{"id":14635,"date":"2026-01-31T08:04:30","date_gmt":"2026-01-31T08:04:30","guid":{"rendered":"https:\/\/blog.geostru.eu\/la-frana-di-niscemi-analisi-del-rischio-idrogeologico-e-strumenti-avanzati-per-la-stabilita-dei-versanti\/"},"modified":"2026-09-20T09:26:12","modified_gmt":"2026-09-20T09:26:12","slug":"alunecarea-niscemi-risc-hidrogeologic-stabilitatea-versantilor","status":"publish","type":"post","link":"https:\/\/blog.geostru.eu\/ro\/alunecarea-niscemi-risc-hidrogeologic-stabilitatea-versantilor\/","title":{"rendered":"Alunecarea de teren de la Niscemi: analiza riscului hidrogeologic \u0219i instrumente avansate pentru stabilitatea versan\u021bilor"},"content":{"rendered":"<div class=\"wpb-content-wrapper\"><p>[vc_row][vc_column][vc_column_text css=&#8221;.vc_custom_1770050812622{background-color: #a3a3a3 !important;}&#8221;]<\/p>\n<div style=\"max-width: 1200px;margin: 0 auto\">\n<div style=\"border-radius: 20px;padding: 28px 28px 22px;color: #fff\">\n<div style=\"flex-wrap: wrap;gap: 14px;align-items: center;justify-content: space-between\">\n<div style=\"min-width: 260px;flex: 1\">\n<div style=\"font-size: 12px;letter-spacing: .08em;text-transform: uppercase;margin-bottom: 10px\">Studiu de caz \u2022 Instabilitate hidrogeologic\u0103<\/div>\n<h1 style=\"margin: 0 0 10px 0;font-size: 34px;line-height: 1.15;font-weight: 800\">Alunecarea de teren de la Niscemi: de la riscul cartografiat la modelarea 3D \u0219i analizele de stabilitate<\/h1>\n<p style=\"margin: 0;font-size: 16px;line-height: 1.6\">O abordare integrat\u0103: GeoRisk pentru hazard, GeoStru Maps pentru reconstruc\u021bia tridimensional\u0103, Slope (LEM+DEM) pentru stabilitatea 2D\/3D \u0219i Debris Flow pentru fenomenele rapide.<\/p>\n<\/div>\n<\/div>\n<\/div>\n<\/div>\n<p>[\/vc_column_text][\/vc_column][\/vc_row][vc_row css=&#8221;.vc_custom_170000000010{padding-top:40px !important;padding-bottom:10px !important;}&#8221;][vc_column width=&#8221;2\/3&#8243;][vc_column_text css=&#8221;&#8221;]<\/p>\n<div style=\"max-width: 900px\">\n<h2 style=\"margin: 0 0 10px 0;font-size: 26px;line-height: 1.25;font-weight: 800;color: #0f172a\">De ce conteaz\u0103 acest eveniment<\/h2>\n<p style=\"margin: 0 0 14px 0;font-size: 16px;line-height: 1.75;color: #334155\">Alunecarea de la Niscemi arat\u0103 c\u00e2t de mult gestionarea riscului necesit\u0103 instrumente capabile s\u0103 treac\u0103 de la <strong>cartografierea hazardului<\/strong> la <strong>modelarea 3D<\/strong> \u0219i la <strong>analizele geotehnice<\/strong> (stabilitatea versan\u021bilor \u0219i posibile evolu\u021bii rapide).<\/p>\n<div style=\"flex-wrap: wrap;gap: 10px;margin-top: 10px\"><span style=\"align-items: center;gap: 8px;padding: 8px 12px;border-radius: 999px;background: #f1f5f9;color: #0f172a;border: 1px solid #e2e8f0;font-size: 13px\">\ud83d\udccd Hazard<\/span><\/div>\n<div style=\"flex-wrap: wrap;gap: 10px;margin-top: 10px\"><span style=\"align-items: center;gap: 8px;padding: 8px 12px;border-radius: 999px;background: #f1f5f9;color: #0f172a;border: 1px solid #e2e8f0;font-size: 13px\">\ud83e\udded Modelare 3D<\/span><\/div>\n<div style=\"flex-wrap: wrap;gap: 10px;margin-top: 10px\"><span style=\"align-items: center;gap: 8px;padding: 8px 12px;border-radius: 999px;background: #f1f5f9;color: #0f172a;border: 1px solid #e2e8f0;font-size: 13px\">\ud83e\uddf1 Stabilitate 2D\/3D<\/span><\/div>\n<div style=\"flex-wrap: wrap;gap: 10px;margin-top: 10px\"><span style=\"align-items: center;gap: 8px;padding: 8px 12px;border-radius: 999px;background: #f1f5f9;color: #0f172a;border: 1px solid #e2e8f0;font-size: 13px\">\ud83c\udf0a Debris flow<\/span><\/div>\n<\/div>\n<p>[\/vc_column_text][\/vc_column][vc_column width=&#8221;1\/3&#8243;][vc_column_text]<\/p>\n<div style=\"border: 1px solid #e2e8f0;border-radius: 18px;padding: 16px;background: #ffffff\">\n<div style=\"font-size: 13px;color: #64748b;margin-bottom: 8px;text-transform: uppercase;letter-spacing: .08em\">Pe scurt<\/div>\n<div style=\"gap: 10px\">\n<div style=\"gap: 10px\">\n<div style=\"width: 38px;height: 38px;border-radius: 12px;background: #ecfeff;align-items: