the7-font-the7-zoom-06\"><span><\/span><\/span><\/span><\/a><\/figure><\/div><div data-post-id=\"12294\" data-date=\"2024-07-15T09:39:44+00:00\" data-name=\"slope 2024 en geostru 2\"><figure class=\"post\"><a href=\"https:\/\/blog.geostru.eu\/wp-content\/uploads\/sites\/9\/2024\/07\/slope-2024-en-geostru-2.png\" class=\"rollover dt-pswp-item layzr-bg\" data-large_image_width=\"1918\" data-large_image_height=\"1006\" data-dt-img-description=\"\" title=\"slope 2024 en geostru 2\"><img decoding=\"async\" class=\"preload-me owl-lazy-load aspect\" src=\"data:image\/svg+xml,%3Csvg%20xmlns%3D&#39;http%3A%2F%2Fwww.w3.org%2F2000%2Fsvg&#39;%20viewBox%3D&#39;0%200%201918%201006&#39;%2F%3E\" data-src=\"https:\/\/blog.geostru.eu\/wp-content\/uploads\/sites\/9\/2024\/07\/slope-2024-en-geostru-2.png\" data-srcset=\"https:\/\/blog.geostru.eu\/wp-content\/uploads\/sites\/9\/2024\/07\/slope-2024-en-geostru-2.png 1918w\" loading=\"eager\" style=\"--ratio: 1918 \/ 1006\" sizes=\"(max-width: 1918px) 100vw, 1918px\" alt=\"\" width=\"1918\" height=\"1006\"  \/><span class=\"gallery-rollover\"><span class=\"gallery-zoom-ico icomoon-the7-font-the7-zoom-06\"><span><\/span><\/span><\/span><\/a><\/figure><\/div><div data-post-id=\"12290\" data-date=\"2024-07-15T09:39:42+00:00\" data-name=\"slope 2024 en geostru 3\"><figure class=\"post\"><a href=\"https:\/\/blog.geostru.eu\/wp-content\/uploads\/sites\/9\/2024\/07\/slope-2024-en-geostru-3.png\" class=\"rollover dt-pswp-item layzr-bg\" data-large_image_width=\"1917\" data-large_image_height=\"1008\" data-dt-img-description=\"\" title=\"slope 2024 en geostru 3\"><img decoding=\"async\" class=\"preload-me owl-lazy-load aspect\" src=\"data:image\/svg+xml,%3Csvg%20xmlns%3D&#39;http%3A%2F%2Fwww.w3.org%2F2000%2Fsvg&#39;%20viewBox%3D&#39;0%200%201917%201008&#39;%2F%3E\" data-src=\"https:\/\/blog.geostru.eu\/wp-content\/uploads\/sites\/9\/2024\/07\/slope-2024-en-geostru-3.png\" data-srcset=\"https:\/\/blog.geostru.eu\/wp-content\/uploads\/sites\/9\/2024\/07\/slope-2024-en-geostru-3.png 1917w\" loading=\"eager\" style=\"--ratio: 1917 \/ 1008\" sizes=\"(max-width: 1917px) 100vw, 1917px\" alt=\"\" width=\"1917\" height=\"1008\"  \/><span class=\"gallery-rollover\"><span class=\"gallery-zoom-ico icomoon-the7-font-the7-zoom-06\"><span><\/span><\/span><\/span><\/a><\/figure><\/div><div data-post-id=\"12286\" data-date=\"2024-07-15T09:39:40+00:00\" data-name=\"slope 2024 en geostru 4\"><figure class=\"post\"><a href=\"https:\/\/blog.geostru.eu\/wp-content\/uploads\/sites\/9\/2024\/07\/slope-2024-en-geostru-4.png\" class=\"rollover dt-pswp-item layzr-bg\" data-large_image_width=\"1913\" data-large_image_height=\"1008\" data-dt-img-description=\"\" title=\"slope 2024 en geostru 4\"><img decoding=\"async\" class=\"preload-me owl-lazy-load aspect\" src=\"data:image\/svg+xml,%3Csvg%20xmlns%3D&#39;http%3A%2F%2Fwww.w3.org%2F2000%2Fsvg&#39;%20viewBox%3D&#39;0%200%201913%201008&#39;%2F%3E\" data-src=\"https:\/\/blog.geostru.eu\/wp-content\/uploads\/sites\/9\/2024\/07\/slope-2024-en-geostru-4.png\" data-srcset=\"https:\/\/blog.geostru.eu\/wp-content\/uploads\/sites\/9\/2024\/07\/slope-2024-en-geostru-4.png 1913w\" loading=\"eager\" style=\"--ratio: 1913 \/ 1008\" sizes=\"(max-width: 1913px) 100vw, 1913px\" alt=\"\" width=\"1913\" height=\"1008\"  \/><span