{"id":520,"date":"2015-11-19T16:45:56","date_gmt":"2015-11-19T16:45:56","guid":{"rendered":"http:\/\/esg.pt\/seismic-v\/?page_id=520"},"modified":"2015-11-19T17:16:32","modified_gmt":"2015-11-19T17:16:32","slug":"region-2","status":"publish","type":"page","link":"https:\/\/esg.pt\/seismic-v\/region-2\/","title":{"rendered":"Region 2"},"content":{"rendered":"<div class=\"row\">\n<div class=\"col-sm-8\">\n<p>The historic seismic activity of the Costa Alentejana is guided by the elevated intensity of the earthquakes of 1755, 1858, 1903 and 1969. The 1858 earthquake, with a local epicentre, hit the region with high intensity (IX MCS).<\/p>\n<p>Alca\u0301cer do Sal was selected as a case study, because of its location in an area of regular seismic activity and due to the identification of several vernacular buildings, with evident seismic-resistant elements. The identified buildings are single storey with gable roofs, have reduced dimensions, and have a rectangular floor plan. The buildings are usually aligned in rows, addorsed on the tops in orthogonal alignment.<\/p>\n<p>Constructively, a mixed technique is used of stone masonry and rammed earth, generally reinforced with a row of brick. In some cases, a common-use stone bench (poial) is present in front of the di erent housing units. The internal partitioning is accomplished through transversal walls with the \u2018gaioleiro\u2019 system. In addition, tie-rods were incorporated into the alignment of the transversal walls.<\/p>\n<p>The Municipality of Melides was selected due to its seismic history and unique constructive culture; mainly outside the town centre. This constructive culture is based on the improvement of traditional constructive systems and the use of seismic-resistant elements. The identified buildings are single storey with gable roofs, have small dimensions, and a rectangular floor plan.<\/p>\n<p>The plan organization is simple with a rectangular configuration. The exterior walls are built in rammed earth, forming a monolithic structure, complemented by the introduction of buttresses, and combined with reinforced base plinths. The buildings have the distinction of simultaneously containing other reinforcing elements, such as, metal tie-rods and stone benches.<\/p>\n<\/div>\n<div class=\"col-sm-4\">\n<strong>Identified reinforcement elements<\/strong><\/p>\n\n\t\t<style type=\"text\/css\">\n\t\t\t#gallery-1 {\n\t\t\t\tmargin: auto;\n\t\t\t}\n\t\t\t#gallery-1 .gallery-item {\n\t\t\t\tfloat: left;\n\t\t\t\tmargin-top: 10px;\n\t\t\t\ttext-align: center;\n\t\t\t\twidth: 33%;\n\t\t\t}\n\t\t\t#gallery-1 img {\n\t\t\t\tborder: 2px solid #cfcfcf;\n\t\t\t}\n\t\t\t#gallery-1 .gallery-caption {\n\t\t\t\tmargin-left: 0;\n\t\t\t}\n\t\t\t\/* see gallery_shortcode() in wp-includes\/media.php *\/\n\t\t<\/style>\n\t\t<div id='gallery-1' class='gallery galleryid-520 gallery-columns-3 gallery-size-full'><dl class='gallery-item'>\n\t\t\t<dt class='gallery-icon portrait'>\n\t\t\t\t<a href='https:\/\/esg.pt\/seismic-v\/reference-case\/seismic_elements_cage-system\/'><img