center;justify-content: center\">\ud83d\uddfa\ufe0f<\/div>\n<div>\n<p><strong style=\"color: #0f172a\">GeoRisk<\/strong><\/p>\n<div style=\"font-size: 13px;color: #475569\">cartografiaz\u0103 hazardul \u0219i riscul<\/div>\n<\/div>\n<\/div>\n<div style=\"gap: 10px\">\n<div style=\"width: 38px;height: 38px;border-radius: 12px;background: #f0fdf4;align-items: center;justify-content: center\">\ud83e\udde9<\/div>\n<div>\n<p><strong style=\"color: #0f172a\">GeoStru Maps<\/strong><\/p>\n<div style=\"font-size: 13px;color: #475569\">model 3D \u0219i re\u021bea<\/div>\n<\/div>\n<\/div>\n<div style=\"gap: 10px\">\n<div style=\"width: 38px;height: 38px;border-radius: 12px;background: #fff7ed;align-items: center;justify-content: center\">\u26f0\ufe0f<\/div>\n<div>\n<p><strong style=\"color: #0f172a\">Slope<\/strong><\/p>\n<div style=\"font-size: 13px;color: #475569\">LEM + DEM (deplas\u0103ri mari)<\/div>\n<\/div>\n<\/div>\n<div style=\"gap: 10px\">\n<div style=\"width: 38px;height: 38px;border-radius: 12px;background: #f5f3ff;align-items: center;justify-content: center\">\ud83c\udf27\ufe0f<\/div>\n<div>\n<p><strong style=\"color: #0f172a\">Debris Flow<\/strong><\/p>\n<div style=\"font-size: 13px;color: #475569\">analiza fenomenelor rapide<\/div>\n<\/div>\n<\/div>\n<\/div>\n<\/div>\n<p>[\/vc_column_text][\/vc_column][\/vc_row][vc_row][vc_column][vc_column_text]<\/p>\n<p>[\/vc_column_text][\/vc_column][\/vc_row][vc_row css=&#8221;.vc_custom_170000000020{padding-top:20px !important;padding-bottom:20px !important;}&#8221;][vc_column width=&#8221;1\/2&#8243;][vc_single_image image=&#8221;14601&#8243; img_size=&#8221;large&#8221; alignment=&#8221;center&#8221; css=&#8221;&#8221;][\/vc_column][vc_column width=&#8221;1\/2&#8243;][vc_column_text css=&#8221;&#8221;]<\/p>\n<h2 style=\"margin: 0 0 10px 0;font-size: 24px;line-height: 1.25;font-weight: 800;color: #0f172a\">1) Cartografierea hazardului \u0219i riscului cu GeoRisk<\/h2>\n<p style=\"margin: 0 0 12px 0;font-size: 16px;line-height: 1.75;color: #334155\">Cartografierea este primul pas: permite \u00eencadrarea evenimentului \u00een contextul teritorial \u0219i corelarea <strong>hazardului de alunecare<\/strong>, a <strong>riscului hidrogeologic<\/strong> \u0219i a <strong>hazardului seismic<\/strong>.<\/p>\n<div style=\"padding: 14px 14px;border-radius: 16px;background: #f8fafc;border: 1px solid #e2e8f0\">\n<ul style=\"margin: 0;padding-left: 18px;color: #334155;line-height: 1.7\">\n<li>citire rapid\u0103 a zonelor PAI (planul hidrogeologic)<\/li>\n<li>suprapunere cu zonele urbanizate<\/li>\n<li>sprijin pentru priorit\u0103\u021bi \u0219i planificare<\/li>\n<\/ul>\n<\/div>\n<div style=\"margin-top: 14px\">[vc_btn title=&#8221;Deschide GeoRisk&#8221; style=&#8221;custom&#8221; custom_background=&#8221;#0ea5e9&#8243; custom_text=&#8221;#061018&#8243; shape=&#8221;round&#8221; size=&#8221;md&#8221; link=&#8221;url:https%3A%2F%2Fgeoapp.geostru.eu%2Fapp%2Fgeorisk%2F|title:GeoRisk|target:_blank&#8221;]<\/div>\n<p>[\/vc_column_text][\/vc_column][\/vc_row][vc_row][vc_column][vc_column_text]<\/p>\n<p>[\/vc_column_text][\/vc_column][\/vc_row][vc_row css=&#8221;.vc_custom_170000000030{padding-top:20px !important;padding-bottom:20px !important;}&#8221;][vc_column width=&#8221;1\/2&#8243;][vc_column_text css=&#8221;&#8221;]<\/p>\n<h2 style=\"margin: 0 0 10px 0;font-size: 24px;line-height: 1.25;font-weight: 800;color: #0f172a\">2) De la teritoriu la 3D cu GeoStru Maps<\/h2>\n<p style=\"margin: 0 0 12px 0;font-size: 16px;line-height: 1.75;color: #334155\">Odat\u0103 definit\u0103 zona critic\u0103, reconstruc\u021bia tridimensional\u0103 permite descrierea corect\u0103 a abrupturilor, a ni\u0219elor de desprindere \u0219i a volumelor instabile. Re\u021beaua 3D triunghiular\u0103 devine o baz\u0103 solid\u0103 pentru analize. <strong style=\"color: #0f172a\">Re\u021bea 3D triunghiular\u0103 (TIN)<\/strong><\/p>\n<div style=\"gap: 10px\">\n<div style=\"border: 1px solid #e2e8f0;border-radius: 16px;padding: 14px;background: #ffffff\">\n<div style=\"font-size: 13px;color: #475569;margin-top: 4px\">re\u021bea creat\u0103 cu GeoStru