{"id":1602,"date":"2020-09-04T16:36:55","date_gmt":"2020-09-04T16:36:55","guid":{"rendered":"https:\/\/blog.geostru.eu\/?p=1602"},"modified":"2022-03-16T11:46:33","modified_gmt":"2022-03-16T11:46:33","slug":"stalpii-pamantului","status":"publish","type":"post","link":"https:\/\/blog.geostru.eu\/ro\/stalpii-pamantului\/","title":{"rendered":"St\u00e2lpii P\u0103m\u00e2ntului"},"content":{"rendered":"<h1><span style=\"color: #000080;font-size: 24pt\"><strong>St\u00e2lpii P\u0103m\u00e2ntului<\/strong><\/span><\/h1>\n<h1>\n<div class=\"hr-thin\"><\/div>\n<\/h1>\n<h2><span style=\"font-size: 18pt\"><strong>Procese de percolare<\/strong><\/span><\/h2>\n<p style=\"text-align: justify\"><span style=\"font-size: 14pt\">Datorit\u0103 precipita\u021biilor, versan\u021bii pot fi supu\u0219i unor procese importante <strong>de percolare<\/strong>. Acestea includ, de exemplu:<\/span><\/p>\n<ul style=\"text-align: justify\">\n<li><span style=\"font-size: 14pt\">eroziune cauzat\u0103 de ploaile abundente <em>(<\/em><em>Splash erosion<\/em>);<\/span><\/li>\n<li><span style=\"font-size: 14pt\">eroziunea zonei (<em>Sheet erosion<\/em><em>);<\/em><\/span><\/li>\n<li><span style=\"font-size: 14pt\">eroziunea \u00een rigole (rill erosion);<\/span><\/li>\n<li><span style=\"font-size: 14pt\">eroziune \u00een f\u0103ga\u0219e (gully erosion)<\/span><\/li>\n<\/ul>\n<p style=\"text-align: justify\"><span style=\"font-size: 14pt\">Aceste procese sunt responsabile pentru \u00eendep\u0103rtarea \u0219i \u00eendep\u0103rtarea unor cantit\u0103\u021bi mari de sedimente, ceea ce duce la definirea fenomenului de denudare a versan\u021bilor (<strong>Fig.1<\/strong>).<\/span><\/p>\n<div id=\"attachment_1571\" style=\"width: 1086px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1571\" class=\"wp-image-1573 \" title=\"Denudamento dei versanti\" src=\"https:\/\/blog.geostru.eu\/wp-content\/uploads\/sites\/9\/2020\/08\/1-1-300x155.png\" alt=\"\" width=\"1076\" height=\"556\" srcset=\"https:\/\/blog.geostru.eu\/wp-content\/uploads\/sites\/9\/2020\/08\/1-1-300x155.png 300w, https:\/\/blog.geostru.eu\/wp-content\/uploads\/sites\/9\/2020\/08\/1-1-1024x528.png 1024w, https:\/\/blog.geostru.eu\/wp-content\/uploads\/sites\/9\/2020\/08\/1-1-768x396.png 768w, https:\/\/blog.geostru.eu\/wp-content\/uploads\/sites\/9\/2020\/08\/1-1-1536x793.png 1536w, https:\/\/blog.geostru.eu\/wp-content\/uploads\/sites\/9\/2020\/08\/1-1.png 1595w\" sizes=\"(max-width: 1076px) 100vw, 1076px\" \/><p id=\"caption-attachment-1571\" class=\"wp-caption-text\"><span style=\"font-size: 10pt\"><em><strong>Figura 1<\/strong> \u2013 Denudarea versan\u021bilor. Formele de eroziune prezente \u00een Belvedere M.mo (CS). <\/em><\/span><\/p><\/div>\n<p style=\"text-align: justify\"><span style=\"font-size: 14pt\">Printre factorii care se adaug\u0103 proceselor, care condi\u021bioneaz\u0103 cantitatea de alunec\u0103ri si forma de modelare a versan\u021bilor, sunt:<\/span><\/p>\n<ul>\n<li style=\"text-align: justify\"><span style=\"font-size: 14pt\">climatici (intensitatea \u0219i durata precipita\u021biilor, temperatura);<\/span><\/li>\n<li style=\"text-align: justify\"><span style=\"font-size: 14pt\">deplasarea apelor curg\u0103toare (laminar\u0103 sau turbulent\u0103);<\/span><\/li>\n<li style=\"text-align: justify\"><span style=\"font-size: 14pt\">caracteristicile solului\/terenului\/rocii de la suprafa\u021b\u0103 (litologie; dimensiunea granulometric\u0103, coeziunea, gradul de cimentare; permeabilitatea);<\/span><\/li>\n<li style=\"text-align: justify\"><span