width=\"600\" height=\"983\" src=\"https:\/\/esg.pt\/seismic-v\/assets\/uploads\/2015\/11\/seismic_elements_cage-system.png\" class=\"attachment-full size-full\" alt=\"\" loading=\"lazy\" aria-describedby=\"gallery-1-490\" srcset=\"https:\/\/esg.pt\/seismic-v\/assets\/uploads\/2015\/11\/seismic_elements_cage-system.png 600w, https:\/\/esg.pt\/seismic-v\/assets\/uploads\/2015\/11\/seismic_elements_cage-system-183x300.png 183w\" sizes=\"(max-width: 600px) 100vw, 600px\" \/><\/a>\n\t\t\t<\/dt>\n\t\t\t\t<dd class='wp-caption-text gallery-caption' id='gallery-1-490'>\n\t\t\t\tCage System\n\t\t\t\t<\/dd><\/dl><dl class='gallery-item'>\n\t\t\t<dt class='gallery-icon portrait'>\n\t\t\t\t<a href='https:\/\/esg.pt\/seismic-v\/seismic_elements_horizontal-reinforcement\/'><img width=\"600\" height=\"983\" src=\"https:\/\/esg.pt\/seismic-v\/assets\/uploads\/2015\/11\/seismic_elements_horizontal-reinforcement.png\" class=\"attachment-full size-full\" alt=\"\" loading=\"lazy\" aria-describedby=\"gallery-1-492\" srcset=\"https:\/\/esg.pt\/seismic-v\/assets\/uploads\/2015\/11\/seismic_elements_horizontal-reinforcement.png 600w, https:\/\/esg.pt\/seismic-v\/assets\/uploads\/2015\/11\/seismic_elements_horizontal-reinforcement-183x300.png 183w\" sizes=\"(max-width: 600px) 100vw, 600px\" \/><\/a>\n\t\t\t<\/dt>\n\t\t\t\t<dd class='wp-caption-text gallery-caption' id='gallery-1-492'>\n\t\t\t\tHorizontal Reinforcement\n\t\t\t\t<\/dd><\/dl><dl class='gallery-item'>\n\t\t\t<dt class='gallery-icon portrait'>\n\t\t\t\t<a href='https:\/\/esg.pt\/seismic-v\/seismic_elements_buttress\/'><img width=\"600\" height=\"983\" src=\"https:\/\/esg.pt\/seismic-v\/assets\/uploads\/2015\/11\/seismic_elements_buttress.png\" class=\"attachment-full size-full\" alt=\"\" loading=\"lazy\" aria-describedby=\"gallery-1-515\" srcset=\"https:\/\/esg.pt\/seismic-v\/assets\/uploads\/2015\/11\/seismic_elements_buttress.png 600w, https:\/\/esg.pt\/seismic-v\/assets\/uploads\/2015\/11\/seismic_elements_buttress-183x300.png 183w\" sizes=\"(max-width: 600px) 100vw, 600px\" \/><\/a>\n\t\t\t<\/dt>\n\t\t\t\t<dd class='wp-caption-text gallery-caption' id='gallery-1-515'>\n\t\t\t\tButtress\n\t\t\t\t<\/dd><\/dl><br style=\"clear: both\" \/><dl class='gallery-item'>\n\t\t\t<dt class='gallery-icon portrait'>\n\t\t\t\t<a href='https:\/\/esg.pt\/seismic-v\/seismic_elements_stone_bench\/'><img width=\"600\" height=\"983\" src=\"https:\/\/esg.pt\/seismic-v\/assets\/uploads\/2015\/11\/seismic_elements_stone_bench.png\" class=\"attachment-full size-full\" alt=\"\" loading=\"lazy\" aria-describedby=\"gallery-1-516\" srcset=\"https:\/\/esg.pt\/seismic-v\/assets\/uploads\/2015\/11\/seismic_elements_stone_bench.png 600w, https:\/\/esg.pt\/seismic-v\/assets\/uploads\/2015\/11\/seismic_elements_stone_bench-183x300.png 183w\" sizes=\"(max-width: 600px) 100vw, 600px\" \/><\/a>\n\t\t\t<\/dt>\n\t\t\t\t<dd class='wp-caption-text gallery-caption' id='gallery-1-516'>\n\t\t\t\tStone bench\n\t\t\t\t<\/dd><\/dl><dl class='gallery-item'>\n\t\t\t<dt class='gallery-icon portrait'>\n\t\t\t\t<a href='https:\/\/esg.pt\/seismic-v\/seismic_elements_reinforced-jambs\/'><img