Maps<\/div>\n<\/div>\n<\/div>\n<div style=\"margin-top: 14px\">[vc_btn title=&#8221;Deschide GeoStru Maps&#8221; style=&#8221;custom&#8221; custom_background=&#8221;#22c55e&#8221; custom_text=&#8221;#07110a&#8221; shape=&#8221;round&#8221; size=&#8221;md&#8221; link=&#8221;url:https%3A%2F%2Fmaps.geoapp.eu|title:GeoStru%20Maps|target:_blank&#8221;]<\/div>\n<p>[\/vc_column_text][\/vc_column][vc_column width=&#8221;1\/2&#8243;][vc_single_image image=&#8221;14597&#8243; img_size=&#8221;large&#8221; alignment=&#8221;center&#8221; css=&#8221;&#8221;][\/vc_column][\/vc_row][vc_row][vc_column][vc_column_text]<\/p>\n<p>[\/vc_column_text][\/vc_column][\/vc_row][vc_row css=&#8221;.vc_custom_170000000040{padding-top:20px !important;padding-bottom:20px !important;}&#8221;][vc_column width=&#8221;1\/2&#8243;][vc_single_image image=&#8221;14630&#8243; img_size=&#8221;large&#8221; alignment=&#8221;center&#8221; css=&#8221;&#8221;][\/vc_column][vc_column width=&#8221;1\/2&#8243;][vc_column_text css=&#8221;&#8221;]<\/p>\n<h2 style=\"margin: 0 0 10px 0;font-size: 24px;line-height: 1.25;font-weight: 800;color: #0f172a\">3) Stabilitate \u0219i deplas\u0103ri mari cu Slope (LEM + DEM)<\/h2>\n<p style=\"margin: 0 0 12px 0;font-size: 16px;line-height: 1.75;color: #334155\">Pentru cazuri complexe, pe l\u00e2ng\u0103 verific\u0103rile la <strong>echilibru limit\u0103 (LEM)<\/strong>, poate fi util studiul evolu\u021biei fenomenului cu o abordare cu <strong>elemente discrete (DEM)<\/strong>, potrivit\u0103 \u00een special pentru <strong>deplas\u0103ri mari<\/strong> \u0219i cinematisme rapide.<\/p>\n<div style=\"padding: 14px;border-radius: 16px;background: #0f172a;color: #e2e8f0\">\n<p><strong style=\"color: #ffffff\">De ce LEM + DEM este util \u00een cazuri ca Niscemi<\/strong><\/p>\n<ul style=\"margin: 10px 0 0 0;padding-left: 18px;line-height: 1.7\">\n<li>analiza global\u0103 a factorului de siguran\u021b\u0103<\/li>\n<li>simularea evolu\u021biilor cinematice \u0219i a deplas\u0103rilor<\/li>\n<li>sprijin pentru scenarii de urgen\u021b\u0103 \u0219i post-colaps<\/li>\n<\/ul>\n<\/div>\n<div style=\"margin-top: 14px\">[vc_btn title=&#8221;Mergi la Slope&#8221; style=&#8221;custom&#8221; custom_background=&#8221;#ffffff&#8221; custom_text=&#8221;#111827&#8243; shape=&#8221;round&#8221; size=&#8221;md&#8221; link=&#8221;url:https%3A%2F%2Fwww.geostru.eu%2Fro%2Fshop%2Fsoftware-ro%2Fgeotehnica-si-geologie%2Fstabilitatea-taluzurilor-slope%2F|title:Slope|target:_blank&#8221;]<\/div>\n<p>[\/vc_column_text][\/vc_column][\/vc_row][vc_row][vc_column][vc_column_text]<\/p>\n<p>[\/vc_column_text][\/vc_column][\/vc_row][vc_row css=&#8221;.vc_custom_170000000050{padding-top:10px !important;padding-bottom:10px !important;}&#8221;][vc_column width=&#8221;1\/2&#8243;][vc_column_text css=&#8221;&#8221;]<\/p>\n<h2 style=\"margin: 0 0 10px 0;font-size: 24px;line-height: 1.25;font-weight: 800;color: #0f172a\">4) C\u00e2nd alunecarea evolueaz\u0103 \u00een debris flow<\/h2>\n<p style=\"margin: 0 0 12px 0;font-size: 16px;line-height: 1.75;color: #334155\">\u00cen prezen\u021ba materialelor necoezive \u0219i a aportului de ap\u0103, mecanismul poate evolua \u00eentr-un <strong>debris flow<\/strong>. \u00cen aceste cazuri este important s\u0103 se estimeze propagarea posibil\u0103, volumele \u0219i zonele poten\u021bial afectate.<\/p>\n<div style=\"gap: 10px;flex-wrap: wrap\">\n<div style=\"flex: 1;min-width: 240px;border: 1px solid #e2e8f0;border-radius: 16px;padding: 14px;background: #ffffff\">\n<p><strong style=\"color: #0f172a\">Propagare<\/strong><\/p>\n<div style=\"font-size: 13px;color: #475569;margin-top: 4px\">trasarea traseelor \u0219i a zonelor de invazie<\/div>\n<\/div>\n<div style=\"flex: 1;min-width: 240px;border: 1px solid #e2e8f0;border-radius: 16px;padding: 14px;background: #ffffff\">\n<p><strong style=\"color: #0f172a\">Estim\u0103ri parametrice<\/strong><\/p>\n<div style=\"font-size: 13px;color: #475569;margin-top: 4px\">volume \u0219i scenarii de intensitate<\/div>\n<\/div>\n<\/div>\n<div style=\"margin-top: 14px\">[vc_btn title=&#8221;Deschide Debris