style=\"font-size: 14pt\">topografia \u0219i morfologia versan\u021bilor (declivitatea \u0219i lungimea versan\u021bilor);<\/span><\/li>\n<li style=\"text-align: justify\"><span style=\"font-size: 14pt\">acoperirea vegetal\u0103 (densitate \u0219i tip);<\/span><\/li>\n<li style=\"text-align: justify\"><span style=\"font-size: 14pt\">ac\u021biunea uman\u0103 (iriga\u021bii, defri\u0219\u0103ri)<\/span><\/li>\n<\/ul>\n<h2><span style=\"font-size: 18pt\"><strong>Piramidele sau st\u00e2lpii p\u0103m\u00e2ntului<\/strong><\/span><\/h2>\n<p style=\"text-align: justify\"><span style=\"font-size: 14pt\">Printre formele de eroziune legate de apele de scurgere sunt <strong>&#8222;Piramidele P\u0103m\u00e2ntului&#8221; <\/strong>sau <strong>&#8222;St\u00e2lpii P\u0103m\u00e2ntului&#8221;<\/strong><em>(<\/em><em> Earth pillars<\/em>). Acestea sunt constituite din roci detritice formate din \u00a0blocuri litoide scufundate \u00eentr-o matrice de sedimente mai fine. Prin urmare, aceste forma\u021biuni sunt contituite dintr-o vast\u0103 eterogenitate granulometric\u0103 \u0219i litologic\u0103, adic\u0103 pietri\u0219, nisip, n\u0103mol \u0219i argil\u0103 (Fig.2).<\/span><\/p>\n<div id=\"attachment_1557\" style=\"width: 1180px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1557\" class=\"wp-image-1559 \" src=\"https:\/\/blog.geostru.eu\/wp-content\/uploads\/sites\/9\/2020\/08\/2-300x170.png\" alt=\"\" width=\"1170\" height=\"662\" srcset=\"https:\/\/blog.geostru.eu\/wp-content\/uploads\/sites\/9\/2020\/08\/2-300x170.png 300w, https:\/\/blog.geostru.eu\/wp-content\/uploads\/sites\/9\/2020\/08\/2-768x436.png 768w\" sizes=\"(max-width: 1170px) 100vw, 1170px\" \/><p id=\"caption-attachment-1557\" class=\"wp-caption-text\"><em><span style=\"font-size: 10pt\"><strong>Figura 2<\/strong> \u2013 St\u00e2lpii p\u0103m\u00e2ntului Belvedere M.mo (CS). Observa\u021bi eterogenitatea granulometric\u0103.<\/span><\/em><\/p><\/div>\n<h2 style=\"text-align: justify\"><span style=\"font-size: 18pt\"><strong><em>Cum se formeaz\u0103?<\/em><\/strong><\/span><\/h2>\n<p style=\"text-align: justify\"><span style=\"font-size: 14pt\">Atunci c\u00e2nd apele curg \u00een p\u0103m\u00e2nt, \u00eenc\u0103 necanalizate \u00een rigole (r\u00e2ule\u021be)<em>,<\/em> erodeaz\u0103 cu u\u0219urin\u021b\u0103 sedimentul fin, f\u0103r\u0103 a aduce vreun efect special blocurilor litoide care sunt competente \u0219i rezistente la eroziune. Aceste blocuri sunt capabile s\u0103 protejeze sedimentul mai fin de dedesubt (care ac\u021bioneaz\u0103 ca o umbrel\u0103 real\u0103), timp \u00een care cel din jur este sp\u0103lat \u0219i erodat. Prelungirea \u0219i repetarea proceselor de scurgere va duce \u00een cele din urm\u0103 la formarea a numero\u0219i &#8222;piloni\/st\u00e2lpi&#8221; de material fin la cap\u0103tul superior al c\u0103rora vor exista pietricele \u0219i blocuri care alc\u0103tuiesc calota (<em>cap-stone<\/em>) (<strong>Fig.3<\/strong>).<\/span><\/p>\n<div id=\"attachment_1562\" style=\"width: 1101px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1562\" class=\" wp-image-1564\" src=\"https:\/\/blog.geostru.eu\/wp-content\/uploads\/sites\/9\/2020\/08\/3-300x200.png\" alt=\"\" width=\"1091\" height=\"727\" srcset=\"https:\/\/blog.geostru.eu\/wp-content\/uploads\/sites\/9\/2020\/08\/3-300x200.png 300w, https:\/\/blog.geostru.eu\/wp-content\/uploads\/sites\/9\/2020\/08\/3-1024x682.png 1024w, https:\/\/blog.geostru.eu\/wp-content\/uploads\/sites\/9\/2020\/08\/3-768x512.png 768w, https:\/\/blog.geostru.eu\/wp-content\/uploads\/sites\/9\/2020\/08\/3.png 1388w\" sizes=\"(max-width: 1091px) 100vw, 1091px\" \/><p id=\"caption-attachment-1562\" class=\"wp-caption-text\"><span style=\"font-size: 12pt\"><em><strong>Figura 3<\/strong> \u2013 \u2013 Eroziune cu &#8222;Organ Pipe&#8221; \u00een loc. St Litterata, Belvedere M.mo (CS). Observa\u021bi modul \u00een care capacul-piatr\u0103 pe partea de sus ac\u021bioneaz\u0103 ca o protec\u021bie.