class=\"gallery-rollover\"><span class=\"gallery-zoom-ico icomoon-the7-font-the7-zoom-06\"><span><\/span><\/span><\/span><\/a><\/figure><\/div><\/div>[vc_empty_space height=&#8221;35px&#8221;][\/vc_column][vc_column width=&#8221;1\/2&#8243;][vc_column_text css=&#8221;&#8221;]<\/p>\n<p class=\"product_title entry-title\"><strong>Stabilitatea taluzurilor \u2013 Slope<\/strong><\/p>\n<p style=\"text-align: justify\">Stabilitatea taluzurilor \u00een soluri af\u00e2nate sau st\u00e2ncoase cu metodele tradi\u021bionale ale geotehnicii (Echilibrul Limita) \u0219i metoda Elementelor Discrete, cu ajutorul c\u0103reia se poate calcula deplasarea taluzului \u0219i examina ruptura progresiv\u0103.<br \/>\n<a href=\"https:\/\/www.geostru.eu\/ro\/shop\/software-ro\/geotehnica-si-geologie\/stabilitatea-taluzurilor-slope\/\" target=\"_blank\" rel=\"noopener\">Slope<\/a> efectueaz\u0103 analize statice, c\u00e2t \u0219i dinamice.<\/p>\n<p>[\/vc_column_text][vc_row_inner][vc_column_inner width=&#8221;1\/2&#8243;]<a href=\"https:\/\/www.geostru.eu\/ro\/shop\/software-ro\/geotehnica-si-geologie\/stabilitatea-taluzurilor-slope\/\" class=\"btn-shortcode dt-btn-m dt-btn default-btn-color default-btn-hover-color default-btn-bg-color default-btn-bg-hover-color\" target=\"_blank\" id=\"dt-btn-1\" rel=\"noopener\"><span>Mai multe informa\u021bii<\/span><\/a>[\/vc_column_inner][vc_column_inner width=&#8221;1\/2&#8243;]<a href=\"https:\/\/help.geostru.eu\/slope\/ro\" class=\"btn-shortcode dt-btn-m dt-btn default-btn-color default-btn-hover-color default-btn-bg-color default-btn-bg-hover-color\" target=\"_blank\" id=\"dt-btn-2\" rel=\"noopener\"><span>Help<\/span><\/a>[\/vc_column_inner][\/vc_row_inner][\/vc_column][\/vc_row][vc_row][vc_column][vc_basic_grid post_type=&#8221;post&#8221; max_items=&#8221;3&#8243; css=&#8221;&#8221; grid_id=&#8221;vc_gid:1731513784318-a6a524b0-868f-0&#8243; taxonomies=&#8221;1608&#8243;][\/vc_column][\/vc_row]<\/p>\n<\/div>","protected":false},"excerpt":{"rendered":"<p>[vc_row][vc_column][vc_column_text css=&#8221;&#8221;] \u00cen geologie, un strat lenticular este un corp de mineral, roc\u0103 sau depozit, de obicei mai gros \u00een centru \u0219i sub\u021bire la margini, asem\u0103n\u0103tor cu o lentil\u0103 convex\u0103 \u00een sec\u021biunea sa transversal\u0103. O lentil\u0103 poate face referire \u0219i la o forma\u021biune de form\u0103 neregulat\u0103, constituit\u0103 dintr-un depozit poros, sedimentar, permeabil, \u00eenconjurat de roc\u0103&hellip;<\/p>\n","protected":false},"author":16658,"featured_media":13131,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[1595,1969,1596,1443],"tags":[1622,1975,2453,2452],"class_list":["post-13116","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-geologie","category-geotehnica-ro","category-ingegneria-2-ro","category-articoli-geotecnica-ro","tag-geotehnica","tag-slope-ro","tag-stabilitatea-taluzurilor","tag-strat-lentiform","category-1595","category-1969","category-1596","category-1443","description-off"],"yoast_head":"<!-- This site is optimized with the Yoast SEO Premium plugin v25.0 (Yoast SEO v25.0) - https:\/\/yoast.com\/wordpress\/plugins\/seo\/ -->\n<title>Strat lenticular: cum s\u0103 \u00eel introduce\u021bi \u00een GeoStru Slope - 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