Flow&#8221; style=&#8221;custom&#8221; custom_background=&#8221;#8b5cf6&#8243; custom_text=&#8221;#0b0720&#8243; shape=&#8221;round&#8221; size=&#8221;md&#8221; link=&#8221;url:https%3A%2F%2Fgeoapp.geostru.eu%2Fapp%2Fdebris-flow%2F|title:Debris%20Flow|target:_blank&#8221;]<\/div>\n<p>[\/vc_column_text][\/vc_column][vc_column width=&#8221;1\/2&#8243;][vc_single_image image=&#8221;14613&#8243; img_size=&#8221;large&#8221; alignment=&#8221;center&#8221; css=&#8221;&#8221;][\/vc_column][\/vc_row][vc_row][vc_column][vc_column_text]<\/p>\n<p>[\/vc_column_text][\/vc_column][\/vc_row][vc_row full_width=&#8221;stretch_row&#8221; css=&#8221;.vc_custom_170000000060{padding-top:28px !important;padding-bottom:28px !important;background-color:#0b1220 !important;}&#8221;][vc_column][vc_column_text css=&#8221;&#8221;]<\/p>\n<div style=\"max-width: 1200px;margin: 0 auto;color: #e2e8f0\">\n<h2 style=\"margin: 0 0 10px 0;font-size: 24px;line-height: 1.25;font-weight: 900;color: #ffffff\">De la analiz\u0103 la solu\u021bie: interven\u021bii posibile<\/h2>\n<p style=\"margin: 0 0 14px 0;font-size: 16px;line-height: 1.75\">Atenuarea porne\u0219te de la un principiu: <strong>reducerea cauzei declan\u0219atoare<\/strong>. Adesea controlul apelor (regularizare \u0219i drenaje) este decisiv, al\u0103turi de m\u0103suri provizorii pentru limitarea deplas\u0103rilor \u0219i de o reprofilare cu lucr\u0103ri definitive.<\/p>\n<div style=\"grid-template-columns: repeat(auto-fit,minmax(260px,1fr));gap: 12px;margin-top: 12px\">\n<div style=\"border-radius: 18px;padding: 14px\">\n<div style=\"font-weight: 800;color: #fff;margin-bottom: 6px\">1) Regularizarea apelor<\/div>\n<div style=\"font-size: 14px;line-height: 1.7\">Canaliz\u0103ri, drenaje ad\u00e2nci \u0219i\/sau pu\u021buri drenante \u00een aval de zona locuit\u0103 pentru reducerea presiunilor intersti\u021biale.<\/div>\n<\/div>\n<div style=\"border-radius: 18px;padding: 14px\">\n<div style=\"font-weight: 800;color: #fff;margin-bottom: 6px\">2) Limitare rapid\u0103<\/div>\n<div style=\"font-size: 14px;line-height: 1.7\">Buloane \u0219i tiran\u021bi \u201erapizi\u201d pentru limitarea deplas\u0103rilor imediate \u0219i cre\u0219terea siguran\u021bei \u00een faza de urgen\u021b\u0103.<\/div>\n<\/div>\n<div style=\"border-radius: 18px;padding: 14px\">\n<div style=\"font-weight: 800;color: #fff;margin-bottom: 6px\">3) Reprofilare \u0219i lucr\u0103ri definitive<\/div>\n<div style=\"font-size: 14px;line-height: 1.7\">Reprofilarea zonei instabile \u0219i lucr\u0103ri de tip structural pentru restabilirea echilibrului versantului.<\/div>\n<\/div>\n<\/div>\n<div style=\"gap: 10px;flex-wrap: wrap;margin-top: 16px\">[vc_btn title=&#8221;GeoRisk&#8221; style=&#8221;custom&#8221; custom_background=&#8221;#0ea5e9&#8243; custom_text=&#8221;#061018&#8243; shape=&#8221;round&#8221; size=&#8221;md&#8221; link=&#8221;url:https%3A%2F%2Fgeoapp.geostru.eu%2Fapp%2Fgeorisk%2F|title:GeoRisk|target:_blank&#8221;]<br \/>\n[vc_btn title=&#8221;GeoStru Maps&#8221; style=&#8221;custom&#8221; custom_background=&#8221;#22c55e&#8221; custom_text=&#8221;#07110a&#8221; shape=&#8221;round&#8221; size=&#8221;md&#8221; link=&#8221;url:https%3A%2F%2Fmaps.geoapp.eu|title:GeoStru%20Maps|target:_blank&#8221;]<br \/>\n[vc_btn title=&#8221;Slope&#8221; style=&#8221;custom&#8221; custom_background=&#8221;#ffffff&#8221; custom_text=&#8221;#111827&#8243; shape=&#8221;round&#8221; size=&#8221;md&#8221; link=&#8221;url:https%3A%2F%2Fwww.geostru.eu%2Fro%2Fshop%2Fsoftware-ro%2Fgeotehnica-si-geologie%2Fstabilitatea-taluzurilor-slope%2F|title:Slope|target:_blank&#8221;]<br \/>\n[vc_btn title=&#8221;Debris Flow&#8221; style=&#8221;custom&#8221; custom_background=&#8221;#8b5cf6&#8243; custom_text=&#8221;#0b0720&#8243; shape=&#8221;round&#8221; size=&#8221;md&#8221; link=&#8221;url:https%3A%2F%2Fgeoapp.geostru.eu%2Fapp%2Fdebris-flow%2F|title:Debris%20Flow|target:_blank&#8221;]<\/div>\n<\/div>\n<p>[\/vc_column_text][\/vc_column][\/vc_row]<\/p>\n<\/div>","protected":false},"excerpt":{"rendered":"<p>[vc_row][vc_column][vc_column_text css=&#8221;.vc_custom_1770050812622{background-color: #a3a3a3 !important;}&#8221;] Studiu