<\/em><\/span><\/p><\/div>\n<h2><span style=\"font-size: 18pt\">Alunecare\u00a0<\/span><\/h2>\n<p style=\"text-align: justify\"><span style=\"font-size: 14pt\">Aceste forme de eroziune sunt efemere, deoarece \u00a0\u201dpiciorul\u201d de baz\u0103 poate fi \u00eendep\u0103rtat de ap\u0103: matricea fin\u0103 care sus\u021bine blocurile grosiere este \u00eendep\u0103rtat\u0103 treptat, astfel \u00eenc\u00e2t piramidele\/st\u00e2lpii, sub\u021bia\u021bi treptat, nu vor mai putea sus\u021bine capacul protectoar de deasupra \u0219i, \u00een consecin\u021b\u0103, se vor pr\u0103bu\u0219i \u00a0\u00a0(<strong>Fig.4<\/strong>).<\/span><\/p>\n<div id=\"attachment_1576\" style=\"width: 1326px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-1576\" class=\" wp-image-1578\" src=\"https:\/\/blog.geostru.eu\/wp-content\/uploads\/sites\/9\/2020\/08\/4-1-300x106.png\" alt=\"\" width=\"1316\" height=\"465\" srcset=\"https:\/\/blog.geostru.eu\/wp-content\/uploads\/sites\/9\/2020\/08\/4-1-300x106.png 300w, https:\/\/blog.geostru.eu\/wp-content\/uploads\/sites\/9\/2020\/08\/4-1-1024x361.png 1024w, https:\/\/blog.geostru.eu\/wp-content\/uploads\/sites\/9\/2020\/08\/4-1-768x270.png 768w, https:\/\/blog.geostru.eu\/wp-content\/uploads\/sites\/9\/2020\/08\/4-1-1536x541.png 1536w\" sizes=\"(max-width: 1316px) 100vw, 1316px\" \/><p id=\"caption-attachment-1576\" class=\"wp-caption-text\"><span style=\"font-size: 12pt\"><em><strong>Figura 4<\/strong> \u2013 Alunec\u0103ri de teren acoperite cu vegeta\u021bie de-a lungul teraselor puternic gravate cu conglomerat de nisip, \u00een apropiere de Belvedere M.mo (CS).<\/em><\/span><\/p><\/div>\n<h2><span style=\"font-size: 18pt\">Aspecte geotehnice<\/span><\/h2>\n<p style=\"text-align: justify\"><span style=\"font-size: 14pt\">Instabilitatea care apare \u00een aceste depozite este puternic condi\u021bionat\u0103 de gradul de abrupere a versan\u021bilor \u0219i de caracteristicile fizico-mecanice ale litotipilor, \u00een plus, un alt factor care contribuie la influen\u021barea gradului de instabilitate este permeabilitatea solurilor. <\/span><br \/>\n<span style=\"font-size: 14pt\">\u00cen special, av\u00e2nd \u00een vedere alternan\u021ba orizonturilor caracterizate de componente granulometrice foarte variabile (a se vedea figura 2), se consider\u0103 necesar s\u0103 se eviden\u021bieze diferitele comportamente fizico-mecanice-hidrogeologice pe care aceste orizonturi le asum\u0103 \u00een generarea formelor specifice de eroziune descrise anterior.<\/span><br \/>\n<span style=\"font-size: 14pt\">Orizonturile litologice caracterizate prin componente granulometrice predominant fine (\u00een cazul studiat: nisipuri fine, silturi \u0219i, rareori, argile) \u00ee\u0219i asum\u0103 o permeabilitate sc\u0103zut\u0103 datorit\u0103 porozit\u0103\u021bii primare, \u00een principal datorit\u0103 dimensiunii reduse a spa\u021biilor intergranulare. Aceast\u0103 caracteristic\u0103, \u00eempreun\u0103 cu aclivitatea ridicat\u0103, face extrem de dificil\u0103 infiltrarea apei din precipita\u021bii, favoriz\u00e2nd \u00een schimb scurgerea, duc\u00e2nd la \u00eendep\u0103rtarea materialului fin nelitificat. De asemenea, trebuie remarcat faptul c\u0103, contribu\u021bia redus\u0103 a apelor de infiltrare genereaz\u0103, \u00een straturile mai superficiale nelitificate, o cre\u0219tere a plasticit\u0103\u021bii \u0219i, \u00een cazul fenomenelor de precipita\u021bii persistente, o cre\u0219tere a gradului de lichiditate care duce la declan\u0219area fenemenelor de instabilitate.