width=\"600\" height=\"983\" src=\"https:\/\/esg.pt\/seismic-v\/assets\/uploads\/2015\/11\/seismic_elements_reinforced-jambs.png\" class=\"attachment-full size-full\" alt=\"\" loading=\"lazy\" aria-describedby=\"gallery-1-494\" srcset=\"https:\/\/esg.pt\/seismic-v\/assets\/uploads\/2015\/11\/seismic_elements_reinforced-jambs.png 600w, https:\/\/esg.pt\/seismic-v\/assets\/uploads\/2015\/11\/seismic_elements_reinforced-jambs-183x300.png 183w\" sizes=\"(max-width: 600px) 100vw, 600px\" \/><\/a>\n\t\t\t<\/dt>\n\t\t\t\t<dd class='wp-caption-text gallery-caption' id='gallery-1-494'>\n\t\t\t\tReinforced Jambs\n\t\t\t\t<\/dd><\/dl><dl class='gallery-item'>\n\t\t\t<dt class='gallery-icon portrait'>\n\t\t\t\t<a href='https:\/\/esg.pt\/seismic-v\/seismic_elements_tie-rod\/'><img width=\"600\" height=\"983\" src=\"https:\/\/esg.pt\/seismic-v\/assets\/uploads\/2015\/11\/seismic_elements_tie-rod.png\" class=\"attachment-full size-full\" alt=\"\" loading=\"lazy\" aria-describedby=\"gallery-1-517\" srcset=\"https:\/\/esg.pt\/seismic-v\/assets\/uploads\/2015\/11\/seismic_elements_tie-rod.png 600w, https:\/\/esg.pt\/seismic-v\/assets\/uploads\/2015\/11\/seismic_elements_tie-rod-183x300.png 183w\" sizes=\"(max-width: 600px) 100vw, 600px\" \/><\/a>\n\t\t\t<\/dt>\n\t\t\t\t<dd class='wp-caption-text gallery-caption' id='gallery-1-517'>\n\t\t\t\tTie-rod\n\t\t\t\t<\/dd><\/dl><br style=\"clear: both\" \/>\n\t\t<\/div>\n\n<\/div>\n<\/div>\n","protected":false},"excerpt":{"rendered":"<p>The historic seismic activity of the Costa Alentejana is guided by the elevated intensity of the earthquakes of 1755, 1858, 1903 and 1969. The 1858 earthquake, with a local epicentre, hit the region with high intensity (IX MCS). Alca\u0301cer do Sal was selected as a case study, because of its location in an area of&#8230;  <a href=\"https:\/\/esg.pt\/seismic-v\/region-2\/\" title=\"ReadRegion 2\">Read more &raquo;<\/a><\/p>\n","protected":false},"author":2,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":[],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v16.8 - https:\/\/yoast.com\/wordpress\/plugins\/seo\/ -->\n<meta name=\"robots\" content=\"index, follow, max-snippet:-1, max-image-preview:large, max-video-preview:-1\" \/>\n<link rel=\"canonical\" href=\"https:\/\/esg.pt\/seismic-v\/region-2\/\" \/>\n<meta property=\"og:locale\" content=\"pt_PT\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"Region 2 - Seismic V\" \/>\n<meta property=\"og:description\" content=\"The historic seismic activity of the Costa Alentejana is guided by the elevated intensity of the earthquakes of 1755, 1858, 1903 and 1969. The 1858 earthquake, with a local epicentre, hit the region with high intensity (IX MCS). Alca\u0301cer do Sal was selected as a case study, because of its location in an area of... 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The 1858 earthquake, with a local epicentre, hit the region with high intensity (IX MCS). Alca\u0301cer do Sal was selected as a case study, because of its location in an area of... 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