de caz \u2022 Instabilitate hidrogeologic\u0103 Alunecarea de teren de la Niscemi: de la riscul cartografiat la modelarea 3D \u0219i analizele de stabilitate O abordare integrat\u0103: GeoRisk pentru hazard, GeoStru Maps pentru reconstruc\u021bia tridimensional\u0103, Slope (LEM+DEM) pentru stabilitatea 2D\/3D \u0219i Debris Flow pentru fenomenele rapide. [\/vc_column_text][\/vc_column][\/vc_row][vc_row css=&#8221;.vc_custom_170000000010{padding-top:40px !important;padding-bottom:10px !important;}&#8221;][vc_column width=&#8221;2\/3&#8243;][vc_column_text css=&#8221;&#8221;]&hellip;<\/p>\n","protected":false},"author":21284,"featured_media":14597,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[1595,1969,1596],"tags":[1879,2552,1608],"class_list":["post-14635","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-geologie","category-geotehnica-ro","category-ingegneria-2-ro","tag-geoapp","tag-niscemi","tag-slope","category-1595","category-1969","category-1596","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>Alunecarea de la Niscemi: risc \u0219i stabilitatea versan\u021bilor<\/title>\n<meta name=\"description\" content=\"Analiza tehnic\u0103 a alunec\u0103rii de la Niscemi: cartografierea riscului cu GeoRisk, modelare 3D cu GeoStru Maps, stabilitatea versan\u021bilor cu Slope (LEM+DEM) \u0219i debris flow.\" \/>\n<meta name=\"robots\" content=\"index, follow, max-snippet:-1, max-image-preview:large, max-video-preview:-1\" \/>\n<link rel=\"canonical\" href=\"https:\/\/blog.geostru.eu\/ro\/alunecarea-niscemi-risc-hidrogeologic-stabilitatea-versantilor\/\" \/>\n<meta property=\"og:locale\" content=\"ro_RO\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"Alunecarea de teren de la Niscemi: analiza riscului hidrogeologic \u0219i instrumente avansate pentru stabilitatea versan\u021bilor\" \/>\n<meta property=\"og:description\" content=\"Studiu de caz \u2022 Instabilitate hidrogeologic\u0103 Alunecarea de teren de la Niscemi: de la riscul cartografiat la modelarea 3D \u0219i analizele de stabilitate O\" \/>\n<meta property=\"og:url\" content=\"https:\/\/blog.geostru.eu\/ro\/alunecarea-niscemi-risc-hidrogeologic-stabilitatea-versantilor\/\" \/>\n<meta property=\"og:site_name\" content=\"Geostru Blog\" \/>\n<meta property=\"article:publisher\" content=\"https:\/\/www.facebook.com\/GeoStruSoftware\/\" \/>\n<meta property=\"article:published_time\" content=\"2026-01-31T08:04:30+00:00\" \/>\n<meta property=\"article:modified_time\" content=\"2026-09-20T09:26:12+00:00\" \/>\n<meta property=\"og:image\" content=\"https:\/\/blog.geostru.eu\/wp-content\/uploads\/sites\/9\/2026\/01\/articolo-niscemi-frana-geostru-1024x538.jpg\" \/>\n<meta name=\"author\" content=\"pressgeostru\" \/>\n<meta name=\"twitter:card\" content=\"summary_large_image\" \/>\n<meta name=\"twitter:label1\" content=\"Scris de\" \/>\n\t<meta name=\"twitter:data1\" content=\"pressgeostru\" \/>\n\t<meta name=\"twitter:label2\" content=\"Timp estimat pentru citire\" \/>\n\t<meta name=\"twitter:data2\" content=\"4 minute\" \/>\n<script type=\"application\/ld+json\" class=\"yoast-schema-graph\">{\"@context\":\"https:\/\/schema.org\",\"@graph\":[{\"@type\":\"Article\",\"@id\":\"https:\/\/blog.geostru.eu\/ro\/alunecarea-niscemi-risc-hidrogeologic-stabilitatea-versantilor\/#article\",\"isPartOf\":{\"@id\":\"https:\/\/blog.geostru.eu\/ro\/alunecarea-niscemi-risc-hidrogeologic-stabilitatea-versantilor\/\"},\"author\":{\"name\":\"pressgeostru\",\"@id\":\"https:\/\/blog.geostru.eu\/ro\/#\/schema\/person\/33348c6ea564fef14f828b68cfcdd2fb\"},\"headline\":\"Alunecarea de teren de la Niscemi: analiza riscului hidrogeologic \u0219i instrumente avansate pentru stabilitatea