<\/span><br \/>\n<span style=\"font-size: 14pt\">Orizonturile nelitificate sau slab cimentate, caracterizate prin componente granulometrice medii-grosiere (nisipuri, pietri\u0219 \u0219i pietricele), au o permeabilitate medie-ridicat\u0103 datorit\u0103 porozit\u0103\u021bii. Circula\u021bia apei subterane, compatibil\u0103 cu gradul de \u00eenclina\u021bie, are loc \u00een principal \u00een interconexiunile largi dintre granule. Aceste litotipuri presupun o rezisten\u021b\u0103 la rupere medie-mare, garantat\u0103 de valori ale unghiului de frecare cu mult peste 35-38 de grade.<\/span><br \/>\n<span style=\"font-size: 14pt\">Orizonturile litoide (gresii \u0219i conglomerate) iau un comportament complet diferit, at\u00e2t permeabilitatea, c\u00e2t \u0219i stabilitatea frontului depind de gradul de fracturare, geometria fracturilor \u0219i cimentarea rocii. <\/span><br \/>\n<span style=\"font-size: 14pt\">O evaluare atent\u0103 a gradului de stabilitate al acestor versan\u021bi depinde \u00een principal de gradul de cunoa\u0219tere a geometriei orizonturilor litologice prezente \u0219i, mai presus de toate, de caracteristicile lor fizico-mecanice.<\/span><\/p>\n<h3><\/h3>\n<blockquote>\n<h2>Software-ul e Geoapp<\/h2>\n<\/blockquote>\n<p style=\"text-align: justify\"><span style=\"font-size: 14pt\">\u00cen aceste scenarii, este esen\u021bial s\u0103 se evalueze cu precizie gradul de stabilitate al versantului prin intermediul unor programe software specifice, cum ar fi:<\/span><\/p>\n<ul>\n<li style=\"list-style-type: none\">\n<ul style=\"list-style-type: square\">\n<li>\n<p style=\"text-align: justify\"><span style=\"font-size: 14pt\"><strong>Slope<\/strong> &#8211; <a href=\"https:\/\/www.geostru.eu\/ro\/shop\/software-ro\/software-geologia-ro-2\/stabilitatea-taluzurilor-slope\/\" target=\"_blank\" rel=\"noopener noreferrer\">Stabilitatea taluzurilor<\/a>: software care permite calculul stabilit\u0103\u021bii taluzurilor \u00een teren af\u00e2nat sau st\u00e2ncos cu metodele tradi\u021bionale ale geotehnicii (Echilibrul Limit\u0103), \u0219i metoda Elementelor Discrete cu care se poate calcula deplasarea taluzului \u0219i se poate examina ruptura progresiv\u0103. \u00cen condi\u021bii seismice, efectueaz\u0103 at\u00e2t analize statice, c\u00e2t \u0219i dinamice.<\/span><\/p>\n<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p style=\"text-align: justify\"><span style=\"font-size: 14pt\">Veridicitatea datelor ob\u021binute prin programul de stabilitate depinde \u00een mod substan\u021bial de acurate\u021bea parametrilor caracteristici terenului studiat. Prin urmare, pentru a face fa\u021b\u0103 unei verific\u0103ri precise a stabilit\u0103\u021bii, este necesar s\u0103 se efectueze teste geotehnice pentru a cunoa\u0219te caracteristicile fizico-mecanice ale litotipurilor afectate.