versan\u021bilor\",\"datePublished\":\"2026-01-31T08:04:30+00:00\",\"dateModified\":\"2026-09-20T09:26:12+00:00\",\"mainEntityOfPage\":{\"@id\":\"https:\/\/blog.geostru.eu\/ro\/alunecarea-niscemi-risc-hidrogeologic-stabilitatea-versantilor\/\"},\"wordCount\":1051,\"publisher\":{\"@id\":\"https:\/\/blog.geostru.eu\/ro\/#organization\"},\"image\":{\"@id\":\"https:\/\/blog.geostru.eu\/ro\/alunecarea-niscemi-risc-hidrogeologic-stabilitatea-versantilor\/#primaryimage\"},\"thumbnailUrl\":\"https:\/\/blog.geostru.eu\/wp-content\/uploads\/sites\/9\/2026\/01\/geostru-niscemi.png\",\"keywords\":[\"geoapp\",\"niscemi\",\"slope\"],\"articleSection\":[\"Geologie\",\"Geotehnic\u0103\",\"Inginerie\"],\"inLanguage\":\"ro-RO\"},{\"@type\":\"WebPage\",\"@id\":\"https:\/\/blog.geostru.eu\/ro\/alunecarea-niscemi-risc-hidrogeologic-stabilitatea-versantilor\/\",\"url\":\"https:\/\/blog.geostru.eu\/ro\/alunecarea-niscemi-risc-hidrogeologic-stabilitatea-versantilor\/\",\"name\":\"Alunecarea de la Niscemi: risc \u0219i stabilitatea versan\u021bilor\",\"isPartOf\":{\"@id\":\"https:\/\/blog.geostru.eu\/ro\/#website\"},\"primaryImageOfPage\":{\"@id\":\"https:\/\/blog.geostru.eu\/ro\/alunecarea-niscemi-risc-hidrogeologic-stabilitatea-versantilor\/#primaryimage\"},\"image\":{\"@id\":\"https:\/\/blog.geostru.eu\/ro\/alunecarea-niscemi-risc-hidrogeologic-stabilitatea-versantilor\/#primaryimage\"},\"thumbnailUrl\":\"https:\/\/blog.geostru.eu\/wp-content\/uploads\/sites\/9\/2026\/01\/geostru-niscemi.png\",\"datePublished\":\"2026-01-31T08:04:30+00:00\",\"dateModified\":\"2026-09-20T09:26:12+00:00\",\"description\":\"Analiza tehnic\u0103 a alunec\u0103rii de la Niscemi: cartografierea riscului cu GeoRisk, modelare 3D cu GeoStru Maps, stabilitatea versan\u021bilor cu Slope (LEM+DEM) \u0219i debris flow.\",\"breadcrumb\":{\"@id\":\"https:\/\/blog.geostru.eu\/ro\/alunecarea-niscemi-risc-hidrogeologic-stabilitatea-versantilor\/#breadcrumb\"},\"inLanguage\":\"ro-RO\",\"potentialAction\":[{\"@type\":\"ReadAction\",\"target\":[\"https:\/\/blog.geostru.eu\/ro\/alunecarea-niscemi-risc-hidrogeologic-stabilitatea-versantilor\/\"]}]},{\"@type\":\"ImageObject\",\"inLanguage\":\"ro-RO\",\"@id\":\"https:\/\/blog.geostru.eu\/ro\/alunecarea-niscemi-risc-hidrogeologic-stabilitatea-versantilor\/#primaryimage\",\"url\":\"https:\/\/blog.geostru.eu\/wp-content\/uploads\/sites\/9\/2026\/01\/geostru-niscemi.png\",\"contentUrl\":\"https:\/\/blog.geostru.eu\/wp-content\/uploads\/sites\/9\/2026\/01\/geostru-niscemi.png\",\"width\":1344,\"height\":768},{\"@type\":\"BreadcrumbList\",\"@id\":\"https:\/\/blog.geostru.eu\/ro\/alunecarea-niscemi-risc-hidrogeologic-stabilitatea-versantilor\/#breadcrumb\",\"itemListElement\":[{\"@type\":\"ListItem\",\"position\":1,\"name\":\"Home\",\"item\":\"https:\/\/blog.geostru.eu\/ro\/\"},{\"@type\":\"ListItem\",\"position\":2,\"name\":\"Alunecarea de teren de la Niscemi: analiza riscului hidrogeologic \u0219i instrumente avansate pentru stabilitatea versan\u021bilor\"}]},{\"@type\":\"WebSite\",\"@id\":\"https:\/\/blog.geostru.eu\/ro\/#website\",\"url\":\"https:\/\/blog.geostru.eu\/ro\/\",\"name\":\"Geostru Blog\",\"description\":\"GeoStru Blog\",\"publisher\":{\"@id\":\"https:\/\/blog.geostru.eu\/ro\/#organization\"},\"potentialAction\":[{\"@type\":\"SearchAction\",\"target\":{\"@type\":\"EntryPoint\",\"urlTemplate\":\"https:\/\/blog.geostru.eu\/ro\/?s={search_term_string}\"},\"query-input\":{\"@type\":\"PropertyValueSpecification\",\"valueRequired\":true,\"valueName\":\"search_term_string\"}}],\"inLanguage\":\"ro-RO\"},{\"@type\":\"Organization\",\"@id\":\"https:\/\/blog.geostru.eu\/ro\/#organization\",\"name\":\"Geostru\",\"url\":\"https:\/\/blog.geostru.eu\/ro\/\",\"logo\":{\"@type\":\"ImageObject\",\"inLanguage\":\"ro-RO\",\"@id\":\"https:\/\/blog.geostru.eu\/ro\/#\/schema\/logo\/image\/\",\"url\":\"https:\/\/blog.geostru.eu\/wp-content\/uploads\/sites\/9\/2020\/05\/geostru_website_logo_24.png\",\"contentUrl\":\"https:\/\/blog.geostru.eu\/wp-content\/uploads\/sites\/9\/2020\/05\/geostru_website_logo_24.png\",\"width\":75,\"height\":24,\"caption\":\"Geostru\"},\"image\":{\"@id\":\"https:\/\/blog.geostru.eu\/ro\/#\/schema\/logo\/image\/\"},\"sameAs\":[\"https:\/\/www.facebook.com\/GeoStruSoftware\/\",\"https:\/\/www.instagram.com\/geostru\/\",\"https:\/\/www.linkedin.com\/in\/geostru-software-146a3646\/\",\"https:\/\/youtube.com\/user\/geostru\"]},{\"@type\":\"Person\",\"@id\":\"https:\/\/blog.geostru.eu\/ro\/#\/schema\/person\/33348c6ea564fef14f828b68cfcdd2fb\",\"name\":\"pressgeostru\",\"image\":{\"@type\":\"ImageObject\",\"inLanguage\":\"ro-RO\",\"@id\":\"https:\/\/blog.geostru.eu\/ro\/#\/schema\/person\/image\/\",\"url\":\"https:\/\/secure.gravatar.com\/avatar\/c69ac407ada44c4ec423647d16016775?s=96&d=mm&r=g\",\"contentUrl\":\"https:\/\/secure.gravatar.com\/avatar\/c69ac407ada44c4ec423647d16016775?s=96&d=mm&r=g\",\"caption\":\"pressgeostru\"},\"url\":\"https:\/\/blog.geostru.eu\/ro\/author\/pressgeostru\/\"}]}<\/script>\n<!-- \/ Yoast SEO Premium plugin. -->","yoast_head_json":{"title":"Alunecarea de la Niscemi: risc \u0219i stabilitatea versan\u021bilor","description":"Analiza tehnic\u0103 a alunec\u0103rii de la Niscemi: cartografierea riscului cu GeoRisk, modelare 3D cu GeoStru Maps, stabilitatea versan\u021bilor cu Slope (LEM+DEM) \u0219i debris flow.","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":"https:\/\/blog.geostru.eu\/ro\/alunecarea-niscemi-risc-hidrogeologic-stabilitatea-versantilor\/","og_locale":"ro_RO","og_type":"article","og_title":"Alunecarea de teren de la Niscemi: analiza riscului hidrogeologic \u0219i instrumente avansate pentru stabilitatea versan\u021bilor","og_description":"Studiu de caz \u2022 Instabilitate hidrogeologic\u0103 Alunecarea de teren de la Niscemi: de la riscul cartografiat la modelarea 3D \u0219i analizele de stabilitate O","og_url":"https:\/\/blog.geostru.eu\/ro\/alunecarea-niscemi-risc-hidrogeologic-stabilitatea-versantilor\/","og_site_name":"Geostru Blog","article_publisher":"https:\/\/www.facebook.com\/GeoStruSoftware\/","article_published_time":"2026-01-31T08:04:30+00:00","article_modified_time":"2026-09-20T09:26:12+00:00","og_image":[{"url":"https:\/\/blog.geostru.eu\/wp-content\/uploads\/sites\/9\/2026\/01\/articolo-niscemi-frana-geostru-1024x538.jpg","type":"","width":"","height":""}],"author":"pressgeostru","twitter_card":"summary_large_image","twitter_misc":{"Scris de":"pressgeostru","Timp estimat pentru citire":"4 minute"},"schema":{"@context":"https:\/\/schema.org","@graph":[{"@type":"Article","@id":"https:\/\/blog.geostru.eu\/ro\/alunecarea-niscemi-risc-hidrogeologic-stabilitatea-versantilor\/#article","isPartOf":{"@id":"https:\/\/blog.geostru.eu\/ro\/alunecarea-niscemi-risc-hidrogeologic-stabilitatea-versantilor\/"},"author":{"name":"pressgeostru","@id":"https:\/\/blog.geostru.eu\/ro\/#\/schema\/person\/33348c6ea564fef14f828b68cfcdd2fb"},"headline":"Alunecarea de teren de la Niscemi: analiza riscului hidrogeologic \u0219i instrumente avansate pentru stabilitatea versan\u021bilor","datePublished":"2026-01-31T08:04:30+00:00","dateModified":"2026-09-20T09:26:12+00:00","mainEntityOfPage":{"@id":"https:\/\/blog.geostru.eu\/ro\/alunecarea-niscemi-risc-hidrogeologic-stabilitatea-versantilor\/"},"wordCount":1051,"publisher":{"@id":"https:\/\/blog.geostru.eu\/ro\/#organization"},"image":{"@id":"https:\/\/blog.geostru.eu\/ro\/alunecarea-niscemi-risc-hidrogeologic-stabilitatea-versantilor\/#primaryimage"},"thumbnailUrl":"https:\/\/blog.geostru.eu\/wp-content\/uploads\/sites\/9\/2026\/01\/geostru-niscemi.png","keywords":["geoapp","niscemi","slope"],"articleSection":["Geologie","Geotehnic\u0103","Inginerie"],"inLanguage":"ro-RO"},{"@type":"WebPage","@id":"https:\/\/blog.geostru.eu\/ro\/alunecarea-niscemi-risc-hidrogeologic-stabilitatea-versantilor\/","url":"https:\/\/blog.geostru.eu\/ro\/alunecarea-niscemi-risc-hidrogeologic-stabilitatea-versantilor\/","name":"Alunecarea de la Niscemi: risc \u0219i stabilitatea versan\u021bilor","isPartOf":{"@id":"https:\/\/blog.geostru.eu\/ro\/#website"},"primaryImageOfPage":{"@id":"https:\/\/blog.geostru.eu\/ro\/alunecarea-niscemi-risc-hidrogeologic-stabilitatea-versantilor\/#primaryimage"},"image":{"@id":"https:\/\/blog.geostru.eu\/ro\/alunecarea-niscemi-risc-hidrogeologic-stabilitatea-versantilor\/#primaryimage"},"thumbnailUrl":"https:\/\/blog.geostru.eu\/wp-content\/uploads\/sites\/9\/2026\/01\/geostru-niscemi.png","datePublished":"2026-01-31T08:04:30+00:00","dateModified":"2026-09-20T09:26:12+00:00","description":"Analiza tehnic\u0103 a alunec\u0103rii de la Niscemi: cartografierea riscului cu GeoRisk, modelare 3D cu GeoStru Maps, stabilitatea versan\u021bilor