<\/span><\/p>\n<p style=\"text-align: justify\"><span style=\"font-size: 14pt\">Printre aplica\u021biile disponibile pe pagina web \u00a0<a href=\"https:\/\/geoapp.geostru.eu\/\">Geoapp<\/a> \u00a0(serviciu disponibil pentru efectuarea calculelor online) care pot fi utilizate pentru subiectul de mai sus, exist\u0103, de exemplu:<\/span><\/p>\n<ul>\n<li style=\"list-style-type: none\">\n<ul style=\"list-style-type: square\">\n<li><span style=\"font-size: 14pt\"><a href=\"https:\/\/geoapp.geostru.eu\/app\/scivolamento-lungo-un-piano\/\">Alunec\u0103ri de-a lungul unui plan<\/a>;<\/span><\/li>\n<li><span style=\"font-size: 14pt\"><a href=\"https:\/\/geoapp.geostru.eu\/app\/chiodatura-barre-passive\/\" target=\"_blank\" rel=\"noopener noreferrer\">Chiodature barre passive<\/a>;<\/span><\/li>\n<li><span style=\"font-size: 14pt\"><a href=\"https:\/\/geoapp.geostru.eu\/app\/tiranti\/\" target=\"_blank\" rel=\"noopener noreferrer\">Tiranti<\/a>;<\/span><\/li>\n<li><span style=\"font-size: 14pt\"><a href=\"https:\/\/geoapp.geostru.eu\/app\/sistemi-reti-ancorate\/\" target=\"_blank\" rel=\"noopener noreferrer\">Sistemi reti ancorate<\/a>;<\/span><\/li>\n<li><span style=\"font-size: 14pt\"><a href=\"https:\/\/geoapp.geostru.eu\/app\/analisi-stabilita-dei-pendii\/\">Analiza stabilit\u0103\u021bii suprafe\u021bei plane<\/a>;<\/span><\/li>\n<li><span style=\"font-size: 14pt\"><a href=\"https:\/\/geoapp.geostru.eu\/app\/classificazione-delle-terre\/\">Clasificarea terenurilor SMC<\/a>.<\/span><\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<h3><span style=\"font-size: 14pt\">Bibliografie \u0219i Mul\u021bumiri<\/span><\/h3>\n<p>Fairbridge R.W. (1968) &#8211; Earth pillars or pyramids. In: Geomorphology. Encyclopedia of Earth Science. Springer, Berlin, Heidelberg.<\/p>\n<p>Guti\u00e9rrez F., Guti\u00e9rrez M., Mart\u00edn-Serrano \u00c1. (2014) The Geology and Geomorphology of Spain: A Concise Introduction. In: Guti\u00e9rrez F., Guti\u00e9rrez M. (eds) Landscapes and Landforms of Spain. World Geomorphological Landscapes. Springer, Dordrecht.<\/p>\n<p>Mul\u021bumiri fotografilor C. Grosso Ciponte \u0219i M.A. Lancellotta pentru fotografiile spectaculoase raportate \u00een acest articol.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>St\u00e2lpii P\u0103m\u00e2ntului Procese de percolare Datorit\u0103 precipita\u021biilor, versan\u021bii pot fi supu\u0219i unor procese importante de percolare. Acestea includ, de exemplu: eroziune cauzat\u0103 de ploaile abundente (Splash erosion); eroziunea zonei (Sheet erosion); eroziunea \u00een rigole (rill erosion); eroziune \u00een f\u0103ga\u0219e (gully erosion) Aceste procese sunt responsabile pentru \u00eendep\u0103rtarea \u0219i \u00eendep\u0103rtarea unor cantit\u0103\u021bi mari de sedimente, ceea&hellip;<\/p>\n","protected":false},"author":18378,"featured_media":1550,"comment_status":"closed","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[1443,3,818,817],"tags":[1593,1594],"class_list":["post-1602","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-articoli-geotecnica-ro","category-mediu","category-publicatii","category-stiri","tag-pilastri-della-terra-ro","tag-piramidi-di-terra-ro","category-1443","category-3","category-818","category-817","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>St\u00e2lpii P\u0103m\u00e2ntului - Geostru Blog<\/title>\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\/stalpii-pamantului\/\" \/>\n<meta property=\"og:locale\" content=\"ro_RO\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"St\u00e2lpii P\u0103m\u00e2ntului\" \/>\n<meta property=\"og:description\" content=\"St\u00e2lpii P\u0103m\u00e2ntului Procese de percolare Datorit\u0103 precipita\u021biilor, versan\u021bii pot fi supu\u0219i unor procese importante de percolare. 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