cu Slope (LEM+DEM) \u0219i debris flow.","breadcrumb":{"@id":"https:\/\/blog.geostru.eu\/ro\/alunecarea-niscemi-risc-hidrogeologic-stabilitatea-versantilor\/#breadcrumb"},"inLanguage":"ro-RO","potentialAction":[{"@type":"ReadAction","target":["https:\/\/blog.geostru.eu\/ro\/alunecarea-niscemi-risc-hidrogeologic-stabilitatea-versantilor\/"]}]},{"@type":"ImageObject","inLanguage":"ro-RO","@id":"https:\/\/blog.geostru.eu\/ro\/alunecarea-niscemi-risc-hidrogeologic-stabilitatea-versantilor\/#primaryimage","url":"https:\/\/blog.geostru.eu\/wp-content\/uploads\/sites\/9\/2026\/01\/geostru-niscemi.png","contentUrl":"https:\/\/blog.geostru.eu\/wp-content\/uploads\/sites\/9\/2026\/01\/geostru-niscemi.png","width":1344,"height":768},{"@type":"BreadcrumbList","@id":"https:\/\/blog.geostru.eu\/ro\/alunecarea-niscemi-risc-hidrogeologic-stabilitatea-versantilor\/#breadcrumb","itemListElement":[{"@type":"ListItem","position":1,"name":"Home","item":"https:\/\/blog.geostru.eu\/ro\/"},{"@type":"ListItem","position":2,"name":"Alunecarea de teren de la Niscemi: analiza riscului hidrogeologic \u0219i instrumente avansate pentru stabilitatea versan\u021bilor"}]},{"@type":"WebSite","@id":"https:\/\/blog.geostru.eu\/ro\/#website","url":"https:\/\/blog.geostru.eu\/ro\/","name":"Geostru Blog","description":"GeoStru Blog","publisher":{"@id":"https:\/\/blog.geostru.eu\/ro\/#organization"},"potentialAction":[{"@type":"SearchAction","target":{"@type":"EntryPoint","urlTemplate":"https:\/\/blog.geostru.eu\/ro\/?s={search_term_string}"},"query-input":{"@type":"PropertyValueSpecification","valueRequired":true,"valueName":"search_term_string"}}],"inLanguage":"ro-RO"},{"@type":"Organization","@id":"https:\/\/blog.geostru.eu\/ro\/#organization","name":"Geostru","url":"https:\/\/blog.geostru.eu\/ro\/","logo":{"@type":"ImageObject","inLanguage":"ro-RO","@id":"https:\/\/blog.geostru.eu\/ro\/#\/schema\/logo\/image\/","url":"https:\/\/blog.geostru.eu\/wp-content\/uploads\/sites\/9\/2020\/05\/geostru_website_logo_24.png","contentUrl":"https:\/\/blog.geostru.eu\/wp-content\/uploads\/sites\/9\/2020\/05\/geostru_website_logo_24.png","width":75,"height":24,"caption":"Geostru"},"image":{"@id":"https:\/\/blog.geostru.eu\/ro\/#\/schema\/logo\/image\/"},"sameAs":["https:\/\/www.facebook.com\/GeoStruSoftware\/","https:\/\/www.instagram.com\/geostru\/","https:\/\/www.linkedin.com\/in\/geostru-software-146a3646\/","https:\/\/youtube.com\/user\/geostru"]},{"@type":"Person","@id":"https:\/\/blog.geostru.eu\/ro\/#\/schema\/person\/33348c6ea564fef14f828b68cfcdd2fb","name":"pressgeostru","image":{"@type":"ImageObject","inLanguage":"ro-RO","@id":"https:\/\/blog.geostru.eu\/ro\/#\/schema\/person\/image\/","url":"https:\/\/secure.gravatar.com\/avatar\/c69ac407ada44c4ec423647d16016775?s=96&d=mm&r=g","contentUrl":"https:\/\/secure.gravatar.com\/avatar\/c69ac407ada44c4ec423647d16016775?s=96&d=mm&r=g","caption":"pressgeostru"},"url":"https:\/\/blog.geostru.eu\/ro\/author\/pressgeostru\/"}]}},"_links":{"self":[{"href":"https:\/\/blog.geostru.eu\/ro\/wp-json\/wp\/v2\/posts\/14635"}],"collection":[{"href":"https:\/\/blog.geostru.eu\/ro\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/blog.geostru.eu\/ro\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/blog.geostru.eu\/ro\/wp-json\/wp\/v2\/users\/21284"}],"replies":[{"embeddable":true,"href":"https:\/\/blog.geostru.eu\/ro\/wp-json\/wp\/v2\/comments?post=14635"}],"version-history":[{"count":3,"href":"https:\/\/blog.geostru.eu\/ro\/wp-json\/wp\/v2\/posts\/14635\/revisions"}],"predecessor-version":[{"id":15407,"href":"https:\/\/blog.geostru.eu\/ro\/wp-json\/wp\/v2\/posts\/14635\/revisions\/15407"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/blog.geostru.eu\/ro\/wp-json\/wp\/v2\/media\/14597"}],"wp:attachment":[{"href":"https:\/\/blog.geostru.eu\/ro\/wp-json\/wp\/v2\/media?parent=14635"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/blog.geostru.eu\/ro\/wp-json\/wp\/v2\/categories?post=14635"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/blog.geostru.eu\/ro\/wp-json\/wp\/v2\/tags?post=14635"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}